From 863f0d37fd832d725c5070f2ce4cc8e1c01fcb26 Mon Sep 17 00:00:00 2001 From: shrouxm Date: Tue, 29 Jul 2025 15:49:46 -0700 Subject: [PATCH 1/5] deps: add syrupy dev dep --- Makefile | 6 ++++++ requirements-dev.txt | 5 +++++ requirements/dev.in | 1 + 3 files changed, 12 insertions(+) diff --git a/Makefile b/Makefile index 3c2227a..4230de4 100644 --- a/Makefile +++ b/Makefile @@ -20,9 +20,15 @@ format: lock: CUSTOM_COMPILE_COMMAND="make lock" uv pip compile --upgrade --generate-hashes requirements/base.in -o requirements.txt +lock-package: + CUSTOM_COMPILE_COMMAND="make lock" uv pip compile --upgrade-package $(PACKAGE) --generate-hashes --emit-build-options requirements/base.in requirements/deploy.in -o requirements.txt + lock-dev: CUSTOM_COMPILE_COMMAND="make lock-dev" uv pip compile --upgrade --generate-hashes requirements/dev.in -o requirements-dev.txt +lock-dev-package: + CUSTOM_COMPILE_COMMAND="make lock-dev" uv pip compile --upgrade-package $(PACKAGE) --generate-hashes requirements/dev.in -o requirements-dev.txt + build: echo "Building TK..." diff --git a/requirements-dev.txt b/requirements-dev.txt index 77995d3..71fd3b9 100644 --- a/requirements-dev.txt +++ b/requirements-dev.txt @@ -174,6 +174,7 @@ pytest==8.4.1 \ # via # -r requirements/dev.in # pytest-profiling + # syrupy pytest-profiling==1.8.1 \ --hash=sha256:3dd8713a96298b42d83de8f5951df3ada3e61b3e5d2a06956684175529e17aea \ --hash=sha256:3f171fa69d5c82fa9aab76d66abd5f59da69135c37d6ae5bf7557f1b154cb08d @@ -265,6 +266,10 @@ soupsieve==2.7 \ --hash=sha256:6e60cc5c1ffaf1cebcc12e8188320b72071e922c2e897f737cadce79ad5d30c4 \ --hash=sha256:ad282f9b6926286d2ead4750552c8a6142bc4c783fd66b0293547c8fe6ae126a # via beautifulsoup4 +syrupy==4.9.1 \ + --hash=sha256:b7d0fcadad80a7d2f6c4c71917918e8ebe2483e8c703dfc8d49cdbb01081f9a4 \ + --hash=sha256:b94cc12ed0e5e75b448255430af642516842a2374a46936dd2650cfb6dd20eda + # via -r requirements/dev.in tqdm==4.67.1 \ --hash=sha256:26445eca388f82e72884e0d580d5464cd801a3ea01e63e5601bdff9ba6a48de2 \ --hash=sha256:f8aef9c52c08c13a65f30ea34f4e5aac3fd1a34959879d7e59e63027286627f2 diff --git a/requirements/dev.in b/requirements/dev.in index e351014..b993bd4 100644 --- a/requirements/dev.in +++ b/requirements/dev.in @@ -4,3 +4,4 @@ ruff pre-commit pytest pytest-profiling +syrupy From d11078a21876866747b91de79579fd023713ac74 Mon Sep 17 00:00:00 2001 From: shrouxm Date: Wed, 30 Jul 2025 10:41:59 -0700 Subject: [PATCH 2/5] feat: add snapshot tests --- Makefile | 11 +- .../test_soil_location[-1.75,13.6].json | 811 ++++ ...st_soil_location[-10.07856,15.107436].json | 2579 +++++++++++++ ...t_soil_location[-10.950086,17.573093].json | 2067 +++++++++++ ...est_soil_location[-19.13333,145.5125].json | 3291 +++++++++++++++++ .../test_soil_location[-2.06972,37.29].json | 3163 ++++++++++++++++ ...est_soil_location[-24.53333,33.36667].json | 2043 ++++++++++ ...est_soil_location[15.73333,120.31667].json | 1371 +++++++ ...test_soil_location[30.38333,35.53333].json | 1315 +++++++ ...test_soil_location[32.11667,20.08333].json | 1195 ++++++ .../test_soil_location[34.5,69.16667].json | 2267 ++++++++++++ .../test_soil_location[37.33333,-5.4].json | 1867 ++++++++++ ...est_soil_location[48.71667,126.13333].json | 1371 +++++++ .../test_soil_location[7.3318,-1.4631].json | 1819 +++++++++ .../test_soil_location[8.48333,76.95].json | 1419 +++++++ soil_id/tests/global/test_global.py | 178 +- ...il_location[33.81246789,-101.9733687].json | 794 ++++ ...st_soil_location[34.92816,-114.80764].json | 1100 ++++++ ...t_soil_location[35.59918,-120.491439].json | 454 +++ .../test_soil_location[37.422,-122.084].json | 522 +++ ...il_location[37.48216451,-99.55016693].json | 1066 ++++++ ...il_location[39.26009312,-85.50621214].json | 1882 ++++++++++ ..._soil_location[42.494912,-123.064531].json | 998 +++++ ...il_location[42.63413723,-94.31005777].json | 522 +++ ...il_location[43.06450312,-119.4596489].json | 658 ++++ ...oil_location[45.6508331,-121.5111084].json | 233 ++ ...il_location[45.88932423,-121.0347381].json | 165 + ...soil_location[47.213922,-69.28246582].json | 930 +++++ ...test_soil_location[48.6956,-121.8166].json | 1162 ++++++ ...il_location[60.42282639,-158.4018264].json | 454 +++ ...il_location[62.32776717,-157.2767099].json | 604 +++ ...il_location[63.52666854,-156.4422738].json | 790 ++++ .../tests/us/generate_bulk_test_results.py | 11 +- soil_id/tests/us/test_us.py | 18 +- soil_id/tests/utils.py | 26 + 35 files changed, 39130 insertions(+), 26 deletions(-) create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json create mode 100644 soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.6508331,-121.5111084].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json create mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json create mode 100644 soil_id/tests/utils.py diff --git a/Makefile b/Makefile index 4230de4..9573ee2 100644 --- a/Makefile +++ b/Makefile @@ -41,9 +41,16 @@ clean: test: clean check_rebuild if [ -z "$(PATTERN)" ]; then \ - $(DC_RUN_CMD) pytest soil_id; \ + $(DC_RUN_CMD) pytest soil_id -vv; \ else \ - $(DC_RUN_CMD) pytest soil_id -k $(PATTERN); \ + $(DC_RUN_CMD) pytest soil_id -vv -k $(PATTERN); \ + fi + +test_update_snapshots: clean check_rebuild + if [ -z "$(PATTERN)" ]; then \ + $(DC_RUN_CMD) pytest soil_id --snapshot-update; \ + else \ + $(DC_RUN_CMD) pytest soil_id --snapshot-update -k $(PATTERN); \ fi test-verbose: diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json new file mode 100644 index 0000000..f48e086 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json @@ -0,0 +1,811 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols", + "rank_loc": "1", + "score_loc": 0.4 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 144044, + "distance": 29708.866, + "mapunitID": 463, + "minCompDistance": 29708.8664, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 5.6, + "sl5": 5.14, + "sl6": 4.6, + "sl7": 4.33 + }, + "clay": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 39.2, + "sl5": 40.71, + "sl6": 42.0, + "sl7": 42.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Xanthic ferralsols", + "name": "Xanthic ferralsols", + "rank_loc": "2", + "score_loc": 0.133 + }, + "ph": { + "sl1": 4.5, + "sl2": 4.5, + "sl3": 4.5, + "sl4": 4.58, + "sl5": 4.63, + "sl6": 4.68, + "sl7": 4.72 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.57, + "sl6": 4.0, + "sl7": 5.0 + }, + "sand": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 50.0, + "sl5": 48.71, + "sl6": 47.6, + "sl7": 47.17 + }, + "site": { + "siteData": { + "componentID": 156033, + "distance": 0.0, + "mapunitID": 918, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", + "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Sandy clay", + "sl2": "Sandy clay", + "sl3": "Sandy clay", + "sl4": "Sandy clay", + "sl5": "Sandy clay", + "sl6": "Sandy clay", + "sl7": "Sandy clay" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.0, + "sl5": 7.43, + "sl6": 7.0, + "sl7": 6.83 + }, + "clay": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 46.4, + "sl5": 47.43, + "sl6": 48.2, + "sl7": 48.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic ferralsols", + "name": "Haplic ferralsols", + "rank_loc": "3", + "score_loc": 0.133 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.92, + "sl5": 4.96, + "sl6": 5.0, + "sl7": 5.02 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.6, + "sl5": 4.71, + "sl6": 5.0, + "sl7": 5.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 37.4, + "sl5": 36.57, + "sl6": 35.8, + "sl7": 35.5 + }, + "site": { + "siteData": { + "componentID": 144043, + "distance": 29708.866, + "mapunitID": 463, + "minCompDistance": 29708.8664, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", + "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.14, + "sl6": 6.8, + "sl7": 6.67 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 33.4, + "sl5": 33.86, + "sl6": 34.0, + "sl7": 33.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 + }, + "id": { + "component": "Ferralic cambisols", + "name": "Ferralic cambisols", + "rank_loc": "4", + "score_loc": 0.083 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.12, + "sl5": 5.14, + "sl6": 5.14, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.2, + "sl5": 11.43, + "sl6": 12.6, + "sl7": 12.83 + }, + "sand": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 43.0, + "sl5": 42.43, + "sl6": 42.0, + "sl7": 42.0 + }, + "site": { + "siteData": { + "componentID": 144042, + "distance": 29708.866, + "mapunitID": 463, + "minCompDistance": 29708.8664, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.4, + "sl5": 8.57, + "sl6": 7.8, + "sl7": 8.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 24.2, + "sl5": 24.29, + "sl6": 24.2, + "sl7": 24.5 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Dystric fluvisols", + "name": "Dystric fluvisols", + "rank_loc": "5", + "score_loc": 0.017 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.96, + "sl5": 4.99, + "sl6": 5.04, + "sl7": 5.08 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.8, + "sl5": 7.0, + "sl6": 9.4, + "sl7": 9.67 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 49.2, + "sl5": 49.71, + "sl6": 50.8, + "sl7": 50.67 + }, + "site": { + "siteData": { + "componentID": 148190, + "distance": 5397.734, + "mapunitID": 546, + "minCompDistance": 5397.7345, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 11.2, + "sl5": 10.57, + "sl6": 10.2, + "sl7": 10.5 + }, + "clay": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 30.0, + "sl5": 31.57, + "sl6": 33.0, + "sl7": 33.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 + }, + "id": { + "component": "Dystric gleysols", + "name": "Dystric gleysols", + "rank_loc": "6", + "score_loc": 0.017 + }, + "ph": { + "sl1": 4.8, + "sl2": 4.8, + "sl3": 4.8, + "sl4": 4.94, + "sl5": 5.0, + "sl6": 5.06, + "sl7": 5.08 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 4.8, + "sl5": 4.86, + "sl6": 5.4, + "sl7": 5.33 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 40.71, + "sl6": 40.6, + "sl7": 40.5 + }, + "site": { + "siteData": { + "componentID": 148189, + "distance": 5397.734, + "mapunitID": 546, + "minCompDistance": 5397.7345, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 7.4, + "sl5": 7.43, + "sl6": 7.6, + "sl7": 7.67 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 28.2, + "sl5": 30.57, + "sl6": 32.8, + "sl7": 34.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Gleyic acrisols", + "name": "Gleyic acrisols", + "rank_loc": "7", + "score_loc": 0.017 + }, + "ph": { + "sl1": 4.8, + "sl2": 4.8, + "sl3": 4.8, + "sl4": 4.88, + "sl5": 4.93, + "sl6": 4.98, + "sl7": 4.98 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.6, + "sl5": 4.86, + "sl6": 5.4, + "sl7": 5.83 + }, + "sand": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 42.0, + "sl5": 40.57, + "sl6": 39.2, + "sl7": 37.67 + }, + "site": { + "siteData": { + "componentID": 144045, + "distance": 29708.866, + "mapunitID": 463, + "minCompDistance": 29708.8664, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", + "Description_es": "Los Acrisoles Gleyicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles gleyicos tienen un nivel freático alto estacional que provoca la saturación durante algunas épocas del año. ", + "Description_fr": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", + "Description_ks": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.
Los períodos de saturación limitan el crecimiento de las raíces y aumentan la pérdida de nitrógeno.
Para evitar la pérdida de N por lixiviación y/o desnitrificación, considere el uso de fertilizantes de liberación lenta de N (urea recubierta de azufre (SCU), por ejemplo), si esos productos de liberación lenta están disponibles, o utilice estiércol u otros residuos orgánicos por sus propiedades de liberación lenta.
Puede ser necesario el drenaje de estos suelos, pero esto puede ser problemático, ya que la humedad se debe al alto nivel freático. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Ferralic cambisols", + "componentData": "Data Complete", + "componentID": 144042, + "name": "Ferralic cambisols", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": 4, + "score_data": 0.621, + "score_data_loc": 1.0, + "score_loc": 0.083 + }, + { + "component": "Haplic ferralsols", + "componentData": "No Data", + "componentID": 144043, + "name": "Haplic ferralsols", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": 3, + "score_data": 0.519, + "score_data_loc": 0.926, + "score_loc": 0.133 + }, + { + "component": "Xanthic ferralsols", + "componentData": "Missing Data", + "componentID": 156033, + "name": "Xanthic ferralsols", + "rank_data": "5", + "rank_data_loc": "3", + "rank_loc": 2, + "score_data": 0.517, + "score_data_loc": 0.924, + "score_loc": 0.133 + }, + { + "component": "Dystric gleysols", + "componentData": "Missing Data", + "componentID": 148189, + "name": "Dystric gleysols", + "rank_data": "2", + "rank_data_loc": "4", + "rank_loc": 6, + "score_data": 0.571, + "score_data_loc": 0.834, + "score_loc": 0.017 + }, + { + "component": "Gleyic acrisols", + "componentData": "Missing Data", + "componentID": 144045, + "name": "Gleyic acrisols", + "rank_data": "3", + "rank_data_loc": "5", + "rank_loc": 7, + "score_data": 0.571, + "score_data_loc": 0.834, + "score_loc": 0.017 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 144044, + "name": "Ferralic arenosols", + "rank_data": "7", + "rank_data_loc": "6", + "rank_loc": 1, + "score_data": 0.0, + "score_data_loc": 0.568, + "score_loc": 0.4 + }, + { + "component": "Dystric fluvisols", + "componentData": "Data Complete", + "componentID": 148190, + "name": "Dystric fluvisols", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": 5, + "score_data": 0.35, + "score_data_loc": 0.521, + "score_loc": 0.017 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json new file mode 100644 index 0000000..93ea6f8 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json @@ -0,0 +1,2579 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 6.4, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.33 + }, + "clay": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 25.8, + "sl5": 27.14, + "sl6": 28.6, + "sl7": 31.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Xanthic ferralsols", + "name": "Xanthic ferralsols1", + "rank_loc": "1", + "score_loc": 0.067 + }, + "ph": { + "sl1": 4.5, + "sl2": 4.5, + "sl3": 4.5, + "sl4": 4.58, + "sl5": 4.63, + "sl6": 4.68, + "sl7": 4.72 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.57, + "sl6": 4.0, + "sl7": 5.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0, + "sl4": 62.8, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 58.5 + }, + "site": { + "siteData": { + "componentID": 105399, + "distance": 4468.846, + "mapunitID": 12207, + "minCompDistance": 4468.8459, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", + "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 6.4, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.33 + }, + "clay": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 25.8, + "sl5": 27.14, + "sl6": 28.6, + "sl7": 31.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic ferralsols", + "name": "Haplic ferralsols1", + "rank_loc": "2", + "score_loc": 0.042 + }, + "ph": { + "sl1": 4.5, + "sl2": 4.5, + "sl3": 4.5, + "sl4": 4.58, + "sl5": 4.63, + "sl6": 4.68, + "sl7": 4.72 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.57, + "sl6": 4.0, + "sl7": 5.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0, + "sl4": 62.8, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 58.5 + }, + "site": { + "siteData": { + "componentID": 105398, + "distance": 4468.846, + "mapunitID": 12207, + "minCompDistance": 4468.8459, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", + "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 5.6, + "sl5": 5.14, + "sl6": 4.6, + "sl7": 4.33 + }, + "clay": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 39.2, + "sl5": 40.71, + "sl6": 42.0, + "sl7": 42.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "3", + "score_loc": 0.042 + }, + "ph": { + "sl1": 4.5, + "sl2": 4.5, + "sl3": 4.5, + "sl4": 4.58, + "sl5": 4.63, + "sl6": 4.68, + "sl7": 4.72 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.57, + "sl6": 4.0, + "sl7": 5.0 + }, + "sand": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 50.0, + "sl5": 48.71, + "sl6": 47.6, + "sl7": 47.17 + }, + "site": { + "siteData": { + "componentID": 104800, + "distance": 31871.197, + "mapunitID": 12046, + "minCompDistance": 31871.1971, + "share": 15, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sandy clay", + "sl2": "Sandy clay", + "sl3": "Sandy clay", + "sl4": "Sandy clay", + "sl5": "Sandy clay", + "sl6": "Sandy clay", + "sl7": "Sandy clay" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.6, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.67 + }, + "clay": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 38.8, + "sl5": 39.86, + "sl6": 40.8, + "sl7": 41.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric leptosols", + "name": "Eutric leptosols1", + "rank_loc": "4", + "score_loc": 0.033 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.16, + "sl5": 5.19, + "sl6": 5.24, + "sl7": 5.28 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.4, + "sl5": 3.29, + "sl6": 3.2, + "sl7": 5.17 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 38.8, + "sl5": 37.86, + "sl6": 36.8, + "sl7": 36.0 + }, + "site": { + "siteData": { + "componentID": 104801, + "distance": 31871.197, + "mapunitID": 12046, + "minCompDistance": 31871.1971, + "share": 15, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "5", + "score_loc": 0.029 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 104657, + "distance": 86884.207, + "mapunitID": 12006, + "minCompDistance": 86884.2069, + "share": 70, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.0, + "sl5": 7.43, + "sl6": 7.0, + "sl7": 6.83 + }, + "clay": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 46.4, + "sl5": 47.43, + "sl6": 48.2, + "sl7": 48.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Rhodic ferralsols", + "name": "Rhodic ferralsols1", + "rank_loc": "6", + "score_loc": 0.025 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.92, + "sl5": 4.96, + "sl6": 5.0, + "sl7": 5.02 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.6, + "sl5": 4.71, + "sl6": 5.0, + "sl7": 5.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 37.4, + "sl5": 36.57, + "sl6": 35.8, + "sl7": 35.5 + }, + "site": { + "siteData": { + "componentID": 105419, + "distance": 21840.312, + "mapunitID": 12213, + "minCompDistance": 21840.3117, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", + "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Luvic phaeozems", + "name": "Luvic phaeozems1", + "rank_loc": "7", + "score_loc": 0.025 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 104814, + "distance": 62973.262, + "mapunitID": 12050, + "minCompDistance": 62973.2622, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", + "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.0 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 27.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 + }, + "id": { + "component": "Haplic arenosols", + "name": "Haplic arenosols", + "rank_loc": "8", + "score_loc": 0.021 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.55 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 30.5 + }, + "sand": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 44.0 + }, + "site": { + "siteData": { + "componentID": 104798, + "distance": 31871.197, + "mapunitID": 12046, + "minCompDistance": 31871.1971, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_es": "Los Arenosoles Háplicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.", + "Description_fr": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_ks": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 21.5 + }, + "clay": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 34.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols1", + "rank_loc": "9", + "score_loc": 0.021 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.55 + }, + "rock_fragments": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 40.5 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 36.5 + }, + "site": { + "siteData": { + "componentID": 104809, + "distance": 75356.147, + "mapunitID": 12048, + "minCompDistance": 75356.1465, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 12.5 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 18.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 2.0 + }, + "id": { + "component": "Ferralic cambisols", + "name": "Ferralic cambisols1", + "rank_loc": "10", + "score_loc": 0.017 + }, + "ph": { + "sl1": 7.7, + "sl2": 7.7, + "sl3": 7.7, + "sl4": 7.65 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.5 + }, + "sand": { + "sl1": 61.0, + "sl2": 61.0, + "sl3": 61.0, + "sl4": 57.0 + }, + "site": { + "siteData": { + "componentID": 105395, + "distance": 4468.846, + "mapunitID": 12207, + "minCompDistance": 4468.8459, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.6, + "sl5": 13.57, + "sl6": 13.0, + "sl7": 13.17 + }, + "clay": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.8, + "sl5": 18.86, + "sl6": 18.8, + "sl7": 18.83 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols1", + "rank_loc": "11", + "score_loc": 0.017 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.62, + "sl5": 7.66, + "sl6": 7.68, + "sl7": 7.7 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.57, + "sl6": 4.4, + "sl7": 5.5 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.2, + "sl5": 54.14, + "sl6": 54.6, + "sl7": 55.0 + }, + "site": { + "siteData": { + "componentID": 105472, + "distance": 40422.283, + "mapunitID": 12228, + "minCompDistance": 40422.2833, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.14, + "sl6": 6.6, + "sl7": 6.33 + }, + "clay": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 49.8, + "sl5": 50.71, + "sl6": 51.4, + "sl7": 51.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols1", + "rank_loc": "12", + "score_loc": 0.017 + }, + "ph": { + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.44, + "sl5": 5.44, + "sl6": 5.46, + "sl7": 5.48 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 7.0, + "sl5": 5.29, + "sl6": 4.2, + "sl7": 4.67 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.57, + "sl6": 32.8, + "sl7": 32.5 + }, + "site": { + "siteData": { + "componentID": 104802, + "distance": 63317.634, + "mapunitID": 12047, + "minCompDistance": 63317.6338, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 23.0, + "sl5": 22.29, + "sl6": 21.8, + "sl7": 21.5 + }, + "clay": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 40.2, + "sl5": 41.57, + "sl6": 42.0, + "sl7": 41.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Xanthic ferralsols", + "name": "Xanthic ferralsols2", + "rank_loc": "Not Displayed", + "score_loc": 0.067 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.26, + "sl5": 6.29, + "sl6": 6.32, + "sl7": 6.32 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 8.4, + "sl5": 8.43, + "sl6": 8.6, + "sl7": 12.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.71, + "sl6": 33.8, + "sl7": 34.67 + }, + "site": { + "siteData": { + "componentID": 105417, + "distance": 21840.312, + "mapunitID": 12213, + "minCompDistance": 4468.8459, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", + "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 23.0, + "sl5": 22.29, + "sl6": 21.8, + "sl7": 21.5 + }, + "clay": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 40.2, + "sl5": 41.57, + "sl6": 42.0, + "sl7": 41.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Xanthic ferralsols", + "name": "Xanthic ferralsols3", + "rank_loc": "Not Displayed", + "score_loc": 0.067 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.26, + "sl5": 6.29, + "sl6": 6.32, + "sl7": 6.32 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 8.4, + "sl5": 8.43, + "sl6": 8.6, + "sl7": 12.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.71, + "sl6": 33.8, + "sl7": 34.67 + }, + "site": { + "siteData": { + "componentID": 104818, + "distance": 96145.535, + "mapunitID": 12052, + "minCompDistance": 4468.8459, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", + "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.4, + "sl5": 7.71, + "sl6": 7.2, + "sl7": 7.0 + }, + "clay": { + "sl1": 48.0, + "sl2": 48.0, + "sl3": 48.0, + "sl4": 52.6, + "sl5": 53.86, + "sl6": 55.0, + "sl7": 55.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic ferralsols", + "name": "Haplic ferralsols2", + "rank_loc": "Not Displayed", + "score_loc": 0.042 + }, + "ph": { + "sl1": 5.6, + "sl2": 5.6, + "sl3": 5.6, + "sl4": 5.62, + "sl5": 5.63, + "sl6": 5.64, + "sl7": 5.65 + }, + "rock_fragments": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 17.0, + "sl5": 12.71, + "sl6": 10.0, + "sl7": 8.83 + }, + "sand": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 32.2, + "sl5": 31.29, + "sl6": 30.4, + "sl7": 29.83 + }, + "site": { + "siteData": { + "componentID": 104799, + "distance": 31871.197, + "mapunitID": 12046, + "minCompDistance": 4468.8459, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", + "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.6, + "sl5": 3.14, + "sl6": 3.0, + "sl7": 2.83 + }, + "clay": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.0, + "sl6": 5.0, + "sl7": 5.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.042 + }, + "ph": { + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.72, + "sl5": 5.74, + "sl6": 5.76, + "sl7": 5.77 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.8, + "sl5": 5.43, + "sl6": 5.0, + "sl7": 4.5 + }, + "sand": { + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 88.0, + "sl5": 88.0, + "sl6": 88.2, + "sl7": 88.17 + }, + "site": { + "siteData": { + "componentID": 105352, + "distance": 99172.777, + "mapunitID": 12196, + "minCompDistance": 31871.1971, + "share": 10, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.6, + "sl5": 21.86, + "sl6": 22.2, + "sl7": 22.67 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.0, + "sl5": 31.43, + "sl6": 31.4, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Eutric leptosols", + "name": "Eutric leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.033 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.47, + "sl6": 6.58, + "sl7": 6.65 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.8, + "sl5": 16.57, + "sl6": 17.8, + "sl7": 16.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.2, + "sl5": 39.14, + "sl6": 39.6, + "sl7": 39.33 + }, + "site": { + "siteData": { + "componentID": 105349, + "distance": 99172.777, + "mapunitID": 12196, + "minCompDistance": 31871.1971, + "share": 45, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 14.8, + "sl5": 14.57, + "sl6": 14.2, + "sl7": 14.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.6, + "sl5": 20.86, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 0.8, + "sl5": 0.71, + "sl6": 0.8, + "sl7": 0.83 + }, + "id": { + "component": "Eutric leptosols", + "name": "Eutric leptosols3", + "rank_loc": "Not Displayed", + "score_loc": 0.033 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.54, + "sl5": 6.6, + "sl6": 6.66, + "sl7": 6.7 + }, + "rock_fragments": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 15.0, + "sl5": 16.57, + "sl6": 18.8, + "sl7": 19.17 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.8, + "sl5": 41.14, + "sl6": 41.8, + "sl7": 42.17 + }, + "site": { + "siteData": { + "componentID": 105229, + "distance": 99332.531, + "mapunitID": 12163, + "minCompDistance": 31871.1971, + "share": 10, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.6, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.67 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 31.4, + "sl5": 32.0, + "sl6": 32.6, + "sl7": 33.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 + }, + "id": { + "component": "Rhodic ferralsols", + "name": "Rhodic ferralsols2", + "rank_loc": "Not Displayed", + "score_loc": 0.025 + }, + "ph": { + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.2, + "sl5": 5.2, + "sl6": 5.2, + "sl7": 5.18 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 9.4, + "sl5": 9.86, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 43.0, + "sl5": 42.29, + "sl6": 41.4, + "sl7": 41.0 + }, + "site": { + "siteData": { + "componentID": 104820, + "distance": 96145.535, + "mapunitID": 12052, + "minCompDistance": 21840.3117, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", + "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.14, + "sl6": 6.8, + "sl7": 6.67 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 33.4, + "sl5": 33.86, + "sl6": 34.0, + "sl7": 33.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 + }, + "id": { + "component": "Luvic phaeozems", + "name": "Luvic phaeozems2", + "rank_loc": "Not Displayed", + "score_loc": 0.025 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.12, + "sl5": 5.14, + "sl6": 5.14, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.2, + "sl5": 11.43, + "sl6": 12.6, + "sl7": 12.83 + }, + "sand": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 43.0, + "sl5": 42.43, + "sl6": 42.0, + "sl7": 42.0 + }, + "site": { + "siteData": { + "componentID": 104807, + "distance": 75356.147, + "mapunitID": 12048, + "minCompDistance": 62973.2622, + "share": 25, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", + "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.14, + "sl6": 1.8, + "sl7": 1.67 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.86, + "sl6": 7.2, + "sl7": 7.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.021 + }, + "ph": { + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.5, + "sl5": 5.5, + "sl6": 5.5, + "sl7": 5.48 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.71, + "sl6": 4.4, + "sl7": 6.0 + }, + "sand": { + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 89.0, + "sl5": 88.86, + "sl6": 88.4, + "sl7": 88.17 + }, + "site": { + "siteData": { + "componentID": 105350, + "distance": 99172.777, + "mapunitID": 12196, + "minCompDistance": 75356.1465, + "share": 25, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.2, + "sl5": 30.29, + "sl6": 33.2, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic cambisols", + "name": "Ferralic cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.017 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.12, + "sl5": 6.07, + "sl6": 6.02, + "sl7": 6.02 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.8, + "sl5": 10.43, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 60.2, + "sl5": 57.57, + "sl6": 54.8, + "sl7": 53.0 + }, + "site": { + "siteData": { + "componentID": 105247, + "distance": 28892.433, + "mapunitID": 12167, + "minCompDistance": 4468.8459, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.017 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 104805, + "distance": 63317.634, + "mapunitID": 12047, + "minCompDistance": 40422.2833, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.0, + "sl5": 6.14, + "sl6": 6.4, + "sl7": 6.5 + }, + "clay": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 25.0, + "sl5": 28.14, + "sl6": 30.6, + "sl7": 31.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.017 + }, + "ph": { + "sl1": 5.6, + "sl2": 5.6, + "sl3": 5.6, + "sl4": 5.68, + "sl5": 5.71, + "sl6": 5.74, + "sl7": 5.73 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 10.8, + "sl5": 10.29, + "sl6": 11.4, + "sl7": 11.17 + }, + "sand": { + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 56.8, + "sl5": 54.14, + "sl6": 52.2, + "sl7": 51.67 + }, + "site": { + "siteData": { + "componentID": 105351, + "distance": 99172.777, + "mapunitID": 12196, + "minCompDistance": 63317.6338, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 104657, + "name": "Eutric fluvisols", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": "5", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.029 + }, + { + "component": "Luvic phaeozems", + "componentData": "Missing Data", + "componentID": 104814, + "name": "Luvic phaeozems1", + "rank_data": "5", + "rank_data_loc": "2", + "rank_loc": "7", + "score_data": 1.0, + "score_data_loc": 0.996, + "score_loc": 0.025 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 104809, + "name": "Eutric cambisols1", + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": "9", + "score_data": 1.0, + "score_data_loc": 0.992, + "score_loc": 0.021 + }, + { + "component": "Haplic arenosols", + "componentData": "Data Complete", + "componentID": 104798, + "name": "Haplic arenosols", + "rank_data": "4", + "rank_data_loc": "4", + "rank_loc": "8", + "score_data": 1.0, + "score_data_loc": 0.992, + "score_loc": 0.021 + }, + { + "component": "Haplic ferralsols", + "componentData": "No Data", + "componentID": 104799, + "name": "Haplic ferralsols2", + "rank_data": "6", + "rank_data_loc": "5", + "rank_loc": "Not Displayed", + "score_data": 0.832, + "score_data_loc": 0.849, + "score_loc": 0.042 + }, + { + "component": "Rhodic ferralsols", + "componentData": "No Data", + "componentID": 105419, + "name": "Rhodic ferralsols1", + "rank_data": "8", + "rank_data_loc": "6", + "rank_loc": "6", + "score_data": 0.832, + "score_data_loc": 0.832, + "score_loc": 0.025 + }, + { + "component": "Haplic lixisols", + "componentData": "Missing Data", + "componentID": 104802, + "name": "Haplic lixisols1", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": "12", + "score_data": 0.832, + "score_data_loc": 0.824, + "score_loc": 0.017 + }, + { + "component": "Xanthic ferralsols", + "componentData": "Missing Data", + "componentID": 104818, + "name": "Xanthic ferralsols3", + "rank_data": "Not Displayed", + "rank_data_loc": "8", + "rank_loc": "Not Displayed", + "score_data": 0.752, + "score_data_loc": 0.795, + "score_loc": 0.067 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 105472, + "name": "Ferralic arenosols1", + "rank_data": "10", + "rank_data_loc": "9", + "rank_loc": "11", + "score_data": 0.711, + "score_data_loc": 0.707, + "score_loc": 0.017 + }, + { + "component": "Ferralic cambisols", + "componentData": "Data Complete", + "componentID": 105395, + "name": "Ferralic cambisols1", + "rank_data": "11", + "rank_data_loc": "10", + "rank_loc": "10", + "score_data": 0.711, + "score_data_loc": 0.707, + "score_loc": 0.017 + }, + { + "component": "Eutric leptosols", + "componentData": "Missing Data", + "componentID": 105229, + "name": "Eutric leptosols3", + "rank_data": "3", + "rank_data_loc": "11", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 0.002, + "score_loc": 0.033 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 104800, + "name": "Lithic leptosols1", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": "3", + "score_data": 0.503, + "score_data_loc": 0.002, + "score_loc": 0.042 + }, + { + "component": "Xanthic ferralsols", + "componentData": "Missing Data", + "componentID": 105417, + "name": "Xanthic ferralsols2", + "rank_data": "9", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.752, + "score_data_loc": 0.795, + "score_loc": 0.067 + }, + { + "component": "Luvic phaeozems", + "componentData": "Missing Data", + "componentID": 104807, + "name": "Luvic phaeozems2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.752, + "score_data_loc": 0.755, + "score_loc": 0.025 + }, + { + "component": "Rhodic ferralsols", + "componentData": "No Data", + "componentID": 104820, + "name": "Rhodic ferralsols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.752, + "score_data_loc": 0.755, + "score_loc": 0.025 + }, + { + "component": "Haplic lixisols", + "componentData": "Data Complete", + "componentID": 105351, + "name": "Haplic lixisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.711, + "score_data_loc": 0.707, + "score_loc": 0.017 + }, + { + "component": "Xanthic ferralsols", + "componentData": "Missing Data", + "componentID": 105399, + "name": "Xanthic ferralsols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.659, + "score_data_loc": 0.705, + "score_loc": 0.067 + }, + { + "component": "Haplic ferralsols", + "componentData": "Missing Data", + "componentID": 105398, + "name": "Haplic ferralsols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "2", + "score_data": 0.659, + "score_data_loc": 0.68, + "score_loc": 0.042 + }, + { + "component": "Ferralic cambisols", + "componentData": "Data Complete", + "componentID": 105247, + "name": "Ferralic cambisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.659, + "score_data_loc": 0.656, + "score_loc": 0.017 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 104805, + "name": "Ferralic arenosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.524, + "score_data_loc": 0.525, + "score_loc": 0.017 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 105350, + "name": "Eutric cambisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.392, + "score_data_loc": 0.401, + "score_loc": 0.021 + }, + { + "component": "Eutric leptosols", + "componentData": "Missing Data", + "componentID": 104801, + "name": "Eutric leptosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "4", + "score_data": 0.752, + "score_data_loc": 0.002, + "score_loc": 0.033 + }, + { + "component": "Eutric leptosols", + "componentData": "Missing Data", + "componentID": 105349, + "name": "Eutric leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.752, + "score_data_loc": 0.002, + "score_loc": 0.033 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 105352, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.392, + "score_data_loc": 0.002, + "score_loc": 0.042 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json new file mode 100644 index 0000000..e52af42 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json @@ -0,0 +1,2067 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.2, + "sl5": 10.43, + "sl6": 10.4, + "sl7": 10.33 + }, + "clay": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 19.4, + "sl5": 21.43, + "sl6": 22.2, + "sl7": 22.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Gleyic alisols", + "name": "Gleyic alisols", + "rank_loc": "1", + "score_loc": 0.127 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.92, + "sl5": 4.89, + "sl6": 4.86, + "sl7": 4.83 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 4.8, + "sl5": 4.29, + "sl6": 3.6, + "sl7": 3.83 + }, + "sand": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 28.0, + "sl5": 28.43, + "sl6": 31.4, + "sl7": 33.83 + }, + "site": { + "siteData": { + "componentID": 104790, + "distance": 0.0, + "mapunitID": 12044, + "minCompDistance": 0.0, + "share": 70, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover.
These soils experience prolonged saturation from shallow groundwater. ", + "Description_es": "Los Alisoles Gleyicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua.
Estos suelos experimentan una saturación prolongada de las aguas subterráneas poco profundas. ", + "Description_fr": "Gleyic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover.
These soils experience prolonged saturation from shallow groundwater. ", + "Description_ks": "Gleyic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover.
These soils experience prolonged saturation from shallow groundwater. ", + "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotation andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity.
Drainage of these soils may be needed. However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers. ", + "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua.
Puede ser necesario el drenaje de estos suelos. Sin embargo, dado que se trata de una saturación a través de aguas subterráneas, esto puede no ser posible, por lo que se debe considerar la posibilidad de realizar cultivos con raíces superficiales.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta.", + "Management_fr": "
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotation andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity.
Drainage of these soils may be needed. However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers. ", + "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotation andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity.
Drainage of these soils may be needed. However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers. " + } + }, + "texture": { + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Silt loam", + "sl5": "Silt loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.4, + "sl5": 10.43, + "sl6": 10.4, + "sl7": 10.5 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 23.2, + "sl5": 24.57, + "sl6": 25.6, + "sl7": 25.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic alisols", + "name": "Haplic alisols1", + "rank_loc": "2", + "score_loc": 0.029 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.24, + "sl5": 5.21, + "sl6": 5.18, + "sl7": 5.17 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.4, + "sl5": 12.14, + "sl6": 13.4, + "sl7": 14.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 37.4, + "sl5": 36.86, + "sl6": 36.8, + "sl7": 37.33 + }, + "site": { + "siteData": { + "componentID": 104943, + "distance": 66876.888, + "mapunitID": 12083, + "minCompDistance": 66876.8882, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_es": "Los Alisoles Háplicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua. ", + "Description_fr": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_ks": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
Debido a su poca profundidad, estos suelos no son adecuados para el cultivo, por lo que debe considerarse su uso para el pastoreo.
La preservación de la superficie del suelo con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua. ", + "Management_fr": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.4, + "sl5": 14.0, + "sl6": 14.6, + "sl7": 14.67 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.2, + "sl5": 30.71, + "sl6": 33.0, + "sl7": 33.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols1", + "rank_loc": "3", + "score_loc": 0.027 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.24, + "sl5": 5.23, + "sl6": 5.22, + "sl7": 5.15 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.4, + "sl5": 3.86, + "sl6": 4.6, + "sl7": 5.5 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 48.6, + "sl5": 46.43, + "sl6": 44.2, + "sl7": 42.5 + }, + "site": { + "siteData": { + "componentID": 104786, + "distance": 58618.178, + "mapunitID": 12042, + "minCompDistance": 58618.178, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.14, + "sl6": 1.8, + "sl7": 1.67 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.86, + "sl6": 7.2, + "sl7": 7.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric leptosols", + "name": "Eutric leptosols", + "rank_loc": "4", + "score_loc": 0.023 + }, + "ph": { + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.5, + "sl5": 5.5, + "sl6": 5.5, + "sl7": 5.48 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.71, + "sl6": 4.4, + "sl7": 6.0 + }, + "sand": { + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 89.0, + "sl5": 88.86, + "sl6": 88.4, + "sl7": 88.17 + }, + "site": { + "siteData": { + "componentID": 104791, + "distance": 0.0, + "mapunitID": 12044, + "minCompDistance": 0.0, + "share": 10, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "5", + "score_loc": 0.023 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 105466, + "distance": 61918.695, + "mapunitID": 12226, + "minCompDistance": 61918.6954, + "share": 25, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 21.5 + }, + "clay": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 34.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 + }, + "id": { + "component": "Haplic ferralsols", + "name": "Haplic ferralsols1", + "rank_loc": "6", + "score_loc": 0.02 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.55 + }, + "rock_fragments": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 40.5 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 36.5 + }, + "site": { + "siteData": { + "componentID": 104785, + "distance": 58618.178, + "mapunitID": 12042, + "minCompDistance": 58618.178, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", + "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Rhodic ferralsols", + "name": "Rhodic ferralsols1", + "rank_loc": "7", + "score_loc": 0.02 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 104784, + "distance": 58618.178, + "mapunitID": 12042, + "minCompDistance": 58618.178, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", + "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Luvic phaeozems", + "name": "Luvic phaeozems1", + "rank_loc": "8", + "score_loc": 0.02 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 104946, + "distance": 88902.515, + "mapunitID": 12084, + "minCompDistance": 88902.5153, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", + "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.6, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.67 + }, + "clay": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 38.8, + "sl5": 39.86, + "sl6": 40.8, + "sl7": 41.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Umbric gleysols", + "name": "Umbric gleysols", + "rank_loc": "9", + "score_loc": 0.018 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.16, + "sl5": 5.19, + "sl6": 5.24, + "sl7": 5.28 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.4, + "sl5": 3.29, + "sl6": 3.2, + "sl7": 5.17 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 38.8, + "sl5": 37.86, + "sl6": 36.8, + "sl7": 36.0 + }, + "site": { + "siteData": { + "componentID": 104792, + "distance": 0.0, + "mapunitID": 12044, + "minCompDistance": 0.0, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ", + "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", + "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.14, + "sl6": 6.6, + "sl7": 6.33 + }, + "clay": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 49.8, + "sl5": 50.71, + "sl6": 51.4, + "sl7": 51.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Gleyic arenosols", + "name": "Gleyic arenosols", + "rank_loc": "10", + "score_loc": 0.018 + }, + "ph": { + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.44, + "sl5": 5.44, + "sl6": 5.46, + "sl7": 5.48 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 7.0, + "sl5": 5.29, + "sl6": 4.2, + "sl7": 4.67 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.57, + "sl6": 32.8, + "sl7": 32.5 + }, + "site": { + "siteData": { + "componentID": 104793, + "distance": 0.0, + "mapunitID": 12044, + "minCompDistance": 0.0, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.", + "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.6, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.67 + }, + "clay": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 38.8, + "sl5": 39.86, + "sl6": 40.8, + "sl7": 41.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "11", + "score_loc": 0.016 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.16, + "sl5": 5.19, + "sl6": 5.24, + "sl7": 5.28 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.4, + "sl5": 3.29, + "sl6": 3.2, + "sl7": 5.17 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 38.8, + "sl5": 37.86, + "sl6": 36.8, + "sl7": 36.0 + }, + "site": { + "siteData": { + "componentID": 105457, + "distance": 53803.703, + "mapunitID": 12224, + "minCompDistance": 53803.703, + "share": 35, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.0, + "sl5": 7.43, + "sl6": 7.0, + "sl7": 6.83 + }, + "clay": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 46.4, + "sl5": 47.43, + "sl6": 48.2, + "sl7": 48.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic cambisols", + "name": "Ferralic cambisols", + "rank_loc": "12", + "score_loc": 0.016 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.92, + "sl5": 4.96, + "sl6": 5.0, + "sl7": 5.02 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.6, + "sl5": 4.71, + "sl6": 5.0, + "sl7": 5.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 37.4, + "sl5": 36.57, + "sl6": 35.8, + "sl7": 35.5 + }, + "site": { + "siteData": { + "componentID": 105461, + "distance": 82783.427, + "mapunitID": 12225, + "minCompDistance": 82783.4266, + "share": 35, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.4, + "sl5": 7.71, + "sl6": 7.2, + "sl7": 7.0 + }, + "clay": { + "sl1": 48.0, + "sl2": 48.0, + "sl3": 48.0, + "sl4": 52.6, + "sl5": 53.86, + "sl6": 55.0, + "sl7": 55.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic alisols", + "name": "Haplic alisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.029 + }, + "ph": { + "sl1": 5.6, + "sl2": 5.6, + "sl3": 5.6, + "sl4": 5.62, + "sl5": 5.63, + "sl6": 5.64, + "sl7": 5.65 + }, + "rock_fragments": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 17.0, + "sl5": 12.71, + "sl6": 10.0, + "sl7": 8.83 + }, + "sand": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 32.2, + "sl5": 31.29, + "sl6": 30.4, + "sl7": 29.83 + }, + "site": { + "siteData": { + "componentID": 104944, + "distance": 88902.515, + "mapunitID": 12084, + "minCompDistance": 66876.8882, + "share": 65, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_es": "Los Alisoles Háplicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua. ", + "Description_fr": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_ks": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
Debido a su poca profundidad, estos suelos no son adecuados para el cultivo, por lo que debe considerarse su uso para el pastoreo.
La preservación de la superficie del suelo con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua. ", + "Management_fr": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 23.0, + "sl5": 22.29, + "sl6": 21.8, + "sl7": 21.5 + }, + "clay": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 40.2, + "sl5": 41.57, + "sl6": 42.0, + "sl7": 41.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.027 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.26, + "sl5": 6.29, + "sl6": 6.32, + "sl7": 6.32 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 8.4, + "sl5": 8.43, + "sl6": 8.6, + "sl7": 12.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.71, + "sl6": 33.8, + "sl7": 34.67 + }, + "site": { + "siteData": { + "componentID": 104894, + "distance": 68854.944, + "mapunitID": 12071, + "minCompDistance": 58618.178, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 21.4, + "sl5": 22.43, + "sl6": 23.0, + "sl7": 22.83 + }, + "clay": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 31.2, + "sl5": 33.71, + "sl6": 35.2, + "sl7": 35.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.023 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.26, + "sl5": 6.37, + "sl6": 6.52, + "sl7": 6.62 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 5.8, + "sl5": 6.71, + "sl6": 7.6, + "sl7": 9.83 + }, + "sand": { + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 30.0, + "sl5": 28.86, + "sl6": 28.0, + "sl7": 28.0 + }, + "site": { + "siteData": { + "componentID": 104895, + "distance": 93153.994, + "mapunitID": 12072, + "minCompDistance": 61918.6954, + "share": 50, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 19.6, + "sl5": 17.14, + "sl6": 14.6, + "sl7": 13.5 + }, + "clay": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 26.4, + "sl5": 26.29, + "sl6": 26.2, + "sl7": 25.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 + }, + "id": { + "component": "Haplic ferralsols", + "name": "Haplic ferralsols2", + "rank_loc": "Not Displayed", + "score_loc": 0.02 + }, + "ph": { + "sl1": 4.7, + "sl2": 4.7, + "sl3": 4.7, + "sl4": 4.86, + "sl5": 4.94, + "sl6": 5.02, + "sl7": 5.07 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 11.86, + "sl6": 13.6, + "sl7": 14.67 + }, + "sand": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 42.0, + "sl5": 43.43, + "sl6": 45.0, + "sl7": 47.17 + }, + "site": { + "siteData": { + "componentID": 105453, + "distance": 60797.484, + "mapunitID": 12223, + "minCompDistance": 58618.178, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", + "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.6, + "sl5": 3.14, + "sl6": 2.8, + "sl7": 2.67 + }, + "clay": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.14, + "sl6": 5.2, + "sl7": 5.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic ferralsols", + "name": "Haplic ferralsols3", + "rank_loc": "Not Displayed", + "score_loc": 0.02 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.8, + "sl5": 5.8, + "sl6": 5.8, + "sl7": 5.82 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 10.4, + "sl5": 11.0, + "sl6": 10.0, + "sl7": 8.83 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 87.2, + "sl5": 87.29, + "sl6": 87.4, + "sl7": 86.83 + }, + "site": { + "siteData": { + "componentID": 104892, + "distance": 68854.944, + "mapunitID": 12071, + "minCompDistance": 58618.178, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", + "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.0, + "sl5": 6.0, + "sl6": 6.0, + "sl7": 6.0 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 25.6, + "sl5": 28.14, + "sl6": 30.0, + "sl7": 30.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Rhodic ferralsols", + "name": "Rhodic ferralsols2", + "rank_loc": "Not Displayed", + "score_loc": 0.02 + }, + "ph": { + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.2, + "sl5": 5.19, + "sl6": 5.16, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.2, + "sl7": 5.83 + }, + "sand": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.8, + "sl5": 45.86, + "sl6": 44.8, + "sl7": 44.83 + }, + "site": { + "siteData": { + "componentID": 104891, + "distance": 68854.944, + "mapunitID": 12071, + "minCompDistance": 58618.178, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", + "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.6, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.67 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 31.4, + "sl5": 32.0, + "sl6": 32.6, + "sl7": 33.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 + }, + "id": { + "component": "Luvic phaeozems", + "name": "Luvic phaeozems2", + "rank_loc": "Not Displayed", + "score_loc": 0.02 + }, + "ph": { + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.2, + "sl5": 5.2, + "sl6": 5.2, + "sl7": 5.18 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 9.4, + "sl5": 9.86, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 43.0, + "sl5": 42.29, + "sl6": 41.4, + "sl7": 41.0 + }, + "site": { + "siteData": { + "componentID": 105449, + "distance": 91158.288, + "mapunitID": 12222, + "minCompDistance": 88902.5153, + "share": 45, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", + "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Haplic alisols", + "componentData": "Data Complete", + "componentID": 104943, + "name": "Haplic alisols1", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "2", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.029 + }, + { + "component": "Haplic ferralsols", + "componentData": "Missing Data", + "componentID": 104785, + "name": "Haplic ferralsols1", + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": "6", + "score_data": 1.0, + "score_data_loc": 0.991, + "score_loc": 0.02 + }, + { + "component": "Luvic phaeozems", + "componentData": "Missing Data", + "componentID": 104946, + "name": "Luvic phaeozems1", + "rank_data": "4", + "rank_data_loc": "3", + "rank_loc": "8", + "score_data": 1.0, + "score_data_loc": 0.991, + "score_loc": 0.02 + }, + { + "component": "Rhodic ferralsols", + "componentData": "No Data", + "componentID": 104784, + "name": "Rhodic ferralsols1", + "rank_data": "5", + "rank_data_loc": "4", + "rank_loc": "7", + "score_data": 1.0, + "score_data_loc": 0.991, + "score_loc": 0.02 + }, + { + "component": "Gleyic alisols", + "componentData": "Data Complete", + "componentID": 104790, + "name": "Gleyic alisols", + "rank_data": "8", + "rank_data_loc": "5", + "rank_loc": "1", + "score_data": 0.845, + "score_data_loc": 0.945, + "score_loc": 0.127 + }, + { + "component": "Gleyic arenosols", + "componentData": "Data Complete", + "componentID": 104793, + "name": "Gleyic arenosols", + "rank_data": "7", + "rank_data_loc": "6", + "rank_loc": "10", + "score_data": 0.895, + "score_data_loc": 0.887, + "score_loc": 0.018 + }, + { + "component": "Ferralic cambisols", + "componentData": "Data Complete", + "componentID": 105461, + "name": "Ferralic cambisols", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": "12", + "score_data": 0.895, + "score_data_loc": 0.885, + "score_loc": 0.016 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 104894, + "name": "Ferralic arenosols2", + "rank_data": "9", + "rank_data_loc": "8", + "rank_loc": "Not Displayed", + "score_data": 0.673, + "score_data_loc": 0.68, + "score_loc": 0.027 + }, + { + "component": "Umbric gleysols", + "componentData": "Data Complete", + "componentID": 104792, + "name": "Umbric gleysols", + "rank_data": "11", + "rank_data_loc": "9", + "rank_loc": "9", + "score_data": 0.673, + "score_data_loc": 0.672, + "score_loc": 0.018 + }, + { + "component": "Haplic acrisols", + "componentData": "Data Complete", + "componentID": 105457, + "name": "Haplic acrisols", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": "11", + "score_data": 0.673, + "score_data_loc": 0.669, + "score_loc": 0.016 + }, + { + "component": "Eutric leptosols", + "componentData": "Missing Data", + "componentID": 104791, + "name": "Eutric leptosols", + "rank_data": "12", + "rank_data_loc": "11", + "rank_loc": "4", + "score_data": 0.383, + "score_data_loc": 0.002, + "score_loc": 0.023 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 104895, + "name": "Lithic leptosols2", + "rank_data": "3", + "rank_data_loc": "12", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 0.002, + "score_loc": 0.023 + }, + { + "component": "Haplic ferralsols", + "componentData": "Missing Data", + "componentID": 105453, + "name": "Haplic ferralsols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 0.991, + "score_loc": 0.02 + }, + { + "component": "Haplic alisols", + "componentData": "Data Complete", + "componentID": 104944, + "name": "Haplic alisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.895, + "score_data_loc": 0.898, + "score_loc": 0.029 + }, + { + "component": "Rhodic ferralsols", + "componentData": "No Data", + "componentID": 104891, + "name": "Rhodic ferralsols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.698, + "score_data_loc": 0.698, + "score_loc": 0.02 + }, + { + "component": "Luvic phaeozems", + "componentData": "Missing Data", + "componentID": 105449, + "name": "Luvic phaeozems2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.673, + "score_data_loc": 0.674, + "score_loc": 0.02 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 104786, + "name": "Ferralic arenosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "3", + "score_data": 0.629, + "score_data_loc": 0.638, + "score_loc": 0.027 + }, + { + "component": "Haplic ferralsols", + "componentData": "No Data", + "componentID": 104892, + "name": "Haplic ferralsols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.516, + "score_data_loc": 0.521, + "score_loc": 0.02 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 105466, + "name": "Lithic leptosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "5", + "score_data": 0.516, + "score_data_loc": 0.002, + "score_loc": 0.023 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json new file mode 100644 index 0000000..93aaba9 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json @@ -0,0 +1,3291 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 16.0, + "sl5": 16.71, + "sl6": 17.4, + "sl7": 17.83 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 25.2, + "sl5": 26.57, + "sl6": 27.8, + "sl7": 28.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz1", + "rank_loc": "1", + "score_loc": 0.05 + }, + "ph": { + "sl1": 7.1, + "sl2": 7.1, + "sl3": 7.1, + "sl4": 7.56, + "sl5": 7.74, + "sl6": 7.94, + "sl7": 8.0 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.8, + "sl5": 6.14, + "sl6": 8.8, + "sl7": 10.67 + }, + "sand": { + "sl1": 50.0, + "sl2": 50.0, + "sl3": 50.0, + "sl4": 43.8, + "sl5": 42.43, + "sl6": 41.0, + "sl7": 40.33 + }, + "site": { + "siteData": { + "componentID": 148584, + "distance": 7539.61, + "mapunitID": 5933, + "minCompDistance": 7539.6102, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 19.2, + "sl5": 19.29, + "sl6": 19.0, + "sl7": 18.67 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 26.0, + "sl5": 26.29, + "sl6": 25.6, + "sl7": 24.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols1", + "rank_loc": "2", + "score_loc": 0.038 + }, + "ph": { + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.56, + "sl5": 8.63, + "sl6": 8.66, + "sl7": 8.65 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.4, + "sl7": 9.0 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 44.6, + "sl5": 44.57, + "sl6": 45.4, + "sl7": 46.17 + }, + "site": { + "siteData": { + "componentID": 148582, + "distance": 7539.61, + "mapunitID": 5933, + "minCompDistance": 7539.6102, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.0, + "sl5": 16.14, + "sl6": 17.2, + "sl7": 17.33 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 21.6, + "sl5": 23.57, + "sl6": 25.2, + "sl7": 25.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Cambic arenosols", + "name": "Cambic arenosols", + "rank_loc": "3", + "score_loc": 0.032 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.86, + "sl5": 7.09, + "sl6": 7.36, + "sl7": 7.47 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.2, + "sl7": 9.0 + }, + "sand": { + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 60.0, + "sl5": 58.14, + "sl6": 56.4, + "sl7": 56.17 + }, + "site": { + "siteData": { + "componentID": 148403, + "distance": 29716.363, + "mapunitID": 5876, + "minCompDistance": 29716.3626, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 19.2, + "sl5": 19.29, + "sl6": 19.0, + "sl7": 18.67 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 26.0, + "sl5": 26.29, + "sl6": 25.6, + "sl7": 24.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "4", + "score_loc": 0.032 + }, + "ph": { + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.56, + "sl5": 8.63, + "sl6": 8.66, + "sl7": 8.65 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.4, + "sl7": 9.0 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 44.6, + "sl5": 44.57, + "sl6": 45.4, + "sl7": 46.17 + }, + "site": { + "siteData": { + "componentID": 148388, + "distance": 50714.61, + "mapunitID": 5874, + "minCompDistance": 50714.6101, + "share": 20, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 13.6, + "sl5": 15.0, + "sl6": 16.4, + "sl7": 16.83 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 24.4, + "sl5": 26.86, + "sl6": 29.2, + "sl7": 30.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Vertisols", + "name": "Vertisols1", + "rank_loc": "5", + "score_loc": 0.032 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.26, + "sl5": 6.37, + "sl6": 6.52, + "sl7": 6.57 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.57, + "sl6": 2.4, + "sl7": 2.33 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 46.0, + "sl5": 44.14, + "sl6": 42.2, + "sl7": 42.0 + }, + "site": { + "siteData": { + "componentID": 148452, + "distance": 74511.638, + "mapunitID": 5890, + "minCompDistance": 74511.6383, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", + "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.6, + "sl5": 12.29, + "sl6": 14.2, + "sl7": 15.0 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 23.2, + "sl5": 27.0, + "sl6": 30.8, + "sl7": 32.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols1", + "rank_loc": "6", + "score_loc": 0.022 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.98, + "sl5": 6.11, + "sl6": 6.28, + "sl7": 6.42 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.0, + "sl5": 10.14, + "sl6": 11.0, + "sl7": 11.5 + }, + "sand": { + "sl1": 58.0, + "sl2": 58.0, + "sl3": 58.0, + "sl4": 52.8, + "sl5": 49.57, + "sl6": 46.0, + "sl7": 44.33 + }, + "site": { + "siteData": { + "componentID": 148401, + "distance": 29716.363, + "mapunitID": 5876, + "minCompDistance": 29716.3626, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 8.8, + "sl5": 10.0, + "sl6": 10.8, + "sl7": 11.33 + }, + "clay": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 18.4, + "sl5": 20.86, + "sl6": 22.2, + "sl7": 22.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.2, + "sl7": 1.33 + }, + "id": { + "component": "Dystric regosols", + "name": "Dystric regosols1", + "rank_loc": "7", + "score_loc": 0.021 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.36, + "sl5": 6.46, + "sl6": 6.64, + "sl7": 6.73 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 13.6, + "sl5": 11.29, + "sl6": 9.6, + "sl7": 8.83 + }, + "sand": { + "sl1": 80.0, + "sl2": 80.0, + "sl3": 80.0, + "sl4": 72.0, + "sl5": 70.0, + "sl6": 69.0, + "sl7": 68.0 + }, + "site": { + "siteData": { + "componentID": 148956, + "distance": 438.366, + "mapunitID": 6037, + "minCompDistance": 438.3662, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", + "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 13.6, + "sl5": 15.0, + "sl6": 16.4, + "sl7": 16.83 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 24.4, + "sl5": 26.86, + "sl6": 29.2, + "sl7": 30.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Albic arenosols", + "name": "Albic arenosols1", + "rank_loc": "8", + "score_loc": 0.021 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.26, + "sl5": 6.37, + "sl6": 6.52, + "sl7": 6.57 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.57, + "sl6": 2.4, + "sl7": 2.33 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 46.0, + "sl5": 44.14, + "sl6": 42.2, + "sl7": 42.0 + }, + "site": { + "siteData": { + "componentID": 148894, + "distance": 32877.453, + "mapunitID": 6017, + "minCompDistance": 32877.4526, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.", + "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.8, + "sl5": 3.57, + "sl6": 3.8, + "sl7": 3.5 + }, + "clay": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.0, + "sl5": 7.14, + "sl6": 7.6, + "sl7": 7.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic luvisols", + "name": "Haplic luvisols1", + "rank_loc": "9", + "score_loc": 0.016 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.46, + "sl6": 6.54, + "sl7": 6.55 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.4, + "sl5": 2.86, + "sl6": 2.8, + "sl7": 5.33 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.29, + "sl6": 85.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 148583, + "distance": 7539.61, + "mapunitID": 5933, + "minCompDistance": 7539.6102, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Calcic luvisols", + "name": "Calcic luvisols1", + "rank_loc": "10", + "score_loc": 0.013 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 148402, + "distance": 29716.363, + "mapunitID": 5876, + "minCompDistance": 29716.3626, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 39.6, + "sl5": 39.57, + "sl6": 39.4, + "sl7": 39.17 + }, + "clay": { + "sl1": 54.0, + "sl2": 54.0, + "sl3": 54.0, + "sl4": 55.2, + "sl5": 55.43, + "sl6": 55.4, + "sl7": 55.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 1.0, + "sl6": 1.4, + "sl7": 1.5 + }, + "id": { + "component": "Rhodic nitisols", + "name": "Rhodic nitisols", + "rank_loc": "11", + "score_loc": 0.013 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.64, + "sl5": 7.7, + "sl6": 7.76, + "sl7": 7.8 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.2, + "sl5": 2.57, + "sl6": 3.0, + "sl7": 3.33 + }, + "sand": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.8, + "sl5": 18.57, + "sl6": 18.6, + "sl7": 18.5 + }, + "site": { + "siteData": { + "componentID": 148454, + "distance": 74511.638, + "mapunitID": 5890, + "minCompDistance": 74511.6383, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", + "Description_es": "Los Nitisoles Ródicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes. *Los Nitisoles Ródicos tienen subsuelos de color rojo oscuro con alta sorción de P.", + "Description_fr": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", + "Description_ks": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", + "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", + "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la absorción de las plantas durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
Es especialmente importante que la fertilización con P se utilice en estos suelos, que se destacan específicamente por tener una alta sorción de P.", + "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", + "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 + }, + "clay": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Acrisols", + "name": "Acrisols1", + "rank_loc": "12", + "score_loc": 0.011 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 + }, + "site": { + "siteData": { + "componentID": 148895, + "distance": 32877.453, + "mapunitID": 6017, + "minCompDistance": 32877.4526, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz2", + "rank_loc": "Not Displayed", + "score_loc": 0.05 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 149438, + "distance": 50505.675, + "mapunitID": 6189, + "minCompDistance": 7539.6102, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.4, + "sl5": 40.29, + "sl6": 40.2, + "sl7": 39.67 + }, + "clay": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 54.8, + "sl5": 55.29, + "sl6": 55.6, + "sl7": 55.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.14, + "sl6": 0.4, + "sl7": 0.67 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz3", + "rank_loc": "Not Displayed", + "score_loc": 0.05 + }, + "ph": { + "sl1": 6.9, + "sl2": 6.9, + "sl3": 6.9, + "sl4": 7.06, + "sl5": 7.14, + "sl6": 7.3, + "sl7": 7.37 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.2, + "sl5": 2.43, + "sl6": 2.4, + "sl7": 2.33 + }, + "sand": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.14, + "sl6": 13.0, + "sl7": 13.0 + }, + "site": { + "siteData": { + "componentID": 148772, + "distance": 57897.214, + "mapunitID": 5986, + "minCompDistance": 7539.6102, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.6, + "sl5": 14.71, + "sl6": 15.0, + "sl7": 15.17 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.6, + "sl5": 29.86, + "sl6": 30.6, + "sl7": 30.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz4", + "rank_loc": "Not Displayed", + "score_loc": 0.05 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.44, + "sl6": 6.44, + "sl7": 6.43 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 9.29, + "sl6": 13.4, + "sl7": 12.5 + }, + "sand": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 49.0, + "sl5": 47.71, + "sl6": 46.6, + "sl7": 46.67 + }, + "site": { + "siteData": { + "componentID": 148560, + "distance": 63106.737, + "mapunitID": 5929, + "minCompDistance": 7539.6102, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.2, + "sl5": 18.43, + "sl6": 18.4, + "sl7": 17.83 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 34.2, + "sl5": 35.86, + "sl6": 37.2, + "sl7": 37.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.038 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.56, + "sl5": 6.57, + "sl6": 6.58, + "sl7": 6.55 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.6, + "sl5": 10.14, + "sl6": 9.8, + "sl7": 11.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.43, + "sl6": 32.6, + "sl7": 33.0 + }, + "site": { + "siteData": { + "componentID": 148773, + "distance": 57897.214, + "mapunitID": 5986, + "minCompDistance": 7539.6102, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols3", + "rank_loc": "Not Displayed", + "score_loc": 0.038 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 + }, + "sand": { + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 + }, + "site": { + "siteData": { + "componentID": 148558, + "distance": 63106.737, + "mapunitID": 5929, + "minCompDistance": 7539.6102, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.0, + "sl6": 6.4, + "sl7": 6.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.0, + "sl5": 17.14, + "sl6": 16.0, + "sl7": 15.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.0 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols4", + "rank_loc": "Not Displayed", + "score_loc": 0.038 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.08, + "sl5": 5.13, + "sl6": 5.16, + "sl7": 5.18 + }, + "rock_fragments": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 30.6, + "sl5": 31.14, + "sl6": 35.2, + "sl7": 36.67 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 57.6, + "sl5": 58.71, + "sl6": 60.2, + "sl7": 60.17 + }, + "site": { + "siteData": { + "componentID": 149078, + "distance": 95465.543, + "mapunitID": 6079, + "minCompDistance": 7539.6102, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 1.8, + "sl5": 1.57, + "sl6": 1.4, + "sl7": 1.33 + }, + "clay": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.0, + "sl7": 4.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.032 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.36, + "sl6": 5.42, + "sl7": 5.43 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.43, + "sl6": 3.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 86.0, + "sl2": 86.0, + "sl3": 86.0, + "sl4": 86.8, + "sl5": 86.86, + "sl6": 86.6, + "sl7": 86.33 + }, + "site": { + "siteData": { + "componentID": 148481, + "distance": 75034.597, + "mapunitID": 5896, + "minCompDistance": 50714.6101, + "share": 100, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.14, + "sl6": 1.8, + "sl7": 1.67 + }, + "clay": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.0, + "sl7": 4.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols3", + "rank_loc": "Not Displayed", + "score_loc": 0.032 + }, + "ph": { + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.5, + "sl5": 5.53, + "sl6": 5.58, + "sl7": 5.6 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.0, + "sl5": 3.14, + "sl6": 3.4, + "sl7": 4.17 + }, + "sand": { + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 88.6, + "sl5": 88.57, + "sl6": 88.4, + "sl7": 88.33 + }, + "site": { + "siteData": { + "componentID": 148386, + "distance": 85053.285, + "mapunitID": 5873, + "minCompDistance": 50714.6101, + "share": 10, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.8, + "sl5": 14.43, + "sl6": 13.2, + "sl7": 12.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 25.4, + "sl5": 25.86, + "sl6": 24.0, + "sl7": 22.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.33 + }, + "id": { + "component": "Vertisols", + "name": "Vertisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.032 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.54, + "sl5": 5.44, + "sl6": 5.42, + "sl7": 5.45 + }, + "rock_fragments": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.6, + "sl5": 21.14, + "sl6": 22.4, + "sl7": 23.67 + }, + "sand": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 40.2, + "sl5": 39.0, + "sl6": 42.4, + "sl7": 44.5 + }, + "site": { + "siteData": { + "componentID": 148225, + "distance": 98631.899, + "mapunitID": 5688, + "minCompDistance": 74511.6383, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", + "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.71, + "sl6": 15.2, + "sl7": 15.33 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 22.8, + "sl5": 24.86, + "sl6": 26.2, + "sl7": 26.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.2, + "sl7": 1.33 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.022 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.96, + "sl5": 5.97, + "sl6": 6.0, + "sl7": 6.03 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.2, + "sl5": 11.71, + "sl6": 12.8, + "sl7": 13.33 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 37.6, + "sl5": 36.57, + "sl6": 36.2, + "sl7": 36.67 + }, + "site": { + "siteData": { + "componentID": 148392, + "distance": 50714.61, + "mapunitID": 5874, + "minCompDistance": 29716.3626, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.6, + "sl5": 16.71, + "sl6": 16.6, + "sl7": 16.5 + }, + "clay": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 30.2, + "sl5": 31.57, + "sl6": 32.4, + "sl7": 32.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.022 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.22, + "sl5": 6.26, + "sl6": 6.32, + "sl7": 6.37 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 14.8, + "sl5": 15.29, + "sl6": 15.2, + "sl7": 14.67 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 43.6, + "sl5": 42.71, + "sl6": 42.4, + "sl7": 42.67 + }, + "site": { + "siteData": { + "componentID": 148455, + "distance": 74511.638, + "mapunitID": 5890, + "minCompDistance": 29716.3626, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 13.8, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 13.83 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.6, + "sl5": 20.14, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Dystric regosols", + "name": "Dystric regosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.021 + }, + "ph": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.14, + "sl5": 7.21, + "sl6": 7.34, + "sl7": 7.42 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.71, + "sl6": 17.8, + "sl7": 17.83 + }, + "sand": { + "sl1": 64.0, + "sl2": 64.0, + "sl3": 64.0, + "sl4": 61.2, + "sl5": 60.86, + "sl6": 60.8, + "sl7": 60.83 + }, + "site": { + "siteData": { + "componentID": 149439, + "distance": 50505.675, + "mapunitID": 6189, + "minCompDistance": 438.3662, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", + "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 16.0, + "sl5": 16.0, + "sl6": 16.0, + "sl7": 15.83 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 22.2, + "sl5": 23.0, + "sl6": 23.6, + "sl7": 23.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Albic arenosols", + "name": "Albic arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.021 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4, + "sl4": 7.56, + "sl5": 7.64, + "sl6": 7.74, + "sl7": 7.82 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 19.0, + "sl5": 21.0, + "sl6": 22.6, + "sl7": 22.83 + }, + "sand": { + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 55.0, + "sl5": 54.57, + "sl6": 54.2, + "sl7": 54.17 + }, + "site": { + "siteData": { + "componentID": 148907, + "distance": 35586.855, + "mapunitID": 6020, + "minCompDistance": 32877.4526, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.", + "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 20.2, + "sl5": 20.14, + "sl6": 19.8, + "sl7": 19.0 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 26.8, + "sl5": 27.86, + "sl6": 29.2, + "sl7": 28.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.8, + "sl7": 0.83 + }, + "id": { + "component": "Haplic luvisols", + "name": "Haplic luvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.016 + }, + "ph": { + "sl1": 7.6, + "sl2": 7.6, + "sl3": 7.6, + "sl4": 7.68, + "sl5": 7.74, + "sl6": 7.82, + "sl7": 7.88 + }, + "rock_fragments": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.0, + "sl5": 18.0, + "sl6": 21.2, + "sl7": 21.67 + }, + "sand": { + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 39.0, + "sl5": 38.29, + "sl6": 36.8, + "sl7": 36.83 + }, + "site": { + "siteData": { + "componentID": 148399, + "distance": 29716.363, + "mapunitID": 5876, + "minCompDistance": 7539.6102, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 14.0 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.2, + "sl5": 20.86, + "sl6": 21.2, + "sl7": 21.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic luvisols", + "name": "Haplic luvisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.016 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.72, + "sl5": 7.81, + "sl6": 7.92, + "sl7": 8.0 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.8, + "sl5": 27.86, + "sl6": 29.8, + "sl7": 30.17 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 62.4, + "sl5": 62.0, + "sl6": 62.0, + "sl7": 61.83 + }, + "site": { + "siteData": { + "componentID": 148456, + "distance": 74511.638, + "mapunitID": 5890, + "minCompDistance": 7539.6102, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 13.2, + "sl5": 12.86, + "sl6": 12.4, + "sl7": 12.17 + }, + "clay": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 52.8, + "sl5": 55.14, + "sl6": 57.4, + "sl7": 58.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcic luvisols", + "name": "Calcic luvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.013 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.74, + "sl5": 5.73, + "sl6": 5.72, + "sl7": 5.72 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.4, + "sl5": 2.71, + "sl6": 3.0, + "sl7": 3.33 + }, + "sand": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 25.0, + "sl5": 23.86, + "sl6": 22.8, + "sl7": 22.17 + }, + "site": { + "siteData": { + "componentID": 148589, + "distance": 46063.093, + "mapunitID": 5935, + "minCompDistance": 29716.3626, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.6, + "sl7": 6.67 + }, + "clay": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 30.8, + "sl5": 33.14, + "sl6": 35.6, + "sl7": 36.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcic luvisols", + "name": "Calcic luvisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.013 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.04, + "sl5": 5.03, + "sl6": 5.02, + "sl7": 5.02 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 17.8, + "sl5": 19.14, + "sl6": 19.6, + "sl7": 20.0 + }, + "sand": { + "sl1": 54.0, + "sl2": 54.0, + "sl3": 54.0, + "sl4": 49.6, + "sl5": 47.71, + "sl6": 45.6, + "sl7": 44.5 + }, + "site": { + "siteData": { + "componentID": 149440, + "distance": 50505.675, + "mapunitID": 6189, + "minCompDistance": 29716.3626, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.6, + "sl5": 3.71, + "sl6": 3.8, + "sl7": 3.83 + }, + "clay": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.4, + "sl5": 17.14, + "sl6": 18.6, + "sl7": 19.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Acrisols", + "name": "Acrisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.4, + "sl2": 5.4, + "sl3": 5.4, + "sl4": 5.22, + "sl5": 5.19, + "sl6": 5.16, + "sl7": 5.17 + }, + "rock_fragments": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.0, + "sl5": 9.14, + "sl6": 8.4, + "sl7": 9.17 + }, + "sand": { + "sl1": 77.0, + "sl2": 77.0, + "sl3": 77.0, + "sl4": 72.6, + "sl5": 71.0, + "sl6": 70.0, + "sl7": 69.33 + }, + "site": { + "siteData": { + "componentID": 148909, + "distance": 35586.855, + "mapunitID": 6020, + "minCompDistance": 32877.4526, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Vertisols", + "componentData": "No Data", + "componentID": 148225, + "name": "Vertisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.919, + "score_data_loc": 1.0, + "score_loc": 0.032 + }, + { + "component": "Chromic luvisols", + "componentData": "Missing Data", + "componentID": 148392, + "name": "Chromic luvisols2", + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.919, + "score_data_loc": 0.99, + "score_loc": 0.022 + }, + { + "component": "Albic arenosols", + "componentData": "Data Complete", + "componentID": 148894, + "name": "Albic arenosols1", + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": "8", + "score_data": 0.919, + "score_data_loc": 0.989, + "score_loc": 0.021 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 148772, + "name": "Haplic solonetz3", + "rank_data": "5", + "rank_data_loc": "4", + "rank_loc": "Not Displayed", + "score_data": 0.805, + "score_data_loc": 0.901, + "score_loc": 0.05 + }, + { + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 148589, + "name": "Calcic luvisols2", + "rank_data": "4", + "rank_data_loc": "5", + "rank_loc": "Not Displayed", + "score_data": 0.805, + "score_data_loc": 0.861, + "score_loc": 0.013 + }, + { + "component": "Rhodic nitisols", + "componentData": "No Data", + "componentID": 148454, + "name": "Rhodic nitisols", + "rank_data": "6", + "rank_data_loc": "6", + "rank_loc": "11", + "score_data": 0.805, + "score_data_loc": 0.861, + "score_loc": 0.013 + }, + { + "component": "Acrisols", + "componentData": "Missing Data", + "componentID": 148895, + "name": "Acrisols1", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": "12", + "score_data": 0.802, + "score_data_loc": 0.856, + "score_loc": 0.011 + }, + { + "component": "Eutric planosols", + "componentData": "Data Complete", + "componentID": 149078, + "name": "Eutric planosols4", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": "Not Displayed", + "score_data": 0.757, + "score_data_loc": 0.836, + "score_loc": 0.038 + }, + { + "component": "Haplic luvisols", + "componentData": "Data Complete", + "componentID": 148399, + "name": "Haplic luvisols2", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": "Not Displayed", + "score_data": 0.753, + "score_data_loc": 0.809, + "score_loc": 0.016 + }, + { + "component": "Cambic arenosols", + "componentData": "Data Complete", + "componentID": 148403, + "name": "Cambic arenosols", + "rank_data": "11", + "rank_data_loc": "10", + "rank_loc": "3", + "score_data": 0.722, + "score_data_loc": 0.793, + "score_loc": 0.032 + }, + { + "component": "Dystric regosols", + "componentData": "Data Complete", + "componentID": 149439, + "name": "Dystric regosols2", + "rank_data": "12", + "rank_data_loc": "11", + "rank_loc": "Not Displayed", + "score_data": 0.722, + "score_data_loc": 0.782, + "score_loc": 0.021 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 148388, + "name": "Lithic leptosols1", + "rank_data": "10", + "rank_data_loc": "12", + "rank_loc": "4", + "score_data": 0.753, + "score_data_loc": 0.002, + "score_loc": 0.032 + }, + { + "component": "Vertisols", + "componentData": "No Data", + "componentID": 148452, + "name": "Vertisols1", + "rank_data": "3", + "rank_data_loc": "Not Displayed", + "rank_loc": "5", + "score_data": 0.919, + "score_data_loc": 1.0, + "score_loc": 0.032 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 149438, + "name": "Haplic solonetz2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.802, + "score_data_loc": 0.897, + "score_loc": 0.05 + }, + { + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 148402, + "name": "Calcic luvisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "10", + "score_data": 0.802, + "score_data_loc": 0.858, + "score_loc": 0.013 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 148584, + "name": "Haplic solonetz1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.753, + "score_data_loc": 0.846, + "score_loc": 0.05 + }, + { + "component": "Eutric planosols", + "componentData": "Data Complete", + "componentID": 148582, + "name": "Eutric planosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "2", + "score_data": 0.753, + "score_data_loc": 0.832, + "score_loc": 0.038 + }, + { + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 148455, + "name": "Chromic luvisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.753, + "score_data_loc": 0.816, + "score_loc": 0.022 + }, + { + "component": "Eutric planosols", + "componentData": "Data Complete", + "componentID": 148558, + "name": "Eutric planosols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.722, + "score_data_loc": 0.799, + "score_loc": 0.038 + }, + { + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 148401, + "name": "Chromic luvisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "6", + "score_data": 0.722, + "score_data_loc": 0.783, + "score_loc": 0.022 + }, + { + "component": "Albic arenosols", + "componentData": "Data Complete", + "componentID": 148907, + "name": "Albic arenosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.722, + "score_data_loc": 0.782, + "score_loc": 0.021 + }, + { + "component": "Haplic luvisols", + "componentData": "Data Complete", + "componentID": 148456, + "name": "Haplic luvisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.722, + "score_data_loc": 0.776, + "score_loc": 0.016 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 148560, + "name": "Haplic solonetz4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.625, + "score_data_loc": 0.711, + "score_loc": 0.05 + }, + { + "component": "Acrisols", + "componentData": "Data Complete", + "componentID": 148909, + "name": "Acrisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.657, + "score_data_loc": 0.703, + "score_loc": 0.011 + }, + { + "component": "Dystric regosols", + "componentData": "Data Complete", + "componentID": 148956, + "name": "Dystric regosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "7", + "score_data": 0.622, + "score_data_loc": 0.677, + "score_loc": 0.021 + }, + { + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 149440, + "name": "Calcic luvisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.625, + "score_data_loc": 0.671, + "score_loc": 0.013 + }, + { + "component": "Eutric planosols", + "componentData": "Missing Data", + "componentID": 148773, + "name": "Eutric planosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.587, + "score_data_loc": 0.658, + "score_loc": 0.038 + }, + { + "component": "Haplic luvisols", + "componentData": "Data Complete", + "componentID": 148583, + "name": "Haplic luvisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "9", + "score_data": 0.557, + "score_data_loc": 0.603, + "score_loc": 0.016 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 148481, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.557, + "score_data_loc": 0.002, + "score_loc": 0.032 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 148386, + "name": "Lithic leptosols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.413, + "score_data_loc": 0.002, + "score_loc": 0.032 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json new file mode 100644 index 0000000..8673d13 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json @@ -0,0 +1,3163 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols1", + "rank_loc": "1", + "score_loc": 0.03 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 111242, + "distance": 45915.675, + "mapunitID": 17468, + "minCompDistance": 45915.6746, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.0, + "sl6": 2.0, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Humic nitisols", + "name": "Humic nitisols", + "rank_loc": "2", + "score_loc": 0.024 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.82, + "sl5": 5.77, + "sl6": 5.72, + "sl7": 5.72 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.71, + "sl6": 4.4, + "sl7": 8.83 + }, + "sand": { + "sl1": 90.0, + "sl2": 90.0, + "sl3": 90.0, + "sl4": 89.4, + "sl5": 89.29, + "sl6": 89.4, + "sl7": 89.5 + }, + "site": { + "siteData": { + "componentID": 111081, + "distance": 85305.924, + "mapunitID": 17379, + "minCompDistance": 85305.9237, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Humic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Humic Nitisols have relatively higher organic matter in surface horizons.", + "Description_es": "Los Nitisoles Húmicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes. *Los Nitisoles Húmicos tienen relativamente más materia orgánica en los horizontes superficiales.", + "Description_fr": "Humic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Humic Nitisols have relatively higher organic matter in surface horizons.", + "Description_ks": "Humic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Humic Nitisols have relatively higher organic matter in surface horizons.", + "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", + "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la planta durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación de fertilizantes fosfatados en banda (directamente sobre la semilla o a un lado y abajo de la semilla), ayudarán a reducir la fijación de P.", + "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", + "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation." + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 19.6, + "sl5": 18.43, + "sl6": 17.4, + "sl7": 16.67 + }, + "clay": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 49.0, + "sl5": 51.14, + "sl6": 54.0, + "sl7": 56.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols1", + "rank_loc": "3", + "score_loc": 0.015 + }, + "ph": { + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.24, + "sl5": 5.31, + "sl6": 5.4, + "sl7": 5.43 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 7.0, + "sl5": 6.71, + "sl6": 7.6, + "sl7": 8.33 + }, + "sand": { + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 25.4, + "sl5": 24.14, + "sl6": 22.6, + "sl7": 21.33 + }, + "site": { + "siteData": { + "componentID": 111208, + "distance": 36128.047, + "mapunitID": 17453, + "minCompDistance": 36128.0473, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.2, + "sl5": 30.29, + "sl6": 33.2, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Chromic cambisols", + "name": "Chromic cambisols1", + "rank_loc": "4", + "score_loc": 0.013 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.12, + "sl5": 6.07, + "sl6": 6.02, + "sl7": 6.02 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.8, + "sl5": 10.43, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 60.2, + "sl5": 57.57, + "sl6": 54.8, + "sl7": 53.0 + }, + "site": { + "siteData": { + "componentID": 111105, + "distance": 54718.541, + "mapunitID": 17393, + "minCompDistance": 54718.5415, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.14, + "sl6": 5.2, + "sl7": 5.33 + }, + "clay": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 18.8, + "sl5": 20.43, + "sl6": 22.2, + "sl7": 22.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric vertisols", + "name": "Eutric vertisols1", + "rank_loc": "5", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.0, + "sl5": 5.99, + "sl6": 6.0, + "sl7": 6.02 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.8, + "sl5": 5.86, + "sl6": 9.2, + "sl7": 9.5 + }, + "sand": { + "sl1": 76.0, + "sl2": 76.0, + "sl3": 76.0, + "sl4": 71.4, + "sl5": 69.86, + "sl6": 68.2, + "sl7": 67.67 + }, + "site": { + "siteData": { + "componentID": 111101, + "distance": 9085.201, + "mapunitID": 17390, + "minCompDistance": 9085.2006, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.0, + "sl5": 6.14, + "sl6": 6.4, + "sl7": 6.5 + }, + "clay": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 25.0, + "sl5": 28.14, + "sl6": 30.6, + "sl7": 31.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols1", + "rank_loc": "6", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.6, + "sl2": 5.6, + "sl3": 5.6, + "sl4": 5.68, + "sl5": 5.71, + "sl6": 5.74, + "sl7": 5.73 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 10.8, + "sl5": 10.29, + "sl6": 11.4, + "sl7": 11.17 + }, + "sand": { + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 56.8, + "sl5": 54.14, + "sl6": 52.2, + "sl7": 51.67 + }, + "site": { + "siteData": { + "componentID": 111282, + "distance": 9861.436, + "mapunitID": 17486, + "minCompDistance": 9861.4358, + "share": 85, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.2, + "sl5": 18.29, + "sl6": 18.2, + "sl7": 17.67 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.4, + "sl5": 31.71, + "sl6": 31.4, + "sl7": 31.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 + }, + "id": { + "component": "Humic cambisols", + "name": "Humic cambisols", + "rank_loc": "7", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.6, + "sl2": 6.6, + "sl3": 6.6, + "sl4": 6.56, + "sl5": 6.6, + "sl6": 6.68, + "sl7": 6.77 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 12.0, + "sl5": 14.14, + "sl6": 12.6, + "sl7": 10.83 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.8, + "sl5": 41.57, + "sl6": 42.0, + "sl7": 42.67 + }, + "site": { + "siteData": { + "componentID": 111631, + "distance": 26306.421, + "mapunitID": 17694, + "minCompDistance": 26306.4211, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Description_es": "Los Cambisoles Húmicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos tienen más materia orgánica en los horizontes superficiales.
Cuando el clima y el paisaje son favorables, estos suelos pueden ser productivos. ", + "Description_fr": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Description_ks": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 19.6, + "sl5": 19.0, + "sl6": 17.8, + "sl7": 17.67 + }, + "clay": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 39.0, + "sl5": 39.57, + "sl6": 40.0, + "sl7": 40.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 + }, + "id": { + "component": "Ferric luvisols", + "name": "Ferric luvisols1", + "rank_loc": "8", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.18, + "sl5": 6.2, + "sl6": 6.2, + "sl7": 6.28 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 9.4, + "sl5": 11.29, + "sl6": 16.4, + "sl7": 19.5 + }, + "sand": { + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 31.4, + "sl5": 31.57, + "sl6": 32.4, + "sl7": 32.33 + }, + "site": { + "siteData": { + "componentID": 111336, + "distance": 36837.751, + "mapunitID": 17518, + "minCompDistance": 36837.7515, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.2, + "sl5": 12.43, + "sl6": 13.0, + "sl7": 13.33 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 22.8, + "sl5": 23.29, + "sl6": 23.4, + "sl7": 23.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz1", + "rank_loc": "9", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.9, + "sl5": 6.96, + "sl6": 7.06, + "sl7": 7.13 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 8.6, + "sl5": 10.14, + "sl6": 10.8, + "sl7": 12.17 + }, + "sand": { + "sl1": 61.0, + "sl2": 61.0, + "sl3": 61.0, + "sl4": 58.6, + "sl5": 58.43, + "sl6": 58.2, + "sl7": 58.5 + }, + "site": { + "siteData": { + "componentID": 111044, + "distance": 38961.991, + "mapunitID": 17359, + "minCompDistance": 38961.9906, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 39.8, + "sl5": 40.0, + "sl6": 39.8, + "sl7": 39.5 + }, + "clay": { + "sl1": 52.0, + "sl2": 52.0, + "sl3": 52.0, + "sl4": 54.6, + "sl5": 55.14, + "sl6": 55.4, + "sl7": 54.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Calcic luvisols", + "name": "Calcic luvisols", + "rank_loc": "10", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.78, + "sl5": 6.84, + "sl6": 6.94, + "sl7": 7.05 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.6, + "sl5": 3.71, + "sl6": 4.0, + "sl7": 4.0 + }, + "sand": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 19.8, + "sl5": 19.71, + "sl6": 19.8, + "sl7": 20.17 + }, + "site": { + "siteData": { + "componentID": 111218, + "distance": 52061.241, + "mapunitID": 17457, + "minCompDistance": 52061.2413, + "share": 70, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 37.4, + "sl5": 36.0, + "sl6": 33.2, + "sl7": 32.0 + }, + "clay": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 42.4, + "sl5": 40.14, + "sl6": 36.4, + "sl7": 34.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Gleyic solonchaks", + "name": "Gleyic solonchaks1", + "rank_loc": "11", + "score_loc": 0.011 + }, + "ph": { + "sl1": 7.6, + "sl2": 7.6, + "sl3": 7.6, + "sl4": 7.76, + "sl5": 7.83, + "sl6": 7.94, + "sl7": 8.02 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 21.8, + "sl5": 24.0, + "sl6": 22.8, + "sl7": 22.83 + }, + "sand": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 29.4, + "sl5": 30.43, + "sl6": 32.4, + "sl7": 33.5 + }, + "site": { + "siteData": { + "componentID": 111319, + "distance": 53068.322, + "mapunitID": 17507, + "minCompDistance": 53068.3217, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", + "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 21.6, + "sl5": 20.29, + "sl6": 18.8, + "sl7": 18.17 + }, + "clay": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 34.4, + "sl5": 34.14, + "sl6": 33.6, + "sl7": 33.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols1", + "rank_loc": "12", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.06, + "sl5": 5.09, + "sl6": 5.12, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 10.8, + "sl5": 11.14, + "sl6": 14.0, + "sl7": 16.17 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 38.2, + "sl5": 38.57, + "sl6": 39.0, + "sl7": 39.33 + }, + "site": { + "siteData": { + "componentID": 111337, + "distance": 70615.69, + "mapunitID": 17519, + "minCompDistance": 70615.6896, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.0, + "sl5": 40.14, + "sl6": 40.2, + "sl7": 40.17 + }, + "clay": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 55.8, + "sl5": 55.86, + "sl6": 55.6, + "sl7": 55.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.03 + }, + "ph": { + "sl1": 7.3, + "sl2": 7.3, + "sl3": 7.3, + "sl4": 7.46, + "sl5": 7.53, + "sl6": 7.58, + "sl7": 7.62 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.71, + "sl6": 3.0, + "sl7": 3.0 + }, + "sand": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 20.2, + "sl5": 20.0, + "sl6": 20.0, + "sl7": 20.17 + }, + "site": { + "siteData": { + "componentID": 111264, + "distance": 72257.485, + "mapunitID": 17476, + "minCompDistance": 45915.6746, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 39.8, + "sl5": 40.0, + "sl6": 39.8, + "sl7": 39.5 + }, + "clay": { + "sl1": 52.0, + "sl2": 52.0, + "sl3": 52.0, + "sl4": 54.6, + "sl5": 55.14, + "sl6": 55.4, + "sl7": 54.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.015 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.78, + "sl5": 6.84, + "sl6": 6.94, + "sl7": 7.05 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.6, + "sl5": 3.71, + "sl6": 4.0, + "sl7": 4.0 + }, + "sand": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 19.8, + "sl5": 19.71, + "sl6": 19.8, + "sl7": 20.17 + }, + "site": { + "siteData": { + "componentID": 111216, + "distance": 41935.929, + "mapunitID": 17456, + "minCompDistance": 36128.0473, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.8, + "sl5": 8.29, + "sl6": 9.0, + "sl7": 9.17 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 18.4, + "sl5": 19.71, + "sl6": 21.2, + "sl7": 21.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.015 + }, + "ph": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.06, + "sl5": 6.07, + "sl6": 6.08, + "sl7": 6.03 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.4, + "sl5": 6.29, + "sl6": 6.0, + "sl7": 5.83 + }, + "sand": { + "sl1": 72.0, + "sl2": 72.0, + "sl3": 72.0, + "sl4": 69.6, + "sl5": 68.43, + "sl6": 67.0, + "sl7": 66.67 + }, + "site": { + "siteData": { + "componentID": 116199, + "distance": 74794.646, + "mapunitID": 27168, + "minCompDistance": 36128.0473, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 19.2, + "sl5": 19.29, + "sl6": 19.0, + "sl7": 18.67 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 26.0, + "sl5": 26.29, + "sl6": 25.6, + "sl7": 24.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Chromic cambisols", + "name": "Chromic cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.013 + }, + "ph": { + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.56, + "sl5": 8.63, + "sl6": 8.66, + "sl7": 8.65 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.4, + "sl7": 9.0 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 44.6, + "sl5": 44.57, + "sl6": 45.4, + "sl7": 46.17 + }, + "site": { + "siteData": { + "componentID": 111117, + "distance": 72048.113, + "mapunitID": 17400, + "minCompDistance": 54718.5415, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 10.29, + "sl6": 11.6, + "sl7": 12.33 + }, + "clay": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 19.0, + "sl5": 22.0, + "sl6": 25.4, + "sl7": 26.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Chromic cambisols", + "name": "Chromic cambisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.013 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.44, + "sl5": 6.43, + "sl6": 6.4, + "sl7": 6.4 + }, + "rock_fragments": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.43, + "sl6": 5.6, + "sl7": 5.17 + }, + "sand": { + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 63.2, + "sl5": 60.43, + "sl6": 56.8, + "sl7": 55.0 + }, + "site": { + "siteData": { + "componentID": 111267, + "distance": 73282.727, + "mapunitID": 17478, + "minCompDistance": 54718.5415, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 41.0, + "sl5": 41.0, + "sl6": 41.0, + "sl7": 40.5 + }, + "clay": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 56.8, + "sl5": 57.14, + "sl6": 57.0, + "sl7": 56.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Eutric vertisols", + "name": "Eutric vertisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.8, + "sl2": 6.8, + "sl3": 6.8, + "sl4": 7.02, + "sl5": 7.13, + "sl6": 7.26, + "sl7": 7.33 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.14, + "sl6": 4.2, + "sl7": 4.0 + }, + "sand": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 12.4, + "sl5": 12.29, + "sl6": 12.4, + "sl7": 12.5 + }, + "site": { + "siteData": { + "componentID": 111286, + "distance": 34446.462, + "mapunitID": 17488, + "minCompDistance": 9085.2006, + "share": 85, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 16.0, + "sl5": 16.0, + "sl6": 16.0, + "sl7": 15.83 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 22.2, + "sl5": 23.0, + "sl6": 23.6, + "sl7": 23.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Eutric vertisols", + "name": "Eutric vertisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4, + "sl4": 7.56, + "sl5": 7.64, + "sl6": 7.74, + "sl7": 7.82 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 19.0, + "sl5": 21.0, + "sl6": 22.6, + "sl7": 22.83 + }, + "sand": { + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 55.0, + "sl5": 54.57, + "sl6": 54.2, + "sl7": 54.17 + }, + "site": { + "siteData": { + "componentID": 111202, + "distance": 35027.212, + "mapunitID": 17450, + "minCompDistance": 9085.2006, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 26.0, + "sl5": 25.43, + "sl6": 25.2, + "sl7": 24.17 + }, + "clay": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 37.6, + "sl5": 38.71, + "sl6": 39.6, + "sl7": 39.0 + }, + "ec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.2, + "sl5": 16.86, + "sl6": 17.4, + "sl7": 17.5 + }, + "id": { + "component": "Eutric vertisols", + "name": "Eutric vertisols4", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 8.96, + "sl5": 8.96, + "sl6": 8.94, + "sl7": 9.0 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 11.4, + "sl5": 13.14, + "sl6": 10.4, + "sl7": 9.0 + }, + "sand": { + "sl1": 32.0, + "sl2": 32.0, + "sl3": 32.0, + "sl4": 30.6, + "sl5": 31.14, + "sl6": 30.8, + "sl7": 30.33 + }, + "site": { + "siteData": { + "componentID": 111193, + "distance": 47856.589, + "mapunitID": 17448, + "minCompDistance": 9085.2006, + "share": 70, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.0, + "sl5": 16.14, + "sl6": 17.2, + "sl7": 17.33 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 21.6, + "sl5": 23.57, + "sl6": 25.2, + "sl7": 25.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Eutric vertisols", + "name": "Eutric vertisols5", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.86, + "sl5": 7.09, + "sl6": 7.36, + "sl7": 7.47 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.2, + "sl7": 9.0 + }, + "sand": { + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 60.0, + "sl5": 58.14, + "sl6": 56.4, + "sl7": 56.17 + }, + "site": { + "siteData": { + "componentID": 111079, + "distance": 62588.145, + "mapunitID": 17378, + "minCompDistance": 9085.2006, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 16.6, + "sl5": 16.29, + "sl6": 16.4, + "sl7": 16.33 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.0, + "sl5": 28.57, + "sl6": 28.8, + "sl7": 29.0 + }, + "ec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 8.5, + "sl2": 8.5, + "sl3": 8.5, + "sl4": 8.56, + "sl5": 8.51, + "sl6": 8.52, + "sl7": 8.52 + }, + "rock_fragments": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 21.6, + "sl5": 22.29, + "sl6": 17.8, + "sl7": 18.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 42.6, + "sl5": 43.0, + "sl6": 42.8, + "sl7": 42.5 + }, + "site": { + "siteData": { + "componentID": 111641, + "distance": 63488.662, + "mapunitID": 17701, + "minCompDistance": 9861.4358, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 41.0, + "sl5": 41.0, + "sl6": 41.0, + "sl7": 40.5 + }, + "clay": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 56.8, + "sl5": 57.14, + "sl6": 57.0, + "sl7": 56.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Ferric luvisols", + "name": "Ferric luvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.8, + "sl2": 6.8, + "sl3": 6.8, + "sl4": 7.02, + "sl5": 7.13, + "sl6": 7.26, + "sl7": 7.33 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.14, + "sl6": 4.2, + "sl7": 4.0 + }, + "sand": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 12.4, + "sl5": 12.29, + "sl6": 12.4, + "sl7": 12.5 + }, + "site": { + "siteData": { + "componentID": 111335, + "distance": 41456.411, + "mapunitID": 17517, + "minCompDistance": 36837.7515, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Ferric luvisols", + "name": "Ferric luvisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 116201, + "distance": 74794.646, + "mapunitID": 27168, + "minCompDistance": 36837.7515, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.6, + "sl5": 21.86, + "sl6": 22.2, + "sl7": 22.67 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.0, + "sl5": 31.43, + "sl6": 31.4, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.47, + "sl6": 6.58, + "sl7": 6.65 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.8, + "sl5": 16.57, + "sl6": 17.8, + "sl7": 16.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.2, + "sl5": 39.14, + "sl6": 39.6, + "sl7": 39.33 + }, + "site": { + "siteData": { + "componentID": 110985, + "distance": 55011.679, + "mapunitID": 17327, + "minCompDistance": 38961.9906, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.2, + "sl5": 11.57, + "sl6": 12.2, + "sl7": 12.67 + }, + "clay": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 28.4, + "sl5": 29.86, + "sl6": 31.2, + "sl7": 31.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.8, + "sl7": 1.0 + }, + "id": { + "component": "Gleyic solonchaks", + "name": "Gleyic solonchaks2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 6.0, + "sl5": 6.03, + "sl6": 6.04, + "sl7": 6.08 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 7.2, + "sl5": 9.71, + "sl6": 10.0, + "sl7": 8.83 + }, + "sand": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 34.2, + "sl5": 32.71, + "sl6": 31.0, + "sl7": 30.17 + }, + "site": { + "siteData": { + "componentID": 111103, + "distance": 60642.675, + "mapunitID": 17392, + "minCompDistance": 53068.3217, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", + "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 14.8, + "sl5": 14.57, + "sl6": 14.2, + "sl7": 14.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.6, + "sl5": 20.86, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 0.8, + "sl5": 0.71, + "sl6": 0.8, + "sl7": 0.83 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.54, + "sl5": 6.6, + "sl6": 6.66, + "sl7": 6.7 + }, + "rock_fragments": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 15.0, + "sl5": 16.57, + "sl6": 18.8, + "sl7": 19.17 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.8, + "sl5": 41.14, + "sl6": 41.8, + "sl7": 42.17 + }, + "site": { + "siteData": { + "componentID": 110980, + "distance": 76138.236, + "mapunitID": 17324, + "minCompDistance": 70615.6896, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.6, + "sl5": 21.86, + "sl6": 22.2, + "sl7": 22.67 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.0, + "sl5": 31.43, + "sl6": 31.4, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.47, + "sl6": 6.58, + "sl7": 6.65 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.8, + "sl5": 16.57, + "sl6": 17.8, + "sl7": 16.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.2, + "sl5": 39.14, + "sl6": 39.6, + "sl7": 39.33 + }, + "site": { + "siteData": { + "componentID": 110986, + "distance": 78053.869, + "mapunitID": 17328, + "minCompDistance": 70615.6896, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Humic cambisols", + "componentData": "Data Complete", + "componentID": 111631, + "name": "Humic cambisols", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "7", + "score_data": 0.747, + "score_data_loc": 1.0, + "score_loc": 0.011 + }, + { + "component": "Chromic cambisols", + "componentData": "Data Complete", + "componentID": 111105, + "name": "Chromic cambisols1", + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": "4", + "score_data": 0.724, + "score_data_loc": 0.973, + "score_loc": 0.013 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 111264, + "name": "Ferralic arenosols2", + "rank_data": "5", + "rank_data_loc": "3", + "rank_loc": "Not Displayed", + "score_data": 0.705, + "score_data_loc": 0.971, + "score_loc": 0.03 + }, + { + "component": "Haplic lixisols", + "componentData": "Missing Data", + "componentID": 111208, + "name": "Haplic lixisols1", + "rank_data": "7", + "rank_data_loc": "4", + "rank_loc": "3", + "score_data": 0.705, + "score_data_loc": 0.951, + "score_loc": 0.015 + }, + { + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 111218, + "name": "Calcic luvisols", + "rank_data": "3", + "rank_data_loc": "5", + "rank_loc": "10", + "score_data": 0.705, + "score_data_loc": 0.945, + "score_loc": 0.011 + }, + { + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111286, + "name": "Eutric vertisols2", + "rank_data": "4", + "rank_data_loc": "6", + "rank_loc": "Not Displayed", + "score_data": 0.705, + "score_data_loc": 0.945, + "score_loc": 0.011 + }, + { + "component": "Ferric luvisols", + "componentData": "Data Complete", + "componentID": 111336, + "name": "Ferric luvisols1", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": "8", + "score_data": 0.705, + "score_data_loc": 0.945, + "score_loc": 0.011 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 111337, + "name": "Eutric cambisols1", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": "12", + "score_data": 0.697, + "score_data_loc": 0.934, + "score_loc": 0.011 + }, + { + "component": "Gleyic solonchaks", + "componentData": "Data Complete", + "componentID": 111103, + "name": "Gleyic solonchaks2", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": "Not Displayed", + "score_data": 0.697, + "score_data_loc": 0.934, + "score_loc": 0.011 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 110985, + "name": "Haplic solonetz2", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": "Not Displayed", + "score_data": 0.697, + "score_data_loc": 0.934, + "score_loc": 0.011 + }, + { + "component": "Calcaric cambisols", + "componentData": "Missing Data", + "componentID": 111282, + "name": "Calcaric cambisols1", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": "6", + "score_data": 0.672, + "score_data_loc": 0.902, + "score_loc": 0.011 + }, + { + "component": "Humic nitisols", + "componentData": "No Data", + "componentID": 111081, + "name": "Humic nitisols", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": "2", + "score_data": 0.125, + "score_data_loc": 0.196, + "score_loc": 0.024 + }, + { + "component": "Haplic lixisols", + "componentData": "Data Complete", + "componentID": 111216, + "name": "Haplic lixisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.705, + "score_data_loc": 0.951, + "score_loc": 0.015 + }, + { + "component": "Ferric luvisols", + "componentData": "Data Complete", + "componentID": 111335, + "name": "Ferric luvisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.705, + "score_data_loc": 0.945, + "score_loc": 0.011 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 110986, + "name": "Eutric cambisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.697, + "score_data_loc": 0.934, + "score_loc": 0.011 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 111641, + "name": "Calcaric cambisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.665, + "score_data_loc": 0.893, + "score_loc": 0.011 + }, + { + "component": "Gleyic solonchaks", + "componentData": "Missing Data", + "componentID": 111319, + "name": "Gleyic solonchaks1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "11", + "score_data": 0.66, + "score_data_loc": 0.885, + "score_loc": 0.011 + }, + { + "component": "Chromic cambisols", + "componentData": "Missing Data", + "componentID": 111117, + "name": "Chromic cambisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.633, + "score_data_loc": 0.853, + "score_loc": 0.013 + }, + { + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111193, + "name": "Eutric vertisols4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.608, + "score_data_loc": 0.818, + "score_loc": 0.011 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 110980, + "name": "Eutric cambisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.597, + "score_data_loc": 0.802, + "score_loc": 0.011 + }, + { + "component": "Ferric luvisols", + "componentData": "Data Complete", + "componentID": 116201, + "name": "Ferric luvisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.597, + "score_data_loc": 0.802, + "score_loc": 0.011 + }, + { + "component": "Haplic lixisols", + "componentData": "Data Complete", + "componentID": 116199, + "name": "Haplic lixisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.583, + "score_data_loc": 0.79, + "score_loc": 0.015 + }, + { + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111101, + "name": "Eutric vertisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "5", + "score_data": 0.587, + "score_data_loc": 0.789, + "score_loc": 0.011 + }, + { + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111202, + "name": "Eutric vertisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.587, + "score_data_loc": 0.789, + "score_loc": 0.011 + }, + { + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111079, + "name": "Eutric vertisols5", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.587, + "score_data_loc": 0.789, + "score_loc": 0.011 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 111044, + "name": "Haplic solonetz1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "9", + "score_data": 0.587, + "score_data_loc": 0.789, + "score_loc": 0.011 + }, + { + "component": "Chromic cambisols", + "componentData": "Data Complete", + "componentID": 111267, + "name": "Chromic cambisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.583, + "score_data_loc": 0.787, + "score_loc": 0.013 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 111242, + "name": "Ferralic arenosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.245, + "score_data_loc": 0.364, + "score_loc": 0.03 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json new file mode 100644 index 0000000..69dee36 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json @@ -0,0 +1,2043 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.2, + "sl5": 12.71, + "sl6": 12.4, + "sl7": 12.5 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 26.2, + "sl5": 25.57, + "sl6": 25.2, + "sl7": 25.0 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Salic fluvisols", + "name": "Salic fluvisols1", + "rank_loc": "1", + "score_loc": 0.091 + }, + "ph": { + "sl1": 8.4, + "sl2": 8.4, + "sl3": 8.4, + "sl4": 8.4, + "sl5": 8.41, + "sl6": 8.44, + "sl7": 8.45 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 6.0, + "sl5": 7.71, + "sl6": 10.4, + "sl7": 10.67 + }, + "sand": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 39.4, + "sl5": 40.43, + "sl6": 41.0, + "sl7": 41.5 + }, + "site": { + "siteData": { + "componentID": 113476, + "distance": 0.5, + "mapunitID": 18586, + "minCompDistance": 0.5004, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", + "Description_es": "Los Fluvisoles Sálicos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles salinos tienen una alta salinidad en la parte superior del suelo.", + "Description_fr": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", + "Description_ks": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
La lixiviación con una fuente de agua de alta calidad (baja salinidad) será necesaria para desplazar las sales fuera de la zona de enraizamiento.
También se recomienda el uso de cultivos y variedades tolerantes a la sal.
Por último, es necesario gestionar los programas de fertilización para evitar la sobreaplicación y la acumulación de sales.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 14.8, + "sl5": 13.71, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 26.8, + "sl5": 26.0, + "sl6": 25.2, + "sl7": 25.0 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz1", + "rank_loc": "2", + "score_loc": 0.064 + }, + "ph": { + "sl1": 8.5, + "sl2": 8.5, + "sl3": 8.5, + "sl4": 8.5, + "sl5": 8.5, + "sl6": 8.52, + "sl7": 8.53 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 5.2, + "sl5": 7.14, + "sl6": 10.0, + "sl7": 8.83 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 41.0, + "sl5": 42.43, + "sl6": 43.4, + "sl7": 44.33 + }, + "site": { + "siteData": { + "componentID": 113444, + "distance": 78150.205, + "mapunitID": 18575, + "minCompDistance": 78150.2053, + "share": 25, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.0, + "sl5": 16.14, + "sl6": 17.2, + "sl7": 17.33 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 21.6, + "sl5": 23.57, + "sl6": 25.2, + "sl7": 25.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Mollic fluvisols", + "name": "Mollic fluvisols", + "rank_loc": "3", + "score_loc": 0.055 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.86, + "sl5": 7.09, + "sl6": 7.36, + "sl7": 7.47 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.2, + "sl7": 9.0 + }, + "sand": { + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 60.0, + "sl5": 58.14, + "sl6": 56.4, + "sl7": 56.17 + }, + "site": { + "siteData": { + "componentID": 113477, + "distance": 0.5, + "mapunitID": 18586, + "minCompDistance": 0.5004, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.", + "Description_es": "Los Fluvisoles Mólicos se encuentran principalmente en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles móllicos tienen una materia orgánica y nutrientes relativamente altos en los horizontes superficiales.", + "Description_fr": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.", + "Description_ks": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 19.2, + "sl5": 19.29, + "sl6": 19.0, + "sl7": 18.67 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 26.0, + "sl5": 26.29, + "sl6": 25.6, + "sl7": 24.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 + }, + "id": { + "component": "Cambic arenosols", + "name": "Cambic arenosols1", + "rank_loc": "4", + "score_loc": 0.055 + }, + "ph": { + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.56, + "sl5": 8.63, + "sl6": 8.66, + "sl7": 8.65 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.4, + "sl7": 9.0 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 44.6, + "sl5": 44.57, + "sl6": 45.4, + "sl7": 46.17 + }, + "site": { + "siteData": { + "componentID": 113015, + "distance": 35390.017, + "mapunitID": 18417, + "minCompDistance": 35390.0171, + "share": 60, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 21.4, + "sl5": 21.0, + "sl6": 20.2, + "sl7": 18.67 + }, + "clay": { + "sl1": 32.0, + "sl2": 32.0, + "sl3": 32.0, + "sl4": 33.4, + "sl5": 32.86, + "sl6": 31.4, + "sl7": 29.83 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Eutric fluvisols", + "name": "Eutric fluvisols1", + "rank_loc": "5", + "score_loc": 0.045 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.52, + "sl5": 6.56, + "sl6": 6.62, + "sl7": 6.7 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.6, + "sl5": 16.43, + "sl6": 17.4, + "sl7": 18.0 + }, + "sand": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 40.0, + "sl5": 41.29, + "sl6": 43.8, + "sl7": 45.33 + }, + "site": { + "siteData": { + "componentID": 113479, + "distance": 0.5, + "mapunitID": 18586, + "minCompDistance": 0.5004, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.0, + "sl7": 4.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.8, + "sl5": 5.57, + "sl6": 5.4, + "sl7": 5.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols", + "rank_loc": "6", + "score_loc": 0.045 + }, + "ph": { + "sl1": 6.9, + "sl2": 6.9, + "sl3": 6.9, + "sl4": 6.82, + "sl5": 6.8, + "sl6": 6.8, + "sl7": 6.82 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 14.4, + "sl5": 16.57, + "sl6": 21.2, + "sl7": 20.67 + }, + "sand": { + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 89.2, + "sl5": 89.29, + "sl6": 89.2, + "sl7": 89.17 + }, + "site": { + "siteData": { + "componentID": 113157, + "distance": 91670.472, + "mapunitID": 18461, + "minCompDistance": 91670.4723, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.8, + "sl5": 3.57, + "sl6": 3.8, + "sl7": 3.5 + }, + "clay": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.0, + "sl5": 7.14, + "sl6": 7.6, + "sl7": 7.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols1", + "rank_loc": "7", + "score_loc": 0.039 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.46, + "sl6": 6.54, + "sl7": 6.55 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.4, + "sl5": 2.86, + "sl6": 2.8, + "sl7": 5.33 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.29, + "sl6": 85.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 112871, + "distance": 14598.857, + "mapunitID": 18373, + "minCompDistance": 14598.8574, + "share": 85, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.14, + "sl6": 17.6, + "sl7": 17.5 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.2, + "sl5": 32.14, + "sl6": 31.6, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols1", + "rank_loc": "8", + "score_loc": 0.036 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.24, + "sl5": 6.3, + "sl6": 6.38, + "sl7": 6.43 + }, + "rock_fragments": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.6, + "sl5": 9.86, + "sl6": 10.2, + "sl7": 10.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.2, + "sl5": 36.86, + "sl6": 38.4, + "sl7": 38.83 + }, + "site": { + "siteData": { + "componentID": 113053, + "distance": 0.0, + "mapunitID": 18428, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.6, + "sl5": 13.57, + "sl6": 13.0, + "sl7": 13.17 + }, + "clay": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.8, + "sl5": 18.86, + "sl6": 18.8, + "sl7": 18.83 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Haplic arenosols", + "name": "Haplic arenosols", + "rank_loc": "9", + "score_loc": 0.036 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.62, + "sl5": 7.66, + "sl6": 7.68, + "sl7": 7.7 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.57, + "sl6": 4.4, + "sl7": 5.5 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.2, + "sl5": 54.14, + "sl6": 54.6, + "sl7": 55.0 + }, + "site": { + "siteData": { + "componentID": 113413, + "distance": 70158.54, + "mapunitID": 18564, + "minCompDistance": 70158.5404, + "share": 80, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_es": "Los Arenosoles Háplicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.", + "Description_fr": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_ks": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.0, + "sl6": 15.8, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.8, + "sl5": 21.14, + "sl6": 21.2, + "sl7": 21.0 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "10", + "score_loc": 0.029 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.64, + "sl5": 7.69, + "sl6": 7.72, + "sl7": 7.77 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 12.4, + "sl5": 14.0, + "sl6": 16.0, + "sl7": 16.0 + }, + "sand": { + "sl1": 52.0, + "sl2": 52.0, + "sl3": 52.0, + "sl4": 51.2, + "sl5": 50.86, + "sl6": 51.0, + "sl7": 51.0 + }, + "site": { + "siteData": { + "componentID": 112901, + "distance": 86897.899, + "mapunitID": 18384, + "minCompDistance": 86897.8986, + "share": 65, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Sandy clay loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Gleyic solonetz", + "name": "Gleyic solonetz", + "rank_loc": "11", + "score_loc": 0.027 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 113054, + "distance": 0.0, + "mapunitID": 18428, + "minCompDistance": 0.0, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Solonetz have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.
Gleyic Solonetz are saturated with shallow groundwater within one meter of the soil surface.", + "Description_es": "Los Solonetz Gléyicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.
Los Solonetz gleyicos están saturados de aguas subterráneas poco profundas a menos de un metro de la superficie del suelo.", + "Description_fr": "Gleyic Solonetz have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.
Gleyic Solonetz are saturated with shallow groundwater within one meter of the soil surface.", + "Description_ks": "Gleyic Solonetz have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.
Gleyic Solonetz are saturated with shallow groundwater within one meter of the soil surface.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
Drainage of these soils will be needed, both to eliminate standing water and remediate sodicity issues.
To further improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto contenido de sodio en los horizontes subsuperficiales, lo que da lugar a una estructura deficiente del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Será necesario drenar estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de sodicidad.
Para mejorar aún más el drenaje interno, debería aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
Drainage of these soils will be needed, both to eliminate standing water and remediate sodicity issues.
To further improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
Drainage of these soils will be needed, both to eliminate standing water and remediate sodicity issues.
To further improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.0, + "sl6": 2.0, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Umbric gleysols", + "name": "Umbric gleysols", + "rank_loc": "12", + "score_loc": 0.027 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.82, + "sl5": 5.77, + "sl6": 5.72, + "sl7": 5.72 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.71, + "sl6": 4.4, + "sl7": 8.83 + }, + "sand": { + "sl1": 90.0, + "sl2": 90.0, + "sl3": 90.0, + "sl4": 89.4, + "sl5": 89.29, + "sl6": 89.4, + "sl7": 89.5 + }, + "site": { + "siteData": { + "componentID": 112974, + "distance": 54381.47, + "mapunitID": 18406, + "minCompDistance": 54381.47, + "share": 60, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ", + "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", + "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 8.8, + "sl5": 10.0, + "sl6": 10.8, + "sl7": 11.33 + }, + "clay": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 18.4, + "sl5": 20.86, + "sl6": 22.2, + "sl7": 22.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.2, + "sl7": 1.33 + }, + "id": { + "component": "Salic fluvisols", + "name": "Salic fluvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.091 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.36, + "sl5": 6.46, + "sl6": 6.64, + "sl7": 6.73 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 13.6, + "sl5": 11.29, + "sl6": 9.6, + "sl7": 8.83 + }, + "sand": { + "sl1": 80.0, + "sl2": 80.0, + "sl3": 80.0, + "sl4": 72.0, + "sl5": 70.0, + "sl6": 69.0, + "sl7": 68.0 + }, + "site": { + "siteData": { + "componentID": 113242, + "distance": 39959.704, + "mapunitID": 18495, + "minCompDistance": 0.5004, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", + "Description_es": "Los Fluvisoles Sálicos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles salinos tienen una alta salinidad en la parte superior del suelo.", + "Description_fr": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", + "Description_ks": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
La lixiviación con una fuente de agua de alta calidad (baja salinidad) será necesaria para desplazar las sales fuera de la zona de enraizamiento.
También se recomienda el uso de cultivos y variedades tolerantes a la sal.
Por último, es necesario gestionar los programas de fertilización para evitar la sobreaplicación y la acumulación de sales.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.6, + "sl5": 3.14, + "sl6": 3.0, + "sl7": 2.83 + }, + "clay": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.0, + "sl6": 5.0, + "sl7": 5.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic solonetz", + "name": "Haplic solonetz2", + "rank_loc": "Not Displayed", + "score_loc": 0.064 + }, + "ph": { + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.72, + "sl5": 5.74, + "sl6": 5.76, + "sl7": 5.77 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.8, + "sl5": 5.43, + "sl6": 5.0, + "sl7": 4.5 + }, + "sand": { + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 88.0, + "sl5": 88.0, + "sl6": 88.2, + "sl7": 88.17 + }, + "site": { + "siteData": { + "componentID": 112902, + "distance": 86897.899, + "mapunitID": 18384, + "minCompDistance": 78150.2053, + "share": 35, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.6, + "sl5": 12.29, + "sl6": 14.2, + "sl7": 15.0 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 23.2, + "sl5": 27.0, + "sl6": 30.8, + "sl7": 32.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Cambic arenosols", + "name": "Cambic arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.055 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.98, + "sl5": 6.11, + "sl6": 6.28, + "sl7": 6.42 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.0, + "sl5": 10.14, + "sl6": 11.0, + "sl7": 11.5 + }, + "sand": { + "sl1": 58.0, + "sl2": 58.0, + "sl3": 58.0, + "sl4": 52.8, + "sl5": 49.57, + "sl6": 46.0, + "sl7": 44.33 + }, + "site": { + "siteData": { + "componentID": 112938, + "distance": 45507.906, + "mapunitID": 18395, + "minCompDistance": 35390.0171, + "share": 85, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Eutric fluvisols", + "name": "Eutric fluvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.045 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 + }, + "sand": { + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 + }, + "site": { + "siteData": { + "componentID": 113211, + "distance": 25925.864, + "mapunitID": 18484, + "minCompDistance": 0.5004, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.0, + "sl5": 16.14, + "sl6": 16.6, + "sl7": 17.0 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 29.2, + "sl5": 30.14, + "sl6": 30.8, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.86, + "sl6": 5.0, + "sl7": 5.17 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.039 + }, + "ph": { + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 8.26, + "sl5": 8.41, + "sl6": 8.6, + "sl7": 8.7 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.2, + "sl7": 4.5 + }, + "sand": { + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 38.4, + "sl5": 37.14, + "sl6": 35.6, + "sl7": 35.0 + }, + "site": { + "siteData": { + "componentID": 113127, + "distance": 95990.463, + "mapunitID": 18450, + "minCompDistance": 14598.8574, + "share": 85, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 26.2, + "sl5": 24.71, + "sl6": 23.0, + "sl7": 21.5 + }, + "clay": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 49.0, + "sl5": 48.43, + "sl6": 46.8, + "sl7": 46.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.036 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.9, + "sl5": 4.91, + "sl6": 4.9, + "sl7": 4.9 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 10.0, + "sl5": 11.43, + "sl6": 13.4, + "sl7": 14.33 + }, + "sand": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 25.0, + "sl5": 26.14, + "sl6": 27.6, + "sl7": 27.83 + }, + "site": { + "siteData": { + "componentID": 113443, + "distance": 78150.205, + "mapunitID": 18575, + "minCompDistance": 0.0, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Salic fluvisols", + "componentData": "Data Complete", + "componentID": 113242, + "name": "Salic fluvisols2", + "rank_data": "7", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.9, + "score_data_loc": 1.0, + "score_loc": 0.091 + }, + { + "component": "Cambic arenosols", + "componentData": "Data Complete", + "componentID": 112938, + "name": "Cambic arenosols2", + "rank_data": "1", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.9, + "score_data_loc": 0.963, + "score_loc": 0.055 + }, + { + "component": "Mollic fluvisols", + "componentData": "Data Complete", + "componentID": 113477, + "name": "Mollic fluvisols", + "rank_data": "6", + "rank_data_loc": "3", + "rank_loc": "3", + "score_data": 0.9, + "score_data_loc": 0.963, + "score_loc": 0.055 + }, + { + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 113211, + "name": "Eutric fluvisols2", + "rank_data": "2", + "rank_data_loc": "4", + "rank_loc": "Not Displayed", + "score_data": 0.9, + "score_data_loc": 0.954, + "score_loc": 0.045 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 112871, + "name": "Ferralic arenosols1", + "rank_data": "3", + "rank_data_loc": "5", + "rank_loc": "7", + "score_data": 0.9, + "score_data_loc": 0.947, + "score_loc": 0.039 + }, + { + "component": "Haplic arenosols", + "componentData": "Data Complete", + "componentID": 113413, + "name": "Haplic arenosols", + "rank_data": "5", + "rank_data_loc": "6", + "rank_loc": "9", + "score_data": 0.9, + "score_data_loc": 0.945, + "score_loc": 0.036 + }, + { + "component": "Gleyic solonetz", + "componentData": "Data Complete", + "componentID": 113054, + "name": "Gleyic solonetz", + "rank_data": "4", + "rank_data_loc": "7", + "rank_loc": "11", + "score_data": 0.9, + "score_data_loc": 0.936, + "score_loc": 0.027 + }, + { + "component": "Eutric planosols", + "componentData": "Missing Data", + "componentID": 113443, + "name": "Eutric planosols2", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": "Not Displayed", + "score_data": 0.833, + "score_data_loc": 0.877, + "score_loc": 0.036 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 112902, + "name": "Haplic solonetz2", + "rank_data": "10", + "rank_data_loc": "9", + "rank_loc": "Not Displayed", + "score_data": 0.756, + "score_data_loc": 0.827, + "score_loc": 0.064 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 113157, + "name": "Eutric cambisols", + "rank_data": "9", + "rank_data_loc": "10", + "rank_loc": "6", + "score_data": 0.756, + "score_data_loc": 0.808, + "score_loc": 0.045 + }, + { + "component": "Umbric gleysols", + "componentData": "Missing Data", + "componentID": 112974, + "name": "Umbric gleysols", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": "12", + "score_data": 0.756, + "score_data_loc": 0.79, + "score_loc": 0.027 + }, + { + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 112901, + "name": "Chromic luvisols", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": "10", + "score_data": 0.576, + "score_data_loc": 0.611, + "score_loc": 0.029 + }, + { + "component": "Salic fluvisols", + "componentData": "Data Complete", + "componentID": 113476, + "name": "Salic fluvisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.576, + "score_data_loc": 0.673, + "score_loc": 0.091 + }, + { + "component": "Haplic solonetz", + "componentData": "Data Complete", + "componentID": 113444, + "name": "Haplic solonetz1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "2", + "score_data": 0.576, + "score_data_loc": 0.645, + "score_loc": 0.064 + }, + { + "component": "Cambic arenosols", + "componentData": "Data Complete", + "componentID": 113015, + "name": "Cambic arenosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "4", + "score_data": 0.576, + "score_data_loc": 0.636, + "score_loc": 0.055 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 113127, + "name": "Ferralic arenosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.576, + "score_data_loc": 0.62, + "score_loc": 0.039 + }, + { + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 113479, + "name": "Eutric fluvisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "5", + "score_data": 0.244, + "score_data_loc": 0.292, + "score_loc": 0.045 + }, + { + "component": "Eutric planosols", + "componentData": "Data Complete", + "componentID": 113053, + "name": "Eutric planosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "8", + "score_data": 0.244, + "score_data_loc": 0.283, + "score_loc": 0.036 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json new file mode 100644 index 0000000..8d5a2f1 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json @@ -0,0 +1,1371 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.0, + "sl5": 11.0, + "sl6": 11.0, + "sl7": 10.83 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 37.6, + "sl5": 41.0, + "sl6": 44.2, + "sl7": 45.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic nitisols", + "name": "Haplic nitisols", + "rank_loc": "1", + "score_loc": 0.094 + }, + "ph": { + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.36, + "sl5": 5.31, + "sl6": 5.28, + "sl7": 5.27 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 13.2, + "sl5": 14.14, + "sl6": 13.0, + "sl7": 11.5 + }, + "sand": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 40.6, + "sl5": 38.0, + "sl6": 35.4, + "sl7": 34.67 + }, + "site": { + "siteData": { + "componentID": 141607, + "distance": 0.357, + "mapunitID": 4413, + "minCompDistance": 0.3573, + "share": 40, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", + "Description_es": "Los Nitisoles Háplicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes.", + "Description_fr": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", + "Description_ks": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", + "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", + "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la planta durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación de fertilizantes fosfatados en banda (directamente sobre la semilla o a un lado y abajo de la semilla), ayudarán a reducir la fijación de P.", + "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", + "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation." + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Clay loam", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.0, + "sl5": 16.14, + "sl6": 16.6, + "sl7": 16.83 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 33.8, + "sl5": 35.57, + "sl6": 37.4, + "sl7": 38.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 + }, + "id": { + "component": "Gleyic cambisols", + "name": "Gleyic cambisols", + "rank_loc": "2", + "score_loc": 0.071 + }, + "ph": { + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.78, + "sl5": 5.83, + "sl6": 5.9, + "sl7": 5.93 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 7.6, + "sl5": 8.29, + "sl6": 8.0, + "sl7": 8.17 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 39.0, + "sl5": 37.57, + "sl6": 35.8, + "sl7": 35.0 + }, + "site": { + "siteData": { + "componentID": 142288, + "distance": 0.0, + "mapunitID": 4478, + "minCompDistance": 0.0, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Cambisols are widely occurring soils with limited soil development.
These soils are saturated with shallow groundwater above one meter of soil depth.", + "Description_es": "Los Cambisoles Gleyicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro de profundidad.", + "Description_fr": "Gleyic Cambisols are widely occurring soils with limited soil development.
These soils are saturated with shallow groundwater above one meter of soil depth.", + "Description_ks": "Gleyic Cambisols are widely occurring soils with limited soil development.
These soils are saturated with shallow groundwater above one meter of soil depth.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación procedente de aguas subterráneas, puede que no sea posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 41.6, + "sl5": 41.57, + "sl6": 41.2, + "sl7": 40.83 + }, + "clay": { + "sl1": 52.0, + "sl2": 52.0, + "sl3": 52.0, + "sl4": 54.6, + "sl5": 55.14, + "sl6": 55.2, + "sl7": 54.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Vertisols", + "name": "Vertisols", + "rank_loc": "3", + "score_loc": 0.047 + }, + "ph": { + "sl1": 6.8, + "sl2": 6.8, + "sl3": 6.8, + "sl4": 6.88, + "sl5": 6.94, + "sl6": 7.04, + "sl7": 7.17 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.6, + "sl5": 4.71, + "sl6": 4.8, + "sl7": 5.0 + }, + "sand": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 19.8, + "sl5": 19.71, + "sl6": 20.0, + "sl7": 20.33 + }, + "site": { + "siteData": { + "componentID": 142292, + "distance": 0.0, + "mapunitID": 4478, + "minCompDistance": 0.0, + "share": 5, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", + "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.8, + "sl5": 11.86, + "sl6": 13.0, + "sl7": 13.5 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 22.2, + "sl5": 25.57, + "sl6": 28.6, + "sl7": 29.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.4, + "sl7": 1.67 + }, + "id": { + "component": "Gleyic luvisols", + "name": "Gleyic luvisols", + "rank_loc": "4", + "score_loc": 0.047 + }, + "ph": { + "sl1": 6.3, + "sl2": 6.3, + "sl3": 6.3, + "sl4": 6.34, + "sl5": 6.41, + "sl6": 6.54, + "sl7": 6.62 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 8.4, + "sl5": 13.14, + "sl6": 17.8, + "sl7": 15.67 + }, + "sand": { + "sl1": 62.0, + "sl2": 62.0, + "sl3": 62.0, + "sl4": 57.4, + "sl5": 54.57, + "sl6": 51.4, + "sl7": 49.83 + }, + "site": { + "siteData": { + "componentID": 142289, + "distance": 0.0, + "mapunitID": 4478, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.", + "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.6, + "sl5": 21.86, + "sl6": 22.2, + "sl7": 22.67 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.0, + "sl5": 31.43, + "sl6": 31.4, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols", + "rank_loc": "5", + "score_loc": 0.047 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.47, + "sl6": 6.58, + "sl7": 6.65 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.8, + "sl5": 16.57, + "sl6": 17.8, + "sl7": 16.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.2, + "sl5": 39.14, + "sl6": 39.6, + "sl7": 39.33 + }, + "site": { + "siteData": { + "componentID": 141611, + "distance": 0.357, + "mapunitID": 4413, + "minCompDistance": 0.3573, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 6.4, + "sl5": 6.29, + "sl6": 6.2, + "sl7": 6.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 28.8, + "sl5": 31.14, + "sl6": 33.4, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "6", + "score_loc": 0.047 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.04, + "sl5": 5.03, + "sl6": 5.02, + "sl7": 5.02 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 14.0 + }, + "sand": { + "sl1": 59.0, + "sl2": 59.0, + "sl3": 59.0, + "sl4": 54.4, + "sl5": 52.29, + "sl6": 50.2, + "sl7": 49.17 + }, + "site": { + "siteData": { + "componentID": 141609, + "distance": 0.357, + "mapunitID": 4413, + "minCompDistance": 0.3573, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 12.8, + "sl5": 12.57, + "sl6": 12.2, + "sl7": 11.83 + }, + "clay": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 50.4, + "sl5": 52.86, + "sl6": 55.2, + "sl7": 56.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Rhodic nitisols", + "name": "Rhodic nitisols", + "rank_loc": "7", + "score_loc": 0.047 + }, + "ph": { + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.64, + "sl5": 5.63, + "sl6": 5.64, + "sl7": 5.65 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.2, + "sl5": 2.86, + "sl6": 3.4, + "sl7": 3.67 + }, + "sand": { + "sl1": 32.0, + "sl2": 32.0, + "sl3": 32.0, + "sl4": 27.0, + "sl5": 25.71, + "sl6": 24.6, + "sl7": 24.17 + }, + "site": { + "siteData": { + "componentID": 141608, + "distance": 0.357, + "mapunitID": 4413, + "minCompDistance": 0.3573, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", + "Description_es": "Los Nitisoles Ródicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes. *Los Nitisoles Ródicos tienen subsuelos de color rojo oscuro con alta sorción de P.", + "Description_fr": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", + "Description_ks": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", + "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", + "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la absorción de las plantas durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
Es especialmente importante que la fertilización con P se utilice en estos suelos, que se destacan específicamente por tener una alta sorción de P.", + "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", + "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 17.0, + "sl5": 16.29, + "sl6": 15.6, + "sl7": 15.33 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.8, + "sl5": 30.14, + "sl6": 30.0, + "sl7": 29.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 + }, + "id": { + "component": "Dystric cambisols", + "name": "Dystric cambisols", + "rank_loc": "8", + "score_loc": 0.047 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.02, + "sl5": 5.06, + "sl6": 5.12, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.4, + "sl5": 14.43, + "sl6": 15.2, + "sl7": 16.67 + }, + "sand": { + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 42.6, + "sl5": 42.57, + "sl6": 42.6, + "sl7": 43.0 + }, + "site": { + "siteData": { + "componentID": 142153, + "distance": 9267.434, + "mapunitID": 4465, + "minCompDistance": 9267.4336, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", + "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.14, + "sl6": 17.6, + "sl7": 17.5 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.2, + "sl5": 32.14, + "sl6": 31.6, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "9", + "score_loc": 0.041 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.24, + "sl5": 6.3, + "sl6": 6.38, + "sl7": 6.43 + }, + "rock_fragments": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.6, + "sl5": 9.86, + "sl6": 10.2, + "sl7": 10.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.2, + "sl5": 36.86, + "sl6": 38.4, + "sl7": 38.83 + }, + "site": { + "siteData": { + "componentID": 142595, + "distance": 92425.303, + "mapunitID": 4503, + "minCompDistance": 92425.3027, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.6, + "sl5": 17.86, + "sl6": 18.4, + "sl7": 18.83 + }, + "clay": { + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 35.8, + "sl5": 36.71, + "sl6": 37.8, + "sl7": 38.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Eutric gleysols", + "name": "Eutric gleysols", + "rank_loc": "10", + "score_loc": 0.035 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.96, + "sl5": 5.97, + "sl6": 6.02, + "sl7": 6.05 + }, + "rock_fragments": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 17.6, + "sl5": 17.14, + "sl6": 14.8, + "sl7": 15.83 + }, + "sand": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.6, + "sl5": 33.29, + "sl6": 32.8, + "sl7": 31.83 + }, + "site": { + "siteData": { + "componentID": 142594, + "distance": 92425.303, + "mapunitID": 4503, + "minCompDistance": 92425.3027, + "share": 60, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.8, + "sl5": 3.57, + "sl6": 3.8, + "sl7": 3.5 + }, + "clay": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.0, + "sl5": 7.14, + "sl6": 7.6, + "sl7": 7.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Cambic arenosols", + "name": "Cambic arenosols", + "rank_loc": "11", + "score_loc": 0.029 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.46, + "sl6": 6.54, + "sl7": 6.55 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.4, + "sl5": 2.86, + "sl6": 2.8, + "sl7": 5.33 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.29, + "sl6": 85.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 143286, + "distance": 57428.221, + "mapunitID": 4564, + "minCompDistance": 57428.2213, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.6, + "sl5": 16.71, + "sl6": 16.6, + "sl7": 16.5 + }, + "clay": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 30.2, + "sl5": 31.57, + "sl6": 32.4, + "sl7": 32.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic luvisols", + "name": "Haplic luvisols", + "rank_loc": "12", + "score_loc": 0.024 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.22, + "sl5": 6.26, + "sl6": 6.32, + "sl7": 6.37 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 14.8, + "sl5": 15.29, + "sl6": 15.2, + "sl7": 14.67 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 43.6, + "sl5": 42.71, + "sl6": 42.4, + "sl7": 42.67 + }, + "site": { + "siteData": { + "componentID": 141610, + "distance": 0.357, + "mapunitID": 4413, + "minCompDistance": 0.3573, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Vertisols", + "componentData": "No Data", + "componentID": 142292, + "name": "Vertisols", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": 3, + "score_data": 0.69, + "score_data_loc": 1.0, + "score_loc": 0.047 + }, + { + "component": "Gleyic cambisols", + "componentData": "Missing Data", + "componentID": 142288, + "name": "Gleyic cambisols", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": 2, + "score_data": 0.605, + "score_data_loc": 0.916, + "score_loc": 0.071 + }, + { + "component": "Dystric cambisols", + "componentData": "Data Complete", + "componentID": 142153, + "name": "Dystric cambisols", + "rank_data": "2", + "rank_data_loc": "3", + "rank_loc": 8, + "score_data": 0.605, + "score_data_loc": 0.884, + "score_loc": 0.047 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 141611, + "name": "Eutric cambisols", + "rank_data": "3", + "rank_data_loc": "4", + "rank_loc": 5, + "score_data": 0.605, + "score_data_loc": 0.884, + "score_loc": 0.047 + }, + { + "component": "Eutric gleysols", + "componentData": "Missing Data", + "componentID": 142594, + "name": "Eutric gleysols", + "rank_data": "5", + "rank_data_loc": "5", + "rank_loc": 10, + "score_data": 0.597, + "score_data_loc": 0.857, + "score_loc": 0.035 + }, + { + "component": "Haplic nitisols", + "componentData": "Missing Data", + "componentID": 141607, + "name": "Haplic nitisols", + "rank_data": "9", + "rank_data_loc": "6", + "rank_loc": 1, + "score_data": 0.516, + "score_data_loc": 0.828, + "score_loc": 0.094 + }, + { + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 142595, + "name": "Eutric fluvisols", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": 9, + "score_data": 0.554, + "score_data_loc": 0.807, + "score_loc": 0.041 + }, + { + "component": "Rhodic nitisols", + "componentData": "No Data", + "componentID": 141608, + "name": "Rhodic nitisols", + "rank_data": "7", + "rank_data_loc": "8", + "rank_loc": 7, + "score_data": 0.533, + "score_data_loc": 0.787, + "score_loc": 0.047 + }, + { + "component": "Haplic luvisols", + "componentData": "Data Complete", + "componentID": 141610, + "name": "Haplic luvisols", + "rank_data": "8", + "rank_data_loc": "9", + "rank_loc": 12, + "score_data": 0.52, + "score_data_loc": 0.737, + "score_loc": 0.024 + }, + { + "component": "Gleyic luvisols", + "componentData": "Data Complete", + "componentID": 142289, + "name": "Gleyic luvisols", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": 4, + "score_data": 0.36, + "score_data_loc": 0.552, + "score_loc": 0.047 + }, + { + "component": "Haplic acrisols", + "componentData": "Data Complete", + "componentID": 141609, + "name": "Haplic acrisols", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": 6, + "score_data": 0.329, + "score_data_loc": 0.51, + "score_loc": 0.047 + }, + { + "component": "Cambic arenosols", + "componentData": "Data Complete", + "componentID": 143286, + "name": "Cambic arenosols", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": 11, + "score_data": 0.267, + "score_data_loc": 0.401, + "score_loc": 0.029 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json new file mode 100644 index 0000000..c7b06c1 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json @@ -0,0 +1,1315 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.8, + "sl5": 13.43, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 20.0, + "sl5": 20.43, + "sl6": 20.4, + "sl7": 20.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.4, + "sl5": 1.71, + "sl6": 1.8, + "sl7": 1.83 + }, + "id": { + "component": "Haplic calcisols", + "name": "Haplic calcisols", + "rank_loc": "1", + "score_loc": 0.094 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.28, + "sl5": 8.31, + "sl6": 8.34, + "sl7": 8.35 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 14.2, + "sl5": 15.29, + "sl6": 16.6, + "sl7": 17.33 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 46.8, + "sl5": 46.14, + "sl6": 46.0, + "sl7": 46.5 + }, + "site": { + "siteData": { + "componentID": 132718, + "distance": 13619.43, + "mapunitID": 3520, + "minCompDistance": 13619.4298, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Description_es": "Los Calcisoles Háplicos se dan principalmente en climas semiáridos y áridos. Son suelos calcáreos, con alta saturación de bases, pH y fijación de P.
Muchos tienen horizontes superficiales de grava. ", + "Description_fr": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Description_ks": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Management_en": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", + "Management_es": "Estos suelos tienen un bajo contenido en materia orgánica, son secos y a menudo pedregosos.
Son calcáreos, y tendrán una alta saturación de bases (Ca, Mg y K) y un alto pH del suelo.
Si se utilizan, los suelos son más adecuados para el pastoreo o para un uso limitado con cultivos tolerantes a la sequía.
En el mejor de los casos, podrían cultivarse cada dos o tres años, con barbecho en los años en que no se utilicen los suelos para cultivos.
Si se riega, hay que tener cuidado para que los suelos no se vuelvan altos en sales (salinos). Para evitar la salinización sería necesario un agua de riego de alta calidad y bajo contenido en sales.", + "Management_fr": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", + "Management_ks": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols", + "rank_loc": "2", + "score_loc": 0.059 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 + }, + "site": { + "siteData": { + "componentID": 132966, + "distance": 41734.66, + "mapunitID": 3534, + "minCompDistance": 41734.66, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 12.5 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 18.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 2.0 + }, + "id": { + "component": "Eutric leptosols", + "name": "Eutric leptosols", + "rank_loc": "3", + "score_loc": 0.059 + }, + "ph": { + "sl1": 7.7, + "sl2": 7.7, + "sl3": 7.7, + "sl4": 7.65 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.5 + }, + "sand": { + "sl1": 61.0, + "sl2": 61.0, + "sl3": 61.0, + "sl4": 57.0 + }, + "site": { + "siteData": { + "componentID": 128778, + "distance": 84403.702, + "mapunitID": 32116, + "minCompDistance": 84403.7016, + "share": 100, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.14, + "sl6": 16.0, + "sl7": 15.83 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.0, + "sl5": 20.0, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Calcaric fluvisols", + "name": "Calcaric fluvisols", + "rank_loc": "4", + "score_loc": 0.059 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.2, + "sl5": 8.2, + "sl6": 8.2, + "sl7": 8.2 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.2, + "sl5": 5.0, + "sl6": 5.2, + "sl7": 5.33 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.6, + "sl5": 39.86, + "sl6": 39.8, + "sl7": 39.67 + }, + "site": { + "siteData": { + "componentID": 128775, + "distance": 84618.477, + "mapunitID": 32113, + "minCompDistance": 84618.4775, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.4, + "sl5": 4.29, + "sl6": 4.2, + "sl7": 4.17 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.71, + "sl6": 7.0, + "sl7": 7.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcaric arenosols", + "name": "Calcaric arenosols", + "rank_loc": "5", + "score_loc": 0.059 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.2, + "sl5": 8.26, + "sl6": 8.3, + "sl7": 8.33 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 17.6, + "sl5": 19.0, + "sl6": 20.2, + "sl7": 19.83 + }, + "sand": { + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 87.6, + "sl5": 87.71, + "sl6": 87.6, + "sl7": 87.33 + }, + "site": { + "siteData": { + "componentID": 128772, + "distance": 92104.211, + "mapunitID": 32109, + "minCompDistance": 92104.2105, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", + "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 + }, + "clay": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols", + "rank_loc": "6", + "score_loc": 0.047 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 + }, + "site": { + "siteData": { + "componentID": 132626, + "distance": 3698.05, + "mapunitID": 3515, + "minCompDistance": 3698.0496, + "share": 50, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.0, + "sl5": 16.86, + "sl6": 16.8, + "sl7": 16.17 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.4, + "sl5": 24.29, + "sl6": 24.0, + "sl7": 23.17 + }, + "ec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 + }, + "id": { + "component": "Haplic solonchaks", + "name": "Haplic solonchaks", + "rank_loc": "7", + "score_loc": 0.047 + }, + "ph": { + "sl1": 8.1, + "sl2": 8.1, + "sl3": 8.1, + "sl4": 8.16, + "sl5": 8.17, + "sl6": 8.2, + "sl7": 8.23 + }, + "rock_fragments": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 16.4, + "sl5": 16.57, + "sl6": 14.0, + "sl7": 14.0 + }, + "sand": { + "sl1": 50.0, + "sl2": 50.0, + "sl3": 50.0, + "sl4": 50.0, + "sl5": 49.86, + "sl6": 50.2, + "sl7": 51.5 + }, + "site": { + "siteData": { + "componentID": 134183, + "distance": 64694.956, + "mapunitID": 3622, + "minCompDistance": 64694.9563, + "share": 60, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_es": "Los Solonchaks Háplicos son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", + "Description_fr": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_ks": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.2, + "sl5": 13.43, + "sl6": 13.8, + "sl7": 14.0 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.6, + "sl5": 16.71, + "sl6": 17.0, + "sl7": 17.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Regosols", + "name": "Regosols", + "rank_loc": "8", + "score_loc": 0.03 + }, + "ph": { + "sl1": 7.8, + "sl2": 7.8, + "sl3": 7.8, + "sl4": 7.86, + "sl5": 7.93, + "sl6": 7.98, + "sl7": 8.02 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.6, + "sl5": 16.57, + "sl6": 17.0, + "sl7": 17.17 + }, + "sand": { + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 56.2, + "sl5": 55.57, + "sl6": 54.4, + "sl7": 53.5 + }, + "site": { + "siteData": { + "componentID": 132625, + "distance": 3698.05, + "mapunitID": 3515, + "minCompDistance": 3698.0496, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Description_es": "Los Regosoles son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad. ", + "Description_fr": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Description_ks": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 13.8, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 13.83 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.6, + "sl5": 20.14, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic luvisols", + "name": "Haplic luvisols", + "rank_loc": "9", + "score_loc": 0.029 + }, + "ph": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.14, + "sl5": 7.21, + "sl6": 7.34, + "sl7": 7.42 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.71, + "sl6": 17.8, + "sl7": 17.83 + }, + "sand": { + "sl1": 64.0, + "sl2": 64.0, + "sl3": 64.0, + "sl4": 61.2, + "sl5": 60.86, + "sl6": 60.8, + "sl7": 60.83 + }, + "site": { + "siteData": { + "componentID": 133773, + "distance": 16922.699, + "mapunitID": 3612, + "minCompDistance": 16922.6993, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.0, + "sl7": 4.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.8, + "sl5": 5.57, + "sl6": 5.4, + "sl7": 5.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Cambic arenosols", + "name": "Cambic arenosols", + "rank_loc": "10", + "score_loc": 0.029 + }, + "ph": { + "sl1": 6.9, + "sl2": 6.9, + "sl3": 6.9, + "sl4": 6.82, + "sl5": 6.8, + "sl6": 6.8, + "sl7": 6.82 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 14.4, + "sl5": 16.57, + "sl6": 21.2, + "sl7": 20.67 + }, + "sand": { + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 89.2, + "sl5": 89.29, + "sl6": 89.2, + "sl7": 89.17 + }, + "site": { + "siteData": { + "componentID": 133053, + "distance": 66261.442, + "mapunitID": 3539, + "minCompDistance": 66261.4422, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.0, + "sl5": 12.86, + "sl6": 12.6, + "sl7": 12.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 23.6, + "sl5": 23.71, + "sl6": 23.8, + "sl7": 23.67 + }, + "ec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 + }, + "id": { + "component": "Solonchaks", + "name": "Solonchaks", + "rank_loc": "11", + "score_loc": 0.023 + }, + "ph": { + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.36, + "sl5": 8.37, + "sl6": 8.38, + "sl7": 8.38 + }, + "rock_fragments": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.0, + "sl5": 21.14, + "sl6": 22.8, + "sl7": 23.33 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 47.6, + "sl5": 47.57, + "sl6": 47.6, + "sl7": 47.67 + }, + "site": { + "siteData": { + "componentID": 132965, + "distance": 41734.66, + "mapunitID": 3534, + "minCompDistance": 41734.66, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_es": "Los Solonchaks son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", + "Description_fr": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_ks": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "12", + "score_loc": 0.023 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 + }, + "sand": { + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 + }, + "site": { + "siteData": { + "componentID": 132963, + "distance": 41734.66, + "mapunitID": 3534, + "minCompDistance": 41734.66, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Haplic calcisols", + "componentData": "Data Complete", + "componentID": 132718, + "name": "Haplic calcisols", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.094 + }, + { + "component": "Calcaric fluvisols", + "componentData": "Data Complete", + "componentID": 128775, + "name": "Calcaric fluvisols", + "rank_data": "1", + "rank_data_loc": "2", + "rank_loc": 4, + "score_data": 1.0, + "score_data_loc": 0.968, + "score_loc": 0.059 + }, + { + "component": "Solonchaks", + "componentData": "Data Complete", + "componentID": 132965, + "name": "Solonchaks", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": 11, + "score_data": 1.0, + "score_data_loc": 0.936, + "score_loc": 0.023 + }, + { + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 132966, + "name": "Calcaric regosols", + "rank_data": "4", + "rank_data_loc": "4", + "rank_loc": 2, + "score_data": 0.624, + "score_data_loc": 0.624, + "score_loc": 0.059 + }, + { + "component": "Regosols", + "componentData": "Data Complete", + "componentID": 132625, + "name": "Regosols", + "rank_data": "9", + "rank_data_loc": "5", + "rank_loc": 8, + "score_data": 0.624, + "score_data_loc": 0.598, + "score_loc": 0.03 + }, + { + "component": "Haplic luvisols", + "componentData": "Data Complete", + "componentID": 133773, + "name": "Haplic luvisols", + "rank_data": "7", + "rank_data_loc": "6", + "rank_loc": 9, + "score_data": 0.624, + "score_data_loc": 0.597, + "score_loc": 0.029 + }, + { + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 132963, + "name": "Chromic luvisols", + "rank_data": "5", + "rank_data_loc": "7", + "rank_loc": 12, + "score_data": 0.624, + "score_data_loc": 0.592, + "score_loc": 0.023 + }, + { + "component": "Haplic solonchaks", + "componentData": "Data Complete", + "componentID": 134183, + "name": "Haplic solonchaks", + "rank_data": "10", + "rank_data_loc": "8", + "rank_loc": 7, + "score_data": 0.537, + "score_data_loc": 0.534, + "score_loc": 0.047 + }, + { + "component": "Calcaric arenosols", + "componentData": "Data Complete", + "componentID": 128772, + "name": "Calcaric arenosols", + "rank_data": "11", + "rank_data_loc": "9", + "rank_loc": 5, + "score_data": 0.399, + "score_data_loc": 0.418, + "score_loc": 0.059 + }, + { + "component": "Cambic arenosols", + "componentData": "Data Complete", + "componentID": 133053, + "name": "Cambic arenosols", + "rank_data": "12", + "rank_data_loc": "10", + "rank_loc": 10, + "score_data": 0.233, + "score_data_loc": 0.24, + "score_loc": 0.029 + }, + { + "component": "Eutric leptosols", + "componentData": "Missing Data", + "componentID": 128778, + "name": "Eutric leptosols", + "rank_data": "6", + "rank_data_loc": "11", + "rank_loc": 3, + "score_data": 0.624, + "score_data_loc": 0.002, + "score_loc": 0.059 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 132626, + "name": "Lithic leptosols", + "rank_data": "8", + "rank_data_loc": "12", + "rank_loc": 6, + "score_data": 0.624, + "score_data_loc": 0.002, + "score_loc": 0.047 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json new file mode 100644 index 0000000..345001a --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json @@ -0,0 +1,1195 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.14, + "sl6": 16.0, + "sl7": 15.83 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.0, + "sl5": 20.0, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Calcaric fluvisols", + "name": "Calcaric fluvisols", + "rank_loc": "1", + "score_loc": 0.172 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.2, + "sl5": 8.2, + "sl6": 8.2, + "sl7": 8.2 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.2, + "sl5": 5.0, + "sl6": 5.2, + "sl7": 5.33 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.6, + "sl5": 39.86, + "sl6": 39.8, + "sl7": 39.67 + }, + "site": { + "siteData": { + "componentID": 101342, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.2, + "sl5": 12.43, + "sl6": 13.0, + "sl7": 13.33 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 22.8, + "sl5": 23.29, + "sl6": 23.4, + "sl7": 23.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Chromic cambisols", + "name": "Chromic cambisols", + "rank_loc": "2", + "score_loc": 0.114 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.9, + "sl5": 6.96, + "sl6": 7.06, + "sl7": 7.13 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 8.6, + "sl5": 10.14, + "sl6": 10.8, + "sl7": 12.17 + }, + "sand": { + "sl1": 61.0, + "sl2": 61.0, + "sl3": 61.0, + "sl4": 58.6, + "sl5": 58.43, + "sl6": 58.2, + "sl7": 58.5 + }, + "site": { + "siteData": { + "componentID": 101344, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.8, + "sl5": 13.43, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 20.0, + "sl5": 20.43, + "sl6": 20.4, + "sl7": 20.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.4, + "sl5": 1.71, + "sl6": 1.8, + "sl7": 1.83 + }, + "id": { + "component": "Haplic calcisols", + "name": "Haplic calcisols", + "rank_loc": "3", + "score_loc": 0.114 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.28, + "sl5": 8.31, + "sl6": 8.34, + "sl7": 8.35 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 14.2, + "sl5": 15.29, + "sl6": 16.6, + "sl7": 17.33 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 46.8, + "sl5": 46.14, + "sl6": 46.0, + "sl7": 46.5 + }, + "site": { + "siteData": { + "componentID": 101345, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Description_es": "Los Calcisoles Háplicos se dan principalmente en climas semiáridos y áridos. Son suelos calcáreos, con alta saturación de bases, pH y fijación de P.
Muchos tienen horizontes superficiales de grava. ", + "Description_fr": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Description_ks": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Management_en": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", + "Management_es": "Estos suelos tienen un bajo contenido en materia orgánica, son secos y a menudo pedregosos.
Son calcáreos, y tendrán una alta saturación de bases (Ca, Mg y K) y un alto pH del suelo.
Si se utilizan, los suelos son más adecuados para el pastoreo o para un uso limitado con cultivos tolerantes a la sequía.
En el mejor de los casos, podrían cultivarse cada dos o tres años, con barbecho en los años en que no se utilicen los suelos para cultivos.
Si se riega, hay que tener cuidado para que los suelos no se vuelvan altos en sales (salinos). Para evitar la salinización sería necesario un agua de riego de alta calidad y bajo contenido en sales.", + "Management_fr": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", + "Management_ks": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.0, + "sl5": 12.86, + "sl6": 12.6, + "sl7": 12.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 23.6, + "sl5": 23.71, + "sl6": 23.8, + "sl7": 23.67 + }, + "ec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 + }, + "id": { + "component": "Solonchaks", + "name": "Solonchaks", + "rank_loc": "4", + "score_loc": 0.114 + }, + "ph": { + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.36, + "sl5": 8.37, + "sl6": 8.38, + "sl7": 8.38 + }, + "rock_fragments": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.0, + "sl5": 21.14, + "sl6": 22.8, + "sl7": 23.33 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 47.6, + "sl5": 47.57, + "sl6": 47.6, + "sl7": 47.67 + }, + "site": { + "siteData": { + "componentID": 101343, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_es": "Los Solonchaks son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", + "Description_fr": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_ks": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 + }, + "clay": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "5", + "score_loc": 0.049 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 + }, + "site": { + "siteData": { + "componentID": 101347, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 5, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Vertic cambisols", + "name": "Vertic cambisols", + "rank_loc": "6", + "score_loc": 0.047 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 150228, + "distance": 72409.687, + "mapunitID": 67, + "minCompDistance": 72409.6869, + "share": 33, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Vertic Cambisols are widely occurring soils with limited soil development.
These soils are clayey soils that are sticky and plastic when wet, with poor soil physical properties. ", + "Description_es": "Los Cambisoles Vérticos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son arcillosos, pegajosos y plásticos cuando están mojados, y tienen malas propiedades físicas. ", + "Description_fr": "Vertic Cambisols are widely occurring soils with limited soil development.
These soils are clayey soils that are sticky and plastic when wet, with poor soil physical properties. ", + "Description_ks": "Vertic Cambisols are widely occurring soils with limited soil development.
These soils are clayey soils that are sticky and plastic when wet, with poor soil physical properties. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil will expand when wetted and shrink when dry.
Although fertile, care should be taken to not excessively till these soils, as soil structure could be negatively affected. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
El tipo de arcilla de este suelo se expande cuando se humedece y se encoge cuando se seca.
Aunque son fértiles, hay que tener cuidado de no labrar excesivamente estos suelos, ya que su estructura podría verse afectada negativamente.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil will expand when wetted and shrink when dry.
Although fertile, care should be taken to not excessively till these soils, as soil structure could be negatively affected. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil will expand when wetted and shrink when dry.
Although fertile, care should be taken to not excessively till these soils, as soil structure could be negatively affected. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 30.2, + "sl5": 29.71, + "sl6": 29.2, + "sl7": 28.83 + }, + "clay": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 48.6, + "sl5": 48.57, + "sl6": 48.0, + "sl7": 46.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "7", + "score_loc": 0.047 + }, + "ph": { + "sl1": 7.3, + "sl2": 7.3, + "sl3": 7.3, + "sl4": 7.38, + "sl5": 7.43, + "sl6": 7.54, + "sl7": 7.57 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 3.86, + "sl6": 3.8, + "sl7": 4.17 + }, + "sand": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 15.8, + "sl5": 15.43, + "sl6": 15.4, + "sl7": 15.83 + }, + "site": { + "siteData": { + "componentID": 150227, + "distance": 72409.687, + "mapunitID": 67, + "minCompDistance": 72409.6869, + "share": 33, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.2, + "sl5": 18.43, + "sl6": 18.4, + "sl7": 17.83 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 34.2, + "sl5": 35.86, + "sl6": 37.2, + "sl7": 37.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols", + "rank_loc": "8", + "score_loc": 0.029 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.56, + "sl5": 6.57, + "sl6": 6.58, + "sl7": 6.55 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.6, + "sl5": 10.14, + "sl6": 9.8, + "sl7": 11.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.43, + "sl6": 32.6, + "sl7": 33.0 + }, + "site": { + "siteData": { + "componentID": 101346, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 5, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Gypsisols", + "name": "Gypsisols", + "rank_loc": "9", + "score_loc": 0.014 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 + }, + "site": { + "siteData": { + "componentID": 135084, + "distance": 35571.412, + "mapunitID": 374, + "minCompDistance": 35571.4122, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": NaN, + "Description_es": NaN, + "Description_fr": NaN, + "Description_ks": NaN, + "Management_en": NaN, + "Management_es": NaN, + "Management_fr": NaN, + "Management_ks": NaN + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.8, + "sl5": 8.43, + "sl6": 8.0, + "sl7": 7.83 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 18.2, + "sl5": 18.29, + "sl6": 18.0, + "sl7": 17.67 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.71, + "sl6": 2.8, + "sl7": 3.0 + }, + "id": { + "component": "Haplic solonchaks", + "name": "Haplic solonchaks", + "rank_loc": "10", + "score_loc": 0.014 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.06, + "sl5": 8.07, + "sl6": 8.08, + "sl7": 8.07 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.4, + "sl5": 3.86, + "sl6": 7.2, + "sl7": 9.5 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 45.8, + "sl5": 45.86, + "sl6": 46.0, + "sl7": 46.33 + }, + "site": { + "siteData": { + "componentID": 135083, + "distance": 35571.412, + "mapunitID": 374, + "minCompDistance": 35571.4122, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_es": "Los Solonchaks Háplicos son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", + "Description_fr": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_ks": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.0, + "sl5": 16.86, + "sl6": 16.8, + "sl7": 16.17 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.4, + "sl5": 24.29, + "sl6": 24.0, + "sl7": 23.17 + }, + "ec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.049 + }, + "ph": { + "sl1": 8.1, + "sl2": 8.1, + "sl3": 8.1, + "sl4": 8.16, + "sl5": 8.17, + "sl6": 8.2, + "sl7": 8.23 + }, + "rock_fragments": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 16.4, + "sl5": 16.57, + "sl6": 14.0, + "sl7": 14.0 + }, + "sand": { + "sl1": 50.0, + "sl2": 50.0, + "sl3": 50.0, + "sl4": 50.0, + "sl5": 49.86, + "sl6": 50.2, + "sl7": 51.5 + }, + "site": { + "siteData": { + "componentID": 150226, + "distance": 72409.687, + "mapunitID": 67, + "minCompDistance": 0.0, + "share": 34, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Gypsisols", + "componentData": "Data Complete", + "componentID": 135084, + "name": "Gypsisols", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "9", + "score_data": 0.59, + "score_data_loc": 1.0, + "score_loc": 0.014 + }, + { + "component": "Solonchaks", + "componentData": "Data Complete", + "componentID": 101343, + "name": "Solonchaks", + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": "4", + "score_data": 0.484, + "score_data_loc": 0.991, + "score_loc": 0.114 + }, + { + "component": "Chromic cambisols", + "componentData": "Data Complete", + "componentID": 101344, + "name": "Chromic cambisols", + "rank_data": "6", + "rank_data_loc": "3", + "rank_loc": "2", + "score_data": 0.334, + "score_data_loc": 0.742, + "score_loc": 0.114 + }, + { + "component": "Calcaric fluvisols", + "componentData": "Data Complete", + "componentID": 101342, + "name": "Calcaric fluvisols", + "rank_data": "9", + "rank_data_loc": "4", + "rank_loc": "1", + "score_data": 0.263, + "score_data_loc": 0.72, + "score_loc": 0.172 + }, + { + "component": "Haplic calcisols", + "componentData": "Data Complete", + "componentID": 101345, + "name": "Haplic calcisols", + "rank_data": "8", + "rank_data_loc": "5", + "rank_loc": "3", + "score_data": 0.302, + "score_data_loc": 0.69, + "score_loc": 0.114 + }, + { + "component": "Vertic cambisols", + "componentData": "Missing Data", + "componentID": 150228, + "name": "Vertic cambisols", + "rank_data": "4", + "rank_data_loc": "6", + "rank_loc": "6", + "score_data": 0.356, + "score_data_loc": 0.668, + "score_loc": 0.047 + }, + { + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 101346, + "name": "Calcaric regosols", + "rank_data": "5", + "rank_data_loc": "7", + "rank_loc": "8", + "score_data": 0.348, + "score_data_loc": 0.624, + "score_loc": 0.029 + }, + { + "component": "Haplic solonchaks", + "componentData": "Data Complete", + "componentID": 135083, + "name": "Haplic solonchaks", + "rank_data": "7", + "rank_data_loc": "8", + "rank_loc": "10", + "score_data": 0.333, + "score_data_loc": 0.574, + "score_loc": 0.014 + }, + { + "component": "Chromic luvisols", + "componentData": "Missing Data", + "componentID": 150227, + "name": "Chromic luvisols", + "rank_data": "10", + "rank_data_loc": "9", + "rank_loc": "7", + "score_data": 0.242, + "score_data_loc": 0.479, + "score_loc": 0.047 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 101347, + "name": "Lithic leptosols1", + "rank_data": "3", + "rank_data_loc": "10", + "rank_loc": "5", + "score_data": 0.377, + "score_data_loc": 0.003, + "score_loc": 0.049 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 150226, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.354, + "score_data_loc": 0.003, + "score_loc": 0.049 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json new file mode 100644 index 0000000..30300a2 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json @@ -0,0 +1,2267 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols1", + "rank_loc": "1", + "score_loc": 0.007 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 128966, + "distance": 3776.17, + "mapunitID": 33042, + "minCompDistance": 3776.1698, + "share": 90, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols1", + "rank_loc": "2", + "score_loc": 0.007 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 128969, + "distance": 924.428, + "mapunitID": 33043, + "minCompDistance": 924.4281, + "share": 45, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "3", + "score_loc": 0.006 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 128898, + "distance": 43357.696, + "mapunitID": 33002, + "minCompDistance": 43357.6959, + "share": 79, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Histosols", + "name": "Histosols", + "rank_loc": "4", + "score_loc": 0.004 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 133064, + "distance": 9275.857, + "mapunitID": 35395, + "minCompDistance": 9275.8574, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage, but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges. ", + "Description_es": "Los Histosoles son suelos orgánicos que suelen formarse en ambientes húmedos.
Sus propiedades dependen en gran medida del tipo y el grado de descomposición de los materiales orgánicos del suelo.
Los suelos pueden ser productivos con una gestión intensiva que incluya el drenaje del suelo, pero su naturaleza frágil y su hábitat sugieren que se garantice la preservación de estos suelos cuando sea posible.
Cuando se cultivan, el hundimiento y la oxidación de los sulfuros plantean problemas de gestión. ", + "Description_fr": "Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage, but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges. ", + "Description_ks": "Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage, but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges. ", + "Management_en": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regular liming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority.
Maintenance of native vegetation is the best use. ", + "Management_es": "Estos suelos pueden ser algunos de los más productivos, especialmente para cultivos especiales como las hortalizas.
Sin embargo, deben ser drenados para su uso, y esto conducirá al hundimiento del suelo, ya que la turba expuesta se mineraliza rápidamente, y el contenido de materia orgánica disminuye rápidamente.
Esto hará que los suelos sean cada vez más ácidos, por lo que será necesario un encalado regular.
Estos suelos orgánicos deben gestionarse de forma diferente a los suelos minerales, y las técnicas que minimizan la degradación de la materia orgánica son una prioridad.
El mantenimiento de la vegetación autóctona es el mejor uso.", + "Management_fr": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regular liming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority.
Maintenance of native vegetation is the best use. ", + "Management_ks": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regular liming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority.
Maintenance of native vegetation is the best use. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.2, + "sl7": 16.33 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 30.2, + "sl5": 30.14, + "sl6": 29.8, + "sl7": 30.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.6, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.5 + }, + "id": { + "component": "Rendzic leptosols", + "name": "Rendzic leptosols", + "rank_loc": "5", + "score_loc": 0.003 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.06, + "sl5": 8.09, + "sl6": 8.1, + "sl7": 8.1 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 6.57, + "sl6": 8.8, + "sl7": 10.17 + }, + "sand": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 29.6, + "sl5": 29.29, + "sl6": 29.2, + "sl7": 28.67 + }, + "site": { + "siteData": { + "componentID": 129097, + "distance": 47480.618, + "mapunitID": 33127, + "minCompDistance": 47480.6175, + "share": 82, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Description_es": "Los Leptosoles Rendzicos tienen un volumen de enraizamiento muy limitado debido a la roca continua, material altamente calcáreo, horizontes cementados, o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles Rendzic son altamente calcáreos en la superficie del suelo. ", + "Description_fr": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Description_ks": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo será alto (> 7,0) en estos suelos, y no será necesario el encalado.
Cualquier uso agrícola debe ser para el pastoreo o la agrosilvicultura, con el mantenimiento continuo de la cubierta.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Calcaric arenosols", + "name": "Calcaric arenosols1", + "rank_loc": "6", + "score_loc": 0.003 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 + }, + "site": { + "siteData": { + "componentID": 130338, + "distance": 94026.373, + "mapunitID": 33860, + "minCompDistance": 94026.3732, + "share": 65, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", + "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Calcic luvisols", + "name": "Calcic luvisols", + "rank_loc": "7", + "score_loc": 0.003 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 + }, + "site": { + "siteData": { + "componentID": 129392, + "distance": 87650.254, + "mapunitID": 33303, + "minCompDistance": 87650.2544, + "share": 77, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Calcaric fluvisols", + "name": "Calcaric fluvisols", + "rank_loc": "8", + "score_loc": 0.002 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 + }, + "site": { + "siteData": { + "componentID": 129425, + "distance": 51610.989, + "mapunitID": 33320, + "minCompDistance": 51610.9891, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Regosols", + "name": "Regosols", + "rank_loc": "9", + "score_loc": 0.001 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 + }, + "site": { + "siteData": { + "componentID": 132579, + "distance": 93564.378, + "mapunitID": 3512, + "minCompDistance": 93564.3781, + "share": 33, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Description_es": "Los Regosoles son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad. ", + "Description_fr": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Description_ks": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.43, + "sl6": 16.6, + "sl7": 16.17 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.6, + "sl5": 25.0, + "sl6": 25.4, + "sl7": 25.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.5 + }, + "id": { + "component": "Umbric leptosols", + "name": "Umbric leptosols", + "rank_loc": "10", + "score_loc": 0.001 + }, + "ph": { + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 7.98, + "sl5": 8.01, + "sl6": 8.06, + "sl7": 8.03 + }, + "rock_fragments": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 13.4, + "sl5": 12.86, + "sl6": 12.4, + "sl7": 12.5 + }, + "sand": { + "sl1": 44.0, + "sl2": 44.0, + "sl3": 44.0, + "sl4": 42.8, + "sl5": 42.14, + "sl6": 41.2, + "sl7": 41.0 + }, + "site": { + "siteData": { + "componentID": 132400, + "distance": 84530.897, + "mapunitID": 3503, + "minCompDistance": 84530.8969, + "share": 25, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", + "Description_es": "Los Leptosoles Úmbricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles umbrosos tienen un horizonte superficial grueso con un alto contenido de materia orgánica y una baja saturación de la base que se superpone a una capa que limita las raíces. ", + "Description_fr": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", + "Description_ks": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo del horizonte superficial será bajo (< 5,0) y se necesitará encalado para el uso de pastoreo o agroforestal.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cubierta.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 + }, + "clay": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Cambisols", + "name": "Cambisols", + "rank_loc": "11", + "score_loc": 0.001 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 + }, + "site": { + "siteData": { + "componentID": 132402, + "distance": 84530.897, + "mapunitID": 3503, + "minCompDistance": 84530.8969, + "share": 25, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los cambisoles tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 128926, + "distance": 8501.441, + "mapunitID": 33019, + "minCompDistance": 3776.1698, + "share": 21, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 87.6, + "sl5": 85.14, + "sl6": 80.0, + "sl7": 75.67 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 27.2, + "sl5": 25.86, + "sl6": 23.8, + "sl7": 22.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.06, + "sl5": 5.09, + "sl6": 5.14, + "sl7": 5.18 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.2, + "sl5": 13.86, + "sl6": 15.0, + "sl7": 15.5 + }, + "sand": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 32.2, + "sl5": 33.86, + "sl6": 37.6, + "sl7": 40.83 + }, + "site": { + "siteData": { + "componentID": 128904, + "distance": 73527.269, + "mapunitID": 33007, + "minCompDistance": 3776.1698, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 14.5 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 23.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 2.0 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols4", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.05 + }, + "rock_fragments": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 38.0 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 46.5 + }, + "site": { + "siteData": { + "componentID": 128910, + "distance": 73924.187, + "mapunitID": 33010, + "minCompDistance": 3776.1698, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.4, + "sl5": 4.29, + "sl6": 4.2, + "sl7": 4.17 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.71, + "sl6": 7.0, + "sl7": 7.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols5", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.2, + "sl5": 8.26, + "sl6": 8.3, + "sl7": 8.33 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 17.6, + "sl5": 19.0, + "sl6": 20.2, + "sl7": 19.83 + }, + "sand": { + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 87.6, + "sl5": 87.71, + "sl6": 87.6, + "sl7": 87.33 + }, + "site": { + "siteData": { + "componentID": 129504, + "distance": 89326.37, + "mapunitID": 33378, + "minCompDistance": 3776.1698, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.4, + "sl5": 4.29, + "sl6": 4.2, + "sl7": 4.17 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.71, + "sl6": 7.0, + "sl7": 7.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.2, + "sl5": 8.26, + "sl6": 8.3, + "sl7": 8.33 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 17.6, + "sl5": 19.0, + "sl6": 20.2, + "sl7": 19.83 + }, + "sand": { + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 87.6, + "sl5": 87.71, + "sl6": 87.6, + "sl7": 87.33 + }, + "site": { + "siteData": { + "componentID": 128933, + "distance": 29725.364, + "mapunitID": 33021, + "minCompDistance": 924.4281, + "share": 39, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 14.0 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.2, + "sl5": 20.86, + "sl6": 21.2, + "sl7": 21.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols3", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.72, + "sl5": 7.81, + "sl6": 7.92, + "sl7": 8.0 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.8, + "sl5": 27.86, + "sl6": 29.8, + "sl7": 30.17 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 62.4, + "sl5": 62.0, + "sl6": 62.0, + "sl7": 61.83 + }, + "site": { + "siteData": { + "componentID": 128899, + "distance": 43357.696, + "mapunitID": 33002, + "minCompDistance": 924.4281, + "share": 21, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.14, + "sl6": 16.0, + "sl7": 15.83 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.0, + "sl5": 20.0, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols4", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.2, + "sl5": 8.2, + "sl6": 8.2, + "sl7": 8.2 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.2, + "sl5": 5.0, + "sl6": 5.2, + "sl7": 5.33 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.6, + "sl5": 39.86, + "sl6": 39.8, + "sl7": 39.67 + }, + "site": { + "siteData": { + "componentID": 129080, + "distance": 68431.355, + "mapunitID": 33111, + "minCompDistance": 924.4281, + "share": 90, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.2, + "sl5": 13.43, + "sl6": 13.8, + "sl7": 14.0 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.6, + "sl5": 16.71, + "sl6": 17.0, + "sl7": 17.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols5", + "rank_loc": "Not Displayed", + "score_loc": 0.007 + }, + "ph": { + "sl1": 7.8, + "sl2": 7.8, + "sl3": 7.8, + "sl4": 7.86, + "sl5": 7.93, + "sl6": 7.98, + "sl7": 8.02 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.6, + "sl5": 16.57, + "sl6": 17.0, + "sl7": 17.17 + }, + "sand": { + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 56.2, + "sl5": 55.57, + "sl6": 54.4, + "sl7": 53.5 + }, + "site": { + "siteData": { + "componentID": 129500, + "distance": 77496.323, + "mapunitID": 33373, + "minCompDistance": 924.4281, + "share": 28, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 15.5 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.5 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.006 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.05 + }, + "rock_fragments": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.5 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 53.0 + }, + "site": { + "siteData": { + "componentID": 129499, + "distance": 77496.323, + "mapunitID": 33373, + "minCompDistance": 43357.6959, + "share": 72, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.6, + "sl5": 15.71, + "sl6": 15.6, + "sl7": 15.5 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 22.4, + "sl5": 22.71, + "sl6": 22.6, + "sl7": 22.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Calcaric arenosols", + "name": "Calcaric arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.003 + }, + "ph": { + "sl1": 7.6, + "sl2": 7.6, + "sl3": 7.6, + "sl4": 7.86, + "sl5": 7.94, + "sl6": 8.02, + "sl7": 8.03 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.4, + "sl5": 10.86, + "sl6": 12.6, + "sl7": 13.0 + }, + "sand": { + "sl1": 48.0, + "sl2": 48.0, + "sl3": 48.0, + "sl4": 46.4, + "sl5": 45.86, + "sl6": 46.0, + "sl7": 46.17 + }, + "site": { + "siteData": { + "componentID": 130333, + "distance": 98648.774, + "mapunitID": 33858, + "minCompDistance": 94026.3732, + "share": 90, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", + "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 128966, + "name": "Calcaric cambisols1", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": "1", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.007 + }, + { + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 128969, + "name": "Calcaric regosols1", + "rank_data": "3", + "rank_data_loc": "2", + "rank_loc": "2", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.007 + }, + { + "component": "Histosols", + "componentData": "Data Complete", + "componentID": 133064, + "name": "Histosols", + "rank_data": "4", + "rank_data_loc": "3", + "rank_loc": "4", + "score_data": 1.0, + "score_data_loc": 0.996, + "score_loc": 0.004 + }, + { + "component": "Calcaric arenosols", + "componentData": "Data Complete", + "componentID": 130333, + "name": "Calcaric arenosols2", + "rank_data": "1", + "rank_data_loc": "4", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 0.996, + "score_loc": 0.003 + }, + { + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 129392, + "name": "Calcic luvisols", + "rank_data": "9", + "rank_data_loc": "5", + "rank_loc": "7", + "score_data": 0.613, + "score_data_loc": 0.611, + "score_loc": 0.003 + }, + { + "component": "Calcaric fluvisols", + "componentData": "Data Complete", + "componentID": 129425, + "name": "Calcaric fluvisols", + "rank_data": "8", + "rank_data_loc": "6", + "rank_loc": "8", + "score_data": 0.613, + "score_data_loc": 0.611, + "score_loc": 0.002 + }, + { + "component": "Regosols", + "componentData": "Data Complete", + "componentID": 132579, + "name": "Regosols", + "rank_data": "11", + "rank_data_loc": "7", + "rank_loc": "9", + "score_data": 0.613, + "score_data_loc": 0.609, + "score_loc": 0.001 + }, + { + "component": "Cambisols", + "componentData": "Data Complete", + "componentID": 132402, + "name": "Cambisols", + "rank_data": "10", + "rank_data_loc": "8", + "rank_loc": "11", + "score_data": 0.613, + "score_data_loc": 0.609, + "score_loc": 0.001 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 128898, + "name": "Lithic leptosols1", + "rank_data": "5", + "rank_data_loc": "9", + "rank_loc": "3", + "score_data": 1.0, + "score_data_loc": 0.002, + "score_loc": 0.006 + }, + { + "component": "Rendzic leptosols", + "componentData": "Missing Data", + "componentID": 129097, + "name": "Rendzic leptosols", + "rank_data": "7", + "rank_data_loc": "10", + "rank_loc": "5", + "score_data": 0.63, + "score_data_loc": 0.002, + "score_loc": 0.003 + }, + { + "component": "Umbric leptosols", + "componentData": "Missing Data", + "componentID": 132400, + "name": "Umbric leptosols", + "rank_data": "6", + "rank_data_loc": "11", + "rank_loc": "10", + "score_data": 1.0, + "score_data_loc": 0.002, + "score_loc": 0.001 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 128926, + "name": "Calcaric cambisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.007 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 128910, + "name": "Calcaric cambisols4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.007 + }, + { + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 129080, + "name": "Calcaric regosols4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.007 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 128904, + "name": "Calcaric cambisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.63, + "score_data_loc": 0.633, + "score_loc": 0.007 + }, + { + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 128899, + "name": "Calcaric regosols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.613, + "score_data_loc": 0.615, + "score_loc": 0.007 + }, + { + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 129500, + "name": "Calcaric regosols5", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.613, + "score_data_loc": 0.615, + "score_loc": 0.007 + }, + { + "component": "Calcaric arenosols", + "componentData": "Data Complete", + "componentID": 130338, + "name": "Calcaric arenosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "6", + "score_data": 0.613, + "score_data_loc": 0.612, + "score_loc": 0.003 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 129504, + "name": "Calcaric cambisols5", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.37, + "score_data_loc": 0.374, + "score_loc": 0.007 + }, + { + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 128933, + "name": "Calcaric regosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.37, + "score_data_loc": 0.374, + "score_loc": 0.007 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 129499, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 0.002, + "score_loc": 0.006 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json new file mode 100644 index 0000000..b526170 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json @@ -0,0 +1,1867 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 41.0, + "sl5": 41.0, + "sl6": 41.0, + "sl7": 40.5 + }, + "clay": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 56.8, + "sl5": 57.14, + "sl6": 57.0, + "sl7": 56.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Eutric vertisols", + "name": "Eutric vertisols", + "rank_loc": "1", + "score_loc": 0.115 + }, + "ph": { + "sl1": 6.8, + "sl2": 6.8, + "sl3": 6.8, + "sl4": 7.02, + "sl5": 7.13, + "sl6": 7.26, + "sl7": 7.33 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.14, + "sl6": 4.2, + "sl7": 4.0 + }, + "sand": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 12.4, + "sl5": 12.29, + "sl6": 12.4, + "sl7": 12.5 + }, + "site": { + "siteData": { + "componentID": 157428, + "distance": 0.0, + "mapunitID": 9683, + "minCompDistance": 0.0, + "share": 80, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.2, + "sl7": 16.33 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 30.2, + "sl5": 30.14, + "sl6": 29.8, + "sl7": 30.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.6, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.5 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols1", + "rank_loc": "2", + "score_loc": 0.086 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.06, + "sl5": 8.09, + "sl6": 8.1, + "sl7": 8.1 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 6.57, + "sl6": 8.8, + "sl7": 10.17 + }, + "sand": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 29.6, + "sl5": 29.29, + "sl6": 29.2, + "sl7": 28.67 + }, + "site": { + "siteData": { + "componentID": 157401, + "distance": 21368.302, + "mapunitID": 9673, + "minCompDistance": 21368.3019, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Gleyic acrisols", + "name": "Gleyic acrisols", + "rank_loc": "3", + "score_loc": 0.033 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 157547, + "distance": 1849.359, + "mapunitID": 9723, + "minCompDistance": 1849.3591, + "share": 45, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", + "Description_es": "Los Acrisoles Gleyicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles gleyicos tienen un nivel freático alto estacional que provoca la saturación durante algunas épocas del año. ", + "Description_fr": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", + "Description_ks": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.
Los períodos de saturación limitan el crecimiento de las raíces y aumentan la pérdida de nitrógeno.
Para evitar la pérdida de N por lixiviación y/o desnitrificación, considere el uso de fertilizantes de liberación lenta de N (urea recubierta de azufre (SCU), por ejemplo), si esos productos de liberación lenta están disponibles, o utilice estiércol u otros residuos orgánicos por sus propiedades de liberación lenta.
Puede ser necesario el drenaje de estos suelos, pero esto puede ser problemático, ya que la humedad se debe al alto nivel freático. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.0, + "sl5": 7.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 21.4, + "sl5": 24.86, + "sl6": 28.2, + "sl7": 29.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcic luvisols", + "name": "Calcic luvisols", + "rank_loc": "4", + "score_loc": 0.029 + }, + "ph": { + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.1, + "sl5": 5.03, + "sl6": 4.96, + "sl7": 4.93 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 3.0, + "sl6": 4.0, + "sl7": 4.5 + }, + "sand": { + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 51.8, + "sl5": 49.57, + "sl6": 48.0, + "sl7": 47.83 + }, + "site": { + "siteData": { + "componentID": 157534, + "distance": 0.0, + "mapunitID": 9718, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 14.0 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.2, + "sl5": 20.86, + "sl6": 21.2, + "sl7": 21.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Eutric regosols", + "name": "Eutric regosols1", + "rank_loc": "5", + "score_loc": 0.029 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.72, + "sl5": 7.81, + "sl6": 7.92, + "sl7": 8.0 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.8, + "sl5": 27.86, + "sl6": 29.8, + "sl7": 30.17 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 62.4, + "sl5": 62.0, + "sl6": 62.0, + "sl7": 61.83 + }, + "site": { + "siteData": { + "componentID": 157429, + "distance": 0.0, + "mapunitID": 9683, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Description_es": "Regosoles Éutricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Eutricos tienen una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Description_ks": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.0, + "sl6": 12.0, + "sl7": 12.0 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 17.2, + "sl5": 17.29, + "sl6": 17.2, + "sl7": 17.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Calcaric fluvisols", + "name": "Calcaric fluvisols", + "rank_loc": "6", + "score_loc": 0.029 + }, + "ph": { + "sl1": 6.6, + "sl2": 6.6, + "sl3": 6.6, + "sl4": 6.7, + "sl5": 6.76, + "sl6": 6.8, + "sl7": 6.83 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.8, + "sl5": 21.0, + "sl6": 22.8, + "sl7": 22.17 + }, + "sand": { + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 55.6, + "sl5": 55.86, + "sl6": 56.2, + "sl7": 54.83 + }, + "site": { + "siteData": { + "componentID": 157400, + "distance": 21368.302, + "mapunitID": 9673, + "minCompDistance": 21368.3019, + "share": 80, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.0, + "sl6": 12.0, + "sl7": 12.0 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 17.2, + "sl5": 17.29, + "sl6": 17.2, + "sl7": 17.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols1", + "rank_loc": "7", + "score_loc": 0.029 + }, + "ph": { + "sl1": 6.6, + "sl2": 6.6, + "sl3": 6.6, + "sl4": 6.7, + "sl5": 6.76, + "sl6": 6.8, + "sl7": 6.83 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.8, + "sl5": 21.0, + "sl6": 22.8, + "sl7": 22.17 + }, + "sand": { + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 55.6, + "sl5": 55.86, + "sl6": 56.2, + "sl7": 54.83 + }, + "site": { + "siteData": { + "componentID": 157483, + "distance": 43336.529, + "mapunitID": 9700, + "minCompDistance": 43336.5293, + "share": 5, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.6, + "sl5": 13.57, + "sl6": 13.6, + "sl7": 14.0 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 21.2, + "sl5": 21.43, + "sl6": 21.8, + "sl7": 22.0 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.29, + "sl6": 2.4, + "sl7": 2.33 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "8", + "score_loc": 0.029 + }, + "ph": { + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 8.02, + "sl5": 8.04, + "sl6": 8.06, + "sl7": 8.05 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.4, + "sl5": 3.86, + "sl6": 5.0, + "sl7": 5.83 + }, + "sand": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 39.6, + "sl5": 39.71, + "sl6": 39.4, + "sl7": 38.67 + }, + "site": { + "siteData": { + "componentID": 157466, + "distance": 45664.921, + "mapunitID": 9696, + "minCompDistance": 45664.9211, + "share": 15, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.2, + "sl5": 18.43, + "sl6": 18.4, + "sl7": 17.83 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 34.2, + "sl5": 35.86, + "sl6": 37.2, + "sl7": 37.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Gleyic luvisols", + "name": "Gleyic luvisols", + "rank_loc": "9", + "score_loc": 0.025 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.56, + "sl5": 6.57, + "sl6": 6.58, + "sl7": 6.55 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.6, + "sl5": 10.14, + "sl6": 9.8, + "sl7": 11.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.43, + "sl6": 32.6, + "sl7": 33.0 + }, + "site": { + "siteData": { + "componentID": 157548, + "distance": 1849.359, + "mapunitID": 9723, + "minCompDistance": 1849.3591, + "share": 35, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.", + "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Luvic arenosols", + "name": "Luvic arenosols", + "rank_loc": "10", + "score_loc": 0.021 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 157414, + "distance": 81555.369, + "mapunitID": 9679, + "minCompDistance": 81555.3694, + "share": 60, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Luvic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Luvic Arenosols have slightly increased clay content with depth and thus increased moisture and nutrient retention.", + "Description_es": "Los Arenosoles Lúvicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles lúvicos tienen un contenido de arcilla ligeramente mayor con la profundidad y, por tanto, una mayor retención de humedad y nutrientes. ", + "Description_fr": "Luvic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Luvic Arenosols have slightly increased clay content with depth and thus increased moisture and nutrient retention.", + "Description_ks": "Luvic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Luvic Arenosols have slightly increased clay content with depth and thus increased moisture and nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 + }, + "clay": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols", + "rank_loc": "11", + "score_loc": 0.018 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 + }, + "site": { + "siteData": { + "componentID": 157545, + "distance": 65551.867, + "mapunitID": 9722, + "minCompDistance": 65551.8665, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Stagnic luvisols", + "name": "Stagnic luvisols", + "rank_loc": "12", + "score_loc": 0.018 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 + }, + "sand": { + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 + }, + "site": { + "siteData": { + "componentID": 157546, + "distance": 65551.867, + "mapunitID": 9722, + "minCompDistance": 65551.8665, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Stagnic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Stagnic Luvisols are ponded and saturated in and above surface horizons during wet times of the year.", + "Description_es": "Los Luvisoles Stágnicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Estálicos están encharcados y saturados en los horizontes superficiales y por encima de ellos durante las épocas húmedas del año.", + "Description_fr": "Stagnic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Stagnic Luvisols are ponded and saturated in and above surface horizons during wet times of the year.", + "Description_ks": "Stagnic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Stagnic Luvisols are ponded and saturated in and above surface horizons during wet times of the year.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Dado que la saturación es causada por el agua superficial, podría ser útil el drenaje superficial y/o el mantenimiento de la cubierta para mejorar la infiltración y la retención de agua.
Considerar el uso de cultivos con raíces poco profundas.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
Se puede conseguir un uso más eficiente del N por parte de los cultivos en estos suelos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.2, + "sl5": 13.43, + "sl6": 13.6, + "sl7": 13.83 + }, + "clay": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.8, + "sl5": 15.14, + "sl6": 15.6, + "sl7": 16.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.086 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4, + "sl4": 7.44, + "sl5": 7.51, + "sl6": 7.66, + "sl7": 7.75 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 23.0, + "sl5": 25.0, + "sl6": 26.0, + "sl7": 26.17 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0, + "sl4": 65.6, + "sl5": 64.86, + "sl6": 63.8, + "sl7": 62.83 + }, + "site": { + "siteData": { + "componentID": 157476, + "distance": 73872.608, + "mapunitID": 9699, + "minCompDistance": 21368.3019, + "share": 65, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.6, + "sl5": 16.43, + "sl6": 17.0, + "sl7": 17.0 + }, + "clay": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.0, + "sl5": 26.43, + "sl6": 27.8, + "sl7": 27.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.57, + "sl6": 1.0, + "sl7": 1.33 + }, + "id": { + "component": "Eutric regosols", + "name": "Eutric regosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.029 + }, + "ph": { + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.76, + "sl5": 5.8, + "sl6": 5.9, + "sl7": 5.98 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.43, + "sl6": 2.6, + "sl7": 2.5 + }, + "sand": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 28.2, + "sl5": 27.14, + "sl6": 26.8, + "sl7": 27.17 + }, + "site": { + "siteData": { + "componentID": 157437, + "distance": 5598.48, + "mapunitID": 9686, + "minCompDistance": 0.0, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Description_es": "Regosoles Éutricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Eutricos tienen una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Description_ks": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.2, + "sl5": 2.86, + "sl6": 2.6, + "sl7": 2.67 + }, + "clay": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 5.71, + "sl6": 6.0, + "sl7": 6.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric regosols", + "name": "Eutric regosols3", + "rank_loc": "Not Displayed", + "score_loc": 0.029 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.82, + "sl5": 5.84, + "sl6": 5.86, + "sl7": 5.92 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 3.29, + "sl6": 4.4, + "sl7": 5.17 + }, + "sand": { + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 87.2, + "sl5": 87.43, + "sl6": 87.6, + "sl7": 87.5 + }, + "site": { + "siteData": { + "componentID": 157568, + "distance": 74171.143, + "mapunitID": 9731, + "minCompDistance": 0.0, + "share": 45, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Description_es": "Regosoles Éutricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Eutricos tienen una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Description_ks": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 13.6, + "sl5": 15.0, + "sl6": 16.4, + "sl7": 16.83 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 24.4, + "sl5": 26.86, + "sl6": 29.2, + "sl7": 30.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.029 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.26, + "sl5": 6.37, + "sl6": 6.52, + "sl7": 6.57 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.57, + "sl6": 2.4, + "sl7": 2.33 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 46.0, + "sl5": 44.14, + "sl6": 42.2, + "sl7": 42.0 + }, + "site": { + "siteData": { + "componentID": 157477, + "distance": 73872.608, + "mapunitID": 9699, + "minCompDistance": 43336.5293, + "share": 35, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.6, + "sl5": 16.29, + "sl6": 16.8, + "sl7": 17.0 + }, + "clay": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 25.6, + "sl5": 27.57, + "sl6": 29.2, + "sl7": 29.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.8, + "sl7": 1.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.029 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.88, + "sl5": 5.94, + "sl6": 6.04, + "sl7": 6.1 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 8.4, + "sl5": 7.29, + "sl6": 6.0, + "sl7": 5.5 + }, + "sand": { + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 23.2, + "sl5": 22.29, + "sl6": 22.2, + "sl7": 22.33 + }, + "site": { + "siteData": { + "componentID": 157488, + "distance": 65814.76, + "mapunitID": 9702, + "minCompDistance": 45664.9211, + "share": 35, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Silt loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 157428, + "name": "Eutric vertisols", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": "1", + "score_data": 0.879, + "score_data_loc": 1.0, + "score_loc": 0.115 + }, + { + "component": "Luvic arenosols", + "componentData": "Data Complete", + "componentID": 157414, + "name": "Luvic arenosols", + "rank_data": "1", + "rank_data_loc": "2", + "rank_loc": "10", + "score_data": 0.885, + "score_data_loc": 0.912, + "score_loc": 0.021 + }, + { + "component": "Eutric planosols", + "componentData": "Data Complete", + "componentID": 157545, + "name": "Eutric planosols", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": "11", + "score_data": 0.865, + "score_data_loc": 0.888, + "score_loc": 0.018 + }, + { + "component": "Eutric regosols", + "componentData": "Data Complete", + "componentID": 157437, + "name": "Eutric regosols2", + "rank_data": "4", + "rank_data_loc": "4", + "rank_loc": "Not Displayed", + "score_data": 0.737, + "score_data_loc": 0.77, + "score_loc": 0.029 + }, + { + "component": "Gleyic acrisols", + "componentData": "Data Complete", + "componentID": 157547, + "name": "Gleyic acrisols", + "rank_data": "5", + "rank_data_loc": "5", + "rank_loc": "3", + "score_data": 0.731, + "score_data_loc": 0.769, + "score_loc": 0.033 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 157401, + "name": "Calcaric cambisols1", + "rank_data": "11", + "rank_data_loc": "6", + "rank_loc": "2", + "score_data": 0.634, + "score_data_loc": 0.725, + "score_loc": 0.086 + }, + { + "component": "Calcaric fluvisols", + "componentData": "Data Complete", + "componentID": 157400, + "name": "Calcaric fluvisols", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": "6", + "score_data": 0.681, + "score_data_loc": 0.714, + "score_loc": 0.029 + }, + { + "component": "Chromic luvisols", + "componentData": "Missing Data", + "componentID": 157483, + "name": "Chromic luvisols1", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": "7", + "score_data": 0.681, + "score_data_loc": 0.714, + "score_loc": 0.029 + }, + { + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 157534, + "name": "Calcic luvisols", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": "4", + "score_data": 0.643, + "score_data_loc": 0.676, + "score_loc": 0.029 + }, + { + "component": "Stagnic luvisols", + "componentData": "Missing Data", + "componentID": 157546, + "name": "Stagnic luvisols", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": "12", + "score_data": 0.643, + "score_data_loc": 0.665, + "score_loc": 0.018 + }, + { + "component": "Gleyic luvisols", + "componentData": "Data Complete", + "componentID": 157548, + "name": "Gleyic luvisols", + "rank_data": "12", + "rank_data_loc": "11", + "rank_loc": "9", + "score_data": 0.634, + "score_data_loc": 0.664, + "score_loc": 0.025 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 157466, + "name": "Lithic leptosols1", + "rank_data": "6", + "rank_data_loc": "12", + "rank_loc": "8", + "score_data": 0.731, + "score_data_loc": 0.002, + "score_loc": 0.029 + }, + { + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 157477, + "name": "Chromic luvisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.629, + "score_data_loc": 0.662, + "score_loc": 0.029 + }, + { + "component": "Eutric regosols", + "componentData": "Data Complete", + "componentID": 157429, + "name": "Eutric regosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "5", + "score_data": 0.625, + "score_data_loc": 0.658, + "score_loc": 0.029 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 157476, + "name": "Calcaric cambisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.528, + "score_data_loc": 0.618, + "score_loc": 0.086 + }, + { + "component": "Eutric regosols", + "componentData": "Data Complete", + "componentID": 157568, + "name": "Eutric regosols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.291, + "score_data_loc": 0.321, + "score_loc": 0.029 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 157488, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.614, + "score_data_loc": 0.002, + "score_loc": 0.029 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json new file mode 100644 index 0000000..c2f07a3 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json @@ -0,0 +1,1371 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 34.0, + "sl2": 34.0, + "sl3": 34.0, + "sl4": 30.2, + "sl5": 28.86, + "sl6": 26.8, + "sl7": 25.67 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 19.8, + "sl5": 19.71, + "sl6": 18.8, + "sl7": 18.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.6, + "sl5": 0.71, + "sl6": 0.8, + "sl7": 0.83 + }, + "id": { + "component": "Haplic andosols", + "name": "Haplic andosols", + "rank_loc": "1", + "score_loc": 0.142 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 6.08, + "sl5": 6.13, + "sl6": 6.18, + "sl7": 6.18 + }, + "rock_fragments": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.6, + "sl5": 14.43, + "sl6": 16.8, + "sl7": 18.5 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.4, + "sl5": 40.14, + "sl6": 42.4, + "sl7": 43.5 + }, + "site": { + "siteData": { + "componentID": 103927, + "distance": 1111.692, + "mapunitID": 11370, + "minCompDistance": 1111.6922, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Description_es": "Los Andosoles Háplicos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas. ", + "Description_fr": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Description_ks": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", + "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Debido a que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.", + "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", + "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.2, + "sl5": 20.57, + "sl6": 19.6, + "sl7": 19.0 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 26.4, + "sl5": 26.14, + "sl6": 25.6, + "sl7": 25.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic phaeozems", + "name": "Haplic phaeozems", + "rank_loc": "2", + "score_loc": 0.054 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.36, + "sl5": 6.46, + "sl6": 6.58, + "sl7": 6.68 + }, + "rock_fragments": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.8, + "sl5": 4.57, + "sl6": 4.6, + "sl7": 4.67 + }, + "sand": { + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 28.4, + "sl5": 29.14, + "sl6": 30.2, + "sl7": 31.0 + }, + "site": { + "siteData": { + "componentID": 103604, + "distance": 2611.703, + "mapunitID": 11112, + "minCompDistance": 2611.7029, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", + "Description_es": "Los Phaeozems Háplicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que se necesite el riego para la producción.", + "Description_fr": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", + "Description_ks": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.", + "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 23.4, + "sl5": 21.0, + "sl6": 18.2, + "sl7": 16.83 + }, + "clay": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 10.0, + "sl5": 10.14, + "sl6": 10.2, + "sl7": 9.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Umbric andosols", + "name": "Umbric andosols", + "rank_loc": "3", + "score_loc": 0.035 + }, + "ph": { + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.82, + "sl5": 5.84, + "sl6": 5.84, + "sl7": 5.85 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.0, + "sl5": 17.43, + "sl6": 20.0, + "sl7": 21.0 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 39.6, + "sl5": 41.29, + "sl6": 43.6, + "sl7": 46.17 + }, + "site": { + "siteData": { + "componentID": 103928, + "distance": 7836.2, + "mapunitID": 11371, + "minCompDistance": 7836.2001, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ", + "Description_es": "Los Andosoles Úmbricos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas.
Los Andosoles úmbricos tienen un horizonte superficial grueso, pero los suelos son más húmedos y tienen menos nutrientes que los Andosoles móllicos. ", + "Description_fr": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ", + "Description_ks": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ", + "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. ", + "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Dado que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciéndolo inaccesible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.
El drenaje adicional puede hacer que estos suelos sean más productivos.
La fertilización será esencial para la producción efectiva de los cultivos.", + "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. ", + "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. " + } + }, + "texture": { + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Silt loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 26.4, + "sl5": 25.57, + "sl6": 24.6, + "sl7": 24.0 + }, + "clay": { + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 28.8, + "sl5": 29.29, + "sl6": 29.4, + "sl7": 29.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Gleyic phaeozems", + "name": "Gleyic phaeozems", + "rank_loc": "4", + "score_loc": 0.035 + }, + "ph": { + "sl1": 7.1, + "sl2": 7.1, + "sl3": 7.1, + "sl4": 7.16, + "sl5": 7.19, + "sl6": 7.24, + "sl7": 7.28 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 7.4, + "sl5": 9.43, + "sl6": 11.2, + "sl7": 10.5 + }, + "sand": { + "sl1": 34.0, + "sl2": 34.0, + "sl3": 34.0, + "sl4": 33.8, + "sl5": 33.71, + "sl6": 34.4, + "sl7": 34.83 + }, + "site": { + "siteData": { + "componentID": 103605, + "distance": 12988.596, + "mapunitID": 11113, + "minCompDistance": 12988.596, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", + "Description_es": "Los Phaeozems Gléyicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems gleyicos están saturados de agua subterránea poco profunda a menos de un metro de la superficie del suelo.", + "Description_fr": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", + "Description_ks": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que hay que considerar los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.4, + "sl5": 17.43, + "sl6": 17.4, + "sl7": 17.0 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 31.8, + "sl5": 32.0, + "sl6": 31.8, + "sl7": 31.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Eutric gleysols", + "name": "Eutric gleysols", + "rank_loc": "5", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.3, + "sl2": 6.3, + "sl3": 6.3, + "sl4": 6.5, + "sl5": 6.57, + "sl6": 6.66, + "sl7": 6.75 + }, + "rock_fragments": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.0, + "sl5": 8.86, + "sl6": 9.0, + "sl7": 9.33 + }, + "sand": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 23.0, + "sl5": 23.14, + "sl6": 23.2, + "sl7": 23.0 + }, + "site": { + "siteData": { + "componentID": 104276, + "distance": 14827.397, + "mapunitID": 11663, + "minCompDistance": 14827.3974, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.0, + "sl5": 15.0, + "sl6": 14.8, + "sl7": 14.5 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 23.0, + "sl5": 24.14, + "sl6": 24.6, + "sl7": 24.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic luvisols", + "name": "Haplic luvisols", + "rank_loc": "6", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.02, + "sl5": 6.06, + "sl6": 6.12, + "sl7": 6.2 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 11.0, + "sl5": 12.29, + "sl6": 13.6, + "sl7": 14.17 + }, + "sand": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 31.2, + "sl5": 31.71, + "sl6": 33.0, + "sl7": 33.83 + }, + "site": { + "siteData": { + "componentID": 104597, + "distance": 22984.344, + "mapunitID": 11909, + "minCompDistance": 22984.3437, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 14.6, + "sl5": 13.57, + "sl6": 12.8, + "sl7": 12.33 + }, + "clay": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.2, + "sl5": 14.43, + "sl6": 14.6, + "sl7": 14.5 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols", + "rank_loc": "7", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.36, + "sl5": 6.44, + "sl6": 6.54, + "sl7": 6.6 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 18.8, + "sl5": 20.71, + "sl6": 23.0, + "sl7": 24.0 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 42.2, + "sl5": 43.43, + "sl6": 45.0, + "sl7": 46.0 + }, + "site": { + "siteData": { + "componentID": 104610, + "distance": 49566.694, + "mapunitID": 11920, + "minCompDistance": 49566.6944, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 17.6, + "sl5": 18.29, + "sl6": 18.6, + "sl7": 18.33 + }, + "clay": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 26.8, + "sl5": 28.71, + "sl6": 29.6, + "sl7": 29.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.4, + "sl7": 1.67 + }, + "id": { + "component": "Gleyic luvisols", + "name": "Gleyic luvisols", + "rank_loc": "8", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.02, + "sl5": 6.03, + "sl6": 6.12, + "sl7": 6.22 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 2.8, + "sl5": 2.71, + "sl6": 3.0, + "sl7": 3.33 + }, + "sand": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 21.4, + "sl5": 20.86, + "sl6": 20.8, + "sl7": 21.0 + }, + "site": { + "siteData": { + "componentID": 104608, + "distance": 59323.866, + "mapunitID": 11919, + "minCompDistance": 59323.8661, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.", + "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Silt loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 17.2, + "sl5": 16.71, + "sl6": 16.4, + "sl7": 16.17 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 26.6, + "sl5": 26.57, + "sl6": 25.8, + "sl7": 25.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Calcaric phaeozems", + "name": "Calcaric phaeozems", + "rank_loc": "9", + "score_loc": 0.035 + }, + "ph": { + "sl1": 7.6, + "sl2": 7.6, + "sl3": 7.6, + "sl4": 7.78, + "sl5": 7.87, + "sl6": 7.94, + "sl7": 7.98 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 7.4, + "sl5": 10.14, + "sl6": 12.2, + "sl7": 11.67 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.2, + "sl5": 40.14, + "sl6": 41.2, + "sl7": 42.33 + }, + "site": { + "siteData": { + "componentID": 103981, + "distance": 73247.232, + "mapunitID": 11413, + "minCompDistance": 73247.2321, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Description_es": "Los Phaeozems Calcáricos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems calcáreos son calcáreos en la parte superior del subsuelo.", + "Description_fr": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Description_ks": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Estos suelos tienen grandes cantidades de carbonato cálcico libre en el horizonte superior del suelo, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 26.8, + "sl5": 26.43, + "sl6": 25.6, + "sl7": 25.0 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.4, + "sl5": 33.43, + "sl6": 34.2, + "sl7": 34.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Stagnic phaeozems", + "name": "Stagnic phaeozems", + "rank_loc": "10", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.56, + "sl5": 6.66, + "sl6": 6.74, + "sl7": 6.78 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.86, + "sl6": 3.4, + "sl7": 3.67 + }, + "sand": { + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 27.6, + "sl5": 27.14, + "sl6": 26.8, + "sl7": 26.67 + }, + "site": { + "siteData": { + "componentID": 103607, + "distance": 84701.498, + "mapunitID": 11115, + "minCompDistance": 84701.4983, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", + "Description_es": "Los Phaeozems Stágnicos son suelos fértiles y productivos de praderas con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los Faeozems estancados están encharcados y saturados en y por encima de los horizontes superficiales durante las épocas húmedas del año.", + "Description_fr": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", + "Description_ks": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Puede ser necesario el drenaje de estos suelos.
Dado que la saturación es causada por el agua superficial, podría ser útil el drenaje superficial y/o el mantenimiento de la cubierta para mejorar la infiltración y la retención de agua.
Considerar el uso de cultivos con raíces poco profundas.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
Se puede conseguir un uso más eficiente del N por parte de los cultivos en estos suelos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 26.6, + "sl5": 25.29, + "sl6": 23.8, + "sl7": 22.67 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 31.4, + "sl5": 31.71, + "sl6": 31.4, + "sl7": 30.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.6, + "sl7": 1.83 + }, + "id": { + "component": "Gleyic chernozems", + "name": "Gleyic chernozems", + "rank_loc": "11", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.9, + "sl2": 6.9, + "sl3": 6.9, + "sl4": 7.06, + "sl5": 7.16, + "sl6": 7.28, + "sl7": 7.35 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.29, + "sl6": 3.2, + "sl7": 3.5 + }, + "sand": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 26.0, + "sl5": 25.86, + "sl6": 26.0, + "sl7": 26.5 + }, + "site": { + "siteData": { + "componentID": 103642, + "distance": 89693.916, + "mapunitID": 11141, + "minCompDistance": 89693.9156, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", + "Description_es": "Los Chernozems Gleyicos son suelos altamente productivos con buenas propiedades físicas y químicas.
Tienen una alta calidad de suelo y capas superficiales oscuras y ricas.
Los chernozems gleyicos están saturados de agua subterránea poco profunda por encima de un metro de profundidad del suelo.", + "Description_fr": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", + "Description_ks": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", + "Management_en": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Son, en general, suelos excelentes para la producción de cultivos.
Tienen una excelente porosidad y retención de agua, y son adecuados para una amplia gama de sistemas de producción de cultivos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación procedente de aguas subterráneas, puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 24.2, + "sl5": 22.86, + "sl6": 21.0, + "sl7": 20.0 + }, + "clay": { + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 28.6, + "sl5": 28.43, + "sl6": 27.6, + "sl7": 27.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.29, + "sl6": 1.8, + "sl7": 2.0 + }, + "id": { + "component": "Calcic chernozems", + "name": "Calcic chernozems", + "rank_loc": "12", + "score_loc": 0.035 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4, + "sl4": 7.58, + "sl5": 7.7, + "sl6": 7.84, + "sl7": 7.9 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.8, + "sl5": 7.57, + "sl6": 9.8, + "sl7": 10.83 + }, + "sand": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 28.4, + "sl5": 28.71, + "sl6": 29.8, + "sl7": 30.33 + }, + "site": { + "siteData": { + "componentID": 103635, + "distance": 90543.48, + "mapunitID": 11138, + "minCompDistance": 90543.4796, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Chernozems Cálcicos son suelos altamente productivos con buenas propiedades físicas y químicas.
Tienen una alta calidad de suelo y capas superficiales oscuras y ricas.
Los Chernozems Cálcicos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Management_en": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", + "Management_es": "Son, en general, suelos excelentes para la producción de cultivos.
Tienen una excelente porosidad y retención de agua, y son adecuados para una amplia gama de sistemas de producción de cultivos.
Algunos cultivos especiales pueden ser sensibles a los suelos con pH más alto, y puede ser necesario un suplemento de hierro.
Puede ser necesario el uso de fertilizantes.
Al tener un subsuelo calcáreo, pueden fijar el fósforo, por lo que puede ser necesaria una fertilización adecuada de P.", + "Management_fr": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", + "Management_ks": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Haplic andosols", + "componentData": "Data Complete", + "componentID": 103927, + "name": "Haplic andosols", + "rank_data": "3", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 0.431, + "score_data_loc": 1.0, + "score_loc": 0.142 + }, + { + "component": "Haplic phaeozems", + "componentData": "Data Complete", + "componentID": 103604, + "name": "Haplic phaeozems", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": 2, + "score_data": 0.431, + "score_data_loc": 0.847, + "score_loc": 0.054 + }, + { + "component": "Calcaric phaeozems", + "componentData": "Data Complete", + "componentID": 103981, + "name": "Calcaric phaeozems", + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": 9, + "score_data": 0.431, + "score_data_loc": 0.814, + "score_loc": 0.035 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 104610, + "name": "Eutric cambisols", + "rank_data": "2", + "rank_data_loc": "4", + "rank_loc": 7, + "score_data": 0.431, + "score_data_loc": 0.814, + "score_loc": 0.035 + }, + { + "component": "Gleyic luvisols", + "componentData": "Missing Data", + "componentID": 104608, + "name": "Gleyic luvisols", + "rank_data": "5", + "rank_data_loc": "5", + "rank_loc": 8, + "score_data": 0.385, + "score_data_loc": 0.733, + "score_loc": 0.035 + }, + { + "component": "Haplic luvisols", + "componentData": "Data Complete", + "componentID": 104597, + "name": "Haplic luvisols", + "rank_data": "6", + "rank_data_loc": "6", + "rank_loc": 6, + "score_data": 0.385, + "score_data_loc": 0.733, + "score_loc": 0.035 + }, + { + "component": "Umbric andosols", + "componentData": "Data Complete", + "componentID": 103928, + "name": "Umbric andosols", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": 3, + "score_data": 0.385, + "score_data_loc": 0.733, + "score_loc": 0.035 + }, + { + "component": "Calcic chernozems", + "componentData": "Data Complete", + "componentID": 103635, + "name": "Calcic chernozems", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": 12, + "score_data": 0.068, + "score_data_loc": 0.181, + "score_loc": 0.035 + }, + { + "component": "Eutric gleysols", + "componentData": "Data Complete", + "componentID": 104276, + "name": "Eutric gleysols", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": 5, + "score_data": 0.068, + "score_data_loc": 0.181, + "score_loc": 0.035 + }, + { + "component": "Gleyic chernozems", + "componentData": "Data Complete", + "componentID": 103642, + "name": "Gleyic chernozems", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": 11, + "score_data": 0.068, + "score_data_loc": 0.181, + "score_loc": 0.035 + }, + { + "component": "Gleyic phaeozems", + "componentData": "Missing Data", + "componentID": 103605, + "name": "Gleyic phaeozems", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": 4, + "score_data": 0.068, + "score_data_loc": 0.181, + "score_loc": 0.035 + }, + { + "component": "Stagnic phaeozems", + "componentData": "Data Complete", + "componentID": 103607, + "name": "Stagnic phaeozems", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": 10, + "score_data": 0.068, + "score_data_loc": 0.181, + "score_loc": 0.035 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json new file mode 100644 index 0000000..3f0a8ba --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json @@ -0,0 +1,1819 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.6, + "sl5": 17.86, + "sl6": 18.4, + "sl7": 18.83 + }, + "clay": { + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 35.8, + "sl5": 36.71, + "sl6": 37.8, + "sl7": 38.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Eutric gleysols", + "name": "Eutric gleysols", + "rank_loc": "1", + "score_loc": 0.025 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.96, + "sl5": 5.97, + "sl6": 6.02, + "sl7": 6.05 + }, + "rock_fragments": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 17.6, + "sl5": 17.14, + "sl6": 14.8, + "sl7": 15.83 + }, + "sand": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.6, + "sl5": 33.29, + "sl6": 32.8, + "sl7": 31.83 + }, + "site": { + "siteData": { + "componentID": 133289, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 49166.7104, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 7.29, + "sl6": 7.8, + "sl7": 7.83 + }, + "clay": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 23.4, + "sl5": 26.57, + "sl6": 29.6, + "sl7": 30.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric plinthosols", + "name": "Eutric plinthosols", + "rank_loc": "2", + "score_loc": 0.022 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.82, + "sl5": 5.8, + "sl6": 5.8, + "sl7": 5.8 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 16.4, + "sl5": 19.71, + "sl6": 23.4, + "sl7": 25.33 + }, + "sand": { + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 57.8, + "sl5": 54.86, + "sl6": 51.8, + "sl7": 50.33 + }, + "site": { + "siteData": { + "componentID": 133231, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 35, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", + "Description_es": "Los Plinthosoles Éutricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles eútricos tienen una alta saturación de bases en los subsuelos.", + "Description_fr": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", + "Description_ks": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", + "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.", + "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una escasa fertilidad del suelo, que combinada con un suelo poco profundo y rocoso hace que no sea posible la agricultura.
Estos suelos deberían utilizarse para cosas como materiales de superficie para carreteras.", + "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.", + "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.2, + "sl5": 5.71, + "sl6": 6.2, + "sl7": 6.33 + }, + "clay": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 19.6, + "sl5": 24.43, + "sl6": 29.4, + "sl7": 31.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Dystric planosols", + "name": "Dystric planosols", + "rank_loc": "3", + "score_loc": 0.016 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.06, + "sl5": 5.07, + "sl6": 5.08, + "sl7": 5.08 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.2, + "sl5": 5.71, + "sl6": 7.6, + "sl7": 8.67 + }, + "sand": { + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 56.0, + "sl5": 52.57, + "sl6": 49.4, + "sl7": 47.83 + }, + "site": { + "siteData": { + "componentID": 133240, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 5, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.", + "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.2, + "sl5": 30.29, + "sl6": 33.2, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols1", + "rank_loc": "4", + "score_loc": 0.016 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.12, + "sl5": 6.07, + "sl6": 6.02, + "sl7": 6.02 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.8, + "sl5": 10.43, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 60.2, + "sl5": 57.57, + "sl6": 54.8, + "sl7": 53.0 + }, + "site": { + "siteData": { + "componentID": 133488, + "distance": 15267.702, + "mapunitID": 36051, + "minCompDistance": 15267.7017, + "share": 45, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.0 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 27.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 + }, + "id": { + "component": "Eutric leptosols", + "name": "Eutric leptosols", + "rank_loc": "5", + "score_loc": 0.016 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.55 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 30.5 + }, + "sand": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 44.0 + }, + "site": { + "siteData": { + "componentID": 133765, + "distance": 30108.037, + "mapunitID": 36118, + "minCompDistance": 30108.037, + "share": 100, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 + }, + "clay": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "6", + "score_loc": 0.016 + }, + "ph": { + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 + }, + "rock_fragments": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 + }, + "sand": { + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 + }, + "site": { + "siteData": { + "componentID": 148823, + "distance": 33726.73, + "mapunitID": 60, + "minCompDistance": 33726.7301, + "share": 100, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "7", + "score_loc": 0.016 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 133287, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 49166.7104, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 6.4, + "sl5": 6.29, + "sl6": 6.2, + "sl7": 6.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 28.8, + "sl5": 31.14, + "sl6": 33.4, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferric lixisols", + "name": "Ferric lixisols", + "rank_loc": "8", + "score_loc": 0.014 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.04, + "sl5": 5.03, + "sl6": 5.02, + "sl7": 5.02 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 14.0 + }, + "sand": { + "sl1": 59.0, + "sl2": 59.0, + "sl3": 59.0, + "sl4": 54.4, + "sl5": 52.29, + "sl6": 50.2, + "sl7": 49.17 + }, + "site": { + "siteData": { + "componentID": 107928, + "distance": 34218.133, + "mapunitID": 1444, + "minCompDistance": 34218.1332, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Lixisoles Férricos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta.
Los Lixisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.
Estos suelos son especialmente sensibles a la erosión, por lo que se necesitan prácticas que trabajen para mantener una estructura fuerte del suelo (como los cultivos perennes).", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.2, + "sl5": 30.29, + "sl6": 33.2, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Dystric gleysols", + "name": "Dystric gleysols", + "rank_loc": "9", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.12, + "sl5": 6.07, + "sl6": 6.02, + "sl7": 6.02 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.8, + "sl5": 10.43, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 60.2, + "sl5": 57.57, + "sl6": 54.8, + "sl7": 53.0 + }, + "site": { + "siteData": { + "componentID": 133232, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 5, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 7.0, + "sl5": 7.0, + "sl6": 7.0, + "sl7": 7.0 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 21.6, + "sl5": 24.71, + "sl6": 28.0, + "sl7": 29.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferric acrisols", + "name": "Ferric acrisols1", + "rank_loc": "10", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.1, + "sl5": 6.03, + "sl6": 5.96, + "sl7": 5.93 + }, + "rock_fragments": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 18.6, + "sl5": 19.43, + "sl6": 20.2, + "sl7": 19.83 + }, + "sand": { + "sl1": 68.0, + "sl2": 68.0, + "sl3": 68.0, + "sl4": 63.2, + "sl5": 60.43, + "sl6": 57.0, + "sl7": 55.33 + }, + "site": { + "siteData": { + "componentID": 133233, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", + "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 11.2, + "sl5": 10.57, + "sl6": 10.2, + "sl7": 10.5 + }, + "clay": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 30.0, + "sl5": 31.57, + "sl6": 33.0, + "sl7": 33.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 + }, + "id": { + "component": "Dystric leptosols", + "name": "Dystric leptosols", + "rank_loc": "11", + "score_loc": 0.011 + }, + "ph": { + "sl1": 4.8, + "sl2": 4.8, + "sl3": 4.8, + "sl4": 4.94, + "sl5": 5.0, + "sl6": 5.06, + "sl7": 5.08 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 4.8, + "sl5": 4.86, + "sl6": 5.4, + "sl7": 5.33 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 40.71, + "sl6": 40.6, + "sl7": 40.5 + }, + "site": { + "siteData": { + "componentID": 133329, + "distance": 48484.096, + "mapunitID": 36018, + "minCompDistance": 48484.0959, + "share": 5, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Dístricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles dísticos tienen una baja saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Description_ks": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Este suelo prácticamente no tiene calcio disponible para el uso de las plantas.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.4, + "sl7": 6.33 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 31.2, + "sl5": 34.0, + "sl6": 36.6, + "sl7": 37.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferralic arenosols", + "name": "Ferralic arenosols", + "rank_loc": "12", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.18, + "sl5": 5.16, + "sl6": 5.14, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.8, + "sl5": 28.29, + "sl6": 27.2, + "sl7": 26.33 + }, + "sand": { + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 50.2, + "sl5": 47.71, + "sl6": 45.2, + "sl7": 43.83 + }, + "site": { + "siteData": { + "componentID": 133291, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 49166.7104, + "share": 5, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 7.0 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 22.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.5 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.016 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 25.5 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 51.5 + }, + "site": { + "siteData": { + "componentID": 134019, + "distance": 52599.161, + "mapunitID": 36178, + "minCompDistance": 15267.7017, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.4, + "sl7": 6.33 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 31.2, + "sl5": 34.0, + "sl6": 36.6, + "sl7": 37.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.016 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.18, + "sl5": 5.16, + "sl6": 5.14, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.8, + "sl5": 28.29, + "sl6": 27.2, + "sl7": 26.33 + }, + "sand": { + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 50.2, + "sl5": 47.71, + "sl6": 45.2, + "sl7": 43.83 + }, + "site": { + "siteData": { + "componentID": 107931, + "distance": 34218.133, + "mapunitID": 1444, + "minCompDistance": 33726.7301, + "share": 10, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferric acrisols", + "name": "Ferric acrisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 133288, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 0.0, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", + "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.4, + "sl7": 6.33 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 31.2, + "sl5": 34.0, + "sl6": 36.6, + "sl7": 37.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferric acrisols", + "name": "Ferric acrisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.18, + "sl5": 5.16, + "sl6": 5.14, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.8, + "sl5": 28.29, + "sl6": 27.2, + "sl7": 26.33 + }, + "sand": { + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 50.2, + "sl5": 47.71, + "sl6": 45.2, + "sl7": 43.83 + }, + "site": { + "siteData": { + "componentID": 133557, + "distance": 52041.457, + "mapunitID": 36068, + "minCompDistance": 0.0, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", + "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.4, + "sl7": 6.33 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 31.2, + "sl5": 34.0, + "sl6": 36.6, + "sl7": 37.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Ferric acrisols", + "name": "Ferric acrisols4", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.18, + "sl5": 5.16, + "sl6": 5.14, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.8, + "sl5": 28.29, + "sl6": 27.2, + "sl7": 26.33 + }, + "sand": { + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 50.2, + "sl5": 47.71, + "sl6": 45.2, + "sl7": 43.83 + }, + "site": { + "siteData": { + "componentID": 133943, + "distance": 83016.795, + "mapunitID": 36160, + "minCompDistance": 0.0, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", + "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Haplic acrisols", + "componentData": "Data Complete", + "componentID": 133287, + "name": "Haplic acrisols", + "rank_data": "3", + "rank_data_loc": "1", + "rank_loc": "7", + "score_data": 1.0, + "score_data_loc": 1.0, + "score_loc": 0.016 + }, + { + "component": "Eutric gleysols", + "componentData": "Missing Data", + "componentID": 133289, + "name": "Eutric gleysols", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": "1", + "score_data": 0.63, + "score_data_loc": 0.645, + "score_loc": 0.025 + }, + { + "component": "Eutric plinthosols", + "componentData": "Data Complete", + "componentID": 133231, + "name": "Eutric plinthosols", + "rank_data": "6", + "rank_data_loc": "3", + "rank_loc": "2", + "score_data": 0.613, + "score_data_loc": 0.625, + "score_loc": 0.022 + }, + { + "component": "Dystric planosols", + "componentData": "Missing Data", + "componentID": 133240, + "name": "Dystric planosols", + "rank_data": "5", + "rank_data_loc": "4", + "rank_loc": "3", + "score_data": 0.613, + "score_data_loc": 0.619, + "score_loc": 0.016 + }, + { + "component": "Ferric acrisols", + "componentData": "Missing Data", + "componentID": 133233, + "name": "Ferric acrisols1", + "rank_data": "7", + "rank_data_loc": "5", + "rank_loc": "10", + "score_data": 0.613, + "score_data_loc": 0.614, + "score_loc": 0.011 + }, + { + "component": "Haplic lixisols", + "componentData": "Missing Data", + "componentID": 133488, + "name": "Haplic lixisols1", + "rank_data": "12", + "rank_data_loc": "6", + "rank_loc": "4", + "score_data": 0.535, + "score_data_loc": 0.542, + "score_loc": 0.016 + }, + { + "component": "Ferric lixisols", + "componentData": "Data Complete", + "componentID": 107928, + "name": "Ferric lixisols", + "rank_data": "11", + "rank_data_loc": "7", + "rank_loc": "8", + "score_data": 0.535, + "score_data_loc": 0.541, + "score_loc": 0.014 + }, + { + "component": "Dystric gleysols", + "componentData": "Missing Data", + "componentID": 133232, + "name": "Dystric gleysols", + "rank_data": "9", + "rank_data_loc": "8", + "rank_loc": "9", + "score_data": 0.535, + "score_data_loc": 0.537, + "score_loc": 0.011 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 133291, + "name": "Ferralic arenosols", + "rank_data": "10", + "rank_data_loc": "9", + "rank_loc": "12", + "score_data": 0.535, + "score_data_loc": 0.537, + "score_loc": 0.011 + }, + { + "component": "Dystric leptosols", + "componentData": "Missing Data", + "componentID": 133329, + "name": "Dystric leptosols", + "rank_data": "1", + "rank_data_loc": "10", + "rank_loc": "11", + "score_data": 1.0, + "score_data_loc": 0.002, + "score_loc": 0.011 + }, + { + "component": "Eutric leptosols", + "componentData": "Missing Data", + "componentID": 133765, + "name": "Eutric leptosols", + "rank_data": "2", + "rank_data_loc": "11", + "rank_loc": "5", + "score_data": 1.0, + "score_data_loc": 0.002, + "score_loc": 0.016 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 148823, + "name": "Lithic leptosols1", + "rank_data": "8", + "rank_data_loc": "12", + "rank_loc": "6", + "score_data": 0.613, + "score_data_loc": 0.002, + "score_loc": 0.016 + }, + { + "component": "Haplic lixisols", + "componentData": "Missing Data", + "componentID": 134019, + "name": "Haplic lixisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.535, + "score_data_loc": 0.542, + "score_loc": 0.016 + }, + { + "component": "Ferric acrisols", + "componentData": "Missing Data", + "componentID": 133557, + "name": "Ferric acrisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.535, + "score_data_loc": 0.537, + "score_loc": 0.011 + }, + { + "component": "Ferric acrisols", + "componentData": "Missing Data", + "componentID": 133943, + "name": "Ferric acrisols4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.535, + "score_data_loc": 0.537, + "score_loc": 0.011 + }, + { + "component": "Ferric acrisols", + "componentData": "Missing Data", + "componentID": 133288, + "name": "Ferric acrisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.37, + "score_data_loc": 0.375, + "score_loc": 0.011 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 107931, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.535, + "score_data_loc": 0.002, + "score_loc": 0.016 + } + ] + } +} diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json new file mode 100644 index 0000000..77da511 --- /dev/null +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json @@ -0,0 +1,1419 @@ +{ + "list": { + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.0, + "sl6": 6.4, + "sl7": 6.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.0, + "sl5": 17.14, + "sl6": 16.0, + "sl7": 15.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.0 + }, + "id": { + "component": "Dystric regosols", + "name": "Dystric regosols", + "rank_loc": "1", + "score_loc": 0.078 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.08, + "sl5": 5.13, + "sl6": 5.16, + "sl7": 5.18 + }, + "rock_fragments": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 30.6, + "sl5": 31.14, + "sl6": 35.2, + "sl7": 36.67 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 57.6, + "sl5": 58.71, + "sl6": 60.2, + "sl7": 60.17 + }, + "site": { + "siteData": { + "componentID": 136281, + "distance": 1300.283, + "mapunitID": 3844, + "minCompDistance": 1300.2831, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", + "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.0, + "sl5": 11.0, + "sl6": 11.0, + "sl7": 10.83 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 37.6, + "sl5": 41.0, + "sl6": 44.2, + "sl7": 45.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic nitisols", + "name": "Haplic nitisols", + "rank_loc": "2", + "score_loc": 0.074 + }, + "ph": { + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.36, + "sl5": 5.31, + "sl6": 5.28, + "sl7": 5.27 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 13.2, + "sl5": 14.14, + "sl6": 13.0, + "sl7": 11.5 + }, + "sand": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 40.6, + "sl5": 38.0, + "sl6": 35.4, + "sl7": 34.67 + }, + "site": { + "siteData": { + "componentID": 134944, + "distance": 46476.447, + "mapunitID": 3728, + "minCompDistance": 46476.4474, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", + "Description_es": "Los Nitisoles Háplicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes.", + "Description_fr": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", + "Description_ks": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", + "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", + "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la planta durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación de fertilizantes fosfatados en banda (directamente sobre la semilla o a un lado y abajo de la semilla), ayudarán a reducir la fijación de P.", + "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", + "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation." + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Clay loam", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 6.0, + "sl6": 6.4, + "sl7": 6.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 26.4, + "sl5": 29.0, + "sl6": 31.6, + "sl7": 33.17 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Dystric plinthosols", + "name": "Dystric plinthosols", + "rank_loc": "3", + "score_loc": 0.063 + }, + "ph": { + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.16, + "sl5": 5.17, + "sl6": 5.18, + "sl7": 5.18 + }, + "rock_fragments": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.2, + "sl5": 20.71, + "sl6": 21.4, + "sl7": 20.33 + }, + "sand": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.2, + "sl5": 44.86, + "sl6": 42.4, + "sl7": 40.83 + }, + "site": { + "siteData": { + "componentID": 134462, + "distance": 22688.376, + "mapunitID": 3656, + "minCompDistance": 22688.3756, + "share": 60, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.", + "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.", + "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil." + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.2, + "sl5": 18.43, + "sl6": 18.4, + "sl7": 17.83 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 34.2, + "sl5": 35.86, + "sl6": 37.2, + "sl7": 37.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "4", + "score_loc": 0.063 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.56, + "sl5": 6.57, + "sl6": 6.58, + "sl7": 6.55 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.6, + "sl5": 10.14, + "sl6": 9.8, + "sl7": 11.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.43, + "sl6": 32.6, + "sl7": 33.0 + }, + "site": { + "siteData": { + "componentID": 135560, + "distance": 56569.283, + "mapunitID": 3780, + "minCompDistance": 56569.2834, + "share": 60, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "5", + "score_loc": 0.053 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 134464, + "distance": 22688.376, + "mapunitID": 3656, + "minCompDistance": 22688.3756, + "share": 10, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Humic acrisols", + "name": "Humic acrisols", + "rank_loc": "6", + "score_loc": 0.053 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 134394, + "distance": 98529.034, + "mapunitID": 3638, + "minCompDistance": 98529.0339, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ", + "Description_es": "Los Acrisoles Húmicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles húmicos contienen grandes cantidades de materia orgánica en la capa superior del suelo.
Suelen tener una estructura pobre, pero se vuelven más productivos en sistemas que incluyen rotaciones de cultivos, cultivos de cobertura o abonos verdes. ", + "Description_fr": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ", + "Description_ks": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 16.4, + "sl5": 15.57, + "sl6": 14.8, + "sl7": 14.5 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 33.6, + "sl5": 35.0, + "sl6": 36.4, + "sl7": 37.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "7", + "score_loc": 0.052 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.16, + "sl5": 5.19, + "sl6": 5.22, + "sl7": 5.25 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.0, + "sl5": 3.14, + "sl6": 3.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.4, + "sl5": 32.71, + "sl6": 32.2, + "sl7": 31.0 + }, + "site": { + "siteData": { + "componentID": 136283, + "distance": 1300.283, + "mapunitID": 3844, + "minCompDistance": 1300.2831, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.14, + "sl6": 17.6, + "sl7": 17.5 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.2, + "sl5": 32.14, + "sl6": 31.6, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Gleysols", + "name": "Gleysols", + "rank_loc": "8", + "score_loc": 0.052 + }, + "ph": { + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.24, + "sl5": 6.3, + "sl6": 6.38, + "sl7": 6.43 + }, + "rock_fragments": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.6, + "sl5": 9.86, + "sl6": 10.2, + "sl7": 10.33 + }, + "sand": { + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.2, + "sl5": 36.86, + "sl6": 38.4, + "sl7": 38.83 + }, + "site": { + "siteData": { + "componentID": 136008, + "distance": 5885.649, + "mapunitID": 3817, + "minCompDistance": 5885.6486, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los Gleysoles tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los gleysoles son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.29, + "sl6": 18.4, + "sl7": 18.5 + }, + "clay": { + "sl1": 34.0, + "sl2": 34.0, + "sl3": 34.0, + "sl4": 36.6, + "sl5": 37.29, + "sl6": 38.0, + "sl7": 38.33 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 + }, + "id": { + "component": "Ferric acrisols", + "name": "Ferric acrisols", + "rank_loc": "9", + "score_loc": 0.032 + }, + "ph": { + "sl1": 5.6, + "sl2": 5.6, + "sl3": 5.6, + "sl4": 5.66, + "sl5": 5.69, + "sl6": 5.74, + "sl7": 5.77 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 9.6, + "sl5": 10.43, + "sl6": 10.8, + "sl7": 11.83 + }, + "sand": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.8, + "sl5": 33.71, + "sl6": 33.6, + "sl7": 33.17 + }, + "site": { + "siteData": { + "componentID": 134463, + "distance": 22688.376, + "mapunitID": 3656, + "minCompDistance": 22688.3756, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", + "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.4, + "sl7": 6.33 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 31.2, + "sl5": 34.0, + "sl6": 36.6, + "sl7": 37.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Humic ferralsols", + "name": "Humic ferralsols", + "rank_loc": "10", + "score_loc": 0.032 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.18, + "sl5": 5.16, + "sl6": 5.14, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.8, + "sl5": 28.29, + "sl6": 27.2, + "sl7": 26.33 + }, + "sand": { + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 50.2, + "sl5": 47.71, + "sl6": 45.2, + "sl7": 43.83 + }, + "site": { + "siteData": { + "componentID": 135998, + "distance": 34926.783, + "mapunitID": 3816, + "minCompDistance": 34926.7828, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Humic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Humic Ferralsols have slightly higher organic matter in the upper portions of the soil. ", + "Description_es": "Los Ferralsoles Húmicos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada para retener nutrientes.
Los ferralisoles húmicos tienen una materia orgánica ligeramente superior en las partes superiores del suelo. ", + "Description_fr": "Humic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Humic Ferralsols have slightly higher organic matter in the upper portions of the soil. ", + "Description_ks": "Humic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Humic Ferralsols have slightly higher organic matter in the upper portions of the soil. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.0, + "sl5": 8.29, + "sl6": 7.4, + "sl7": 7.0 + }, + "clay": { + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 47.2, + "sl5": 48.0, + "sl6": 48.6, + "sl7": 49.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Vertisols", + "name": "Vertisols", + "rank_loc": "11", + "score_loc": 0.032 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.92, + "sl5": 4.94, + "sl6": 4.98, + "sl7": 5.0 + }, + "rock_fragments": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.4, + "sl5": 15.14, + "sl6": 16.6, + "sl7": 17.17 + }, + "sand": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 37.8, + "sl5": 37.14, + "sl6": 36.8, + "sl7": 36.5 + }, + "site": { + "siteData": { + "componentID": 135561, + "distance": 56569.283, + "mapunitID": 3780, + "minCompDistance": 56569.2834, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", + "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.4, + "sl5": 40.29, + "sl6": 40.2, + "sl7": 39.67 + }, + "clay": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 54.8, + "sl5": 55.29, + "sl6": 55.6, + "sl7": 55.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.14, + "sl6": 0.4, + "sl7": 0.67 + }, + "id": { + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "12", + "score_loc": 0.032 + }, + "ph": { + "sl1": 6.9, + "sl2": 6.9, + "sl3": 6.9, + "sl4": 7.06, + "sl5": 7.14, + "sl6": 7.3, + "sl7": 7.37 + }, + "rock_fragments": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.2, + "sl5": 2.43, + "sl6": 2.4, + "sl7": 2.33 + }, + "sand": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.14, + "sl6": 13.0, + "sl7": 13.0 + }, + "site": { + "siteData": { + "componentID": 134395, + "distance": 98529.034, + "mapunitID": 3638, + "minCompDistance": 98529.0339, + "share": 30, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.0, + "sl5": 6.0, + "sl6": 6.0, + "sl7": 6.0 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 25.6, + "sl5": 28.14, + "sl6": 30.0, + "sl7": 30.5 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.053 + }, + "ph": { + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.2, + "sl5": 5.19, + "sl6": 5.16, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.2, + "sl7": 5.83 + }, + "sand": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.8, + "sl5": 45.86, + "sl6": 44.8, + "sl7": 44.83 + }, + "site": { + "siteData": { + "componentID": 134396, + "distance": 98529.034, + "mapunitID": 3638, + "minCompDistance": 22688.3756, + "share": 10, + "soilDepth": 20 + }, + "siteDescription": { + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + } + ] + }, + "rank": { + "metadata": { + "location": "global", + "model": "v2" + }, + "soilRank": [ + { + "component": "Gleysols", + "componentData": "Missing Data", + "componentID": 136008, + "name": "Gleysols", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "8", + "score_data": 0.669, + "score_data_loc": 1.0, + "score_loc": 0.052 + }, + { + "component": "Vertisols", + "componentData": "No Data", + "componentID": 135561, + "name": "Vertisols", + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": "11", + "score_data": 0.6, + "score_data_loc": 0.876, + "score_loc": 0.032 + }, + { + "component": "Chromic luvisols", + "componentData": "Missing Data", + "componentID": 135560, + "name": "Chromic luvisols", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": "4", + "score_data": 0.537, + "score_data_loc": 0.832, + "score_loc": 0.063 + }, + { + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 136283, + "name": "Eutric fluvisols", + "rank_data": "4", + "rank_data_loc": "4", + "rank_loc": "7", + "score_data": 0.518, + "score_data_loc": 0.79, + "score_loc": 0.052 + }, + { + "component": "Dystric plinthosols", + "componentData": "Missing Data", + "componentID": 134462, + "name": "Dystric plinthosols", + "rank_data": "5", + "rank_data_loc": "5", + "rank_loc": "3", + "score_data": 0.469, + "score_data_loc": 0.738, + "score_loc": 0.063 + }, + { + "component": "Haplic nitisols", + "componentData": "Missing Data", + "componentID": 134944, + "name": "Haplic nitisols", + "rank_data": "8", + "rank_data_loc": "6", + "rank_loc": "2", + "score_data": 0.428, + "score_data_loc": 0.696, + "score_loc": 0.074 + }, + { + "component": "Ferric acrisols", + "componentData": "Missing Data", + "componentID": 134463, + "name": "Ferric acrisols", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": "9", + "score_data": 0.438, + "score_data_loc": 0.651, + "score_loc": 0.032 + }, + { + "component": "Humic acrisols", + "componentData": "Missing Data", + "componentID": 134394, + "name": "Humic acrisols", + "rank_data": "9", + "rank_data_loc": "8", + "rank_loc": "6", + "score_data": 0.37, + "score_data_loc": 0.587, + "score_loc": 0.053 + }, + { + "component": "Haplic acrisols", + "componentData": "Data Complete", + "componentID": 134395, + "name": "Haplic acrisols", + "rank_data": "10", + "rank_data_loc": "9", + "rank_loc": "12", + "score_data": 0.37, + "score_data_loc": 0.556, + "score_loc": 0.032 + }, + { + "component": "Humic ferralsols", + "componentData": "No Data", + "componentID": 135998, + "name": "Humic ferralsols", + "rank_data": "11", + "rank_data_loc": "10", + "rank_loc": "10", + "score_data": 0.279, + "score_data_loc": 0.431, + "score_loc": 0.032 + }, + { + "component": "Dystric regosols", + "componentData": "Data Complete", + "componentID": 136281, + "name": "Dystric regosols", + "rank_data": "12", + "rank_data_loc": "11", + "rank_loc": "1", + "score_data": 0.09, + "score_data_loc": 0.233, + "score_loc": 0.078 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 134464, + "name": "Lithic leptosols1", + "rank_data": "6", + "rank_data_loc": "12", + "rank_loc": "5", + "score_data": 0.457, + "score_data_loc": 0.003, + "score_loc": 0.053 + }, + { + "component": "Lithic leptosols", + "componentData": "Missing Data", + "componentID": 134396, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.296, + "score_data_loc": 0.003, + "score_loc": 0.053 + } + ] + } +} diff --git a/soil_id/tests/global/test_global.py b/soil_id/tests/global/test_global.py index bdaabe4..e207873 100644 --- a/soil_id/tests/global/test_global.py +++ b/soil_id/tests/global/test_global.py @@ -15,35 +15,193 @@ import logging import time -import pytest +import pytest from soil_id.db import get_datastore_connection from soil_id.global_soil import list_soils_global, rank_soils_global +from syrupy.extensions.json import JSONSnapshotExtension test_locations = [ {"lon": -1.4631, "lat": 7.3318}, {"lat": -10.950086, "lon": 17.573093}, {"lat": 34.5, "lon": 69.16667}, {"lat": -10.07856, "lon": 15.107436}, + { + "lat": -19.13333, + "lon": 145.5125, + "data": { + "bottomDepth": [10, 24], + "lab_Color": [ + [81.36696398, 2.011595682, 13.47178439], + [81.36696398, 2.011595682, 13.47178439], + ], + "rfvDepth": [None, None], + "soilHorizon": ["Sandy loam", "Loam"], + "topDepth": [0, 10], + }, + }, + { + "lat": 48.71667, + "lon": 126.13333, + "data": { + "bottomDepth": [20], + "lab_Color": [[51.58348661, 4.985592123, 11.10506759]], + "rfvDepth": [None], + "soilHorizon": ["Loamy sand"], + "topDepth": [0], + }, + }, + { + "lat": 37.33333, + "lon": -5.4, + "data": { + "bottomDepth": [25, 160], + "lab_Color": [ + [41.22423435, 1.447890286, 6.167240052], + [51.59649652, 4.791128549, 18.92743224], + ], + "rfvDepth": [None, None], + "soilHorizon": ["Clay", "Clay"], + "topDepth": [0, 125], + }, + }, + { + "lat": -1.75, + "lon": 13.6, + "data": { + "bottomDepth": [10, 30], + "lab_Color": [ + [30.77416274, 5.568356326, 18.03952892], + [41.23714543, 7.282579218, 25.96353458], + ], + "rfvDepth": [None, None], + "soilHorizon": ["Clay", "Clay"], + "topDepth": [0, 10], + }, + }, + { + "lat": 8.48333, + "lon": 76.95, + "data": { + "bottomDepth": [9, 25, 52], + "lab_Color": [ + [61.6838179, 11.454856, 19.93103357], + [61.68224615, 17.08123986, 30.77963923], + [51.60588072, 9.821763719, 38.77054648], + ], + "rfvDepth": [42.0, 41.0, 56.0], + "soilHorizon": ["Clay", "Clay", "Clay"], + "topDepth": [0, 9, 25], + }, + }, + { + "lat": 30.38333, + "lon": 35.53333, + "data": { + "bottomDepth": [5], + "lab_Color": [[71.62679033, 5.183026621, 25.83506164]], + "rfvDepth": [50.0], + "soilHorizon": ["Loam"], + "topDepth": [0], + }, + }, + { + "lat": -2.06972, + "lon": 37.29, + "data": { + "bottomDepth": [80, 125, 140], + "lab_Color": [ + [30.73434089, 19.87611528, 21.31856213], + [30.73434089, 19.87611528, 21.31856213], + [30.73434089, 19.87611528, 21.31856213], + ], + "rfvDepth": [None, None, None], + "soilHorizon": ["Clay", "Clay", "Silty clay loam"], + "topDepth": [37, 80, 125], + }, + }, + { + "lat": 32.11667, + "lon": 20.08333, + "data": { + "bottomDepth": [20, 47, 120], + "lab_Color": [ + [81.35859545, 3.799237833, 11.54430451], + [81.35859545, 3.799237833, 11.54430451], + [81.35859545, 3.799237833, 11.54430451], + ], + "rfvDepth": [None, None, None], + "soilHorizon": ["Sand", "Sand", "Sand"], + "topDepth": [0, 20, 47], + }, + }, + { + "lat": -24.53333, + "lon": 33.36667, + "data": { + "bottomDepth": [5, 10], + "lab_Color": [ + [51.59117331, 3.180150056, 12.67936276], + [71.60636516, 1.125498577, 6.932398776], + ], + "rfvDepth": [None, None], + "soilHorizon": ["Sandy loam", "Loamy sand"], + "topDepth": [0, 5], + }, + }, + { + "lat": 15.73333, + "lon": 120.31667, + "data": { + "bottomDepth": [10, 23, 38], + "lab_Color": [ + [41.22423435, 1.447890286, 6.167240052], + [41.22423435, 1.447890286, 6.167240052], + [51.5981893, 1.26834264, 13.74773572], + ], + "rfvDepth": [None, None, None], + "soilHorizon": ["Silty clay loam", "Silty clay loam", "Silt loam"], + "topDepth": [0, 10, 23], + }, + }, ] -@pytest.mark.parametrize("location", test_locations) -def test_soil_location(location): +test_params = [] +for idx, coords in enumerate(test_locations): + test_params.append(pytest.param(coords, id=f"{coords["lat"]},{coords["lon"]}")) + + +@pytest.mark.parametrize("location", test_params) +def test_soil_location(location, snapshot): + if "data" in location: + data = location["data"] + else: + data = { + "soilHorizon": ["Loam"], + "topDepth": [0], + "bottomDepth": [15], + "rfvDepth": [20], + "lab_Color": [[41.23035939, 3.623018224, 13.27654356]], + } + with get_datastore_connection() as connection: logging.info(f"Testing {location['lon']}, {location['lat']}") start_time = time.perf_counter() - list_soils_result = list_soils_global(connection, location["lon"], location["lat"]) + list_soils_result = list_soils_global( + connection, location["lon"], location["lat"] + ) logging.info(f"...time: {(time.perf_counter()-start_time):.2f}s") - rank_soils_global( + rank_result = rank_soils_global( connection, location["lon"], location["lat"], list_output_data=list_soils_result, - soilHorizon=["Loam"], - topDepth=[0], - bottomDepth=[15], - rfvDepth=[20], - lab_Color=[[41.23035939, 3.623018224, 13.27654356]], + **data, bedrock=None, cracks=None, ) + + assert snapshot.with_defaults(extension_class=JSONSnapshotExtension) == { + "list": list_soils_result.soil_list_json, + "rank": rank_result, + } diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json new file mode 100644 index 0000000..7ea87be --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json @@ -0,0 +1,794 @@ +{ + "list": { + "AWS_PIW90": 5.2, + "Soil Data Value": [ + [ + "rfv_class_30", + 0.10133185276505285 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ], + [ + "rfv_class_0", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Randall", + "name": "Randall", + "rank_loc": "1", + "score_loc": 0.8 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623332", + "componentKind": "Series", + "componentPct": 80, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "369864", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=randall", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#randall", + "slope": 0.5, + "taxsubgrp": "Ustic Epiaquerts", + "textureInfill": "No" + }, + "siteDescription": "The Randall series consists of very deep, poorly drained, very slowly permeable soils that formed in clayey lacustrine sediments derived from the Blackwater Draw Formation of Pleistocene age. These nearly level soils are on the floor of playa basins 3 to 15 m (10 to 50 ft) below the surrounding plain and range in size from 10 to more than 150 acres. Slope ranges from 0 to 1 percent. Mean annual precipitation is 483 mm (19 in), and mean annual temperature is 15 degrees C (59 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY036TX" + ], + "ecoclassname": [ + "Sandy Loam 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY036TX" + ] + } + }, + "id": { + "component": "Acuff", + "name": "Acuff1", + "rank_loc": "2", + "score_loc": 0.414 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623211", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 90.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "369839", + "minCompDistance": 90.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff", + "slope": 2.0, + "taxsubgrp": "Aridic Paleustolls", + "textureInfill": "No" + }, + "siteDescription": "The Acuff series consists of very deep, well drained, moderately permeable soils. These soils formed in loamy eolian sediments in the Blackwater Draw Formation of Pleistocene age. Acuff soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is about 483 mm (19 in) and the mean annual air temperature is about 16 degrees C (60 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Olton", + "name": "Olton", + "rank_loc": "3", + "score_loc": 0.212 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623299", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 204.0, + "irrcapcl": "1", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "369851", + "minCompDistance": 204.0, + "nirrcapcl": "2", + "nirrcapscl": "c", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=olton", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#olton", + "slope": 0.4, + "taxsubgrp": "Aridic Paleustolls", + "textureInfill": "No" + }, + "siteDescription": "The Olton series consists of very deep, well drained, moderately slowly permeable soils that formed in clayey, calcareous eolian sediments in the\nBlackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains and upper side slopes of playas and draws. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in), and mean annual temperature is 15 degrees C (59 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Mclean", + "name": "Mclean", + "rank_loc": "4", + "score_loc": 0.1 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623333", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "4", + "irrcapscl": "w", + "irrcapunit": "None", + "mapunitID": "369864", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=mclean", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#mclean", + "slope": 0.5, + "taxsubgrp": "Udic Haplusterts", + "textureInfill": "No" + }, + "siteDescription": "The McLean series consists of very deep, somewhat poorly drained, very slowly permeable soils that formed in clayey lacustrine deposits of Quaternary age. These nearly level soils are on the floor of playas 1.5 to 23 m (5 to 75 ft) below the surrounding plain and range in size from a few acres to more than 200 acres. Slope ranges from 0 to 1 percent. Mean annual precipitation is 483 mm (19 in), and mean annual temperature is 16 degrees C (61 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Lockney", + "name": "Lockney", + "rank_loc": "5", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623334", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "2", + "irrcapscl": "s", + "irrcapunit": "None", + "mapunitID": "369864", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lockney", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lockney", + "slope": 0.5, + "taxsubgrp": "Typic Haplusterts", + "textureInfill": "No" + }, + "siteDescription": "The Lockney series consists of very deep, moderately well drained, very slowly permeable soils that formed in clayey lacustrine deposits of Quaternary age. These nearly level soils are on a playa step in large playa basins. Slope ranges from 0 to 1 percent. Mean annual precipitation is 483 mm (19 inches) and mean annual temperature is 16 degrees C (61 F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Estacado", + "name": "Estacado1", + "rank_loc": "6", + "score_loc": 0.029 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623213", + "componentKind": "Series", + "componentPct": 6, + "dataSource": "SSURGO", + "distance": 90.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "369839", + "minCompDistance": 90.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado", + "slope": 2.0, + "taxsubgrp": "Aridic Paleustolls", + "textureInfill": "No" + }, + "siteDescription": "The Estacado series consists of very deep, well drained, moderately slowly permeable soils that formed in calcareous, loamy eolian deposits of the Blackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in) and mean annual air temperature is 16 degrees C (61 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY027TX" + ], + "ecoclassname": [ + "Playa 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY027TX" + ] + } + }, + "id": { + "component": "Friona", + "name": "Friona", + "rank_loc": "7", + "score_loc": 0.024 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623214", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 90.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "369839", + "minCompDistance": 90.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=friona", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#friona", + "slope": 2.0, + "taxsubgrp": "Petrocalcic Paleustolls", + "textureInfill": "No" + }, + "siteDescription": "The Friona series consists of soils that are moderately deep to a petrocalcic horizon. They are well drained, moderately permeable soils that formed in loamy eolian sediments from the Blackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains. Slope ranges from 0 to 3 percent. Mean annual precipitation is about 483 mm (19 in), and mean annual air temperature is about 16 degrees C (61 degrees F)" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY027TX" + ], + "ecoclassname": [ + "Playa 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY027TX" + ] + } + }, + "id": { + "component": "Amarillo", + "name": "Amarillo", + "rank_loc": "8", + "score_loc": 0.019 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623212", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "SSURGO", + "distance": 90.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "369839", + "minCompDistance": 90.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=amarillo", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#amarillo", + "slope": 2.0, + "taxsubgrp": "Aridic Paleustalfs", + "textureInfill": "No" + }, + "siteDescription": "The Amarillo series consists of very deep, well drained, moderately permeable soils. These soils formed in loamy eolian deposits from the Blackwater Draw Formation of Pleistocene age. Amarillo soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in) and the mean annual air temperature is 16 degrees C (61 degrees F)" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Pullman", + "name": "Pullman", + "rank_loc": "9", + "score_loc": 0.018 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623298", + "componentKind": "Series", + "componentPct": 7, + "dataSource": "SSURGO", + "distance": 204.0, + "irrcapcl": "3", + "irrcapscl": "s", + "irrcapunit": "None", + "mapunitID": "369851", + "minCompDistance": 204.0, + "nirrcapcl": "3", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=pullman", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#pullman", + "slope": 0.4, + "taxsubgrp": "Torrertic Paleustolls", + "textureInfill": "No" + }, + "siteDescription": "The Pullman series consists of very deep, well drained, slowly permeable soils that formed in clayey eolian deposits from the Blackwater Draw Formation of Pleistocene age. These soils occur on nearly level to very gently sloping plains or playa slopes. Slope ranges from 0 to 3 percent. The mean annual precipitation is about 483 mm (19 in) and the mean annual temperature is about 16 degrees C (60 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Acuff", + "name": "Acuff2", + "rank_loc": "Not Displayed", + "score_loc": 0.414 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623297", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 204.0, + "irrcapcl": "2", + "irrcapscl": "s", + "irrcapunit": "None", + "mapunitID": "369851", + "minCompDistance": 90.0, + "nirrcapcl": "2", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff", + "slope": 0.5, + "taxsubgrp": "Aridic Paleustolls", + "textureInfill": "No" + }, + "siteDescription": "The Acuff series consists of very deep, well drained, moderately permeable soils. These soils formed in loamy eolian sediments in the Blackwater Draw Formation of Pleistocene age. Acuff soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is about 483 mm (19 in) and the mean annual air temperature is about 16 degrees C (60 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R077CY022TX" + ], + "ecoclassname": [ + "Deep Hardland 16-21 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/077C/R077CY022TX" + ] + } + }, + "id": { + "component": "Estacado", + "name": "Estacado2", + "rank_loc": "Not Displayed", + "score_loc": 0.029 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25623296", + "componentKind": "Series", + "componentPct": 3, + "dataSource": "SSURGO", + "distance": 204.0, + "irrcapcl": "1", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "369851", + "minCompDistance": 90.0, + "nirrcapcl": "2", + "nirrcapscl": "c", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado", + "slope": 0.5, + "taxsubgrp": "Aridic Paleustolls", + "textureInfill": "No" + }, + "siteDescription": "The Estacado series consists of very deep, well drained, moderately slowly permeable soils that formed in calcareous, loamy eolian deposits of the Blackwater Draw Formation of Pleistocene age. These soils are on nearly level to gently sloping plains and playa slopes. Slope ranges from 0 to 5 percent. Mean annual precipitation is 483 mm (19 in) and mean annual air temperature is 16 degrees C (61 degrees F)." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Randall", + "componentData": "Missing Data", + "componentID": 25623332, + "name": "Randall", + "rank_data": "7", + "rank_data_loc": "1", + "rank_loc": "1", + "score_data": 0.465, + "score_data_loc": 0.633, + "score_loc": 0.8 + }, + { + "component": "Acuff", + "componentData": "Data Complete", + "componentID": 25623297, + "name": "Acuff2", + "rank_data": "5", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.499, + "score_data_loc": 0.457, + "score_loc": 0.414 + }, + { + "component": "Olton", + "componentData": "Data Complete", + "componentID": 25623299, + "name": "Olton", + "rank_data": "8", + "rank_data_loc": "3", + "rank_loc": "3", + "score_data": 0.454, + "score_data_loc": 0.333, + "score_loc": 0.212 + }, + { + "component": "Estacado", + "componentData": "Data Complete", + "componentID": 25623296, + "name": "Estacado2", + "rank_data": "1", + "rank_data_loc": "4", + "rank_loc": "Not Displayed", + "score_data": 0.598, + "score_data_loc": 0.314, + "score_loc": 0.029 + }, + { + "component": "Lockney", + "componentData": "Missing Data", + "componentID": 25623334, + "name": "Lockney", + "rank_data": "3", + "rank_data_loc": "5", + "rank_loc": "5", + "score_data": 0.571, + "score_data_loc": 0.31, + "score_loc": 0.05 + }, + { + "component": "Amarillo", + "componentData": "Data Complete", + "componentID": 25623212, + "name": "Amarillo", + "rank_data": "2", + "rank_data_loc": "6", + "rank_loc": "8", + "score_data": 0.576, + "score_data_loc": 0.298, + "score_loc": 0.019 + }, + { + "component": "Mclean", + "componentData": "Missing Data", + "componentID": 25623333, + "name": "Mclean", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": "4", + "score_data": 0.482, + "score_data_loc": 0.291, + "score_loc": 0.1 + }, + { + "component": "Friona", + "componentData": "Data Complete", + "componentID": 25623214, + "name": "Friona", + "rank_data": "4", + "rank_data_loc": "8", + "rank_loc": "7", + "score_data": 0.506, + "score_data_loc": 0.265, + "score_loc": 0.024 + }, + { + "component": "Pullman", + "componentData": "Data Complete", + "componentID": 25623298, + "name": "Pullman", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": "9", + "score_data": 0.357, + "score_data_loc": 0.188, + "score_loc": 0.018 + }, + { + "component": "Acuff", + "componentData": "Data Complete", + "componentID": 25623211, + "name": "Acuff1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "2", + "score_data": 0.492, + "score_data_loc": 0.453, + "score_loc": 0.414 + }, + { + "component": "Estacado", + "componentData": "Data Complete", + "componentID": 25623213, + "name": "Estacado1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "6", + "score_data": 0.596, + "score_data_loc": 0.313, + "score_loc": 0.029 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json new file mode 100644 index 0000000..8ce0e57 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json @@ -0,0 +1,1100 @@ +{ + "list": { + "AWS_PIW90": 14.84, + "Soil Data Value": [ + [ + "rfv_class_30", + 0.5233758769036427 + ], + [ + "rfv_class_0", + 0.48072314826451956 + ], + [ + "texture_30", + 0.25751396689198724 + ], + [ + "texture_0", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Carrizo", + "name": "Carrizo1", + "rank_loc": "1", + "score_loc": 0.363 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185637", + "componentKind": "Series", + "componentPct": 6, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Typic Torriorthents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Gunsight", + "name": "Gunsight1", + "rank_loc": "2", + "score_loc": 0.27 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185636", + "componentKind": "Series", + "componentPct": 27, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 21.0, + "taxsubgrp": "Typic Haplocalcids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Rillito", + "name": "Rillito", + "rank_loc": "3", + "score_loc": 0.19 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185645", + "componentKind": "Series", + "componentPct": 19, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 20.0, + "taxsubgrp": "Typic Haplocalcids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Rositas", + "name": "Rositas1", + "rank_loc": "4", + "score_loc": 0.091 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185600", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "STATSGO", + "distance": 353.554689070506, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660584", + "minCompDistance": 353.554689070506, + "nirrcapcl": "8", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 5.0, + "taxsubgrp": "Typic Torripsamments", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Chuckawalla", + "name": "Chuckawalla", + "rank_loc": "5", + "score_loc": 0.08 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185601", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "STATSGO", + "distance": 353.554689070506, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660584", + "minCompDistance": 353.554689070506, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 15.0, + "taxsubgrp": "Typic Calciargids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Beeline", + "name": "Beeline", + "rank_loc": "6", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185640", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 24.0, + "taxsubgrp": "Typic Torriorthents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Momoli", + "name": "Momoli", + "rank_loc": "7", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185638", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 6.0, + "taxsubgrp": "Typic Haplocambids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Gilman", + "name": "Gilman", + "rank_loc": "8", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185646", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "2", + "irrcapscl": "w", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 3.0, + "taxsubgrp": "Typic Torrifluvents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Mohall", + "name": "Mohall", + "rank_loc": "9", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185644", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 4.0, + "taxsubgrp": "Typic Calciargids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Cipriano", + "name": "Cipriano", + "rank_loc": "10", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185643", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 18.0, + "taxsubgrp": "Typic Haplodurids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Pinamt", + "name": "Pinamt", + "rank_loc": "11", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185641", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 20.0, + "taxsubgrp": "Typic Calciargids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Denure", + "name": "Denure", + "rank_loc": "12", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185639", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 4.0, + "taxsubgrp": "Typic Haplocambids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Carrizo", + "name": "Carrizo2", + "rank_loc": "Not Displayed", + "score_loc": 0.363 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185605", + "componentKind": "Series", + "componentPct": 40, + "dataSource": "STATSGO", + "distance": 353.554689070506, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660584", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 4.0, + "taxsubgrp": "Typic Torriorthents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Carrizo", + "name": "Carrizo3", + "rank_loc": "Not Displayed", + "score_loc": 0.363 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185597", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "STATSGO", + "distance": 353.554689070506, + "irrcapcl": "6", + "irrcapscl": "w", + "irrcapunit": "None", + "mapunitID": "660584", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Typic Torriorthents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Gunsight", + "name": "Gunsight2", + "rank_loc": "Not Displayed", + "score_loc": 0.27 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185602", + "componentKind": "Series", + "componentPct": 8, + "dataSource": "STATSGO", + "distance": 353.554689070506, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "660584", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 5.0, + "taxsubgrp": "Typic Haplocalcids", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Rositas", + "name": "Rositas2", + "rank_loc": "Not Displayed", + "score_loc": 0.091 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185596", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "STATSGO", + "distance": 353.554689070506, + "irrcapcl": "3", + "irrcapscl": "s", + "irrcapunit": "None", + "mapunitID": "660584", + "minCompDistance": 353.554689070506, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Typic Torripsamments", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Rositas", + "name": "Rositas3", + "rank_loc": "Not Displayed", + "score_loc": 0.091 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14185606", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 353.554689070506, + "irrcapcl": "3", + "irrcapscl": "s", + "irrcapunit": "None", + "mapunitID": "660584", + "minCompDistance": 353.554689070506, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 5.0, + "taxsubgrp": "Typic Torripsamments", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Carrizo", + "componentData": "Missing Data", + "componentID": 14185605, + "name": "Carrizo2", + "rank_data": "8", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.724, + "score_data_loc": 0.544, + "score_loc": 0.363 + }, + { + "component": "Gunsight", + "componentData": "Missing Data", + "componentID": 14185636, + "name": "Gunsight1", + "rank_data": "7", + "rank_data_loc": "2", + "rank_loc": "2", + "score_data": 0.733, + "score_data_loc": 0.502, + "score_loc": 0.27 + }, + { + "component": "Chuckawalla", + "componentData": "Missing Data", + "componentID": 14185601, + "name": "Chuckawalla", + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": "5", + "score_data": 0.901, + "score_data_loc": 0.491, + "score_loc": 0.08 + }, + { + "component": "Cipriano", + "componentData": "Missing Data", + "componentID": 14185643, + "name": "Cipriano", + "rank_data": "2", + "rank_data_loc": "4", + "rank_loc": "10", + "score_data": 0.857, + "score_data_loc": 0.454, + "score_loc": 0.05 + }, + { + "component": "Denure", + "componentData": "Missing Data", + "componentID": 14185639, + "name": "Denure", + "rank_data": "3", + "rank_data_loc": "5", + "rank_loc": "12", + "score_data": 0.819, + "score_data_loc": 0.434, + "score_loc": 0.05 + }, + { + "component": "Beeline", + "componentData": "Missing Data", + "componentID": 14185640, + "name": "Beeline", + "rank_data": "4", + "rank_data_loc": "6", + "rank_loc": "6", + "score_data": 0.817, + "score_data_loc": 0.434, + "score_loc": 0.05 + }, + { + "component": "Rositas", + "componentData": "Missing Data", + "componentID": 14185600, + "name": "Rositas1", + "rank_data": "5", + "rank_data_loc": "7", + "rank_loc": "4", + "score_data": 0.769, + "score_data_loc": 0.43, + "score_loc": 0.091 + }, + { + "component": "Rillito", + "componentData": "Missing Data", + "componentID": 14185645, + "name": "Rillito", + "rank_data": "9", + "rank_data_loc": "8", + "rank_loc": "3", + "score_data": 0.66, + "score_data_loc": 0.425, + "score_loc": 0.19 + }, + { + "component": "Pinamt", + "componentData": "Missing Data", + "componentID": 14185641, + "name": "Pinamt", + "rank_data": "6", + "rank_data_loc": "9", + "rank_loc": "11", + "score_data": 0.761, + "score_data_loc": 0.406, + "score_loc": 0.05 + }, + { + "component": "Momoli", + "componentData": "Missing Data", + "componentID": 14185638, + "name": "Momoli", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": "7", + "score_data": 0.652, + "score_data_loc": 0.351, + "score_loc": 0.05 + }, + { + "component": "Mohall", + "componentData": "Missing Data", + "componentID": 14185644, + "name": "Mohall", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": "9", + "score_data": 0.636, + "score_data_loc": 0.343, + "score_loc": 0.05 + }, + { + "component": "Gilman", + "componentData": "Missing Data", + "componentID": 14185646, + "name": "Gilman", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": "8", + "score_data": 0.613, + "score_data_loc": 0.331, + "score_loc": 0.05 + }, + { + "component": "Carrizo", + "componentData": "Missing Data", + "componentID": 14185597, + "name": "Carrizo3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.719, + "score_data_loc": 0.541, + "score_loc": 0.363 + }, + { + "component": "Carrizo", + "componentData": "Missing Data", + "componentID": 14185637, + "name": "Carrizo1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.629, + "score_data_loc": 0.496, + "score_loc": 0.363 + }, + { + "component": "Gunsight", + "componentData": "Missing Data", + "componentID": 14185602, + "name": "Gunsight2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.705, + "score_data_loc": 0.487, + "score_loc": 0.27 + }, + { + "component": "Rositas", + "componentData": "Missing Data", + "componentID": 14185606, + "name": "Rositas3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.671, + "score_data_loc": 0.381, + "score_loc": 0.091 + }, + { + "component": "Rositas", + "componentData": "Missing Data", + "componentID": 14185596, + "name": "Rositas2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.582, + "score_data_loc": 0.337, + "score_loc": 0.091 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json new file mode 100644 index 0000000..3e3c28a --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json @@ -0,0 +1,454 @@ +{ + "list": { + "AWS_PIW90": 5.52, + "Soil Data Value": [ + [ + "rfv_class_0", + 0.0035457277021757605 + ], + [ + "rfv_class_30", + 0.0035457277021757605 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R015XE082CA" + ], + "ecoclassname": [ + "Loamy South" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE082CA" + ] + } + }, + "id": { + "component": "Balcom", + "name": "Balcom2", + "rank_loc": "1", + "score_loc": 0.316 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26027166", + "componentKind": "Series", + "componentPct": 45, + "dataSource": "SSURGO", + "distance": 44.0, + "irrcapcl": "6", + "irrcapscl": "e", + "irrcapunit": "nan", + "mapunitID": "457218", + "minCompDistance": 44.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "nan", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom", + "slope": 40.0, + "taxsubgrp": "Calcixerollic Xerochrepts", + "textureInfill": "No" + }, + "siteDescription": "The Balcom series consists of moderately deep, well drained soils that formed in material that weathered from soft, calcareous shale and sandstone. Balcom soils are on hills and have slopes of 5 to 75 percent. The mean annual precipitation is about 18 inches and the mean annual air temperature is about 61 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R015XE082CA" + ], + "ecoclassname": [ + "Loamy South" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE082CA" + ] + } + }, + "id": { + "component": "Nacimiento", + "name": "Nacimiento1", + "rank_loc": "2", + "score_loc": 0.3 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26027170", + "componentKind": "Series", + "componentPct": 20, + "dataSource": "SSURGO", + "distance": 44.0, + "irrcapcl": "6", + "irrcapscl": "e", + "irrcapunit": "nan", + "mapunitID": "457218", + "minCompDistance": 44.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "nan", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom", + "slope": 40.0, + "taxsubgrp": "Calcic Haploxerolls", + "textureInfill": "No" + }, + "siteDescription": "The Nacimiento series consists of moderately deep, well drained soils that formed in material weathered from calcareous shale and sandstone. Nacimiento soils are on rolling uplands and have mostly complex slopes of 9 to 75 percent. The mean annual precipitation is about 16 inches and the mean annual air temperature is about 60 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R015XE020CA" + ], + "ecoclassname": [ + "Fine Loamy 9-13" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE020CA" + ] + } + }, + "id": { + "component": "Los osos", + "name": "Los osos1", + "rank_loc": "3", + "score_loc": 0.2 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26027683", + "componentKind": "Series", + "componentPct": 20, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "6", + "irrcapscl": "e", + "irrcapunit": "nan", + "mapunitID": "457283", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "nan", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nacimiento", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nacimiento", + "slope": 40.0, + "taxsubgrp": "Typic Argixerolls", + "textureInfill": "No" + }, + "siteDescription": "The Los Osos series consists of moderately deep, well drained soils that formed in material weathered from sandstone and shale. Los Osos soils are on uplands and have slopes of 5 to 75 percent. The mean annual precipitation is about 25 inches and the mean annual air temperature is about 60 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R015XE020CA" + ], + "ecoclassname": [ + "Fine Loamy 9-13" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE020CA" + ] + } + }, + "id": { + "component": "Balcom", + "name": "Balcom3", + "rank_loc": "Not Displayed", + "score_loc": 0.316 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26027125", + "componentKind": "Series", + "componentPct": 45, + "dataSource": "SSURGO", + "distance": 670.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "1.0", + "mapunitID": "457217", + "minCompDistance": 44.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "1.0", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom", + "slope": 20.0, + "taxsubgrp": "Calcixerollic Xerochrepts", + "textureInfill": "No" + }, + "siteDescription": "The Balcom series consists of moderately deep, well drained soils that formed in material that weathered from soft, calcareous shale and sandstone. Balcom soils are on hills and have slopes of 5 to 75 percent. The mean annual precipitation is about 18 inches and the mean annual air temperature is about 61 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R015XE020CA" + ], + "ecoclassname": [ + "Fine Loamy 9-13" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE020CA" + ] + } + }, + "id": { + "component": "Nacimiento", + "name": "Nacimiento2", + "rank_loc": "Not Displayed", + "score_loc": 0.3 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26027161", + "componentKind": "Series", + "componentPct": 20, + "dataSource": "SSURGO", + "distance": 670.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "1.0", + "mapunitID": "457217", + "minCompDistance": 44.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "1.0", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nacimiento", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nacimiento", + "slope": 20.0, + "taxsubgrp": "Calcic Haploxerolls", + "textureInfill": "No" + }, + "siteDescription": "The Nacimiento series consists of moderately deep, well drained soils that formed in material weathered from calcareous shale and sandstone. Nacimiento soils are on rolling uplands and have mostly complex slopes of 9 to 75 percent. The mean annual precipitation is about 16 inches and the mean annual air temperature is about 60 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R015XE020CA" + ], + "ecoclassname": [ + "Fine Loamy 9-13" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE020CA" + ] + } + }, + "id": { + "component": "Los osos", + "name": "Los osos2", + "rank_loc": "Not Displayed", + "score_loc": 0.2 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26027715", + "componentKind": "Series", + "componentPct": 20, + "dataSource": "SSURGO", + "distance": 385.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "3.0", + "mapunitID": "457282", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "3.0", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=los_osos", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#los_osos", + "slope": 20.0, + "taxsubgrp": "Typic Argixerolls", + "textureInfill": "No" + }, + "siteDescription": "The Los Osos series consists of moderately deep, well drained soils that formed in material weathered from sandstone and shale. Los Osos soils are on uplands and have slopes of 5 to 75 percent. The mean annual precipitation is about 25 inches and the mean annual air temperature is about 60 degrees F." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Balcom", + "componentData": "Data Complete", + "componentID": 26027125, + "name": "Balcom3", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.573, + "score_data_loc": 0.445, + "score_loc": 0.316 + }, + { + "component": "Nacimiento", + "componentData": "Data Complete", + "componentID": 26027161, + "name": "Nacimiento2", + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.573, + "score_data_loc": 0.437, + "score_loc": 0.3 + }, + { + "component": "Los osos", + "componentData": NaN, + "componentID": 26027715, + "name": "Los osos2", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": "Not Displayed", + "score_data": 0.435, + "score_data_loc": 0.318, + "score_loc": 0.2 + }, + { + "component": "Balcom", + "componentData": "Data Complete", + "componentID": 26027166, + "name": "Balcom2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.355, + "score_data_loc": 0.336, + "score_loc": 0.316 + }, + { + "component": "Nacimiento", + "componentData": "Data Complete", + "componentID": 26027170, + "name": "Nacimiento1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "2", + "score_data": 0.331, + "score_data_loc": 0.315, + "score_loc": 0.3 + }, + { + "component": "Los osos", + "componentData": "Data Complete", + "componentID": 26027683, + "name": "Los osos1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "3", + "score_data": 0.331, + "score_data_loc": 0.265, + "score_loc": 0.2 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json new file mode 100644 index 0000000..c9056d0 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json @@ -0,0 +1,522 @@ +{ + "list": { + "AWS_PIW90": 6.72, + "Soil Data Value": [ + [ + "rfv_class_0", + 1.3573460169189175 + ], + [ + "rfv_class_30", + 0.9685073841396465 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R014XG903CA" + ], + "ecoclassname": [ + "Salt Marsh" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG903CA" + ] + } + }, + "id": { + "component": "Hangerone", + "name": "Hangerone", + "rank_loc": "1", + "score_loc": 0.311 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26038467", + "componentKind": "Series", + "componentPct": 25, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "2", + "irrcapscl": "s", + "irrcapunit": "5.0", + "mapunitID": "1543362", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "s", + "nirrcapunit": "5.0", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hangerone", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hangerone", + "slope": 1.0, + "taxsubgrp": "Cumulic Vertic Endoaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Hangerone series consists of very deep, poorly drained soils that formed in alluvium from mixed rock sources. Hangerone soils are in basins. Slopes range from 0 to 2 percent. The mean annual precipitation is about 14 inches and the mean annual temperature is about 60 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R014XG903CA" + ], + "ecoclassname": [ + "Salt Marsh" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG903CA" + ] + } + }, + "id": { + "component": "Xerorthents", + "name": "Xerorthents1", + "rank_loc": "2", + "score_loc": 0.304 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26038503", + "componentKind": "Taxon above family", + "componentPct": 100, + "dataSource": "SSURGO", + "distance": 149.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "9.0", + "mapunitID": "1602803", + "minCompDistance": 149.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "9.0", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 22.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Aquic xerorthents", + "name": "Aquic xerorthents", + "rank_loc": "3", + "score_loc": 0.237 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26038456", + "componentKind": "Family", + "componentPct": 95, + "dataSource": "SSURGO", + "distance": 717.0, + "irrcapcl": "3", + "irrcapscl": "w", + "irrcapunit": "2.0", + "mapunitID": "1602806", + "minCompDistance": 717.0, + "nirrcapcl": "3", + "nirrcapscl": "w", + "nirrcapunit": "2.0", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=aquic_xerorthents", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#aquic_xerorthents", + "slope": 4.0, + "taxsubgrp": "Aquic Xerorthents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R014XG904CA" + ], + "ecoclassname": [ + "Dry Clayey Bottom" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG904CA" + ] + } + }, + "id": { + "component": "Clear lake", + "name": "Clear lake", + "rank_loc": "4", + "score_loc": 0.021 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26038466", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "2", + "irrcapscl": "s", + "irrcapunit": "5.0", + "mapunitID": "1543362", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "s", + "nirrcapunit": "5.0", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clear_lake", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clear_lake", + "slope": 1.0, + "taxsubgrp": "Xeric Endoaquerts", + "textureInfill": "No" + }, + "siteDescription": "The Clear Lake series consists of very deep, poorly drained soils that formed in fine textured alluvium derived from mixed rock sources. Clear Lake soils are in flood basins, flood plains and in swales of drainageways. Slopes are 0 to 5 percent. The mean annual precipitation is about 20 inches and the mean annual air temperature is about 60 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Bayshore", + "name": "Bayshore", + "rank_loc": "5", + "score_loc": 0.02 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26038468", + "componentKind": "Taxadjunct", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "1", + "irrcapscl": "None", + "irrcapunit": "nan", + "mapunitID": "1543362", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "s", + "nirrcapunit": "nan", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bayshore", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bayshore", + "slope": 1.0, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Bayshore series consists of very deep, somewhat poorly and poorly drained soils formed in nearly level basins from alluvium. Slopes are 0 to 1 percent. The mean annual precipitation is about 13 to 15 inches and the mean annual temperature is about 59 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R014XG903CA" + ], + "ecoclassname": [ + "Salt Marsh" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/014X/R014XG903CA" + ] + } + }, + "id": { + "component": "Embarcadero", + "name": "Embarcadero", + "rank_loc": "6", + "score_loc": 0.01 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26038464", + "componentKind": "Series", + "componentPct": 1, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "4", + "irrcapscl": "s", + "irrcapunit": "6.0", + "mapunitID": "1543362", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "s", + "nirrcapunit": "6.0", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=embarcadero", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#embarcadero", + "slope": 1.0, + "taxsubgrp": "Fluvaquentic Endoaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Embarcadero series consists of very deep, naturally poorly drained soils, now artificially drained that formed in alluvium from mixed rock sources. Embarcadero soils are in basins near the edge of marshes. Slopes range from 0 to 2 percent. The mean annual precipitation is about 13 inches and the mean annual temperature is about 60 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Xerorthents", + "name": "Xerorthents2", + "rank_loc": "Not Displayed", + "score_loc": 0.304 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26038454", + "componentKind": "Taxon above family", + "componentPct": 100, + "dataSource": "SSURGO", + "distance": 776.0, + "irrcapcl": "6", + "irrcapscl": "e", + "irrcapunit": "9.0", + "mapunitID": "1602804", + "minCompDistance": 149.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "9.0", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 40.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Xerorthents", + "componentData": "Missing Data", + "componentID": 26038503, + "name": "Xerorthents1", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "2", + "score_data": 0.757, + "score_data_loc": 0.53, + "score_loc": 0.304 + }, + { + "component": "Hangerone", + "componentData": "Data Complete", + "componentID": 26038467, + "name": "Hangerone", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": "1", + "score_data": 0.709, + "score_data_loc": 0.51, + "score_loc": 0.311 + }, + { + "component": "Aquic xerorthents", + "componentData": "Missing Data", + "componentID": 26038456, + "name": "Aquic xerorthents", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": "3", + "score_data": 0.734, + "score_data_loc": 0.486, + "score_loc": 0.237 + }, + { + "component": "Embarcadero", + "componentData": "Data Complete", + "componentID": 26038464, + "name": "Embarcadero", + "rank_data": "2", + "rank_data_loc": "4", + "rank_loc": "6", + "score_data": 0.735, + "score_data_loc": 0.372, + "score_loc": 0.01 + }, + { + "component": "Clear lake", + "componentData": "Data Complete", + "componentID": 26038466, + "name": "Clear lake", + "rank_data": "5", + "rank_data_loc": "5", + "rank_loc": "4", + "score_data": 0.554, + "score_data_loc": 0.288, + "score_loc": 0.021 + }, + { + "component": "Bayshore", + "componentData": "Data Complete", + "componentID": 26038468, + "name": "Bayshore", + "rank_data": "6", + "rank_data_loc": "6", + "rank_loc": "5", + "score_data": 0.478, + "score_data_loc": 0.249, + "score_loc": 0.02 + }, + { + "component": "Xerorthents", + "componentData": "Missing Data", + "componentID": 26038454, + "name": "Xerorthents2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.56, + "score_data_loc": 0.432, + "score_loc": 0.304 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json new file mode 100644 index 0000000..757e700 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json @@ -0,0 +1,1066 @@ +{ + "list": { + "AWS_PIW90": 5.79, + "Soil Data Value": [ + [ + "rfv_class_30", + 0.2682995614938375 + ], + [ + "rfv_class_0", + 0.22974042594081867 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY101KS" + ], + "ecoclassname": [ + "Limy Slopes" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS" + ] + } + }, + "id": { + "component": "Uly", + "name": "Uly1", + "rank_loc": "1", + "score_loc": 0.9 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865345", + "componentKind": "Series", + "componentPct": 90, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "2669027", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=uly", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#uly", + "slope": 5.0, + "taxsubgrp": "Typic Haplustolls", + "textureInfill": "No" + }, + "siteDescription": "The Uly series includes very deep, well drained formed in loess on uplands. Slopes range from 0 to 30 percent. Mean annual temperature is 10 degrees C. (50 degrees F), and mean annual precipitation is 53 centimeters (21 inches) at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY100KS" + ], + "ecoclassname": [ + "Loamy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS" + ] + } + }, + "id": { + "component": "Harney", + "name": "Harney1", + "rank_loc": "2", + "score_loc": 0.753 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865346", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "2669027", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney", + "slope": 5.0, + "taxsubgrp": "Typic Argiustolls", + "textureInfill": "No" + }, + "siteDescription": "The Harney series consists of deep, well drained, moderately slowly permeable soils that formed in loess. These soils are on uplands on slopes that range from 0 to 8 percent." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY108KS" + ], + "ecoclassname": [ + "Loamy Floodplain" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY108KS" + ] + } + }, + "id": { + "component": "Coly", + "name": "Coly1", + "rank_loc": "3", + "score_loc": 0.38 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865492", + "componentKind": "Series", + "componentPct": 40, + "dataSource": "SSURGO", + "distance": 42.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "1380503", + "minCompDistance": 42.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly", + "slope": 6.0, + "taxsubgrp": "Typic Ustorthents", + "textureInfill": "No" + }, + "siteDescription": "The Coly series consists of very deep, well drained, moderately permeable soils formed in loess. Coly soils are on sideslopes of uplands in MLRA 73-Rolling Plains and Breaks. Slopes range from 1 to 60 percent. Mean annual temperature is 10 degrees C ( 50 degrees F), and mean annual precipitation is 53 centimeters ( 21 inches) at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY108KS" + ], + "ecoclassname": [ + "Loamy Floodplain" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY108KS" + ] + } + }, + "id": { + "component": "Holdrege", + "name": "Holdrege", + "rank_loc": "4", + "score_loc": 0.322 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865493", + "componentKind": "Taxadjunct", + "componentPct": 45, + "dataSource": "SSURGO", + "distance": 42.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "1380503", + "minCompDistance": 42.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=holdrege", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#holdrege", + "slope": 6.0, + "taxsubgrp": "Typic Haplustalfs", + "textureInfill": "No" + }, + "siteDescription": "The Holdrege series consists of very deep, well drained, moderately permeable soils formed in calcareous loess. These upland soils have slopes ranging from 0 to 15 percent. Mean annual temperature is about 54 degrees F, and mean annual precipitation is about 23 inches at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY112KS" + ], + "ecoclassname": [ + "Shallow Limy" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY112KS" + ] + } + }, + "id": { + "component": "Tobin", + "name": "Tobin", + "rank_loc": "5", + "score_loc": 0.176 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865519", + "componentKind": "Series", + "componentPct": 30, + "dataSource": "SSURGO", + "distance": 67.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "1380504", + "minCompDistance": 67.0, + "nirrcapcl": "5", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=tobin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#tobin", + "slope": 1.0, + "taxsubgrp": "Cumulic Haplustolls", + "textureInfill": "No" + }, + "siteDescription": "The Tobin series consists of very deep, well drained soils that formed in silty alluvium. Tobin soils are on flood plains on river valleys in MLRA 73, Rolling Plains and Breaks. Slopes range from 0 to 2 percent. Mean annual precipitation is about 740 millimeters (29 inches) and the mean annual temperature is about 12 degrees C (54 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY100KS" + ], + "ecoclassname": [ + "Loamy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS" + ] + } + }, + "id": { + "component": "Case", + "name": "Case", + "rank_loc": "6", + "score_loc": 0.071 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865495", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "SSURGO", + "distance": 42.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "1380503", + "minCompDistance": 42.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=case", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#case", + "slope": 6.0, + "taxsubgrp": "Typic Calciustepts", + "textureInfill": "No" + }, + "siteDescription": "The Case series consists of very deep, well drained, moderately permeable soils formed in calcareous old alluvium of Tertiary age on uplands of the Southern High Plains Breaks (MLRA-77E). Slopes range from 1 to 15 percent. Mean annual temperature is about 58 degrees F, and mean annual precipitation is about 24 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY100KS" + ], + "ecoclassname": [ + "Loamy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS" + ] + } + }, + "id": { + "component": "Penden", + "name": "Penden", + "rank_loc": "7", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865344", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "2669027", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=penden", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#penden", + "slope": 5.0, + "taxsubgrp": "Typic Calciustolls", + "textureInfill": "No" + }, + "siteDescription": "The Penden series consists of deep, well drained soils formed in calcareous loamy sediments on uplands. Slope ranges from 0 to 15 percent. Mean annual temperature is 13 degrees C. (56 degrees F.), and mean annual precipitation is 48 centimeters (19 inches)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY101KS" + ], + "ecoclassname": [ + "Limy Slopes" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS" + ] + } + }, + "id": { + "component": "Bridgeport", + "name": "Bridgeport", + "rank_loc": "8", + "score_loc": 0.036 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865494", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 42.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "1380503", + "minCompDistance": 42.0, + "nirrcapcl": "5", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bridgeport", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bridgeport", + "slope": 3.0, + "taxsubgrp": "Fluventic Haplustolls", + "textureInfill": "No" + }, + "siteDescription": "The Bridgeport series consists of deep, well drained, moderately permeable soils that formed in calcareous alluvial sediments. These soils are on flood plains or low stream terraces." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY100KS" + ], + "ecoclassname": [ + "Loamy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS" + ] + } + }, + "id": { + "component": "Wakeen", + "name": "Wakeen", + "rank_loc": "9", + "score_loc": 0.032 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865551", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "SSURGO", + "distance": 29.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2605949", + "minCompDistance": 29.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=wakeen", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#wakeen", + "slope": 2.0, + "taxsubgrp": "Entic Haplustolls", + "textureInfill": "No" + }, + "siteDescription": "The Wakeen series consists of well drained soils that are moderately deep over chalky limestone. These soils are on plains, knolls and ridgetops in the Rolling Plains and Breaks (MLRA 73). Slopes range from 1 to 20 percent. Mean annual temperature is about 12 degrees C. (54 degrees F.), and mean annual precipitation is about 58 centimeters (23 inches)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY101KS" + ], + "ecoclassname": [ + "Limy Slopes" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS" + ] + } + }, + "id": { + "component": "Aquolls", + "name": "Aquolls", + "rank_loc": "10", + "score_loc": 0.008 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865552", + "componentKind": "Taxon above family", + "componentPct": 1, + "dataSource": "SSURGO", + "distance": 29.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2605949", + "minCompDistance": 29.0, + "nirrcapcl": "nan", + "nirrcapscl": "None", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY103KS" + ], + "ecoclassname": [ + "Subirrigated" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY103KS" + ] + } + }, + "id": { + "component": "Canlon", + "name": "Canlon", + "rank_loc": "11", + "score_loc": 0.006 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865520", + "componentKind": "Series", + "componentPct": 1, + "dataSource": "SSURGO", + "distance": 67.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "1380504", + "minCompDistance": 67.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=canlon", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#canlon", + "slope": 12.0, + "taxsubgrp": "Lithic Ustorthents", + "textureInfill": "No" + }, + "siteDescription": "The Canlon series consist of shallow, well drained and somewhat excessively drained, moderately permeable soils on uplands. They formed in residuum weathered from lime-cemented sandstone or caliche and have slopes ranging from 2 to 50 percent. The average annual precipitation is about 24 inches, and the mean annual temperature is about 54 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY100KS" + ], + "ecoclassname": [ + "Loamy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS" + ] + } + }, + "id": { + "component": "Uly", + "name": "Uly2", + "rank_loc": "Not Displayed", + "score_loc": 0.9 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865522", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 67.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "1380504", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=uly", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#uly", + "slope": 5.0, + "taxsubgrp": "Typic Haplustolls", + "textureInfill": "No" + }, + "siteDescription": "The Uly series includes very deep, well drained formed in loess on uplands. Slopes range from 0 to 30 percent. Mean annual temperature is 10 degrees C. (50 degrees F), and mean annual precipitation is 53 centimeters (21 inches) at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY101KS" + ], + "ecoclassname": [ + "Limy Slopes" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY101KS" + ] + } + }, + "id": { + "component": "Harney", + "name": "Harney2", + "rank_loc": "Not Displayed", + "score_loc": 0.753 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865550", + "componentKind": "Series", + "componentPct": 95, + "dataSource": "SSURGO", + "distance": 29.0, + "irrcapcl": "2", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "2605949", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney", + "slope": 2.0, + "taxsubgrp": "Typic Argiustolls", + "textureInfill": "No" + }, + "siteDescription": "The Harney series consists of deep, well drained, moderately slowly permeable soils that formed in loess. These soils are on uplands on slopes that range from 0 to 8 percent." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R073XY100KS" + ], + "ecoclassname": [ + "Loamy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/073X/R073XY100KS" + ] + } + }, + "id": { + "component": "Harney", + "name": "Harney3", + "rank_loc": "Not Displayed", + "score_loc": 0.753 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865521", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 67.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "1380504", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney", + "slope": 4.0, + "taxsubgrp": "Typic Argiustolls", + "textureInfill": "No" + }, + "siteDescription": "The Harney series consists of deep, well drained, moderately slowly permeable soils that formed in loess. These soils are on uplands on slopes that range from 0 to 8 percent." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R079XY112KS" + ], + "ecoclassname": [ + "Limy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/079X/R079XY112KS" + ] + } + }, + "id": { + "component": "Coly", + "name": "Coly2", + "rank_loc": "Not Displayed", + "score_loc": 0.38 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25865523", + "componentKind": "Series", + "componentPct": 65, + "dataSource": "SSURGO", + "distance": 67.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "1380504", + "minCompDistance": 42.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly", + "slope": 12.0, + "taxsubgrp": "Typic Ustorthents", + "textureInfill": "No" + }, + "siteDescription": "The Coly series consists of very deep, well drained, moderately permeable soils formed in loess. Coly soils are on sideslopes of uplands in MLRA 73-Rolling Plains and Breaks. Slopes range from 1 to 60 percent. Mean annual temperature is 10 degrees C ( 50 degrees F), and mean annual precipitation is 53 centimeters ( 21 inches) at the type location." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Uly", + "componentData": "Data Complete", + "componentID": 25865345, + "name": "Uly1", + "rank_data": "6", + "rank_data_loc": "1", + "rank_loc": "1", + "score_data": 0.598, + "score_data_loc": 0.749, + "score_loc": 0.9 + }, + { + "component": "Harney", + "componentData": "Data Complete", + "componentID": 25865346, + "name": "Harney1", + "rank_data": "7", + "rank_data_loc": "2", + "rank_loc": "2", + "score_data": 0.598, + "score_data_loc": 0.675, + "score_loc": 0.753 + }, + { + "component": "Coly", + "componentData": "Data Complete", + "componentID": 25865523, + "name": "Coly2", + "rank_data": "2", + "rank_data_loc": "3", + "rank_loc": "Not Displayed", + "score_data": 0.697, + "score_data_loc": 0.538, + "score_loc": 0.38 + }, + { + "component": "Holdrege", + "componentData": "Data Complete", + "componentID": 25865493, + "name": "Holdrege", + "rank_data": "5", + "rank_data_loc": "4", + "rank_loc": "4", + "score_data": 0.611, + "score_data_loc": 0.467, + "score_loc": 0.322 + }, + { + "component": "Tobin", + "componentData": "Data Complete", + "componentID": 25865519, + "name": "Tobin", + "rank_data": "9", + "rank_data_loc": "5", + "rank_loc": "5", + "score_data": 0.561, + "score_data_loc": 0.369, + "score_loc": 0.176 + }, + { + "component": "Canlon", + "componentData": "Data Complete", + "componentID": 25865520, + "name": "Canlon", + "rank_data": "1", + "rank_data_loc": "6", + "rank_loc": "11", + "score_data": 0.71, + "score_data_loc": 0.358, + "score_loc": 0.006 + }, + { + "component": "Penden", + "componentData": "Data Complete", + "componentID": 25865344, + "name": "Penden", + "rank_data": "3", + "rank_data_loc": "7", + "rank_loc": "7", + "score_data": 0.649, + "score_data_loc": 0.35, + "score_loc": 0.05 + }, + { + "component": "Case", + "componentData": "Data Complete", + "componentID": 25865495, + "name": "Case", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": "6", + "score_data": 0.593, + "score_data_loc": 0.332, + "score_loc": 0.071 + }, + { + "component": "Wakeen", + "componentData": "Data Complete", + "componentID": 25865551, + "name": "Wakeen", + "rank_data": "4", + "rank_data_loc": "9", + "rank_loc": "9", + "score_data": 0.612, + "score_data_loc": 0.322, + "score_loc": 0.032 + }, + { + "component": "Bridgeport", + "componentData": "Data Complete", + "componentID": 25865494, + "name": "Bridgeport", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": "8", + "score_data": 0.523, + "score_data_loc": 0.279, + "score_loc": 0.036 + }, + { + "component": "Aquolls", + "componentData": "Missing Data", + "componentID": 25865552, + "name": "Aquolls", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": "10", + "score_data": 0.393, + "score_data_loc": 0.201, + "score_loc": 0.008 + }, + { + "component": "Uly", + "componentData": "Data Complete", + "componentID": 25865522, + "name": "Uly2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.588, + "score_data_loc": 0.744, + "score_loc": 0.9 + }, + { + "component": "Harney", + "componentData": "Data Complete", + "componentID": 25865550, + "name": "Harney2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.551, + "score_data_loc": 0.652, + "score_loc": 0.753 + }, + { + "component": "Harney", + "componentData": "Data Complete", + "componentID": 25865521, + "name": "Harney3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.483, + "score_data_loc": 0.618, + "score_loc": 0.753 + }, + { + "component": "Coly", + "componentData": "Data Complete", + "componentID": 25865492, + "name": "Coly1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "3", + "score_data": 0.611, + "score_data_loc": 0.495, + "score_loc": 0.38 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json new file mode 100644 index 0000000..487099a --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json @@ -0,0 +1,1882 @@ +{ + "list": { + "AWS_PIW90": 3.71, + "Soil Data Value": [ + [ + "rfv_class_0", + 0.6957144623170968 + ], + [ + "rfv_class_30", + 0.4977936090221524 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA008IN" + ], + "ecoclassname": [ + "Wet Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" + ] + } + }, + "id": { + "component": "Miami", + "name": "Miami1", + "rank_loc": "1", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325339", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162394", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", + "slope": 4.0, + "taxsubgrp": "Oxyaquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Williamstown", + "name": "Williamstown1", + "rank_loc": "2", + "score_loc": 0.53 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325400", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 59.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162415", + "minCompDistance": 59.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=williamstown", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#williamstown", + "slope": 3.0, + "taxsubgrp": "Aquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Williamstown series consists of very deep, moderately well drained soils that are moderately deep to dense till. The soils formed in as much as 56 cm (22 inches) of loess and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA007IN" + ], + "ecoclassname": [ + "Till Depression Flatwood" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" + ] + } + }, + "id": { + "component": "Hennepin", + "name": "Hennepin1", + "rank_loc": "3", + "score_loc": 0.225 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325347", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 59.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162396", + "minCompDistance": 59.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", + "slope": 38.0, + "taxsubgrp": "Typic Eutrudepts", + "textureInfill": "No" + }, + "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Fincastle", + "name": "Fincastle", + "rank_loc": "4", + "score_loc": 0.218 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325308", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 170.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162380", + "minCompDistance": 170.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=fincastle", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#fincastle", + "slope": 1.0, + "taxsubgrp": "Aeric Epiaqualfs", + "textureInfill": "No" + }, + "siteDescription": "The Fincastle series consists of very deep, somewhat poorly drained soils that are deep to dense till. Fincastle soils formed in loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Hickory", + "name": "Hickory", + "rank_loc": "5", + "score_loc": 0.217 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325331", + "componentKind": "Series", + "componentPct": 87, + "dataSource": "SSURGO", + "distance": 936.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162389", + "minCompDistance": 936.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hickory", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hickory", + "slope": 40.0, + "taxsubgrp": "Typic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Hickory series consists of very deep, well drained, soils on dissected till plains. They formed in till that can be capped with up to 20 inches of loess. Slope ranges from 5 to 70 percent. Mean annual air temperature is about 54 degrees F., and mean annual precipitation is about 40 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Xenia", + "name": "Xenia", + "rank_loc": "6", + "score_loc": 0.212 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325405", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 193.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162416", + "minCompDistance": 193.0, + "nirrcapcl": "1", + "nirrcapscl": "None", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=xenia", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#xenia", + "slope": 1.0, + "taxsubgrp": "Aquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Xenia series consists of very deep, moderately well drained soils that are deep or very deep to dense till. Xenia soils formed in loess or other silty material and in the underlying loamy till on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1067 mm (42 inches), and mean annual temperature is about 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA007IN" + ], + "ecoclassname": [ + "Till Depression Flatwood" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" + ] + } + }, + "id": { + "component": "Crosby", + "name": "Crosby1", + "rank_loc": "7", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325341", + "componentKind": "Series", + "componentPct": 9, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162394", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", + "slope": 2.0, + "taxsubgrp": "Aeric Epiaqualfs", + "textureInfill": "No" + }, + "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA008IN" + ], + "ecoclassname": [ + "Wet Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" + ] + } + }, + "id": { + "component": "Brookston", + "name": "Brookston", + "rank_loc": "8", + "score_loc": 0.04 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325342", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162394", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brookston", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brookston", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Brookston series consists of very deep, poorly drained soils formed in as much as 51 cm (20 inches) of silty material and the underlying loamy till in depressions on till plains and moraines. Slope ranges from 0 to 3 percent. Mean annual precipitation is about 889 mm (35 inches), and mean annual temperature is about 10.0 degrees C (50 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD010IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + ] + } + }, + "id": { + "component": "Treaty", + "name": "Treaty1", + "rank_loc": "9", + "score_loc": 0.031 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325340", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162394", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD008IN" + ], + "ecoclassname": [ + "Till Depression Flatwood" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD008IN" + ] + } + }, + "id": { + "component": "Cyclone", + "name": "Cyclone1", + "rank_loc": "10", + "score_loc": 0.026 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325348", + "componentKind": "Series", + "componentPct": 3, + "dataSource": "SSURGO", + "distance": 59.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162396", + "minCompDistance": 59.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD010IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + ] + } + }, + "id": { + "component": "Celina", + "name": "Celina", + "rank_loc": "11", + "score_loc": 0.013 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325406", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 193.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162416", + "minCompDistance": 193.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=celina", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#celina", + "slope": 4.0, + "taxsubgrp": "Aquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Celina series consists of very deep, moderately well drained soils that are moderately deep to dense till. They formed in as much as 46 cm (18 inches) of loess and the underlying loamy till of high-lime content. They are on till plains and moraines. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 12 degrees C (53 degree F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD010IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + ] + } + }, + "id": { + "component": "Rainsville", + "name": "Rainsville", + "rank_loc": "12", + "score_loc": 0.013 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325345", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 980.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162395", + "minCompDistance": 980.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rainsville", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rainsville", + "slope": 8.0, + "taxsubgrp": "Oxyaquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Rainsville series consists of very deep, moderately well drained soils that are deep or very deep to dense till. The Rainsville soils formed in as much as 51 cm (20 inches) of loess or other silty material and in the underlying loamy outwash and till. They are on ground moraines and end moraines. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 940 mm (37 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Miami", + "name": "Miami2", + "rank_loc": "Not Displayed", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325349", + "componentKind": "Taxadjunct", + "componentPct": 92, + "dataSource": "SSURGO", + "distance": 59.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162396", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", + "slope": 15.0, + "taxsubgrp": "Typic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA006IN" + ], + "ecoclassname": [ + "Till Depression" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA006IN" + ] + } + }, + "id": { + "component": "Miami", + "name": "Miami3", + "rank_loc": "Not Displayed", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325350", + "componentKind": "Series", + "componentPct": 96, + "dataSource": "SSURGO", + "distance": 85.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162397", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", + "slope": 9.0, + "taxsubgrp": "Oxyaquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD010IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + ] + } + }, + "id": { + "component": "Miami", + "name": "Miami4", + "rank_loc": "Not Displayed", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325326", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "SSURGO", + "distance": 175.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162386", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", + "slope": 4.0, + "taxsubgrp": "Oxyaquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD010IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + ] + } + }, + "id": { + "component": "Miami", + "name": "Miami5", + "rank_loc": "Not Displayed", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325352", + "componentKind": "Series", + "componentPct": 90, + "dataSource": "SSURGO", + "distance": 502.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162398", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", + "slope": 15.0, + "taxsubgrp": "Oxyaquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F114XB503IN" + ], + "ecoclassname": [ + "Till Upland Forest" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/114X/F114XB503IN" + ] + } + }, + "id": { + "component": "Miami", + "name": "Miami6", + "rank_loc": "Not Displayed", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325346", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 980.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162395", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", + "slope": 8.0, + "taxsubgrp": "Oxyaquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA007IN" + ], + "ecoclassname": [ + "Till Depression Flatwood" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" + ] + } + }, + "id": { + "component": "Williamstown", + "name": "Williamstown2", + "rank_loc": "Not Displayed", + "score_loc": 0.53 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325309", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 170.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162380", + "minCompDistance": 59.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=williamstown", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#williamstown", + "slope": 4.0, + "taxsubgrp": "Aquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Williamstown series consists of very deep, moderately well drained soils that are moderately deep to dense till. The soils formed in as much as 56 cm (22 inches) of loess and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA008IN" + ], + "ecoclassname": [ + "Wet Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" + ] + } + }, + "id": { + "component": "Williamstown", + "name": "Williamstown3", + "rank_loc": "Not Displayed", + "score_loc": 0.53 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325354", + "componentKind": "Series", + "componentPct": 1, + "dataSource": "SSURGO", + "distance": 502.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162398", + "minCompDistance": 59.0, + "nirrcapcl": "2", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=williamstown", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#williamstown", + "slope": 1.0, + "taxsubgrp": "Aquic Hapludalfs", + "textureInfill": "No" + }, + "siteDescription": "The Williamstown series consists of very deep, moderately well drained soils that are moderately deep to dense till. The soils formed in as much as 56 cm (22 inches) of loess and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 11.1 degrees C (52 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA007IN" + ], + "ecoclassname": [ + "Till Depression Flatwood" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" + ] + } + }, + "id": { + "component": "Hennepin", + "name": "Hennepin2", + "rank_loc": "Not Displayed", + "score_loc": 0.225 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325325", + "componentKind": "Series", + "componentPct": 90, + "dataSource": "SSURGO", + "distance": 175.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162386", + "minCompDistance": 59.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", + "slope": 35.0, + "taxsubgrp": "Typic Eutrudepts", + "textureInfill": "No" + }, + "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA008IN" + ], + "ecoclassname": [ + "Wet Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" + ] + } + }, + "id": { + "component": "Hennepin", + "name": "Hennepin3", + "rank_loc": "Not Displayed", + "score_loc": 0.225 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325355", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 502.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162398", + "minCompDistance": 59.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", + "slope": 22.0, + "taxsubgrp": "Typic Eutrudepts", + "textureInfill": "No" + }, + "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Crosby", + "name": "Crosby2", + "rank_loc": "Not Displayed", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325351", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "SSURGO", + "distance": 85.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162397", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", + "slope": 1.0, + "taxsubgrp": "Aeric Epiaqualfs", + "textureInfill": "No" + }, + "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Crosby", + "name": "Crosby3", + "rank_loc": "Not Displayed", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325344", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 980.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162395", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", + "slope": 1.0, + "taxsubgrp": "Aeric Epiaqualfs", + "textureInfill": "No" + }, + "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Treaty", + "name": "Treaty2", + "rank_loc": "Not Displayed", + "score_loc": 0.031 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325401", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 59.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162415", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XA009IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + ] + } + }, + "id": { + "component": "Treaty", + "name": "Treaty3", + "rank_loc": "Not Displayed", + "score_loc": 0.031 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325403", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 193.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162416", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD010IN" + ], + "ecoclassname": [ + "Till Ridge" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + ] + } + }, + "id": { + "component": "Treaty", + "name": "Treaty4", + "rank_loc": "Not Displayed", + "score_loc": 0.031 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325343", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 980.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162395", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F111XD008IN" + ], + "ecoclassname": [ + "Till Depression Flatwood" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD008IN" + ] + } + }, + "id": { + "component": "Cyclone", + "name": "Cyclone2", + "rank_loc": "Not Displayed", + "score_loc": 0.026 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25325310", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "SSURGO", + "distance": 170.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "162380", + "minCompDistance": 59.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Miami", + "componentData": "Data Complete", + "componentID": 25325349, + "name": "Miami2", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.648, + "score_data_loc": 0.749, + "score_loc": 0.85 + }, + { + "component": "Williamstown", + "componentData": "Data Complete", + "componentID": 25325354, + "name": "Williamstown3", + "rank_data": "5", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.608, + "score_data_loc": 0.569, + "score_loc": 0.53 + }, + { + "component": "Hennepin", + "componentData": "Data Complete", + "componentID": 25325355, + "name": "Hennepin3", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": "Not Displayed", + "score_data": 0.634, + "score_data_loc": 0.43, + "score_loc": 0.225 + }, + { + "component": "Fincastle", + "componentData": "Data Complete", + "componentID": 25325308, + "name": "Fincastle", + "rank_data": "6", + "rank_data_loc": "4", + "rank_loc": "4", + "score_data": 0.505, + "score_data_loc": 0.361, + "score_loc": 0.218 + }, + { + "component": "Crosby", + "componentData": "Data Complete", + "componentID": 25325344, + "name": "Crosby3", + "rank_data": "4", + "rank_data_loc": "5", + "rank_loc": "Not Displayed", + "score_data": 0.619, + "score_data_loc": 0.354, + "score_loc": 0.09 + }, + { + "component": "Xenia", + "componentData": "Data Complete", + "componentID": 25325405, + "name": "Xenia", + "rank_data": "8", + "rank_data_loc": "6", + "rank_loc": "6", + "score_data": 0.482, + "score_data_loc": 0.347, + "score_loc": 0.212 + }, + { + "component": "Treaty", + "componentData": "Data Complete", + "componentID": 25325401, + "name": "Treaty2", + "rank_data": "1", + "rank_data_loc": "7", + "rank_loc": "Not Displayed", + "score_data": 0.66, + "score_data_loc": 0.345, + "score_loc": 0.031 + }, + { + "component": "Hickory", + "componentData": "Data Complete", + "componentID": 25325331, + "name": "Hickory", + "rank_data": "12", + "rank_data_loc": "8", + "rank_loc": "5", + "score_data": 0.403, + "score_data_loc": 0.31, + "score_loc": 0.217 + }, + { + "component": "Rainsville", + "componentData": "Data Complete", + "componentID": 25325345, + "name": "Rainsville", + "rank_data": "7", + "rank_data_loc": "9", + "rank_loc": "12", + "score_data": 0.502, + "score_data_loc": 0.258, + "score_loc": 0.013 + }, + { + "component": "Cyclone", + "componentData": "Data Complete", + "componentID": 25325310, + "name": "Cyclone2", + "rank_data": "9", + "rank_data_loc": "10", + "rank_loc": "Not Displayed", + "score_data": 0.472, + "score_data_loc": 0.249, + "score_loc": 0.026 + }, + { + "component": "Brookston", + "componentData": "Data Complete", + "componentID": 25325342, + "name": "Brookston", + "rank_data": "10", + "rank_data_loc": "11", + "rank_loc": "8", + "score_data": 0.439, + "score_data_loc": 0.239, + "score_loc": 0.04 + }, + { + "component": "Celina", + "componentData": "Data Complete", + "componentID": 25325406, + "name": "Celina", + "rank_data": "11", + "rank_data_loc": "12", + "rank_loc": "11", + "score_data": 0.424, + "score_data_loc": 0.218, + "score_loc": 0.013 + }, + { + "component": "Miami", + "componentData": "Data Complete", + "componentID": 25325352, + "name": "Miami5", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.593, + "score_data_loc": 0.721, + "score_loc": 0.85 + }, + { + "component": "Miami", + "componentData": "Data Complete", + "componentID": 25325346, + "name": "Miami6", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.572, + "score_data_loc": 0.711, + "score_loc": 0.85 + }, + { + "component": "Miami", + "componentData": "Data Complete", + "componentID": 25325339, + "name": "Miami1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.538, + "score_data_loc": 0.694, + "score_loc": 0.85 + }, + { + "component": "Miami", + "componentData": "Data Complete", + "componentID": 25325326, + "name": "Miami4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.509, + "score_data_loc": 0.68, + "score_loc": 0.85 + }, + { + "component": "Miami", + "componentData": "Data Complete", + "componentID": 25325350, + "name": "Miami3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.483, + "score_data_loc": 0.667, + "score_loc": 0.85 + }, + { + "component": "Williamstown", + "componentData": "Data Complete", + "componentID": 25325309, + "name": "Williamstown2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.548, + "score_data_loc": 0.539, + "score_loc": 0.53 + }, + { + "component": "Williamstown", + "componentData": "Data Complete", + "componentID": 25325400, + "name": "Williamstown1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "2", + "score_data": 0.513, + "score_data_loc": 0.521, + "score_loc": 0.53 + }, + { + "component": "Hennepin", + "componentData": "Data Complete", + "componentID": 25325325, + "name": "Hennepin2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.549, + "score_data_loc": 0.387, + "score_loc": 0.225 + }, + { + "component": "Crosby", + "componentData": "Data Complete", + "componentID": 25325351, + "name": "Crosby2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.597, + "score_data_loc": 0.344, + "score_loc": 0.09 + }, + { + "component": "Hennepin", + "componentData": "Data Complete", + "componentID": 25325347, + "name": "Hennepin1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "3", + "score_data": 0.449, + "score_data_loc": 0.337, + "score_loc": 0.225 + }, + { + "component": "Treaty", + "componentData": "Data Complete", + "componentID": 25325403, + "name": "Treaty3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.602, + "score_data_loc": 0.316, + "score_loc": 0.031 + }, + { + "component": "Crosby", + "componentData": "Data Complete", + "componentID": 25325341, + "name": "Crosby1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "7", + "score_data": 0.447, + "score_data_loc": 0.269, + "score_loc": 0.09 + }, + { + "component": "Treaty", + "componentData": "Data Complete", + "componentID": 25325343, + "name": "Treaty4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.501, + "score_data_loc": 0.266, + "score_loc": 0.031 + }, + { + "component": "Treaty", + "componentData": "Data Complete", + "componentID": 25325340, + "name": "Treaty1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "9", + "score_data": 0.439, + "score_data_loc": 0.235, + "score_loc": 0.031 + }, + { + "component": "Cyclone", + "componentData": "Data Complete", + "componentID": 25325348, + "name": "Cyclone1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "10", + "score_data": 0.428, + "score_data_loc": 0.227, + "score_loc": 0.026 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json new file mode 100644 index 0000000..246b0db --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json @@ -0,0 +1,998 @@ +{ + "list": { + "AWS_PIW90": 9.5, + "Soil Data Value": [ + [ + "rfv_class_0", + 1.382609666499055 + ], + [ + "rfv_class_30", + 1.3411411272079812 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ018CA" + ], + "ecoclassname": [ + "Moderately Deep Gravelly Mesic Mountains 40-60Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ018CA" + ] + } + }, + "id": { + "component": "Ruch", + "name": "Ruch", + "rank_loc": "1", + "score_loc": 0.8 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443415", + "componentKind": "Series", + "componentPct": 80, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "469633", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ruch", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ruch", + "slope": 14.0, + "taxsubgrp": "Mollic Palexeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Ruch series consists of very deep, well drained soils that formed in mixed alluvium. Ruch soils are on high stream terraces, alluvial fans and footslopes and have slopes of 2 to 60 percent. The mean annual precipitation is about 30 inches and the mean annual temperature is about 52 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ018CA" + ], + "ecoclassname": [ + "Moderately Deep Gravelly Mesic Mountains 40-60Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ018CA" + ] + } + }, + "id": { + "component": "Vannoy", + "name": "Vannoy1", + "rank_loc": "2", + "score_loc": 0.528 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443533", + "componentKind": "Series", + "componentPct": 80, + "dataSource": "SSURGO", + "distance": 52.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469685", + "minCompDistance": 52.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=vannoy", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#vannoy", + "slope": 24.0, + "taxsubgrp": "Mollic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Vannoy series consists of moderately deep, well drained soils that formed in colluvium weathered from metamorphic and sedimentary rocks. Vannoy soils are on uplands and have slopes of 2 to 60 percent. The mean annual precipitation is about 30 inches. The mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ003CA" + ], + "ecoclassname": [ + "Terraces" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA" + ] + } + }, + "id": { + "component": "Abegg", + "name": "Abegg", + "rank_loc": "3", + "score_loc": 0.207 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443548", + "componentKind": "Series", + "componentPct": 83, + "dataSource": "SSURGO", + "distance": 310.0, + "irrcapcl": "4", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "469691", + "minCompDistance": 310.0, + "nirrcapcl": "3", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abegg", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abegg", + "slope": 10.0, + "taxsubgrp": "Ultic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Abegg series consists of very deep, well drained soils that formed in alluvium and colluvium weathered from metamorphosed sedimentary and volcanic bedrock. Abegg soils are on stream terraces and alluvial fans and have slopes of 2 to 30 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 52 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ007CA" + ], + "ecoclassname": [ + "Moderately Deep Mesic Hills 40-60Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ007CA" + ] + } + }, + "id": { + "component": "Caris", + "name": "Caris", + "rank_loc": "4", + "score_loc": 0.15 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443598", + "componentKind": "Series", + "componentPct": 60, + "dataSource": "SSURGO", + "distance": 347.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469709", + "minCompDistance": 347.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=caris", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#caris", + "slope": 63.0, + "taxsubgrp": "Typic Xerochrepts", + "textureInfill": "No" + }, + "siteDescription": "The Caris series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Caris soils are on mountains and have slopes of 50 to 90 percent. The mean annual temperature is about 50 degrees F and the mean annual precipitation is about 32 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ024CA" + ], + "ecoclassname": [ + "Ridges" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ024CA" + ] + } + }, + "id": { + "component": "Beekman", + "name": "Beekman", + "rank_loc": "5", + "score_loc": 0.138 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443287", + "componentKind": "Series", + "componentPct": 55, + "dataSource": "SSURGO", + "distance": 497.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469583", + "minCompDistance": 497.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=beekman", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#beekman", + "slope": 65.0, + "taxsubgrp": "Dystric Xerochrepts", + "textureInfill": "No" + }, + "siteDescription": "The Beekman series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Beekman soils are on steep mountainous slopes ranging from 30 to 100 percent. The mean annual precipitation is about 50 inches and the mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ014CA" + ], + "ecoclassname": [ + "Mesic Mountains <40Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" + ] + } + }, + "id": { + "component": "Josephine", + "name": "Josephine1", + "rank_loc": "6", + "score_loc": 0.138 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443480", + "componentKind": "Series", + "componentPct": 40, + "dataSource": "SSURGO", + "distance": 712.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469660", + "minCompDistance": 712.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=josephine", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#josephine", + "slope": 45.0, + "taxsubgrp": "Typic Haploxerults", + "textureInfill": "No" + }, + "siteDescription": "The Josephine series consists of deep, well drained soils that formed in colluvium and residuum weathered from altered sedimentary and extrusive igneous rocks. Josephine soils are on broad ridgetops, toeslopes, footslopes, and side slopes of mountains. Slopes are 2 to 75 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ014CA" + ], + "ecoclassname": [ + "Mesic Mountains <40Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" + ] + } + }, + "id": { + "component": "Voorhies", + "name": "Voorhies", + "rank_loc": "7", + "score_loc": 0.135 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443535", + "componentKind": "Series", + "componentPct": 30, + "dataSource": "SSURGO", + "distance": 100.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469686", + "minCompDistance": 100.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=voorhies", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#voorhies", + "slope": 45.0, + "taxsubgrp": "Mollic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Voorhies series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Voorhies soils are on mountain slopes and have slopes of 35 to 55 percent. Mean annual precipitation is about 30 inches and mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ003CA" + ], + "ecoclassname": [ + "Terraces" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA" + ] + } + }, + "id": { + "component": "Speaker", + "name": "Speaker", + "rank_loc": "8", + "score_loc": 0.113 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443479", + "componentKind": "Series", + "componentPct": 45, + "dataSource": "SSURGO", + "distance": 712.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469660", + "minCompDistance": 712.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=speaker", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#speaker", + "slope": 45.0, + "taxsubgrp": "Ultic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Speaker series consists of moderately deep, well drained soils that formed in colluvium weathered from sedimentary and metamorphic rocks. Speaker soils are on low rolling foot slopes and side slopes and have gradients of 2 to 75 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ014CA" + ], + "ecoclassname": [ + "Mesic Mountains <40Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" + ] + } + }, + "id": { + "component": "Colestine", + "name": "Colestine", + "rank_loc": "9", + "score_loc": 0.075 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443286", + "componentKind": "Series", + "componentPct": 30, + "dataSource": "SSURGO", + "distance": 497.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469583", + "minCompDistance": 497.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=colestine", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#colestine", + "slope": 65.0, + "taxsubgrp": "Dystric Xerochrepts", + "textureInfill": "No" + }, + "siteDescription": "The Colestine series consists of moderately deep, well drained soils that formed in colluvium and residuum from altered sedimentary and extrusive igneous rocks. Colestine soils are on mountain slopes of 20 to 90 percent. The mean annual precipitation is about 50 inches and the mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ014CA" + ], + "ecoclassname": [ + "Mesic Mountains <40Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" + ] + } + }, + "id": { + "component": "Pollard", + "name": "Pollard", + "rank_loc": "10", + "score_loc": 0.075 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443850", + "componentKind": "Series", + "componentPct": 30, + "dataSource": "SSURGO", + "distance": 829.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469806", + "minCompDistance": 829.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=pollard", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#pollard", + "slope": 24.0, + "taxsubgrp": "Typic Haploxerults", + "textureInfill": "No" + }, + "siteDescription": "The Pollard series consists of very deep, well drained soils that formed in colluvium and residuum weathered from altered sedimentary and extrusive igneous rocks. Pollard soils are on hill slopes and toeslopes, foot slopes, saddles, ridges, and side slopes of mountains. Slopes are 2 to 60 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ024CA" + ], + "ecoclassname": [ + "Ridges" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ024CA" + ] + } + }, + "id": { + "component": "Offenbacher", + "name": "Offenbacher", + "rank_loc": "11", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443597", + "componentKind": "Series", + "componentPct": 20, + "dataSource": "SSURGO", + "distance": 347.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469709", + "minCompDistance": 347.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=offenbacher", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#offenbacher", + "slope": 63.0, + "taxsubgrp": "Typic Xerochrepts", + "textureInfill": "No" + }, + "siteDescription": "The Offenbacher series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Offenbacher soils are on mountains and have slopes of 50 to 80 percent. The mean annual temperature is about 47 degrees F, and the mean annual precipitation is about 32 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ009CA" + ], + "ecoclassname": [ + "Very Deep Mesic Hills 40-60Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ009CA" + ] + } + }, + "id": { + "component": "Gregory", + "name": "Gregory", + "rank_loc": "12", + "score_loc": 0.02 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443414", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "2", + "irrcapscl": "w", + "irrcapunit": "None", + "mapunitID": "469633", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gregory", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gregory", + "slope": 2.0, + "taxsubgrp": "Pachic Argixerolls", + "textureInfill": "No" + }, + "siteDescription": "The Gregory series consists of deep, poorly drained soils on terraces. They formed in recent alluvium dominantly from sedimentary and metamorphic rocks. Slopes are 0 to 3 percent. The mean annual precipitation is about 24 inches and the mean annual temperature is about 52 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R005XY016OR" + ], + "ecoclassname": [ + "Poorly Drained Bottom" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/R005XY016OR" + ] + } + }, + "id": { + "component": "Vannoy", + "name": "Vannoy2", + "rank_loc": "Not Displayed", + "score_loc": 0.528 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443534", + "componentKind": "Series", + "componentPct": 50, + "dataSource": "SSURGO", + "distance": 100.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469686", + "minCompDistance": 52.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=vannoy", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#vannoy", + "slope": 45.0, + "taxsubgrp": "Mollic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Vannoy series consists of moderately deep, well drained soils that formed in colluvium weathered from metamorphic and sedimentary rocks. Vannoy soils are on uplands and have slopes of 2 to 60 percent. The mean annual precipitation is about 30 inches. The mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F005XZ014CA" + ], + "ecoclassname": [ + "Mesic Mountains <40Ppt" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" + ] + } + }, + "id": { + "component": "Josephine", + "name": "Josephine2", + "rank_loc": "Not Displayed", + "score_loc": 0.138 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443848", + "componentKind": "Series", + "componentPct": 55, + "dataSource": "SSURGO", + "distance": 829.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "469806", + "minCompDistance": 712.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=josephine", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#josephine", + "slope": 24.0, + "taxsubgrp": "Typic Haploxerults", + "textureInfill": "No" + }, + "siteDescription": "The Josephine series consists of deep, well drained soils that formed in colluvium and residuum weathered from altered sedimentary and extrusive igneous rocks. Josephine soils are on broad ridgetops, toeslopes, footslopes, and side slopes of mountains. Slopes are 2 to 75 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Ruch", + "componentData": "Data Complete", + "componentID": 25443415, + "name": "Ruch", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": "1", + "score_data": 0.704, + "score_data_loc": 0.752, + "score_loc": 0.8 + }, + { + "component": "Vannoy", + "componentData": "Data Complete", + "componentID": 25443534, + "name": "Vannoy2", + "rank_data": "5", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.593, + "score_data_loc": 0.56, + "score_loc": 0.528 + }, + { + "component": "Abegg", + "componentData": "Data Complete", + "componentID": 25443548, + "name": "Abegg", + "rank_data": "4", + "rank_data_loc": "3", + "rank_loc": "3", + "score_data": 0.648, + "score_data_loc": 0.427, + "score_loc": 0.207 + }, + { + "component": "Josephine", + "componentData": "Data Complete", + "componentID": 25443848, + "name": "Josephine2", + "rank_data": "3", + "rank_data_loc": "4", + "rank_loc": "Not Displayed", + "score_data": 0.671, + "score_data_loc": 0.404, + "score_loc": 0.138 + }, + { + "component": "Gregory", + "componentData": "Data Complete", + "componentID": 25443414, + "name": "Gregory", + "rank_data": "1", + "rank_data_loc": "5", + "rank_loc": "12", + "score_data": 0.731, + "score_data_loc": 0.376, + "score_loc": 0.02 + }, + { + "component": "Pollard", + "componentData": "Data Complete", + "componentID": 25443850, + "name": "Pollard", + "rank_data": "6", + "rank_data_loc": "6", + "rank_loc": "10", + "score_data": 0.538, + "score_data_loc": 0.306, + "score_loc": 0.075 + }, + { + "component": "Voorhies", + "componentData": "Data Complete", + "componentID": 25443535, + "name": "Voorhies", + "rank_data": "8", + "rank_data_loc": "7", + "rank_loc": "7", + "score_data": 0.442, + "score_data_loc": 0.288, + "score_loc": 0.135 + }, + { + "component": "Beekman", + "componentData": "Data Complete", + "componentID": 25443287, + "name": "Beekman", + "rank_data": "9", + "rank_data_loc": "8", + "rank_loc": "5", + "score_data": 0.432, + "score_data_loc": 0.285, + "score_loc": 0.138 + }, + { + "component": "Speaker", + "componentData": "Data Complete", + "componentID": 25443479, + "name": "Speaker", + "rank_data": "10", + "rank_data_loc": "9", + "rank_loc": "8", + "score_data": 0.432, + "score_data_loc": 0.272, + "score_loc": 0.113 + }, + { + "component": "Offenbacher", + "componentData": "Data Complete", + "componentID": 25443597, + "name": "Offenbacher", + "rank_data": "7", + "rank_data_loc": "10", + "rank_loc": "11", + "score_data": 0.487, + "score_data_loc": 0.268, + "score_loc": 0.05 + }, + { + "component": "Caris", + "componentData": "Data Complete", + "componentID": 25443598, + "name": "Caris", + "rank_data": "12", + "rank_data_loc": "11", + "rank_loc": "4", + "score_data": 0.382, + "score_data_loc": 0.266, + "score_loc": 0.15 + }, + { + "component": "Colestine", + "componentData": "Data Complete", + "componentID": 25443286, + "name": "Colestine", + "rank_data": "11", + "rank_data_loc": "12", + "rank_loc": "9", + "score_data": 0.405, + "score_data_loc": 0.24, + "score_loc": 0.075 + }, + { + "component": "Vannoy", + "componentData": "Data Complete", + "componentID": 25443533, + "name": "Vannoy1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "2", + "score_data": 0.572, + "score_data_loc": 0.55, + "score_loc": 0.528 + }, + { + "component": "Josephine", + "componentData": "Data Complete", + "componentID": 25443480, + "name": "Josephine1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "6", + "score_data": 0.509, + "score_data_loc": 0.323, + "score_loc": 0.138 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json new file mode 100644 index 0000000..8239ca5 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json @@ -0,0 +1,522 @@ +{ + "list": { + "AWS_PIW90": 2.48, + "Soil Data Value": [ + [ + "rfv_class_0", + 0.17699904870697836 + ], + [ + "rfv_class_30", + 0.17494019898158308 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R103XY002MN" + ], + "ecoclassname": [ + "Calcareous Upland Prairies" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY002MN" + ] + } + }, + "id": { + "component": "Nicollet", + "name": "Nicollet", + "rank_loc": "1", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25584608", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 93.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "797923", + "minCompDistance": 93.0, + "nirrcapcl": "1", + "nirrcapscl": "None", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nicollet", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nicollet", + "slope": 2.0, + "taxsubgrp": "Aquic Hapludolls", + "textureInfill": "No" + }, + "siteDescription": "The Nicollet series consists of very deep, somewhat poorly drained soils that formed in calcareous loamy glacial till on till plains and moraines. Slopes range from 0 to 5 percent. Mean annual air temperature is about 9 degrees C (48 degrees F). Mean annual precipitation is about 660 mm (28 inches)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R103XY004MN" + ], + "ecoclassname": [ + "Loamy Upland Prairies" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY004MN" + ] + } + }, + "id": { + "component": "Webster", + "name": "Webster", + "rank_loc": "2", + "score_loc": 0.679 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25584606", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 93.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "797923", + "minCompDistance": 93.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=webster", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#webster", + "slope": 1.0, + "taxsubgrp": "Typic Endoaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Webster series consists of very deep, poorly drained, moderately permeable soils formed in glacial till or local alluvium derived from till on uplands. Slope ranges from 0 to 3 percent. Mean annual air temperature is about 48 degrees F, and mean annual precipitation is about 30 inches." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R103XY001MN" + ], + "ecoclassname": [ + "Loamy Wet Prairies" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY001MN" + ] + } + }, + "id": { + "component": "Clarion", + "name": "Clarion", + "rank_loc": "3", + "score_loc": 0.404 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25584604", + "componentKind": "Taxadjunct", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 93.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "797923", + "minCompDistance": 93.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clarion", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clarion", + "slope": 3.0, + "taxsubgrp": "Oxyaquic Hapludolls", + "textureInfill": "No" + }, + "siteDescription": "The Clarion series consists of very deep, moderately well drained soils on uplands. These soils formed in glacial till. Slopes range from 1 to 9 percent. Mean annual air temperature is about 8 degrees C (47 degrees F). Mean annual precipitation is about 74 centimeters (29 inches)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R103XY004MN" + ], + "ecoclassname": [ + "Loamy Upland Prairies" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY004MN" + ] + } + }, + "id": { + "component": "Okoboji", + "name": "Okoboji", + "rank_loc": "4", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25584952", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "797917", + "minCompDistance": 0.0, + "nirrcapcl": "3", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=okoboji", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#okoboji", + "slope": 0.0, + "taxsubgrp": "Cumulic Vertic Endoaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Okoboji series consists of very deep, very poorly drained soils formed in alluvium or lacustrine sediments. These soils are in closed depressions on till plains and moraines. Slope ranges from 0 to 1 percent. Mean annual air temperature is about 8 degrees C. Mean annual precipitation is about 740 millimeters." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R103XY015MN" + ], + "ecoclassname": [ + "Depressional Marsh" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY015MN" + ] + } + }, + "id": { + "component": "Glencoe", + "name": "Glencoe", + "rank_loc": "5", + "score_loc": 0.024 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25584960", + "componentKind": "Series", + "componentPct": 3, + "dataSource": "SSURGO", + "distance": 28.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "797921", + "minCompDistance": 28.0, + "nirrcapcl": "3", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=glencoe", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#glencoe", + "slope": 0.0, + "taxsubgrp": "Cumulic Endoaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Glencoe series consists of very deep, very poorly drained soils that formed in loamy sediments from till. These soils are in closed depressions on moraines. Slope ranges from 0 to 1 percent. Mean annual air temperature is about 8 degrees C. Mean annual precipitation is about 735 millimeters." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R103XY015MN" + ], + "ecoclassname": [ + "Depressional Marsh" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY015MN" + ] + } + }, + "id": { + "component": "Storden", + "name": "Storden", + "rank_loc": "6", + "score_loc": 0.024 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25584602", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 93.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "797923", + "minCompDistance": 93.0, + "nirrcapcl": "3", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=storden", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#storden", + "slope": 8.0, + "taxsubgrp": "Typic Eutrudepts", + "textureInfill": "No" + }, + "siteDescription": "The Storden series consists of very deep, well drained soils that formed in calcareous loamy glacial till on glacial moraines. Slope ranges from 4 to 70 percent. Mean annual precipitation is about 660 mm (26 inches). Mean annual air temperature is about 9 degrees C (48 degrees F)." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R103XY001MN" + ], + "ecoclassname": [ + "Loamy Wet Prairies" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/103X/R103XY001MN" + ] + } + }, + "id": { + "component": "Canisteo", + "name": "Canisteo", + "rank_loc": "7", + "score_loc": 0.016 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25584962", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 28.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "797921", + "minCompDistance": 28.0, + "nirrcapcl": "2", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=canisteo", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#canisteo", + "slope": 1.0, + "taxsubgrp": "Typic Endoaquolls", + "textureInfill": "No" + }, + "siteDescription": "The Canisteo series consists of very deep, poorly and very poorly drained soils that formed in calcareous, loamy till or in a thin mantle of loamy or silty sediments and the underlying calcareous, loamy till. These soils are on rims of depressions, depressions and flats on moraines or till plains. Slope ranges from 0 to 2 percent. Mean air annual temperature is about 9 degrees C. Mean annual precipitation is about 785 millimeters." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Nicollet", + "componentData": "Data Complete", + "componentID": 25584608, + "name": "Nicollet", + "rank_data": "5", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 0.344, + "score_data_loc": 0.597, + "score_loc": 0.85 + }, + { + "component": "Webster", + "componentData": "Data Complete", + "componentID": 25584606, + "name": "Webster", + "rank_data": "6", + "rank_data_loc": "2", + "rank_loc": 2, + "score_data": 0.268, + "score_data_loc": 0.473, + "score_loc": 0.679 + }, + { + "component": "Clarion", + "componentData": "Data Complete", + "componentID": 25584604, + "name": "Clarion", + "rank_data": "4", + "rank_data_loc": "3", + "rank_loc": 3, + "score_data": 0.365, + "score_data_loc": 0.385, + "score_loc": 0.404 + }, + { + "component": "Storden", + "componentData": "Data Complete", + "componentID": 25584602, + "name": "Storden", + "rank_data": "1", + "rank_data_loc": "4", + "rank_loc": 6, + "score_data": 0.458, + "score_data_loc": 0.241, + "score_loc": 0.024 + }, + { + "component": "Glencoe", + "componentData": "Data Complete", + "componentID": 25584960, + "name": "Glencoe", + "rank_data": "2", + "rank_data_loc": "5", + "rank_loc": 5, + "score_data": 0.436, + "score_data_loc": 0.23, + "score_loc": 0.024 + }, + { + "component": "Okoboji", + "componentData": "Missing Data", + "componentID": 25584952, + "name": "Okoboji", + "rank_data": "3", + "rank_data_loc": "6", + "rank_loc": 4, + "score_data": 0.402, + "score_data_loc": 0.226, + "score_loc": 0.05 + }, + { + "component": "Canisteo", + "componentData": "Data Complete", + "componentID": 25584962, + "name": "Canisteo", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": 7, + "score_data": 0.205, + "score_data_loc": 0.11, + "score_loc": 0.016 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json new file mode 100644 index 0000000..8b84e0b --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json @@ -0,0 +1,658 @@ +{ + "list": { + "AWS_PIW90": 11.64, + "Soil Data Value": [ + [ + "rfv_class_30", + 1.6951525379286227 + ], + [ + "rfv_class_0", + 1.3041643458994874 + ], + [ + "texture_30", + 0.35526589991601565 + ], + [ + "texture_0", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY212OR" + ], + "ecoclassname": [ + "Loamy 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR" + ] + } + }, + "id": { + "component": "Lonely", + "name": "Lonely", + "rank_loc": "1", + "score_loc": 0.5 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25442849", + "componentKind": "Series", + "componentPct": 50, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "490552", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonely", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonely", + "slope": 19.0, + "taxsubgrp": "Xeric Haplocambids", + "textureInfill": "No" + }, + "siteDescription": "The Lonely series consists of moderately deep, well drained soils that formed in colluvium overlying igneous bedrock. Lonely soils are on dissected rock pediments and mountain sideslopes and have slopes of 2 to 30 percent. The mean annual precipitation is about 10 inches and the mean annual temperature is about 43 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R024XY003OR" + ], + "ecoclassname": [ + "Sodic Bottom " + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/024X/R024XY003OR" + ] + } + }, + "id": { + "component": "Robson", + "name": "Robson", + "rank_loc": "2", + "score_loc": 0.35 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25442848", + "componentKind": "Series", + "componentPct": 35, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "490552", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=robson", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#robson", + "slope": 10.0, + "taxsubgrp": "Lithic Xeric Haplargids", + "textureInfill": "No" + }, + "siteDescription": "The Robson series consists of shallow, well drained soils that formed in residuum derived from igneous rock. Robson soils are on hill and mountain crests and side slopes. Slopes are 2 to 75 percent. The mean annual precipitation is about 380 mm and the mean annual temperature is about 6 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY212OR" + ], + "ecoclassname": [ + "Loamy 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR" + ] + } + }, + "id": { + "component": "Reallis", + "name": "Reallis", + "rank_loc": "3", + "score_loc": 0.212 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25442630", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 227.0, + "irrcapcl": "4", + "irrcapscl": "s", + "irrcapunit": "None", + "mapunitID": "490685", + "minCompDistance": 227.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=reallis", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#reallis", + "slope": 2.0, + "taxsubgrp": "Durinodic Xeric Haplocambids", + "textureInfill": "No" + }, + "siteDescription": "The Reallis series consists of very deep, well drained soils that formed in alluvium derived from volcanic rocks and minor amounts of eolian material. Reallis soils are on alluvial fans and lake terraces. Slopes are 0 to 8 percent. The mean annual precipitation is about 250 mm and the mean annual temperature is about 6 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY212OR" + ], + "ecoclassname": [ + "Loamy 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR" + ] + } + }, + "id": { + "component": "Rinconflat", + "name": "Rinconflat", + "rank_loc": "4", + "score_loc": 0.212 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25442616", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 717.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "490696", + "minCompDistance": 717.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rinconflat", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rinconflat", + "slope": 7.0, + "taxsubgrp": "Xeric Haplocambids", + "textureInfill": "No" + }, + "siteDescription": "The Rinconflat series consists of very deep, well drained soils that formed in alluvium derived from mixed volcanic rocks. Rinconflat soils are on alluvial fans and fan remnants. Slopes are 3 to 10 percent. The mean annual precipitation is about 280 mm and the mean annual temperature is about 7 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY212OR" + ], + "ecoclassname": [ + "Loamy 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR" + ] + } + }, + "id": { + "component": "Actem", + "name": "Actem", + "rank_loc": "5", + "score_loc": 0.212 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443068", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 858.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "490458", + "minCompDistance": 858.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=actem", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#actem", + "slope": 11.0, + "taxsubgrp": "Xeric Argidurids", + "textureInfill": "No" + }, + "siteDescription": "The Actem series consists of shallow to a duripan, well drained soils that formed in alluvium and colluvium derived from volcanic rocks. Actem soils are on hills and lava plateaus. Slopes are 2 to 20 percent. The mean annual precipitation is about 250 mm and the mean annual temperature is about 7 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY220OR" + ], + "ecoclassname": [ + "Clayey 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY220OR" + ] + } + }, + "id": { + "component": "Lonegrave", + "name": "Lonegrave", + "rank_loc": "6", + "score_loc": 0.163 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25443055", + "componentKind": "Series", + "componentPct": 65, + "dataSource": "SSURGO", + "distance": 546.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "490463", + "minCompDistance": 546.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonegrave", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonegrave", + "slope": 55.0, + "taxsubgrp": "Xeric Haplocambids", + "textureInfill": "No" + }, + "siteDescription": "The Lonegrave series consists of moderately deep, well drained soils that formed in colluvium derived from volcanic rocks. Lonegrave soils are on plateaus, hills, canyonlands, and mountains. Slopes are 5 to 70 percent. The mean annual precipitation is about 280 mm and the mean annual temperature is about 7 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY212OR" + ], + "ecoclassname": [ + "Loamy 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY212OR" + ] + } + }, + "id": { + "component": "Raz", + "name": "Raz", + "rank_loc": "7", + "score_loc": 0.125 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25442636", + "componentKind": "Series", + "componentPct": 50, + "dataSource": "SSURGO", + "distance": 878.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "490682", + "minCompDistance": 878.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=raz", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#raz", + "slope": 11.0, + "taxsubgrp": "Xeric Haplodurids", + "textureInfill": "No" + }, + "siteDescription": "The Raz series consists of shallow to a duripan, well drained soils that formed in slope alluvium, colluvium and residuum derived from basalt and tuff. Raz soils are on lava plateaus. Slopes are 1 to 20 percent. The mean annual precipitation is about 230 mm and the mean annual temperature is about 7 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY300OR" + ], + "ecoclassname": [ + "South Slopes 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY300OR" + ] + } + }, + "id": { + "component": "Brace", + "name": "Brace", + "rank_loc": "8", + "score_loc": 0.087 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25442637", + "componentKind": "Series", + "componentPct": 35, + "dataSource": "SSURGO", + "distance": 878.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "490682", + "minCompDistance": 878.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brace", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brace", + "slope": 11.0, + "taxsubgrp": "Xeric Argidurids", + "textureInfill": "No" + }, + "siteDescription": "The Brace series consists of moderately deep to a duripan, well drained soils that formed in slope alluvium, colluvium, and residuum derived from welded rhyolitic tuff and basalt. Brace soils are on structural benches, hills, and lava plateaus. Slopes are 1 to 20 percent. The mean annual precipitation is about 300 mm and the mean annual temperature is about 6 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R023XY220OR" + ], + "ecoclassname": [ + "Clayey 10-12 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/023X/R023XY220OR" + ] + } + }, + "id": { + "component": "Ausmus", + "name": "Ausmus", + "rank_loc": "9", + "score_loc": 0.01 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25442629", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "SSURGO", + "distance": 227.0, + "irrcapcl": "4", + "irrcapscl": "s", + "irrcapunit": "None", + "mapunitID": "490685", + "minCompDistance": 227.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ausmus", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ausmus", + "slope": 1.0, + "taxsubgrp": "Aquic Natrargids", + "textureInfill": "Yes" + }, + "siteDescription": "The Ausmus series consists of very deep, somewhat poorly drained or moderately well drained soils that formed in alluvium and lacustrine deposits derived from volcanic rocks and volcanic ash. Ausmus soils are on low lake terraces. Slopes are 0 to 2 percent. The mean annual precipitation is about 230 mm and the mean annual temperature is about 6.5 degrees C." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Lonely", + "componentData": "Data Complete", + "componentID": 25442849, + "name": "Lonely", + "rank_data": "6", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 0.63, + "score_data_loc": 0.565, + "score_loc": 0.5 + }, + { + "component": "Robson", + "componentData": "Data Complete", + "componentID": 25442848, + "name": "Robson", + "rank_data": "5", + "rank_data_loc": "2", + "rank_loc": 2, + "score_data": 0.646, + "score_data_loc": 0.498, + "score_loc": 0.35 + }, + { + "component": "Actem", + "componentData": "Data Complete", + "componentID": 25443068, + "name": "Actem", + "rank_data": "4", + "rank_data_loc": "3", + "rank_loc": 5, + "score_data": 0.657, + "score_data_loc": 0.435, + "score_loc": 0.212 + }, + { + "component": "Raz", + "componentData": "Data Complete", + "componentID": 25442636, + "name": "Raz", + "rank_data": "3", + "rank_data_loc": "4", + "rank_loc": 7, + "score_data": 0.723, + "score_data_loc": 0.424, + "score_loc": 0.125 + }, + { + "component": "Brace", + "componentData": "Data Complete", + "componentID": 25442637, + "name": "Brace", + "rank_data": "1", + "rank_data_loc": "5", + "rank_loc": 8, + "score_data": 0.756, + "score_data_loc": 0.421, + "score_loc": 0.087 + }, + { + "component": "Reallis", + "componentData": "Data Complete", + "componentID": 25442630, + "name": "Reallis", + "rank_data": "7", + "rank_data_loc": "6", + "rank_loc": 3, + "score_data": 0.588, + "score_data_loc": 0.4, + "score_loc": 0.212 + }, + { + "component": "Rinconflat", + "componentData": "Data Complete", + "componentID": 25442616, + "name": "Rinconflat", + "rank_data": "8", + "rank_data_loc": "7", + "rank_loc": 4, + "score_data": 0.587, + "score_data_loc": 0.4, + "score_loc": 0.212 + }, + { + "component": "Ausmus", + "componentData": "Data Complete", + "componentID": 25442629, + "name": "Ausmus", + "rank_data": "2", + "rank_data_loc": "8", + "rank_loc": 9, + "score_data": 0.746, + "score_data_loc": 0.378, + "score_loc": 0.01 + }, + { + "component": "Lonegrave", + "componentData": "Data Complete", + "componentID": 25443055, + "name": "Lonegrave", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": 6, + "score_data": 0.406, + "score_data_loc": 0.284, + "score_loc": 0.163 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.6508331,-121.5111084].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.6508331,-121.5111084].json new file mode 100644 index 0000000..d285c9a --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.6508331,-121.5111084].json @@ -0,0 +1,233 @@ +{ + "list": { + "AWS_PIW90": "Data not available", + "Soil Data Value": "Data not available", + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F006XA804OR" + ], + "ecoclassname": [ + "Mesic Xeric Maritime Foothills 30-50 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XA804OR" + ] + } + }, + "id": { + "component": "Hood", + "name": "Hood1", + "rank_loc": "1", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25279329", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "1", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "61998", + "minCompDistance": 0.0, + "nirrcapcl": "1", + "nirrcapscl": "None", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hood", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hood", + "slope": 2.0, + "taxsubgrp": "Ultic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Hood series consists of very deep, well drained soils formed in silty or loamy lacustrine deposits. Hood soils are on dissected terraces and terrace escarpments. Slopes are 0 to 65 percent. The mean annual precipitation is 38 inches and mean annual temperature is 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F006XA804OR" + ], + "ecoclassname": [ + "Mesic Xeric Maritime Foothills 30-50 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XA804OR" + ] + } + }, + "id": { + "component": "Hood", + "name": "Hood2", + "rank_loc": "Not Displayed", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25279333", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 52.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "62002", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hood", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hood", + "slope": 30.0, + "taxsubgrp": "Ultic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Hood series consists of very deep, well drained soils formed in silty or loamy lacustrine deposits. Hood soils are on dissected terraces and terrace escarpments. Slopes are 0 to 65 percent. The mean annual precipitation is 38 inches and mean annual temperature is 50 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F006XA804OR" + ], + "ecoclassname": [ + "Mesic Xeric Maritime Foothills 30-50 Pz" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XA804OR" + ] + } + }, + "id": { + "component": "Hood", + "name": "Hood3", + "rank_loc": "Not Displayed", + "score_loc": 0.85 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25279330", + "componentKind": "Series", + "componentPct": 85, + "dataSource": "SSURGO", + "distance": 82.0, + "irrcapcl": "2", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "61999", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hood", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hood", + "slope": 6.0, + "taxsubgrp": "Ultic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "The Hood series consists of very deep, well drained soils formed in silty or loamy lacustrine deposits. Hood soils are on dissected terraces and terrace escarpments. Slopes are 0 to 65 percent. The mean annual precipitation is 38 inches and mean annual temperature is 50 degrees F." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Hood", + "componentData": "Data Complete", + "componentID": 25279330, + "name": "Hood3", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.588, + "score_data_loc": 0.719, + "score_loc": 0.85 + }, + { + "component": "Hood", + "componentData": "Data Complete", + "componentID": 25279329, + "name": "Hood1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.556, + "score_data_loc": 0.703, + "score_loc": 0.85 + }, + { + "component": "Hood", + "componentData": "Data Complete", + "componentID": 25279333, + "name": "Hood2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.54, + "score_data_loc": 0.695, + "score_loc": 0.85 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json new file mode 100644 index 0000000..fdf0304 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json @@ -0,0 +1,165 @@ +{ + "list": { + "AWS_PIW90": "Data not available", + "Soil Data Value": "Data not available", + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F006XD004WA" + ], + "ecoclassname": [ + "Mesic Xeric Slopes And Plateaus (Oregon White Oak-Ponderosa Pine Hot Dry Herb/Shrub)" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XD004WA" + ] + } + }, + "id": { + "component": "Gunn", + "name": "Gunn1", + "rank_loc": "1", + "score_loc": 0.95 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25483307", + "componentKind": "Series", + "componentPct": 95, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "3", + "irrcapscl": "e", + "irrcapunit": "None", + "mapunitID": "76223", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gunn", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gunn", + "slope": 5.0, + "taxsubgrp": "Ultic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "Landscape--plateaus, hills\nLandform--structural benches, hillslopes, ridgetops\nSlope--0 to 65 percent\nParent material--loess mixed with colluvium and residuum derived from basalt\nMean annual precipitation--about 530 mm\nMean annual air temperature--about 9 degrees C\nDepth class--deep, very deep\nDrainage class--well drained\nSoil moisture regime--xeric\nSoil temperature regime--mesic\nSoil moisture subclass--typic" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F006XD004WA" + ], + "ecoclassname": [ + "Mesic Xeric Slopes And Plateaus (Oregon White Oak-Ponderosa Pine Hot Dry Herb/Shrub)" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/006X/F006XD004WA" + ] + } + }, + "id": { + "component": "Gunn", + "name": "Gunn2", + "rank_loc": "Not Displayed", + "score_loc": 0.95 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25483316", + "componentKind": "Series", + "componentPct": 90, + "dataSource": "SSURGO", + "distance": 42.0, + "irrcapcl": "nan", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "76225", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gunn", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gunn", + "slope": 19.0, + "taxsubgrp": "Ultic Haploxeralfs", + "textureInfill": "No" + }, + "siteDescription": "Landscape--plateaus, hills\nLandform--structural benches, hillslopes, ridgetops\nSlope--0 to 65 percent\nParent material--loess mixed with colluvium and residuum derived from basalt\nMean annual precipitation--about 530 mm\nMean annual air temperature--about 9 degrees C\nDepth class--deep, very deep\nDrainage class--well drained\nSoil moisture regime--xeric\nSoil temperature regime--mesic\nSoil moisture subclass--typic" + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Gunn", + "componentData": "Data Complete", + "componentID": 25483316, + "name": "Gunn2", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.443, + "score_data_loc": 0.697, + "score_loc": 0.95 + }, + { + "component": "Gunn", + "componentData": "Data Complete", + "componentID": 25483307, + "name": "Gunn1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.401, + "score_data_loc": 0.675, + "score_loc": 0.95 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json new file mode 100644 index 0000000..1e94264 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json @@ -0,0 +1,930 @@ +{ + "list": { + "AWS_PIW90": 10.09, + "Soil Data Value": [ + [ + "rfv_class_30", + 1.3277379187696259 + ], + [ + "rfv_class_0", + 1.0964549995974866 + ], + [ + "texture_30", + 0.9800953659873861 + ], + [ + "texture_0", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Knob lock", + "name": "Knob lock1", + "rank_loc": "1", + "score_loc": 0.46 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25208412", + "componentKind": "Series", + "componentPct": 46, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549870", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock", + "slope": 40.0, + "taxsubgrp": "Lithic Udifolists", + "textureInfill": "No" + }, + "siteDescription": "The Knob Lock series consists of very shallow and shallow, well drained through excessively drained organic soils on mountains and hills. They formed in thin organic deposits underlain in most places by a very thin mineral horizon over bedrock. Saturated hydraulic conductivity is moderately high through very high throughout the soil. Slope ranges from 3 through 80 percent. Mean annual precipitation is about 1092 mm and mean annual temperature is about 5 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Chesuncook", + "name": "Chesuncook1", + "rank_loc": "2", + "score_loc": 0.429 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209555", + "componentKind": "Series", + "componentPct": 50, + "dataSource": "SSURGO", + "distance": 19.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549860", + "minCompDistance": 19.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=chesuncook", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#chesuncook", + "slope": 20.0, + "taxsubgrp": "Aquic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Chesuncook series consists of very deep, moderately well drained soils on till plains, hills, ridges, and mountains. These soils formed in dense glacial till. Saturated hydraulic conductivity is moderately high or high in the solum, and low to moderately high in the dense substratum. Slope ranges from 3 to 45 percent. Mean annual temperature is about 4 degrees C, and mean annual precipitation is about 1092 mm at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Elliottsville", + "name": "Elliottsville1", + "rank_loc": "3", + "score_loc": 0.301 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209557", + "componentKind": "Series", + "componentPct": 35, + "dataSource": "SSURGO", + "distance": 19.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549860", + "minCompDistance": 19.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville", + "slope": 25.0, + "taxsubgrp": "Typic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Elliottsville series consists of moderately deep, well drained soils formed in glacial till on till plains, hills, ridges and mountains. Permeability is moderate. Slope ranges from 3 to 65 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 970 mm at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Monson", + "name": "Monson1", + "rank_loc": "4", + "score_loc": 0.1 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209554", + "componentKind": "Series", + "componentPct": 6, + "dataSource": "SSURGO", + "distance": 19.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549860", + "minCompDistance": 19.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson", + "slope": 25.0, + "taxsubgrp": "Lithic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Monson series consists of shallow, somewhat excessively drained soils formed in glacial till on knolls of till plains, and on hills, ridges and mountains. Estimated saturated hydraulic conductivity is moderate or high. Slope ranges from 3 to 60 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 965 mm at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Hogback", + "name": "Hogback", + "rank_loc": "5", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25208410", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549870", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hogback", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hogback", + "slope": 50.0, + "taxsubgrp": "Lithic Haplohumods", + "textureInfill": "No" + }, + "siteDescription": "The Hogback series consists of shallow, well drained soils on glaciated uplands. They formed in loamy till. Estimated saturated hydraulic conductivity is moderately high to high throughout the mineral soil. Slope ranges from 3 to 70 percent. Mean annual precipitation is about 50 inches, and mean annual temperature is about 43 degrees F." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F143XY704ME" + ], + "ecoclassname": [ + "Shallow Organic Rock Pocket" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY704ME" + ] + } + }, + "id": { + "component": "Rawsonville", + "name": "Rawsonville", + "rank_loc": "6", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25208409", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549870", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rawsonville", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rawsonville", + "slope": 20.0, + "taxsubgrp": "Typic Haplohumods", + "textureInfill": "No" + }, + "siteDescription": "The Rawsonville series consists of moderately deep, well drained soils on glaciated uplands. They formed in loamy till. Estimated saturated hydraulic conductivity is moderately high or high in the mineral soil. Slope ranges from 3 to 70 percent. Mean annual precipitation is about 1,270 mm, and mean annual temperature is about 6 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F143XY702ME" + ], + "ecoclassname": [ + "Shallow And Moderately Deep Till" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY702ME" + ] + } + }, + "id": { + "component": "Abram", + "name": "Abram1", + "rank_loc": "7", + "score_loc": 0.034 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209553", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "SSURGO", + "distance": 19.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549860", + "minCompDistance": 19.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram", + "slope": 30.0, + "taxsubgrp": "Lithic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Abram series consists of very shallow, excessively drained soils formed in a thin mantle of glacial till on ridges and mountains. Permeability is moderately rapid. Slope ranges from 0 to 80 percent. Mean annual temperature is about 7 degrees C, and mean annual precipitation is about 1118 mm at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Knob lock", + "name": "Knob lock2", + "rank_loc": "Not Displayed", + "score_loc": 0.46 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209556", + "componentKind": "Series", + "componentPct": 2, + "dataSource": "SSURGO", + "distance": 19.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549860", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock", + "slope": 30.0, + "taxsubgrp": "Lithic Udifolists", + "textureInfill": "No" + }, + "siteDescription": "The Knob Lock series consists of very shallow and shallow, well drained through excessively drained organic soils on mountains and hills. They formed in thin organic deposits underlain in most places by a very thin mineral horizon over bedrock. Saturated hydraulic conductivity is moderately high through very high throughout the soil. Slope ranges from 3 through 80 percent. Mean annual precipitation is about 1092 mm and mean annual temperature is about 5 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F143XY704ME" + ], + "ecoclassname": [ + "Shallow Organic Rock Pocket" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY704ME" + ] + } + }, + "id": { + "component": "Knob lock", + "name": "Knob lock3", + "rank_loc": "Not Displayed", + "score_loc": 0.46 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209692", + "componentKind": "Series", + "componentPct": 25, + "dataSource": "SSURGO", + "distance": 192.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549867", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock", + "slope": 50.0, + "taxsubgrp": "Lithic Udifolists", + "textureInfill": "No" + }, + "siteDescription": "The Knob Lock series consists of very shallow and shallow, well drained through excessively drained organic soils on mountains and hills. They formed in thin organic deposits underlain in most places by a very thin mineral horizon over bedrock. Saturated hydraulic conductivity is moderately high through very high throughout the soil. Slope ranges from 3 through 80 percent. Mean annual precipitation is about 1092 mm and mean annual temperature is about 5 degrees C." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "" + ], + "ecoclassname": [ + "" + ], + "edit_url": [ + "" + ] + } + }, + "id": { + "component": "Chesuncook", + "name": "Chesuncook2", + "rank_loc": "Not Displayed", + "score_loc": 0.429 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209552", + "componentKind": "Series", + "componentPct": 3, + "dataSource": "SSURGO", + "distance": 19.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549860", + "minCompDistance": 19.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=chesuncook", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#chesuncook", + "slope": 12.0, + "taxsubgrp": "Aquic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Chesuncook series consists of very deep, moderately well drained soils on till plains, hills, ridges, and mountains. These soils formed in dense glacial till. Saturated hydraulic conductivity is moderately high or high in the solum, and low to moderately high in the dense substratum. Slope ranges from 3 to 45 percent. Mean annual temperature is about 4 degrees C, and mean annual precipitation is about 1092 mm at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F143XY501ME" + ], + "ecoclassname": [ + "Loamy Slope" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY501ME" + ] + } + }, + "id": { + "component": "Elliottsville", + "name": "Elliottsville2", + "rank_loc": "Not Displayed", + "score_loc": 0.301 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209694", + "componentKind": "Series", + "componentPct": 20, + "dataSource": "SSURGO", + "distance": 192.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549867", + "minCompDistance": 19.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville", + "slope": 40.0, + "taxsubgrp": "Typic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Elliottsville series consists of moderately deep, well drained soils formed in glacial till on till plains, hills, ridges and mountains. Permeability is moderate. Slope ranges from 3 to 65 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 970 mm at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F143XY501ME" + ], + "ecoclassname": [ + "Loamy Slope" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY501ME" + ] + } + }, + "id": { + "component": "Monson", + "name": "Monson2", + "rank_loc": "Not Displayed", + "score_loc": 0.1 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209693", + "componentKind": "Series", + "componentPct": 40, + "dataSource": "SSURGO", + "distance": 192.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549867", + "minCompDistance": 19.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson", + "slope": 40.0, + "taxsubgrp": "Lithic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Monson series consists of shallow, somewhat excessively drained soils formed in glacial till on knolls of till plains, and on hills, ridges and mountains. Estimated saturated hydraulic conductivity is moderate or high. Slope ranges from 3 to 60 percent. Mean annual temperature is about 3 degrees C, and mean annual precipitation is about 965 mm at the type location." + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F143XY702ME" + ], + "ecoclassname": [ + "Shallow And Moderately Deep Till" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/143X/F143XY702ME" + ] + } + }, + "id": { + "component": "Abram", + "name": "Abram2", + "rank_loc": "Not Displayed", + "score_loc": 0.034 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "25209690", + "componentKind": "Series", + "componentPct": 10, + "dataSource": "SSURGO", + "distance": 192.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2549867", + "minCompDistance": 19.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram", + "slope": 45.0, + "taxsubgrp": "Lithic Haplorthods", + "textureInfill": "No" + }, + "siteDescription": "The Abram series consists of very shallow, excessively drained soils formed in a thin mantle of glacial till on ridges and mountains. Permeability is moderately rapid. Slope ranges from 0 to 80 percent. Mean annual temperature is about 7 degrees C, and mean annual precipitation is about 1118 mm at the type location." + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Chesuncook", + "componentData": "Data Complete", + "componentID": 25209555, + "name": "Chesuncook1", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "2", + "score_data": 0.725, + "score_data_loc": 0.577, + "score_loc": 0.429 + }, + { + "component": "Knob lock", + "componentData": "Data Complete", + "componentID": 25209556, + "name": "Knob lock2", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.645, + "score_data_loc": 0.553, + "score_loc": 0.46 + }, + { + "component": "Elliottsville", + "componentData": "Data Complete", + "componentID": 25209557, + "name": "Elliottsville1", + "rank_data": "2", + "rank_data_loc": "3", + "rank_loc": "3", + "score_data": 0.685, + "score_data_loc": 0.493, + "score_loc": 0.301 + }, + { + "component": "Monson", + "componentData": "Data Complete", + "componentID": 25209554, + "name": "Monson1", + "rank_data": "3", + "rank_data_loc": "4", + "rank_loc": "4", + "score_data": 0.648, + "score_data_loc": 0.374, + "score_loc": 0.1 + }, + { + "component": "Rawsonville", + "componentData": "Data Complete", + "componentID": 25208409, + "name": "Rawsonville", + "rank_data": "6", + "rank_data_loc": "5", + "rank_loc": "6", + "score_data": 0.624, + "score_data_loc": 0.337, + "score_loc": 0.05 + }, + { + "component": "Abram", + "componentData": "Data Complete", + "componentID": 25209553, + "name": "Abram1", + "rank_data": "5", + "rank_data_loc": "6", + "rank_loc": "7", + "score_data": 0.631, + "score_data_loc": 0.332, + "score_loc": 0.034 + }, + { + "component": "Hogback", + "componentData": "Data Complete", + "componentID": 25208410, + "name": "Hogback", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": "5", + "score_data": 0.486, + "score_data_loc": 0.268, + "score_loc": 0.05 + }, + { + "component": "Chesuncook", + "componentData": "Data Complete", + "componentID": 25209552, + "name": "Chesuncook2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.692, + "score_data_loc": 0.561, + "score_loc": 0.429 + }, + { + "component": "Knob lock", + "componentData": "Data Complete", + "componentID": 25208412, + "name": "Knob lock1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "1", + "score_data": 0.584, + "score_data_loc": 0.522, + "score_loc": 0.46 + }, + { + "component": "Knob lock", + "componentData": "Data Complete", + "componentID": 25209692, + "name": "Knob lock3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.529, + "score_data_loc": 0.494, + "score_loc": 0.46 + }, + { + "component": "Elliottsville", + "componentData": "Data Complete", + "componentID": 25209694, + "name": "Elliottsville2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.434, + "score_data_loc": 0.367, + "score_loc": 0.301 + }, + { + "component": "Monson", + "componentData": "Data Complete", + "componentID": 25209693, + "name": "Monson2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.603, + "score_data_loc": 0.351, + "score_loc": 0.1 + }, + { + "component": "Abram", + "componentData": "Data Complete", + "componentID": 25209690, + "name": "Abram2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.571, + "score_data_loc": 0.302, + "score_loc": 0.034 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json new file mode 100644 index 0000000..28f661a --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json @@ -0,0 +1,1162 @@ +{ + "list": { + "AWS_PIW90": 5.71, + "Soil Data Value": [ + [ + "rfv_class_0", + 0.976020648236615 + ], + [ + "rfv_class_30", + 0.976020648236615 + ], + [ + "texture_0", + 0.0 + ], + [ + "texture_30", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Andic cryumbrepts", + "name": "Andic cryumbrepts", + "rank_loc": "1", + "score_loc": 0.152 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14269504", + "componentKind": "Taxon above family", + "componentPct": 20, + "dataSource": "STATSGO", + "distance": 994.2109898924772, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "676031", + "minCompDistance": 994.2109898924772, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 53.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Nimue", + "name": "Nimue1", + "rank_loc": "2", + "score_loc": 0.13 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268942", + "componentKind": "Series", + "componentPct": 13, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 48.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Cryorthods", + "name": "Cryorthods", + "rank_loc": "3", + "score_loc": 0.114 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14269505", + "componentKind": "Taxon above family", + "componentPct": 15, + "dataSource": "STATSGO", + "distance": 994.2109898924772, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "676031", + "minCompDistance": 994.2109898924772, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 60.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Playco", + "name": "Playco1", + "rank_loc": "4", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268933", + "componentKind": "Series", + "componentPct": 9, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 48.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Cryumbrepts", + "name": "Cryumbrepts", + "rank_loc": "5", + "score_loc": 0.076 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14269506", + "componentKind": "Taxon above family", + "componentPct": 10, + "dataSource": "STATSGO", + "distance": 994.2109898924772, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "676031", + "minCompDistance": 994.2109898924772, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 60.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Getchell", + "name": "Getchell1", + "rank_loc": "6", + "score_loc": 0.06 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268946", + "componentKind": "Series", + "componentPct": 6, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 48.0, + "taxsubgrp": "Aquic Haplocryands", + "textureInfill": "Yes" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Oso", + "name": "Oso", + "rank_loc": "7", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268939", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 78.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "Yes" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Wollard", + "name": "Wollard", + "rank_loc": "8", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268937", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 48.0, + "taxsubgrp": "Alic Haplocryands", + "textureInfill": "Yes" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Diobsud", + "name": "Diobsud", + "rank_loc": "9", + "score_loc": 0.04 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268932", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 48.0, + "taxsubgrp": "Andic Humicryods", + "textureInfill": "Yes" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Shuksan", + "name": "Shuksan", + "rank_loc": "10", + "score_loc": 0.04 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268938", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 45.0, + "taxsubgrp": "Andic Humicryods", + "textureInfill": "Yes" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Cryaquepts", + "name": "Cryaquepts", + "rank_loc": "11", + "score_loc": 0.038 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14269507", + "componentKind": "Taxon above family", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 994.2109898924772, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "676031", + "minCompDistance": 994.2109898924772, + "nirrcapcl": "7", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 2.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Cryohumods", + "name": "Cryohumods", + "rank_loc": "12", + "score_loc": 0.038 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14269509", + "componentKind": "Taxon above family", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 994.2109898924772, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "676031", + "minCompDistance": 994.2109898924772, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 60.0, + "taxsubgrp": "None", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Nimue", + "name": "Nimue2", + "rank_loc": "Not Displayed", + "score_loc": 0.13 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268930", + "componentKind": "Series", + "componentPct": 7, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 45.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Nimue", + "name": "Nimue3", + "rank_loc": "Not Displayed", + "score_loc": 0.13 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268934", + "componentKind": "Series", + "componentPct": 3, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 19.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Playco", + "name": "Playco2", + "rank_loc": "Not Displayed", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268941", + "componentKind": "Series", + "componentPct": 7, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 48.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Playco", + "name": "Playco3", + "rank_loc": "Not Displayed", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268940", + "componentKind": "Series", + "componentPct": 4, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 19.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Playco", + "name": "Playco4", + "rank_loc": "Not Displayed", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268936", + "componentKind": "Series", + "componentPct": 3, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 19.0, + "taxsubgrp": "Andic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "Getchell", + "name": "Getchell2", + "rank_loc": "Not Displayed", + "score_loc": 0.06 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "14268944", + "componentKind": "Series", + "componentPct": 5, + "dataSource": "STATSGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "675975", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 17.0, + "taxsubgrp": "Aquic Haplocryands", + "textureInfill": "Yes" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Playco", + "componentData": "Missing Data", + "componentID": 14268936, + "name": "Playco4", + "rank_data": "1", + "rank_data_loc": "1", + "rank_loc": "Not Displayed", + "score_data": 0.776, + "score_data_loc": 0.433, + "score_loc": 0.09 + }, + { + "component": "Nimue", + "componentData": "Missing Data", + "componentID": 14268942, + "name": "Nimue1", + "rank_data": "5", + "rank_data_loc": "2", + "rank_loc": "2", + "score_data": 0.578, + "score_data_loc": 0.354, + "score_loc": 0.13 + }, + { + "component": "Shuksan", + "componentData": "Missing Data", + "componentID": 14268938, + "name": "Shuksan", + "rank_data": "2", + "rank_data_loc": "3", + "rank_loc": "10", + "score_data": 0.663, + "score_data_loc": 0.351, + "score_loc": 0.04 + }, + { + "component": "Getchell", + "componentData": "Missing Data", + "componentID": 14268946, + "name": "Getchell1", + "rank_data": "3", + "rank_data_loc": "4", + "rank_loc": "6", + "score_data": 0.606, + "score_data_loc": 0.333, + "score_loc": 0.06 + }, + { + "component": "Cryorthods", + "componentData": "Missing Data", + "componentID": 14269505, + "name": "Cryorthods", + "rank_data": "7", + "rank_data_loc": "5", + "rank_loc": "3", + "score_data": 0.543, + "score_data_loc": 0.329, + "score_loc": 0.114 + }, + { + "component": "Diobsud", + "componentData": "Missing Data", + "componentID": 14268932, + "name": "Diobsud", + "rank_data": "4", + "rank_data_loc": "6", + "rank_loc": "9", + "score_data": 0.606, + "score_data_loc": 0.323, + "score_loc": 0.04 + }, + { + "component": "Wollard", + "componentData": "Missing Data", + "componentID": 14268937, + "name": "Wollard", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": "8", + "score_data": 0.56, + "score_data_loc": 0.305, + "score_loc": 0.05 + }, + { + "component": "Oso", + "componentData": "Missing Data", + "componentID": 14268939, + "name": "Oso", + "rank_data": "9", + "rank_data_loc": "8", + "rank_loc": "7", + "score_data": 0.463, + "score_data_loc": 0.256, + "score_loc": 0.05 + }, + { + "component": "Cryaquepts", + "componentData": "Missing Data", + "componentID": 14269507, + "name": "Cryaquepts", + "rank_data": "8", + "rank_data_loc": "9", + "rank_loc": "11", + "score_data": 0.473, + "score_data_loc": 0.255, + "score_loc": 0.038 + }, + { + "component": "Andic cryumbrepts", + "componentData": "Missing Data", + "componentID": 14269504, + "name": "Andic cryumbrepts", + "rank_data": "12", + "rank_data_loc": "10", + "rank_loc": "1", + "score_data": 0.333, + "score_data_loc": 0.242, + "score_loc": 0.152 + }, + { + "component": "Cryumbrepts", + "componentData": "Missing Data", + "componentID": 14269506, + "name": "Cryumbrepts", + "rank_data": "10", + "rank_data_loc": "11", + "rank_loc": "5", + "score_data": 0.379, + "score_data_loc": 0.228, + "score_loc": 0.076 + }, + { + "component": "Cryohumods", + "componentData": "Missing Data", + "componentID": 14269509, + "name": "Cryohumods", + "rank_data": "11", + "rank_data_loc": "12", + "rank_loc": "12", + "score_data": 0.379, + "score_data_loc": 0.209, + "score_loc": 0.038 + }, + { + "component": "Playco", + "componentData": "Missing Data", + "componentID": 14268933, + "name": "Playco1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "4", + "score_data": 0.614, + "score_data_loc": 0.352, + "score_loc": 0.09 + }, + { + "component": "Nimue", + "componentData": "Missing Data", + "componentID": 14268934, + "name": "Nimue3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.48, + "score_data_loc": 0.305, + "score_loc": 0.13 + }, + { + "component": "Playco", + "componentData": "Missing Data", + "componentID": 14268940, + "name": "Playco3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.516, + "score_data_loc": 0.303, + "score_loc": 0.09 + }, + { + "component": "Getchell", + "componentData": "Missing Data", + "componentID": 14268944, + "name": "Getchell2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.505, + "score_data_loc": 0.283, + "score_loc": 0.06 + }, + { + "component": "Nimue", + "componentData": "Missing Data", + "componentID": 14268930, + "name": "Nimue2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.404, + "score_data_loc": 0.267, + "score_loc": 0.13 + }, + { + "component": "Playco", + "componentData": "Missing Data", + "componentID": 14268941, + "name": "Playco2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.431, + "score_data_loc": 0.26, + "score_loc": 0.09 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json new file mode 100644 index 0000000..1e84820 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json @@ -0,0 +1,454 @@ +{ + "list": { + "AWS_PIW90": 7.59, + "Soil Data Value": [ + [ + "rfv_class_30", + 1.3417496839612755 + ], + [ + "texture_30", + 0.4820661480830928 + ], + [ + "rfv_class_0", + 0.2164794609217049 + ], + [ + "texture_0", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R236XY109AK" + ], + "ecoclassname": [ + "Subarctic Low Scrub Peat Drainages" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/236X/R236XY109AK" + ] + } + }, + "id": { + "component": "D36-western maritime tussock scrub loamy eolian slopes", + "name": "D36-western maritime tussock scrub loamy eolian slopes", + "rank_loc": "1", + "score_loc": 0.24 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26176414", + "componentKind": "Taxon above family", + "componentPct": 24, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2661500", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 2.0, + "taxsubgrp": "Histic Gelaquepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R236XY107AK" + ], + "ecoclassname": [ + "Western Alaska Maritime Scrub Gravelly Drainages" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/236X/R236XY107AK" + ] + } + }, + "id": { + "component": "D36-western maritime dwarf scrub loamy glaciated slopes", + "name": "D36-western maritime dwarf scrub loamy glaciated slopes", + "rank_loc": "2", + "score_loc": 0.23 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26176416", + "componentKind": "Taxon above family", + "componentPct": 23, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2661500", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 6.0, + "taxsubgrp": "Typic Dystrocryepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R236XY140AK" + ], + "ecoclassname": [ + "Subarctic Tussock Tundra Wet Loamy Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/236X/R236XY140AK" + ] + } + }, + "id": { + "component": "D36-western maritime sedge organic depressions", + "name": "D36-western maritime sedge organic depressions", + "rank_loc": "3", + "score_loc": 0.2 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26176412", + "componentKind": "Taxon above family", + "componentPct": 20, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2661500", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 0.0, + "taxsubgrp": "Terric Cryohemists", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "F236XY139AK" + ], + "ecoclassname": [ + "Boreal Woodland Loamy Rises" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/236X/F236XY139AK" + ] + } + }, + "id": { + "component": "D36-western maritime scrub organic peat mounds", + "name": "D36-western maritime scrub organic peat mounds", + "rank_loc": "4", + "score_loc": 0.17 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26176417", + "componentKind": "Taxon above family", + "componentPct": 17, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2661500", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 4.0, + "taxsubgrp": "Folistic Umbriturbels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R236XY132AK" + ], + "ecoclassname": [ + "Subarctic Dwarf Scrub Dry Loamy Slopes" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/236X/R236XY132AK" + ] + } + }, + "id": { + "component": "D36-boreal forest loamy eolian slopes", + "name": "D36-boreal forest loamy eolian slopes", + "rank_loc": "5", + "score_loc": 0.1 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26176415", + "componentKind": "Taxon above family", + "componentPct": 10, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2661500", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 3.0, + "taxsubgrp": "Typic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": [ + "R236XY131AK" + ], + "ecoclassname": [ + "Subarctic Tussock-Scrub Frozen Plains" + ], + "edit_url": [ + "https://edit.jornada.nmsu.edu/catalogs/esd/236X/R236XY131AK" + ] + } + }, + "id": { + "component": "D36-western maritime scrub drainageways", + "name": "D36-western maritime scrub drainageways", + "rank_loc": "6", + "score_loc": 0.01 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "26176413", + "componentKind": "Taxon above family", + "componentPct": 1, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "2661500", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 3.0, + "taxsubgrp": "Oxyaquic Humicryepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "D36-western maritime tussock scrub loamy eolian slopes", + "componentData": "Missing Data", + "componentID": 26176414, + "name": "D36-western maritime tussock scrub loamy eolian slopes", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 0.48, + "score_data_loc": 0.36, + "score_loc": 0.24 + }, + { + "component": "D36-western maritime sedge organic depressions", + "componentData": "Missing Data", + "componentID": 26176412, + "name": "D36-western maritime sedge organic depressions", + "rank_data": "3", + "rank_data_loc": "2", + "rank_loc": 3, + "score_data": 0.45, + "score_data_loc": 0.325, + "score_loc": 0.2 + }, + { + "component": "D36-boreal forest loamy eolian slopes", + "componentData": "Missing Data", + "componentID": 26176415, + "name": "D36-boreal forest loamy eolian slopes", + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": 5, + "score_data": 0.522, + "score_data_loc": 0.311, + "score_loc": 0.1 + }, + { + "component": "D36-western maritime dwarf scrub loamy glaciated slopes", + "componentData": "Missing Data", + "componentID": 26176416, + "name": "D36-western maritime dwarf scrub loamy glaciated slopes", + "rank_data": "5", + "rank_data_loc": "4", + "rank_loc": 2, + "score_data": 0.377, + "score_data_loc": 0.303, + "score_loc": 0.23 + }, + { + "component": "D36-western maritime scrub organic peat mounds", + "componentData": "Missing Data", + "componentID": 26176417, + "name": "D36-western maritime scrub organic peat mounds", + "rank_data": "4", + "rank_data_loc": "5", + "rank_loc": 4, + "score_data": 0.421, + "score_data_loc": 0.295, + "score_loc": 0.17 + }, + { + "component": "D36-western maritime scrub drainageways", + "componentData": "Missing Data", + "componentID": 26176413, + "name": "D36-western maritime scrub drainageways", + "rank_data": "6", + "rank_data_loc": "6", + "rank_loc": 6, + "score_data": 0.376, + "score_data_loc": 0.193, + "score_loc": 0.01 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json new file mode 100644 index 0000000..4bb5ec3 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json @@ -0,0 +1,604 @@ +{ + "list": { + "AWS_PIW90": 12.07, + "Soil Data Value": [ + [ + "rfv_class_0", + 1.7621306108711137 + ], + [ + "rfv_class_30", + 1.6416647689252122 + ], + [ + "texture_30", + 0.9858150371789198 + ], + [ + "texture_0", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal forest-silty slopes", + "name": "E30-boreal forest-silty slopes", + "rank_loc": "1", + "score_loc": 0.3 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913863", + "componentKind": "Taxon above family", + "componentPct": 30, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 18.0, + "taxsubgrp": "Typic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal alpine scrub-gravelly colluvial slopes", + "name": "E30-boreal alpine scrub-gravelly colluvial slopes", + "rank_loc": "2", + "score_loc": 0.29 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913856", + "componentKind": "Taxon above family", + "componentPct": 29, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 25.0, + "taxsubgrp": "Typic Haplogelepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga-loamy frozen colluvial slopes", + "name": "E30-boreal taiga-loamy frozen colluvial slopes", + "rank_loc": "3", + "score_loc": 0.13 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913864", + "componentKind": "Taxon above family", + "componentPct": 13, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 14.0, + "taxsubgrp": "Typic Histoturbels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga-silty slopes", + "name": "E30-boreal taiga-silty slopes", + "rank_loc": "4", + "score_loc": 0.07 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913862", + "componentKind": "Taxon above family", + "componentPct": 7, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 15.0, + "taxsubgrp": "Typic Dystrocryepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga/tussock-silty frozen slopes", + "name": "E30-boreal taiga/tussock-silty frozen slopes", + "rank_loc": "5", + "score_loc": 0.06 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913861", + "componentKind": "Taxon above family", + "componentPct": 6, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 2.0, + "taxsubgrp": "Typic Histoturbels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal subalpine scrub-loamy colluvial slopes", + "name": "E30-boreal subalpine scrub-loamy colluvial slopes", + "rank_loc": "6", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913860", + "componentKind": "Taxon above family", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 14.0, + "taxsubgrp": "Typic Dystrocryepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal scrub-silty frozen drainageways", + "name": "E30-boreal scrub-silty frozen drainageways", + "rank_loc": "7", + "score_loc": 0.04 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913859", + "componentKind": "Taxon above family", + "componentPct": 4, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Fluvaquentic Historthels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal alpine dwarf scrub-gravelly colluvial slopes", + "name": "E30-boreal alpine dwarf scrub-gravelly colluvial slopes", + "rank_loc": "8", + "score_loc": 0.03 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913857", + "componentKind": "Taxon above family", + "componentPct": 3, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 35.0, + "taxsubgrp": "Typic Haplogelepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal subalpine woodland-gravelly colluvial slopes", + "name": "E30-boreal subalpine woodland-gravelly colluvial slopes", + "rank_loc": "9", + "score_loc": 0.03 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24913858", + "componentKind": "Taxon above family", + "componentPct": 3, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3352670", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 20.0, + "taxsubgrp": "Typic Dystrocryepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "E30-boreal forest-silty slopes", + "componentData": "Missing Data", + "componentID": 24913863, + "name": "E30-boreal forest-silty slopes", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 0.758, + "score_data_loc": 0.529, + "score_loc": 0.3 + }, + { + "component": "E30-boreal alpine scrub-gravelly colluvial slopes", + "componentData": "Missing Data", + "componentID": 24913856, + "name": "E30-boreal alpine scrub-gravelly colluvial slopes", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": 2, + "score_data": 0.678, + "score_data_loc": 0.484, + "score_loc": 0.29 + }, + { + "component": "E30-boreal taiga-silty slopes", + "componentData": "Missing Data", + "componentID": 24913862, + "name": "E30-boreal taiga-silty slopes", + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": 4, + "score_data": 0.794, + "score_data_loc": 0.432, + "score_loc": 0.07 + }, + { + "component": "E30-boreal taiga-loamy frozen colluvial slopes", + "componentData": "Missing Data", + "componentID": 24913864, + "name": "E30-boreal taiga-loamy frozen colluvial slopes", + "rank_data": "3", + "rank_data_loc": "4", + "rank_loc": 3, + "score_data": 0.701, + "score_data_loc": 0.415, + "score_loc": 0.13 + }, + { + "component": "E30-boreal scrub-silty frozen drainageways", + "componentData": "Missing Data", + "componentID": 24913859, + "name": "E30-boreal scrub-silty frozen drainageways", + "rank_data": "5", + "rank_data_loc": "5", + "rank_loc": 7, + "score_data": 0.644, + "score_data_loc": 0.342, + "score_loc": 0.04 + }, + { + "component": "E30-boreal taiga/tussock-silty frozen slopes", + "componentData": "Missing Data", + "componentID": 24913861, + "name": "E30-boreal taiga/tussock-silty frozen slopes", + "rank_data": "7", + "rank_data_loc": "6", + "rank_loc": 5, + "score_data": 0.605, + "score_data_loc": 0.333, + "score_loc": 0.06 + }, + { + "component": "E30-boreal alpine dwarf scrub-gravelly colluvial slopes", + "componentData": "Missing Data", + "componentID": 24913857, + "name": "E30-boreal alpine dwarf scrub-gravelly colluvial slopes", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": 8, + "score_data": 0.613, + "score_data_loc": 0.321, + "score_loc": 0.03 + }, + { + "component": "E30-boreal subalpine scrub-loamy colluvial slopes", + "componentData": "Missing Data", + "componentID": 24913860, + "name": "E30-boreal subalpine scrub-loamy colluvial slopes", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": 6, + "score_data": 0.592, + "score_data_loc": 0.321, + "score_loc": 0.05 + }, + { + "component": "E30-boreal subalpine woodland-gravelly colluvial slopes", + "componentData": "Missing Data", + "componentID": 24913858, + "name": "E30-boreal subalpine woodland-gravelly colluvial slopes", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": 9, + "score_data": 0.468, + "score_data_loc": 0.249, + "score_loc": 0.03 + } + ] + } +} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json new file mode 100644 index 0000000..e9672a7 --- /dev/null +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json @@ -0,0 +1,790 @@ +{ + "list": { + "AWS_PIW90": 15.63, + "Soil Data Value": [ + [ + "rfv_class_30", + 1.4455018975807923 + ], + [ + "rfv_class_0", + 0.9758207999450619 + ], + [ + "texture_30", + 0.43867507444769327 + ], + [ + "texture_0", + 0.0 + ] + ], + "metadata": { + "location": "us", + "model": "v3", + "unit_measure": { + "cec": "cmol(c)/kg", + "clay": "%", + "depth": "cm", + "distance": "m", + "ec": "ds/m", + "rock_fragments": "cm3/100cm3", + "sand": "%" + } + }, + "soilList": [ + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga-loamy frozen colluvial slopes", + "name": "E30-boreal taiga-loamy frozen colluvial slopes", + "rank_loc": "1", + "score_loc": 0.34 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914406", + "componentKind": "Taxon above family", + "componentPct": 34, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 4.0, + "taxsubgrp": "Typic Historthels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal scrub-gravelly low flood plains", + "name": "E30-boreal scrub-gravelly low flood plains", + "rank_loc": "2", + "score_loc": 0.19 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914408", + "componentKind": "Taxon above family", + "componentPct": 19, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Oxyaquic Cryorthents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga-organic frozen peat plateaus", + "name": "E30-boreal taiga-organic frozen peat plateaus", + "rank_loc": "3", + "score_loc": 0.12 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914411", + "componentKind": "Taxon above family", + "componentPct": 12, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 0.0, + "taxsubgrp": "Glacic Folistels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga/tussock-silty frozen terraces", + "name": "E30-boreal taiga/tussock-silty frozen terraces", + "rank_loc": "4", + "score_loc": 0.11 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914407", + "componentKind": "Taxon above family", + "componentPct": 11, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Typic Histoturbels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga-silty frozen loess slopes", + "name": "E30-boreal taiga-silty frozen loess slopes", + "rank_loc": "5", + "score_loc": 0.107 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914462", + "componentKind": "Taxon above family", + "componentPct": 43, + "dataSource": "SSURGO", + "distance": 350.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375378", + "minCompDistance": 350.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 8.0, + "taxsubgrp": "Typic Historthels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal forest-loamy flood plains", + "name": "E30-boreal forest-loamy flood plains", + "rank_loc": "6", + "score_loc": 0.09 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914409", + "componentKind": "Taxon above family", + "componentPct": 9, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "4", + "nirrcapscl": "w", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Typic Cryofluvents", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal forest-silty slopes", + "name": "E30-boreal forest-silty slopes", + "rank_loc": "7", + "score_loc": 0.07 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914405", + "componentKind": "Taxon above family", + "componentPct": 7, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 12.0, + "taxsubgrp": "Typic Haplocryods", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal forest-silty loess slopes", + "name": "E30-boreal forest-silty loess slopes", + "rank_loc": "8", + "score_loc": 0.058 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914386", + "componentKind": "Taxon above family", + "componentPct": 23, + "dataSource": "SSURGO", + "distance": 350.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375378", + "minCompDistance": 350.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 14.0, + "taxsubgrp": "Typic Haplocryepts", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal wet meadow-organic depressions", + "name": "E30-boreal wet meadow-organic depressions", + "rank_loc": "9", + "score_loc": 0.05 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914412", + "componentKind": "Taxon above family", + "componentPct": 5, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 0.0, + "taxsubgrp": "Terric Cryofibrists", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal scrub/sphagnum-organic depressions", + "name": "E30-boreal scrub/sphagnum-organic depressions", + "rank_loc": "10", + "score_loc": 0.03 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914410", + "componentKind": "Taxon above family", + "componentPct": 3, + "dataSource": "SSURGO", + "distance": 0.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375385", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 0.0, + "taxsubgrp": "Hydric Cryofibrists", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal taiga/tussock-silty frozen slopes", + "name": "E30-boreal taiga/tussock-silty frozen slopes", + "rank_loc": "11", + "score_loc": 0.03 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914464", + "componentKind": "Taxon above family", + "componentPct": 12, + "dataSource": "SSURGO", + "distance": 350.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375378", + "minCompDistance": 350.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 2.0, + "taxsubgrp": "Typic Histoturbels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal scrub-silty frozen drainageways", + "name": "E30-boreal scrub-silty frozen drainageways", + "rank_loc": "12", + "score_loc": 0.028 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914387", + "componentKind": "Taxon above family", + "componentPct": 11, + "dataSource": "SSURGO", + "distance": 350.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375378", + "minCompDistance": 350.0, + "nirrcapcl": "6", + "nirrcapscl": "s", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 1.0, + "taxsubgrp": "Fluvaquentic Historthels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "E30-boreal taiga-loamy frozen colluvial slopes", + "componentData": "Missing Data", + "componentID": 24914406, + "name": "E30-boreal taiga-loamy frozen colluvial slopes", + "rank_data": "4", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 0.613, + "score_data_loc": 0.477, + "score_loc": 0.34 + }, + { + "component": "E30-boreal forest-silty slopes", + "componentData": "Missing Data", + "componentID": 24914405, + "name": "E30-boreal forest-silty slopes", + "rank_data": "1", + "rank_data_loc": "2", + "rank_loc": 7, + "score_data": 0.745, + "score_data_loc": 0.408, + "score_loc": 0.07 + }, + { + "component": "E30-boreal taiga-silty frozen loess slopes", + "componentData": "Missing Data", + "componentID": 24914462, + "name": "E30-boreal taiga-silty frozen loess slopes", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": 5, + "score_data": 0.658, + "score_data_loc": 0.383, + "score_loc": 0.107 + }, + { + "component": "E30-boreal forest-silty loess slopes", + "componentData": "Missing Data", + "componentID": 24914386, + "name": "E30-boreal forest-silty loess slopes", + "rank_data": "2", + "rank_data_loc": "4", + "rank_loc": 8, + "score_data": 0.663, + "score_data_loc": 0.36, + "score_loc": 0.058 + }, + { + "component": "E30-boreal taiga/tussock-silty frozen terraces", + "componentData": "Missing Data", + "componentID": 24914407, + "name": "E30-boreal taiga/tussock-silty frozen terraces", + "rank_data": "7", + "rank_data_loc": "5", + "rank_loc": 4, + "score_data": 0.497, + "score_data_loc": 0.304, + "score_loc": 0.11 + }, + { + "component": "E30-boreal scrub-silty frozen drainageways", + "componentData": "Missing Data", + "componentID": 24914387, + "name": "E30-boreal scrub-silty frozen drainageways", + "rank_data": "5", + "rank_data_loc": "6", + "rank_loc": 12, + "score_data": 0.552, + "score_data_loc": 0.29, + "score_loc": 0.028 + }, + { + "component": "E30-boreal taiga/tussock-silty frozen slopes", + "componentData": "Missing Data", + "componentID": 24914464, + "name": "E30-boreal taiga/tussock-silty frozen slopes", + "rank_data": "6", + "rank_data_loc": "7", + "rank_loc": 11, + "score_data": 0.521, + "score_data_loc": 0.275, + "score_loc": 0.03 + }, + { + "component": "E30-boreal wet meadow-organic depressions", + "componentData": "Missing Data", + "componentID": 24914412, + "name": "E30-boreal wet meadow-organic depressions", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": 9, + "score_data": 0.46, + "score_data_loc": 0.255, + "score_loc": 0.05 + }, + { + "component": "E30-boreal forest-loamy flood plains", + "componentData": "Missing Data", + "componentID": 24914409, + "name": "E30-boreal forest-loamy flood plains", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": 6, + "score_data": 0.372, + "score_data_loc": 0.231, + "score_loc": 0.09 + }, + { + "component": "E30-boreal taiga-organic frozen peat plateaus", + "componentData": "Missing Data", + "componentID": 24914411, + "name": "E30-boreal taiga-organic frozen peat plateaus", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": 3, + "score_data": 0.277, + "score_data_loc": 0.199, + "score_loc": 0.12 + }, + { + "component": "E30-boreal scrub/sphagnum-organic depressions", + "componentData": "Missing Data", + "componentID": 24914410, + "name": "E30-boreal scrub/sphagnum-organic depressions", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": 10, + "score_data": 0.277, + "score_data_loc": 0.154, + "score_loc": 0.03 + }, + { + "component": "E30-boreal scrub-gravelly low flood plains", + "componentData": "Missing Data", + "componentID": 24914408, + "name": "E30-boreal scrub-gravelly low flood plains", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": 2, + "score_data": 0.08, + "score_data_loc": 0.135, + "score_loc": 0.19 + } + ] + } +} diff --git a/soil_id/tests/us/generate_bulk_test_results.py b/soil_id/tests/us/generate_bulk_test_results.py index 2264c00..beabd8e 100644 --- a/soil_id/tests/us/generate_bulk_test_results.py +++ b/soil_id/tests/us/generate_bulk_test_results.py @@ -15,7 +15,6 @@ import datetime import json -import math import os import time import traceback @@ -23,17 +22,9 @@ import pandas from soil_id.us_soil import list_soils, rank_soils +from soil_id.tests.utils import clean_soil_list_json -def clean_soil_list_json(obj): - if isinstance(obj, float) and math.isnan(obj): - return None - elif isinstance(obj, dict): - return dict((k, clean_soil_list_json(v)) for k, v in obj.items()) - elif isinstance(obj, (list, set, tuple)): - return list(map(clean_soil_list_json, obj)) - return obj - test_data_df = pandas.read_csv( os.path.join(os.path.dirname(__file__), "US_SoilID_KSSL_LPKS_Testing.csv") ) diff --git a/soil_id/tests/us/test_us.py b/soil_id/tests/us/test_us.py index 1a104d3..83dc9db 100644 --- a/soil_id/tests/us/test_us.py +++ b/soil_id/tests/us/test_us.py @@ -17,8 +17,9 @@ import time import pytest - +from soil_id.tests.utils import clean_soil_list_json from soil_id.us_soil import list_soils, rank_soils +from syrupy.extensions.json import JSONSnapshotExtension test_locations = [ {"lon": -121.5111084, "lat": 45.6508331}, @@ -40,9 +41,13 @@ # {"lat": 40.79861, "lon": -112.35477}, # crash: str object has no attribute rank_data_csv ] +test_params = [] +for idx, coords in enumerate(test_locations): + test_params.append(pytest.param(coords, id=f"{coords["lat"]},{coords["lon"]}")) + -@pytest.mark.parametrize("location", test_locations) -def test_soil_location(location): +@pytest.mark.parametrize("location", test_params) +def test_soil_location(location, snapshot): # Dummy Soil Profile Data (replicating the structure provided) soilHorizon = ["LOAM"] * 7 topDepth = [0, 1, 10, 20, 50, 70, 100] @@ -57,7 +62,7 @@ def test_soil_location(location): start_time = time.perf_counter() list_soils_result = list_soils(location["lon"], location["lat"]) logging.info(f"...time: {(time.perf_counter() - start_time):.2f}s") - rank_soils( + rank_result = rank_soils( location["lon"], location["lat"], list_soils_result, @@ -72,6 +77,11 @@ def test_soil_location(location): cracks, ) + assert snapshot.with_defaults(extension_class=JSONSnapshotExtension) == { + "list": clean_soil_list_json(list_soils_result.soil_list_json), + "rank": rank_result, + } + def test_empty_rank(): SoilListOutputData = list_soils(test_locations[0]["lon"], test_locations[0]["lat"]) diff --git a/soil_id/tests/utils.py b/soil_id/tests/utils.py new file mode 100644 index 0000000..6ec66e7 --- /dev/null +++ b/soil_id/tests/utils.py @@ -0,0 +1,26 @@ +# Copyright © 2025 Technology Matters +# +# This program is free software: you can redistribute it and/or modify +# it under the terms of the GNU Affero General Public License as published +# by the Free Software Foundation, either version 3 of the License, or +# (at your option) any later version. +# +# This program is distributed in the hope that it will be useful, +# but WITHOUT ANY WARRANTY; without even the implied warranty of +# MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the +# GNU Affero General Public License for more details. +# +# You should have received a copy of the GNU Affero General Public License +# along with this program. If not, see https://www.gnu.org/licenses/. + +import math + + +def clean_soil_list_json(obj): + if isinstance(obj, float) and math.isnan(obj): + return None + elif isinstance(obj, dict): + return dict((k, clean_soil_list_json(v)) for k, v in obj.items()) + elif isinstance(obj, (list, set, tuple)): + return list(map(clean_soil_list_json, obj)) + return obj From a490b921a326ee5e529c0bf49c8efd6bddc51c8b Mon Sep 17 00:00:00 2001 From: shrouxm Date: Wed, 30 Jul 2025 10:42:30 -0700 Subject: [PATCH 3/5] fix: user order by to make HWSD query deterministic --- soil_id/db.py | 3 ++- 1 file changed, 2 insertions(+), 1 deletion(-) diff --git a/soil_id/db.py b/soil_id/db.py index 7d20042..1de1f86 100644 --- a/soil_id/db.py +++ b/soil_id/db.py @@ -353,7 +353,8 @@ def extract_hwsd2_data(connection, lon, lat, buffer_dist, table_name): BOOL_OR(ST_Intersects(shape, {point})) AS pt_intersect FROM hwsd2_segment WHERE ST_DWithin(shape, {point}, {buffer_dist}) - GROUP BY hwsd2_id; + GROUP BY hwsd2_id + ORDER BY hwsd2_id; """ # Use GeoPandas to execute the main query and load results into a GeoDataFrame. From 94869fad21f8009d824e65c653868ed647898281 Mon Sep 17 00:00:00 2001 From: shrouxm Date: Wed, 30 Jul 2025 10:47:46 -0700 Subject: [PATCH 4/5] chore: rerun snapshot tests --- ...st_soil_location[-10.07856,15.107436].json | 710 +++----- ...t_soil_location[-10.950086,17.573093].json | 624 +++---- ...est_soil_location[-19.13333,145.5125].json | 300 ++-- .../test_soil_location[-2.06972,37.29].json | 1460 +++++++++-------- ...est_soil_location[-24.53333,33.36667].json | 172 +- .../test_soil_location[34.5,69.16667].json | 444 +++-- .../test_soil_location[37.33333,-5.4].json | 204 +-- ...est_soil_location[48.71667,126.13333].json | 172 +- .../test_soil_location[7.3318,-1.4631].json | 944 +++++------ ...st_soil_location[34.92816,-114.80764].json | 166 +- .../test_soil_location[37.422,-122.084].json | 54 +- ...il_location[39.26009312,-85.50621214].json | 262 +-- 12 files changed, 2644 insertions(+), 2868 deletions(-) diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json index 93ea6f8..0366726 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json @@ -605,7 +605,7 @@ }, "id": { "component": "Luvic phaeozems", - "name": "Luvic phaeozems1", + "name": "Luvic phaeozems", "rank_loc": "7", "score_loc": 0.025 }, @@ -626,11 +626,11 @@ }, "site": { "siteData": { - "componentID": 104814, - "distance": 62973.262, - "mapunitID": 12050, - "minCompDistance": 62973.2622, - "share": 20, + "componentID": 104807, + "distance": 75356.147, + "mapunitID": 12048, + "minCompDistance": 75356.1465, + "share": 25, "soilDepth": 200 }, "siteDescription": { @@ -1016,8 +1016,8 @@ "sl7": 0.0 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols1", + "component": "Chromic luvisols", + "name": "Chromic luvisols", "rank_loc": "12", "score_loc": 0.017 }, @@ -1050,22 +1050,22 @@ }, "site": { "siteData": { - "componentID": 104802, - "distance": 63317.634, - "mapunitID": 12047, - "minCompDistance": 63317.6338, - "share": 40, + "componentID": 104806, + "distance": 75356.147, + "mapunitID": 12048, + "minCompDistance": 75356.1465, + "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { @@ -1178,106 +1178,6 @@ "sl7": "Unknown" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 23.0, - "sl5": 22.29, - "sl6": 21.8, - "sl7": 21.5 - }, - "clay": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0, - "sl4": 40.2, - "sl5": 41.57, - "sl6": 42.0, - "sl7": 41.5 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Xanthic ferralsols", - "name": "Xanthic ferralsols3", - "rank_loc": "Not Displayed", - "score_loc": 0.067 - }, - "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.26, - "sl5": 6.29, - "sl6": 6.32, - "sl7": 6.32 - }, - "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 8.4, - "sl5": 8.43, - "sl6": 8.6, - "sl7": 12.33 - }, - "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 34.4, - "sl5": 33.71, - "sl6": 33.8, - "sl7": 34.67 - }, - "site": { - "siteData": { - "componentID": 104818, - "distance": 96145.535, - "mapunitID": 12052, - "minCompDistance": 4468.8459, - "share": 30, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", - "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, { "bottom_depth": { "sl1": 1, @@ -1316,10 +1216,10 @@ "sl7": 0.0 }, "id": { - "component": "Haplic ferralsols", - "name": "Haplic ferralsols2", + "component": "Xanthic ferralsols", + "name": "Xanthic ferralsols3", "rank_loc": "Not Displayed", - "score_loc": 0.042 + "score_loc": 0.067 }, "ph": { "sl1": 5.6, @@ -1350,22 +1250,22 @@ }, "site": { "siteData": { - "componentID": 104799, - "distance": 31871.197, - "mapunitID": 12046, + "componentID": 104818, + "distance": 96145.535, + "mapunitID": 12052, "minCompDistance": 4468.8459, - "share": 20, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", - "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", + "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." } }, "texture": { @@ -1416,8 +1316,8 @@ "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", + "component": "Haplic ferralsols", + "name": "Haplic ferralsols2", "rank_loc": "Not Displayed", "score_loc": 0.042 }, @@ -1450,22 +1350,22 @@ }, "site": { "siteData": { - "componentID": 105352, - "distance": 99172.777, - "mapunitID": 12196, - "minCompDistance": 31871.1971, - "share": 10, - "soilDepth": 20 + "componentID": 104799, + "distance": 31871.197, + "mapunitID": 12046, + "minCompDistance": 4468.8459, + "share": 20, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", + "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." } }, "texture": { @@ -1516,10 +1416,10 @@ "sl7": 1.17 }, "id": { - "component": "Eutric leptosols", - "name": "Eutric leptosols2", + "component": "Lithic leptosols", + "name": "Lithic leptosols2", "rank_loc": "Not Displayed", - "score_loc": 0.033 + "score_loc": 0.042 }, "ph": { "sl1": 6.4, @@ -1550,22 +1450,22 @@ }, "site": { "siteData": { - "componentID": 105349, + "componentID": 105352, "distance": 99172.777, "mapunitID": 12196, "minCompDistance": 31871.1971, - "share": 45, - "soilDepth": 40 + "share": 10, + "soilDepth": 20 }, "siteDescription": { - "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", - "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " } }, "texture": { @@ -1617,7 +1517,7 @@ }, "id": { "component": "Eutric leptosols", - "name": "Eutric leptosols3", + "name": "Eutric leptosols2", "rank_loc": "Not Displayed", "score_loc": 0.033 }, @@ -1650,11 +1550,11 @@ }, "site": { "siteData": { - "componentID": 105229, - "distance": 99332.531, - "mapunitID": 12163, + "componentID": 105349, + "distance": 99172.777, + "mapunitID": 12196, "minCompDistance": 31871.1971, - "share": 10, + "share": 45, "soilDepth": 40 }, "siteDescription": { @@ -1716,10 +1616,10 @@ "sl7": 0.17 }, "id": { - "component": "Rhodic ferralsols", - "name": "Rhodic ferralsols2", + "component": "Eutric leptosols", + "name": "Eutric leptosols3", "rank_loc": "Not Displayed", - "score_loc": 0.025 + "score_loc": 0.033 }, "ph": { "sl1": 5.2, @@ -1750,22 +1650,22 @@ }, "site": { "siteData": { - "componentID": 104820, - "distance": 96145.535, - "mapunitID": 12052, - "minCompDistance": 21840.3117, - "share": 20, - "soilDepth": 200 + "componentID": 105229, + "distance": 99332.531, + "mapunitID": 12163, + "minCompDistance": 31871.1971, + "share": 10, + "soilDepth": 40 }, "siteDescription": { - "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", - "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " } }, "texture": { @@ -1816,8 +1716,8 @@ "sl7": 0.5 }, "id": { - "component": "Luvic phaeozems", - "name": "Luvic phaeozems2", + "component": "Rhodic ferralsols", + "name": "Rhodic ferralsols2", "rank_loc": "Not Displayed", "score_loc": 0.025 }, @@ -1850,22 +1750,22 @@ }, "site": { "siteData": { - "componentID": 104807, - "distance": 75356.147, - "mapunitID": 12048, - "minCompDistance": 62973.2622, - "share": 25, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", - "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " + "componentID": 104820, + "distance": 96145.535, + "mapunitID": 12052, + "minCompDistance": 21840.3117, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", + "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." } }, "texture": { @@ -1978,106 +1878,6 @@ "sl7": "Loamy sand" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.71, - "sl6": 6.8, - "sl7": 6.83 - }, - "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.2, - "sl5": 30.29, - "sl6": 33.2, - "sl7": 34.33 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Ferralic cambisols", - "name": "Ferralic cambisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.017 - }, - "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.12, - "sl5": 6.07, - "sl6": 6.02, - "sl7": 6.02 - }, - "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 9.8, - "sl5": 10.43, - "sl6": 10.6, - "sl7": 10.5 - }, - "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 60.2, - "sl5": 57.57, - "sl6": 54.8, - "sl7": 53.0 - }, - "site": { - "siteData": { - "componentID": 105247, - "distance": 28892.433, - "mapunitID": 12167, - "minCompDistance": 4468.8459, - "share": 15, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", - "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, { "bottom_depth": { "sl1": 1, @@ -2116,8 +1916,8 @@ "sl7": 0.0 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols2", + "component": "Ferralic cambisols", + "name": "Ferralic cambisols2", "rank_loc": "Not Displayed", "score_loc": 0.017 }, @@ -2150,22 +1950,22 @@ }, "site": { "siteData": { - "componentID": 104805, - "distance": 63317.634, - "mapunitID": 12047, - "minCompDistance": 40422.2833, + "componentID": 105247, + "distance": 28892.433, + "mapunitID": 12167, + "minCompDistance": 4468.8459, "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " } }, "texture": { @@ -2189,89 +1989,89 @@ "sl7": 120 }, "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.0, - "sl5": 6.14, - "sl6": 6.4, - "sl7": 6.5 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.6, + "sl5": 14.71, + "sl6": 15.0, + "sl7": 15.17 }, "clay": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 25.0, - "sl5": 28.14, + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.6, + "sl5": 29.86, "sl6": 30.6, - "sl7": 31.17 + "sl7": 30.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols2", + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", "rank_loc": "Not Displayed", "score_loc": 0.017 }, "ph": { - "sl1": 5.6, - "sl2": 5.6, - "sl3": 5.6, - "sl4": 5.68, - "sl5": 5.71, - "sl6": 5.74, - "sl7": 5.73 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.44, + "sl6": 6.44, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 10.8, - "sl5": 10.29, - "sl6": 11.4, - "sl7": 11.17 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 9.29, + "sl6": 13.4, + "sl7": 12.5 }, "sand": { - "sl1": 63.0, - "sl2": 63.0, - "sl3": 63.0, - "sl4": 56.8, - "sl5": 54.14, - "sl6": 52.2, - "sl7": 51.67 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 49.0, + "sl5": 47.71, + "sl6": 46.6, + "sl7": 46.67 }, "site": { "siteData": { - "componentID": 105351, - "distance": 99172.777, - "mapunitID": 12196, - "minCompDistance": 63317.6338, - "share": 20, + "componentID": 104805, + "distance": 63317.634, + "mapunitID": 12047, + "minCompDistance": 40422.2833, + "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", @@ -2301,8 +2101,8 @@ { "component": "Luvic phaeozems", "componentData": "Missing Data", - "componentID": 104814, - "name": "Luvic phaeozems1", + "componentID": 104807, + "name": "Luvic phaeozems", "rank_data": "5", "rank_data_loc": "2", "rank_loc": "7", @@ -2335,60 +2135,48 @@ "score_loc": 0.021 }, { - "component": "Haplic ferralsols", - "componentData": "No Data", - "componentID": 104799, - "name": "Haplic ferralsols2", - "rank_data": "6", + "component": "Xanthic ferralsols", + "componentData": "Missing Data", + "componentID": 104818, + "name": "Xanthic ferralsols3", + "rank_data": "8", "rank_data_loc": "5", "rank_loc": "Not Displayed", - "score_data": 0.832, - "score_data_loc": 0.849, - "score_loc": 0.042 + "score_data": 0.829, + "score_data_loc": 0.87, + "score_loc": 0.067 }, { "component": "Rhodic ferralsols", "componentData": "No Data", "componentID": 105419, "name": "Rhodic ferralsols1", - "rank_data": "8", + "rank_data": "7", "rank_data_loc": "6", "rank_loc": "6", - "score_data": 0.832, - "score_data_loc": 0.832, + "score_data": 0.829, + "score_data_loc": 0.83, "score_loc": 0.025 }, { - "component": "Haplic lixisols", - "componentData": "Missing Data", - "componentID": 104802, - "name": "Haplic lixisols1", - "rank_data": "7", + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 104806, + "name": "Chromic luvisols", + "rank_data": "6", "rank_data_loc": "7", "rank_loc": "12", - "score_data": 0.832, - "score_data_loc": 0.824, + "score_data": 0.829, + "score_data_loc": 0.821, "score_loc": 0.017 }, - { - "component": "Xanthic ferralsols", - "componentData": "Missing Data", - "componentID": 104818, - "name": "Xanthic ferralsols3", - "rank_data": "Not Displayed", - "rank_data_loc": "8", - "rank_loc": "Not Displayed", - "score_data": 0.752, - "score_data_loc": 0.795, - "score_loc": 0.067 - }, { "component": "Ferralic arenosols", "componentData": "Data Complete", "componentID": 105472, "name": "Ferralic arenosols1", "rank_data": "10", - "rank_data_loc": "9", + "rank_data_loc": "8", "rank_loc": "11", "score_data": 0.711, "score_data_loc": 0.707, @@ -2400,17 +2188,29 @@ "componentID": 105395, "name": "Ferralic cambisols1", "rank_data": "11", - "rank_data_loc": "10", + "rank_data_loc": "9", "rank_loc": "10", "score_data": 0.711, "score_data_loc": 0.707, "score_loc": 0.017 }, + { + "component": "Haplic ferralsols", + "componentData": "Missing Data", + "componentID": 105398, + "name": "Haplic ferralsols1", + "rank_data": "12", + "rank_data_loc": "10", + "rank_loc": "2", + "score_data": 0.659, + "score_data_loc": 0.68, + "score_loc": 0.042 + }, { "component": "Eutric leptosols", "componentData": "Missing Data", - "componentID": 105229, - "name": "Eutric leptosols3", + "componentID": 105349, + "name": "Eutric leptosols2", "rank_data": "3", "rank_data_loc": "11", "rank_loc": "Not Displayed", @@ -2421,12 +2221,12 @@ { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 104800, - "name": "Lithic leptosols1", - "rank_data": "12", + "componentID": 105352, + "name": "Lithic leptosols2", + "rank_data": "9", "rank_data_loc": "12", - "rank_loc": "3", - "score_data": 0.503, + "rank_loc": "Not Displayed", + "score_data": 0.752, "score_data_loc": 0.002, "score_loc": 0.042 }, @@ -2435,25 +2235,13 @@ "componentData": "Missing Data", "componentID": 105417, "name": "Xanthic ferralsols2", - "rank_data": "9", + "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", "score_data": 0.752, "score_data_loc": 0.795, "score_loc": 0.067 }, - { - "component": "Luvic phaeozems", - "componentData": "Missing Data", - "componentID": 104807, - "name": "Luvic phaeozems2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.752, - "score_data_loc": 0.755, - "score_loc": 0.025 - }, { "component": "Rhodic ferralsols", "componentData": "No Data", @@ -2466,18 +2254,6 @@ "score_data_loc": 0.755, "score_loc": 0.025 }, - { - "component": "Haplic lixisols", - "componentData": "Data Complete", - "componentID": 105351, - "name": "Haplic lixisols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.711, - "score_data_loc": 0.707, - "score_loc": 0.017 - }, { "component": "Xanthic ferralsols", "componentData": "Missing Data", @@ -2491,16 +2267,16 @@ "score_loc": 0.067 }, { - "component": "Haplic ferralsols", - "componentData": "Missing Data", - "componentID": 105398, - "name": "Haplic ferralsols1", + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 104805, + "name": "Ferralic arenosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "2", + "rank_loc": "Not Displayed", "score_data": 0.659, - "score_data_loc": 0.68, - "score_loc": 0.042 + "score_data_loc": 0.656, + "score_loc": 0.017 }, { "component": "Ferralic cambisols", @@ -2510,21 +2286,21 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.659, - "score_data_loc": 0.656, + "score_data": 0.524, + "score_data_loc": 0.525, "score_loc": 0.017 }, { - "component": "Ferralic arenosols", - "componentData": "Data Complete", - "componentID": 104805, - "name": "Ferralic arenosols2", + "component": "Haplic ferralsols", + "componentData": "No Data", + "componentID": 104799, + "name": "Haplic ferralsols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.524, - "score_data_loc": 0.525, - "score_loc": 0.017 + "score_data": 0.392, + "score_data_loc": 0.421, + "score_loc": 0.042 }, { "component": "Eutric cambisols", @@ -2553,8 +2329,8 @@ { "component": "Eutric leptosols", "componentData": "Missing Data", - "componentID": 105349, - "name": "Eutric leptosols2", + "componentID": 105229, + "name": "Eutric leptosols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2565,12 +2341,12 @@ { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 105352, - "name": "Lithic leptosols2", + "componentID": 104800, + "name": "Lithic leptosols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.392, + "rank_loc": "3", + "score_data": 0.503, "score_data_loc": 0.002, "score_loc": 0.042 } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json index e52af42..8bb8a9c 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json @@ -764,8 +764,8 @@ "sl7": 0.0 }, "id": { - "component": "Umbric gleysols", - "name": "Umbric gleysols", + "component": "Gleyic arenosols", + "name": "Gleyic arenosols", "rank_loc": "9", "score_loc": 0.018 }, @@ -798,7 +798,7 @@ }, "site": { "siteData": { - "componentID": 104792, + "componentID": 104793, "distance": 0.0, "mapunitID": 12044, "minCompDistance": 0.0, @@ -806,14 +806,14 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ", - "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", - "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. " + "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.", + "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " } }, "texture": { @@ -864,8 +864,8 @@ "sl7": 0.0 }, "id": { - "component": "Gleyic arenosols", - "name": "Gleyic arenosols", + "component": "Umbric gleysols", + "name": "Umbric gleysols", "rank_loc": "10", "score_loc": 0.018 }, @@ -898,7 +898,7 @@ }, "site": { "siteData": { - "componentID": 104793, + "componentID": 104792, "distance": 0.0, "mapunitID": 12044, "minCompDistance": 0.0, @@ -906,14 +906,14 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", - "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.", - "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", - "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ", + "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", + "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. " } }, "texture": { @@ -926,106 +926,6 @@ "sl7": "Unknown" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.6, - "sl5": 6.14, - "sl6": 5.8, - "sl7": 5.67 - }, - "clay": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0, - "sl4": 38.8, - "sl5": 39.86, - "sl6": 40.8, - "sl7": 41.5 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Haplic acrisols", - "name": "Haplic acrisols", - "rank_loc": "11", - "score_loc": 0.016 - }, - "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.16, - "sl5": 5.19, - "sl6": 5.24, - "sl7": 5.28 - }, - "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 3.4, - "sl5": 3.29, - "sl6": 3.2, - "sl7": 5.17 - }, - "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 38.8, - "sl5": 37.86, - "sl6": 36.8, - "sl7": 36.0 - }, - "site": { - "siteData": { - "componentID": 105457, - "distance": 53803.703, - "mapunitID": 12224, - "minCompDistance": 53803.703, - "share": 35, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, { "bottom_depth": { "sl1": 1, @@ -1064,9 +964,9 @@ "sl7": 0.0 }, "id": { - "component": "Ferralic cambisols", - "name": "Ferralic cambisols", - "rank_loc": "12", + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "11", "score_loc": 0.016 }, "ph": { @@ -1098,22 +998,22 @@ }, "site": { "siteData": { - "componentID": 105461, - "distance": 82783.427, - "mapunitID": 12225, - "minCompDistance": 82783.4266, + "componentID": 105457, + "distance": 53803.703, + "mapunitID": 12224, + "minCompDistance": 53803.703, "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", - "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { @@ -1164,10 +1064,10 @@ "sl7": 0.0 }, "id": { - "component": "Haplic alisols", - "name": "Haplic alisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.029 + "component": "Ferralic cambisols", + "name": "Ferralic cambisols", + "rank_loc": "12", + "score_loc": 0.016 }, "ph": { "sl1": 5.6, @@ -1198,22 +1098,22 @@ }, "site": { "siteData": { - "componentID": 104944, - "distance": 88902.515, - "mapunitID": 12084, - "minCompDistance": 66876.8882, - "share": 65, + "componentID": 105461, + "distance": 82783.427, + "mapunitID": 12225, + "minCompDistance": 82783.4266, + "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", - "Description_es": "Los Alisoles Háplicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua. ", - "Description_fr": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", - "Description_ks": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", - "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", - "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
Debido a su poca profundidad, estos suelos no son adecuados para el cultivo, por lo que debe considerarse su uso para el pastoreo.
La preservación de la superficie del suelo con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua. ", - "Management_fr": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", - "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. " + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " } }, "texture": { @@ -1264,10 +1164,10 @@ "sl7": 0.0 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols2", + "component": "Haplic alisols", + "name": "Haplic alisols2", "rank_loc": "Not Displayed", - "score_loc": 0.027 + "score_loc": 0.029 }, "ph": { "sl1": 6.2, @@ -1298,22 +1198,22 @@ }, "site": { "siteData": { - "componentID": 104894, - "distance": 68854.944, - "mapunitID": 12071, - "minCompDistance": 58618.178, - "share": 10, + "componentID": 104944, + "distance": 88902.515, + "mapunitID": 12084, + "minCompDistance": 66876.8882, + "share": 65, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_es": "Los Alisoles Háplicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua. ", + "Description_fr": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_ks": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
Debido a su poca profundidad, estos suelos no son adecuados para el cultivo, por lo que debe considerarse su uso para el pastoreo.
La preservación de la superficie del suelo con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua. ", + "Management_fr": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. " } }, "texture": { @@ -1364,10 +1264,10 @@ "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", "rank_loc": "Not Displayed", - "score_loc": 0.023 + "score_loc": 0.027 }, "ph": { "sl1": 6.1, @@ -1388,13 +1288,113 @@ "sl7": 9.83 }, "sand": { - "sl1": 33.0, - "sl2": 33.0, - "sl3": 33.0, - "sl4": 30.0, - "sl5": 28.86, - "sl6": 28.0, - "sl7": 28.0 + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 30.0, + "sl5": 28.86, + "sl6": 28.0, + "sl7": 28.0 + }, + "site": { + "siteData": { + "componentID": 104894, + "distance": 68854.944, + "mapunitID": 12071, + "minCompDistance": 58618.178, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.6, + "sl5": 3.14, + "sl6": 2.8, + "sl7": 2.67 + }, + "clay": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.14, + "sl6": 5.2, + "sl7": 5.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Lithic leptosols", + "name": "Lithic leptosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.023 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.8, + "sl5": 5.8, + "sl6": 5.8, + "sl7": 5.82 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 10.4, + "sl5": 11.0, + "sl6": 10.0, + "sl7": 8.83 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 87.2, + "sl5": 87.29, + "sl6": 87.4, + "sl7": 86.83 }, "site": { "siteData": { @@ -1417,13 +1417,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -1498,11 +1498,11 @@ }, "site": { "siteData": { - "componentID": 105453, - "distance": 60797.484, - "mapunitID": 12223, + "componentID": 104892, + "distance": 68854.944, + "mapunitID": 12071, "minCompDistance": 58618.178, - "share": 40, + "share": 30, "soilDepth": 200 }, "siteDescription": { @@ -1526,106 +1526,6 @@ "sl7": "Sandy clay loam" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 3.6, - "sl5": 3.14, - "sl6": 2.8, - "sl7": 2.67 - }, - "clay": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0, - "sl5": 5.14, - "sl6": 5.2, - "sl7": 5.33 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Haplic ferralsols", - "name": "Haplic ferralsols3", - "rank_loc": "Not Displayed", - "score_loc": 0.02 - }, - "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 5.8, - "sl5": 5.8, - "sl6": 5.8, - "sl7": 5.82 - }, - "rock_fragments": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 10.4, - "sl5": 11.0, - "sl6": 10.0, - "sl7": 8.83 - }, - "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 87.2, - "sl5": 87.29, - "sl6": 87.4, - "sl7": 86.83 - }, - "site": { - "siteData": { - "componentID": 104892, - "distance": 68854.944, - "mapunitID": 12071, - "minCompDistance": 58618.178, - "share": 30, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", - "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." - } - }, - "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" - } - }, { "bottom_depth": { "sl1": 1, @@ -1839,20 +1739,32 @@ "componentData": "Data Complete", "componentID": 104943, "name": "Haplic alisols1", - "rank_data": "1", + "rank_data": "2", "rank_data_loc": "1", "rank_loc": "2", "score_data": 1.0, "score_data_loc": 1.0, "score_loc": 0.029 }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 104894, + "name": "Ferralic arenosols2", + "rank_data": "1", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 0.998, + "score_loc": 0.027 + }, { "component": "Haplic ferralsols", "componentData": "Missing Data", "componentID": 104785, "name": "Haplic ferralsols1", - "rank_data": "2", - "rank_data_loc": "2", + "rank_data": "3", + "rank_data_loc": "3", "rank_loc": "6", "score_data": 1.0, "score_data_loc": 0.991, @@ -1864,7 +1776,7 @@ "componentID": 104946, "name": "Luvic phaeozems1", "rank_data": "4", - "rank_data_loc": "3", + "rank_data_loc": "4", "rank_loc": "8", "score_data": 1.0, "score_data_loc": 0.991, @@ -1876,7 +1788,7 @@ "componentID": 104784, "name": "Rhodic ferralsols1", "rank_data": "5", - "rank_data_loc": "4", + "rank_data_loc": "5", "rank_loc": "7", "score_data": 1.0, "score_data_loc": 0.991, @@ -1887,23 +1799,23 @@ "componentData": "Data Complete", "componentID": 104790, "name": "Gleyic alisols", - "rank_data": "8", - "rank_data_loc": "5", + "rank_data": "9", + "rank_data_loc": "6", "rank_loc": "1", "score_data": 0.845, "score_data_loc": 0.945, "score_loc": 0.127 }, { - "component": "Gleyic arenosols", + "component": "Umbric gleysols", "componentData": "Data Complete", - "componentID": 104793, - "name": "Gleyic arenosols", - "rank_data": "7", - "rank_data_loc": "6", + "componentID": 104792, + "name": "Umbric gleysols", + "rank_data": "8", + "rank_data_loc": "7", "rank_loc": "10", - "score_data": 0.895, - "score_data_loc": 0.887, + "score_data": 0.905, + "score_data_loc": 0.896, "score_loc": 0.018 }, { @@ -1912,47 +1824,35 @@ "componentID": 105461, "name": "Ferralic cambisols", "rank_data": "6", - "rank_data_loc": "7", + "rank_data_loc": "8", "rank_loc": "12", - "score_data": 0.895, - "score_data_loc": 0.885, + "score_data": 0.905, + "score_data_loc": 0.894, "score_loc": 0.016 }, { - "component": "Ferralic arenosols", - "componentData": "Data Complete", - "componentID": 104894, - "name": "Ferralic arenosols2", - "rank_data": "9", - "rank_data_loc": "8", - "rank_loc": "Not Displayed", - "score_data": 0.673, - "score_data_loc": 0.68, - "score_loc": 0.027 - }, - { - "component": "Umbric gleysols", + "component": "Haplic acrisols", "componentData": "Data Complete", - "componentID": 104792, - "name": "Umbric gleysols", - "rank_data": "11", + "componentID": 105457, + "name": "Haplic acrisols", + "rank_data": "7", "rank_data_loc": "9", - "rank_loc": "9", - "score_data": 0.673, - "score_data_loc": 0.672, - "score_loc": 0.018 + "rank_loc": "11", + "score_data": 0.905, + "score_data_loc": 0.894, + "score_loc": 0.016 }, { - "component": "Haplic acrisols", + "component": "Gleyic arenosols", "componentData": "Data Complete", - "componentID": 105457, - "name": "Haplic acrisols", + "componentID": 104793, + "name": "Gleyic arenosols", "rank_data": "10", "rank_data_loc": "10", - "rank_loc": "11", + "rank_loc": "9", "score_data": 0.673, - "score_data_loc": 0.669, - "score_loc": 0.016 + "score_data_loc": 0.672, + "score_loc": 0.018 }, { "component": "Eutric leptosols", @@ -1969,19 +1869,19 @@ { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 104895, - "name": "Lithic leptosols2", - "rank_data": "3", + "componentID": 105466, + "name": "Lithic leptosols1", + "rank_data": "11", "rank_data_loc": "12", - "rank_loc": "Not Displayed", - "score_data": 1.0, + "rank_loc": "5", + "score_data": 0.516, "score_data_loc": 0.002, "score_loc": 0.023 }, { "component": "Haplic ferralsols", - "componentData": "Missing Data", - "componentID": 105453, + "componentData": "No Data", + "componentID": 104892, "name": "Haplic ferralsols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", @@ -1990,18 +1890,6 @@ "score_data_loc": 0.991, "score_loc": 0.02 }, - { - "component": "Haplic alisols", - "componentData": "Data Complete", - "componentID": 104944, - "name": "Haplic alisols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.895, - "score_data_loc": 0.898, - "score_loc": 0.029 - }, { "component": "Rhodic ferralsols", "componentData": "No Data", @@ -2014,6 +1902,18 @@ "score_data_loc": 0.698, "score_loc": 0.02 }, + { + "component": "Haplic alisols", + "componentData": "Data Complete", + "componentID": 104944, + "name": "Haplic alisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.673, + "score_data_loc": 0.683, + "score_loc": 0.029 + }, { "component": "Luvic phaeozems", "componentData": "Missing Data", @@ -2038,26 +1938,14 @@ "score_data_loc": 0.638, "score_loc": 0.027 }, - { - "component": "Haplic ferralsols", - "componentData": "No Data", - "componentID": 104892, - "name": "Haplic ferralsols3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.516, - "score_data_loc": 0.521, - "score_loc": 0.02 - }, { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 105466, - "name": "Lithic leptosols1", + "componentID": 104895, + "name": "Lithic leptosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "5", + "rank_loc": "Not Displayed", "score_data": 0.516, "score_data_loc": 0.002, "score_loc": 0.023 diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json index 93aaba9..bf01167 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json @@ -1104,8 +1104,8 @@ "sl3": 1.0 }, "id": { - "component": "Acrisols", - "name": "Acrisols1", + "component": "Haplic podzols", + "name": "Haplic podzols1", "rank_loc": "12", "score_loc": 0.011 }, @@ -1126,22 +1126,22 @@ }, "site": { "siteData": { - "componentID": 148895, - "distance": 32877.453, - "mapunitID": 6017, - "minCompDistance": 32877.4526, + "componentID": 148915, + "distance": 3068.563, + "mapunitID": 6024, + "minCompDistance": 3068.5627, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", + "Description_es": "Los Podzoles Háplicos son suelos de textura gruesa, ácidos e improductivos, con horizontes superficiales muy lixiviados sobre los que se asientan subsuelos que contienen materia orgánica acumulada y metales (aluminio y hierro).*En los paisajes de llanura costera plana, estos suelos también son húmedos.", + "Description_fr": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", + "Description_ks": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", + "Management_en": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", + "Management_es": "Los podzoles están muy lixiviados y, como tales, tienen una baja fertilidad.
Las capas superficiales suelen ser bastante ácidas (pH < 4,5), por lo que es necesario el encalado.
Debido al alto grado de meteorización, los suelos también tienen un alto contenido de aluminio soluble y fijan el fósforo, creando deficiencias de P. Aunque no se recomienda, si estos suelos se utilizan para el cultivo necesitarán un arado profundo (para romper las capas del subsuelo), encalado y fertilización.
Será necesario un cuidado específico con la fertilización de P, y se recomienda el uso de banda en la colocación de P en la semilla.", + "Management_fr": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", + "Management_ks": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended." } }, "texture": { @@ -2729,22 +2729,22 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.57, - "sl6": 6.6, - "sl7": 6.67 - }, - "clay": { "sl1": 25.0, "sl2": 25.0, "sl3": 25.0, - "sl4": 30.8, - "sl5": 33.14, - "sl6": 35.6, - "sl7": 36.67 + "sl4": 17.4, + "sl5": 14.57, + "sl6": 11.8, + "sl7": 10.67 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.4, + "sl5": 5.43, + "sl6": 5.6, + "sl7": 5.67 }, "ec": { "sl1": 0.0, @@ -2762,31 +2762,31 @@ "score_loc": 0.013 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.04, - "sl5": 5.03, - "sl6": 5.02, - "sl7": 5.02 + "sl1": 4.6, + "sl2": 4.6, + "sl3": 4.6, + "sl4": 4.88, + "sl5": 4.99, + "sl6": 5.1, + "sl7": 5.17 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 17.8, - "sl5": 19.14, - "sl6": 19.6, - "sl7": 20.0 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 16.8, + "sl5": 18.71, + "sl6": 20.6, + "sl7": 21.5 }, "sand": { - "sl1": 54.0, - "sl2": 54.0, - "sl3": 54.0, - "sl4": 49.6, - "sl5": 47.71, - "sl6": 45.6, - "sl7": 44.5 + "sl1": 58.0, + "sl2": 58.0, + "sl3": 58.0, + "sl4": 60.4, + "sl5": 61.57, + "sl6": 63.2, + "sl7": 64.17 }, "site": { "siteData": { @@ -2809,13 +2809,13 @@ } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay", - "sl7": "Clay loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -2829,22 +2829,22 @@ "sl7": 120 }, "cec": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 3.8, + "sl5": 3.86, + "sl6": 3.6, + "sl7": 3.83 + }, + "clay": { "sl1": 3.0, "sl2": 3.0, "sl3": 3.0, - "sl4": 3.6, - "sl5": 3.71, + "sl4": 2.8, + "sl5": 3.29, "sl6": 3.8, - "sl7": 3.83 - }, - "clay": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 15.4, - "sl5": 17.14, - "sl6": 18.6, - "sl7": 19.17 + "sl7": 4.17 }, "ec": { "sl1": 0.0, @@ -2856,66 +2856,66 @@ "sl7": 0.0 }, "id": { - "component": "Acrisols", - "name": "Acrisols2", + "component": "Haplic podzols", + "name": "Haplic podzols2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, "ph": { - "sl1": 5.4, - "sl2": 5.4, - "sl3": 5.4, - "sl4": 5.22, - "sl5": 5.19, - "sl6": 5.16, - "sl7": 5.17 + "sl1": 4.7, + "sl2": 4.7, + "sl3": 4.7, + "sl4": 4.92, + "sl5": 4.94, + "sl6": 4.96, + "sl7": 4.95 }, "rock_fragments": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 11.0, - "sl5": 9.14, - "sl6": 8.4, - "sl7": 9.17 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 16.8, + "sl5": 18.71, + "sl6": 20.6, + "sl7": 19.5 }, "sand": { - "sl1": 77.0, - "sl2": 77.0, - "sl3": 77.0, - "sl4": 72.6, - "sl5": 71.0, - "sl6": 70.0, - "sl7": 69.33 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 88.6, + "sl5": 88.57, + "sl6": 88.4, + "sl7": 88.33 }, "site": { "siteData": { - "componentID": 148909, - "distance": 35586.855, - "mapunitID": 6020, - "minCompDistance": 32877.4526, - "share": 20, + "componentID": 148893, + "distance": 32877.453, + "mapunitID": 6017, + "minCompDistance": 3068.5627, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", + "Description_es": "Los Podzoles Háplicos son suelos de textura gruesa, ácidos e improductivos, con horizontes superficiales muy lixiviados sobre los que se asientan subsuelos que contienen materia orgánica acumulada y metales (aluminio y hierro).*En los paisajes de llanura costera plana, estos suelos también son húmedos.", + "Description_fr": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", + "Description_ks": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", + "Management_en": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", + "Management_es": "Los podzoles están muy lixiviados y, como tales, tienen una baja fertilidad.
Las capas superficiales suelen ser bastante ácidas (pH < 4,5), por lo que es necesario el encalado.
Debido al alto grado de meteorización, los suelos también tienen un alto contenido de aluminio soluble y fijan el fósforo, creando deficiencias de P. Aunque no se recomienda, si estos suelos se utilizan para el cultivo necesitarán un arado profundo (para romper las capas del subsuelo), encalado y fertilización.
Será necesario un cuidado específico con la fertilización de P, y se recomienda el uso de banda en la colocación de P en la semilla.", + "Management_fr": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", + "Management_ks": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended." } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" } } ] @@ -2970,8 +2970,8 @@ "rank_data": "5", "rank_data_loc": "4", "rank_loc": "Not Displayed", - "score_data": 0.805, - "score_data_loc": 0.901, + "score_data": 0.808, + "score_data_loc": 0.904, "score_loc": 0.05 }, { @@ -2982,8 +2982,8 @@ "rank_data": "4", "rank_data_loc": "5", "rank_loc": "Not Displayed", - "score_data": 0.805, - "score_data_loc": 0.861, + "score_data": 0.808, + "score_data_loc": 0.864, "score_loc": 0.013 }, { @@ -2994,20 +2994,20 @@ "rank_data": "6", "rank_data_loc": "6", "rank_loc": "11", - "score_data": 0.805, - "score_data_loc": 0.861, + "score_data": 0.808, + "score_data_loc": 0.864, "score_loc": 0.013 }, { - "component": "Acrisols", - "componentData": "Missing Data", - "componentID": 148895, - "name": "Acrisols1", + "component": "Haplic podzols", + "componentData": "Data Complete", + "componentID": 148915, + "name": "Haplic podzols1", "rank_data": "7", "rank_data_loc": "7", "rank_loc": "12", - "score_data": 0.802, - "score_data_loc": 0.856, + "score_data": 0.805, + "score_data_loc": 0.859, "score_loc": 0.011 }, { @@ -3090,8 +3090,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.802, - "score_data_loc": 0.897, + "score_data": 0.805, + "score_data_loc": 0.901, "score_loc": 0.05 }, { @@ -3102,8 +3102,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "10", - "score_data": 0.802, - "score_data_loc": 0.858, + "score_data": 0.805, + "score_data_loc": 0.861, "score_loc": 0.013 }, { @@ -3142,6 +3142,18 @@ "score_data_loc": 0.816, "score_loc": 0.022 }, + { + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 149440, + "name": "Calcic luvisols3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.757, + "score_data_loc": 0.809, + "score_loc": 0.013 + }, { "component": "Eutric planosols", "componentData": "Data Complete", @@ -3202,18 +3214,6 @@ "score_data_loc": 0.711, "score_loc": 0.05 }, - { - "component": "Acrisols", - "componentData": "Data Complete", - "componentID": 148909, - "name": "Acrisols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.657, - "score_data_loc": 0.703, - "score_loc": 0.011 - }, { "component": "Dystric regosols", "componentData": "Data Complete", @@ -3226,18 +3226,6 @@ "score_data_loc": 0.677, "score_loc": 0.021 }, - { - "component": "Calcic luvisols", - "componentData": "Data Complete", - "componentID": 149440, - "name": "Calcic luvisols3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.625, - "score_data_loc": 0.671, - "score_loc": 0.013 - }, { "component": "Eutric planosols", "componentData": "Missing Data", @@ -3262,6 +3250,18 @@ "score_data_loc": 0.603, "score_loc": 0.016 }, + { + "component": "Haplic podzols", + "componentData": "Data Complete", + "componentID": 148893, + "name": "Haplic podzols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.413, + "score_data_loc": 0.445, + "score_loc": 0.011 + }, { "component": "Lithic leptosols", "componentData": "Missing Data", diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json index 8673d13..a5f0846 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json @@ -286,11 +286,11 @@ }, "site": { "siteData": { - "componentID": 111208, - "distance": 36128.047, - "mapunitID": 17453, - "minCompDistance": 36128.0473, - "share": 30, + "componentID": 111240, + "distance": 9468.474, + "mapunitID": 17466, + "minCompDistance": 9468.4741, + "share": 10, "soilDepth": 200 }, "siteDescription": { @@ -414,6 +414,106 @@ "sl7": "Sandy clay loam" } }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.2, + "sl5": 30.29, + "sl6": 33.2, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric vertisols", + "name": "Eutric vertisols1", + "rank_loc": "5", + "score_loc": 0.011 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.12, + "sl5": 6.07, + "sl6": 6.02, + "sl7": 6.02 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.8, + "sl5": 10.43, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 60.2, + "sl5": 57.57, + "sl6": 54.8, + "sl7": 53.0 + }, + "site": { + "siteData": { + "componentID": 111101, + "distance": 9085.201, + "mapunitID": 17390, + "minCompDistance": 9085.2006, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, { "bottom_depth": { "sl1": 1, @@ -452,9 +552,9 @@ "sl7": 0.0 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols1", - "rank_loc": "5", + "component": "Calcaric cambisols", + "name": "Calcaric cambisols1", + "rank_loc": "6", "score_loc": 0.011 }, "ph": { @@ -486,22 +586,22 @@ }, "site": { "siteData": { - "componentID": 111101, - "distance": 9085.201, - "mapunitID": 17390, - "minCompDistance": 9085.2006, - "share": 100, + "componentID": 111282, + "distance": 9861.436, + "mapunitID": 17486, + "minCompDistance": 9861.4358, + "share": 85, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -552,9 +652,9 @@ "sl7": 0.0 }, "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols1", - "rank_loc": "6", + "component": "Humic cambisols", + "name": "Humic cambisols", + "rank_loc": "7", "score_loc": 0.011 }, "ph": { @@ -586,20 +686,20 @@ }, "site": { "siteData": { - "componentID": 111282, - "distance": 9861.436, - "mapunitID": 17486, - "minCompDistance": 9861.4358, - "share": 85, + "componentID": 111631, + "distance": 26306.421, + "mapunitID": 17694, + "minCompDistance": 26306.4211, + "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_en": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Description_es": "Los Cambisoles Húmicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos tienen más materia orgánica en los horizontes superficiales.
Cuando el clima y el paisaje son favorables, estos suelos pueden ser productivos. ", + "Description_fr": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Description_ks": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } @@ -652,9 +752,9 @@ "sl7": 0.5 }, "id": { - "component": "Humic cambisols", - "name": "Humic cambisols", - "rank_loc": "7", + "component": "Ferric luvisols", + "name": "Ferric luvisols1", + "rank_loc": "8", "score_loc": 0.011 }, "ph": { @@ -686,22 +786,22 @@ }, "site": { "siteData": { - "componentID": 111631, - "distance": 26306.421, - "mapunitID": 17694, - "minCompDistance": 26306.4211, + "componentID": 111336, + "distance": 36837.751, + "mapunitID": 17518, + "minCompDistance": 36837.7515, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Description_es": "Los Cambisoles Húmicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos tienen más materia orgánica en los horizontes superficiales.
Cuando el clima y el paisaje son favorables, estos suelos pueden ser productivos. ", - "Description_fr": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Description_ks": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " } }, "texture": { @@ -752,9 +852,9 @@ "sl7": 0.17 }, "id": { - "component": "Ferric luvisols", - "name": "Ferric luvisols1", - "rank_loc": "8", + "component": "Calcic luvisols", + "name": "Calcic luvisols", + "rank_loc": "9", "score_loc": 0.011 }, "ph": { @@ -786,22 +886,22 @@ }, "site": { "siteData": { - "componentID": 111336, - "distance": 36837.751, - "mapunitID": 17518, - "minCompDistance": 36837.7515, - "share": 100, + "componentID": 111218, + "distance": 52061.241, + "mapunitID": 17457, + "minCompDistance": 52061.2413, + "share": 70, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " } }, "texture": { @@ -852,9 +952,9 @@ "sl7": 1.0 }, "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz1", - "rank_loc": "9", + "component": "Gleyic solonchaks", + "name": "Gleyic solonchaks1", + "rank_loc": "10", "score_loc": 0.011 }, "ph": { @@ -886,22 +986,22 @@ }, "site": { "siteData": { - "componentID": 111044, - "distance": 38961.991, - "mapunitID": 17359, - "minCompDistance": 38961.9906, + "componentID": 111319, + "distance": 53068.322, + "mapunitID": 17507, + "minCompDistance": 53068.3217, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", - "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", - "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", + "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." } }, "texture": { @@ -952,9 +1052,9 @@ "sl7": 0.83 }, "id": { - "component": "Calcic luvisols", - "name": "Calcic luvisols", - "rank_loc": "10", + "component": "Eutric cambisols", + "name": "Eutric cambisols1", + "rank_loc": "11", "score_loc": 0.011 }, "ph": { @@ -986,22 +1086,22 @@ }, "site": { "siteData": { - "componentID": 111218, - "distance": 52061.241, - "mapunitID": 17457, - "minCompDistance": 52061.2413, - "share": 70, + "componentID": 111337, + "distance": 70615.69, + "mapunitID": 17519, + "minCompDistance": 70615.6896, + "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", - "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -1052,9 +1152,9 @@ "sl7": 0.67 }, "id": { - "component": "Gleyic solonchaks", - "name": "Gleyic solonchaks1", - "rank_loc": "11", + "component": "Eutric gleysols", + "name": "Eutric gleysols", + "rank_loc": "12", "score_loc": 0.011 }, "ph": { @@ -1086,22 +1186,22 @@ }, "site": { "siteData": { - "componentID": 111319, - "distance": 53068.322, - "mapunitID": 17507, - "minCompDistance": 53068.3217, + "componentID": 111314, + "distance": 95128.611, + "mapunitID": 17504, + "minCompDistance": 95128.6114, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", - "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", - "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { @@ -1152,10 +1252,10 @@ "sl7": 0.5 }, "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols1", - "rank_loc": "12", - "score_loc": 0.011 + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.03 }, "ph": { "sl1": 5.0, @@ -1186,22 +1286,22 @@ }, "site": { "siteData": { - "componentID": 111337, - "distance": 70615.69, - "mapunitID": 17519, - "minCompDistance": 70615.6896, - "share": 100, + "componentID": 111264, + "distance": 72257.485, + "mapunitID": 17476, + "minCompDistance": 45915.6746, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { @@ -1252,10 +1352,10 @@ "sl7": 0.83 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols2", + "component": "Haplic lixisols", + "name": "Haplic lixisols2", "rank_loc": "Not Displayed", - "score_loc": 0.03 + "score_loc": 0.015 }, "ph": { "sl1": 7.3, @@ -1286,22 +1386,22 @@ }, "site": { "siteData": { - "componentID": 111264, - "distance": 72257.485, - "mapunitID": 17476, - "minCompDistance": 45915.6746, + "componentID": 111208, + "distance": 36128.047, + "mapunitID": 17453, + "minCompDistance": 9468.4741, "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " } }, "texture": { @@ -1353,7 +1453,7 @@ }, "id": { "component": "Haplic lixisols", - "name": "Haplic lixisols2", + "name": "Haplic lixisols3", "rank_loc": "Not Displayed", "score_loc": 0.015 }, @@ -1389,7 +1489,7 @@ "componentID": 111216, "distance": 41935.929, "mapunitID": 17456, - "minCompDistance": 36128.0473, + "minCompDistance": 9468.4741, "share": 30, "soilDepth": 200 }, @@ -1453,7 +1553,7 @@ }, "id": { "component": "Haplic lixisols", - "name": "Haplic lixisols3", + "name": "Haplic lixisols4", "rank_loc": "Not Displayed", "score_loc": 0.015 }, @@ -1489,7 +1589,7 @@ "componentID": 116199, "distance": 74794.646, "mapunitID": 27168, - "minCompDistance": 36128.0473, + "minCompDistance": 9468.4741, "share": 20, "soilDepth": 200 }, @@ -1514,106 +1614,6 @@ "sl7": "Sandy clay loam" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 19.2, - "sl5": 19.29, - "sl6": 19.0, - "sl7": 18.67 - }, - "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 26.0, - "sl5": 26.29, - "sl6": 25.6, - "sl7": 24.67 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 - }, - "id": { - "component": "Chromic cambisols", - "name": "Chromic cambisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.013 - }, - "ph": { - "sl1": 8.3, - "sl2": 8.3, - "sl3": 8.3, - "sl4": 8.56, - "sl5": 8.63, - "sl6": 8.66, - "sl7": 8.65 - }, - "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 5.0, - "sl5": 5.29, - "sl6": 7.4, - "sl7": 9.0 - }, - "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 44.6, - "sl5": 44.57, - "sl6": 45.4, - "sl7": 46.17 - }, - "site": { - "siteData": { - "componentID": 111117, - "distance": 72048.113, - "mapunitID": 17400, - "minCompDistance": 54718.5415, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", - "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" - } - }, { "bottom_depth": { "sl1": 1, @@ -1653,7 +1653,7 @@ }, "id": { "component": "Chromic cambisols", - "name": "Chromic cambisols3", + "name": "Chromic cambisols2", "rank_loc": "Not Displayed", "score_loc": 0.013 }, @@ -1686,11 +1686,11 @@ }, "site": { "siteData": { - "componentID": 111267, - "distance": 73282.727, - "mapunitID": 17478, + "componentID": 111117, + "distance": 72048.113, + "mapunitID": 17400, "minCompDistance": 54718.5415, - "share": 40, + "share": 100, "soilDepth": 200 }, "siteDescription": { @@ -1752,10 +1752,10 @@ "sl7": 0.67 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols2", + "component": "Chromic cambisols", + "name": "Chromic cambisols3", "rank_loc": "Not Displayed", - "score_loc": 0.011 + "score_loc": 0.013 }, "ph": { "sl1": 6.8, @@ -1786,22 +1786,22 @@ }, "site": { "siteData": { - "componentID": 111286, - "distance": 34446.462, - "mapunitID": 17488, - "minCompDistance": 9085.2006, - "share": 85, + "componentID": 111267, + "distance": 73282.727, + "mapunitID": 17478, + "minCompDistance": 54718.5415, + "share": 40, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -1853,7 +1853,7 @@ }, "id": { "component": "Eutric vertisols", - "name": "Eutric vertisols3", + "name": "Eutric vertisols2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -1886,11 +1886,11 @@ }, "site": { "siteData": { - "componentID": 111202, - "distance": 35027.212, - "mapunitID": 17450, + "componentID": 111286, + "distance": 34446.462, + "mapunitID": 17488, "minCompDistance": 9085.2006, - "share": 100, + "share": 85, "soilDepth": 200 }, "siteDescription": { @@ -1953,7 +1953,7 @@ }, "id": { "component": "Eutric vertisols", - "name": "Eutric vertisols4", + "name": "Eutric vertisols3", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -1986,11 +1986,11 @@ }, "site": { "siteData": { - "componentID": 111193, - "distance": 47856.589, - "mapunitID": 17448, + "componentID": 111202, + "distance": 35027.212, + "mapunitID": 17450, "minCompDistance": 9085.2006, - "share": 70, + "share": 100, "soilDepth": 200 }, "siteDescription": { @@ -2025,122 +2025,22 @@ "sl7": 120 }, "cec": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 15.0, - "sl5": 16.14, - "sl6": 17.2, - "sl7": 17.33 - }, - "clay": { "sl1": 17.0, "sl2": 17.0, "sl3": 17.0, - "sl4": 21.6, - "sl5": 23.57, - "sl6": 25.2, - "sl7": 25.17 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 - }, - "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols5", - "rank_loc": "Not Displayed", - "score_loc": 0.011 - }, - "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.86, - "sl5": 7.09, - "sl6": 7.36, - "sl7": 7.47 - }, - "rock_fragments": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0, - "sl5": 5.29, - "sl6": 7.2, - "sl7": 9.0 - }, - "sand": { - "sl1": 63.0, - "sl2": 63.0, - "sl3": 63.0, - "sl4": 60.0, - "sl5": 58.14, - "sl6": 56.4, - "sl7": 56.17 - }, - "site": { - "siteData": { - "componentID": 111079, - "distance": 62588.145, - "mapunitID": 17378, - "minCompDistance": 9085.2006, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 16.6, - "sl5": 16.29, - "sl6": 16.4, - "sl7": 16.33 - }, - "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 29.0, - "sl5": 28.57, - "sl6": 28.8, - "sl7": 29.0 + "sl4": 16.6, + "sl5": 16.29, + "sl6": 16.4, + "sl7": 16.33 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.0, + "sl5": 28.57, + "sl6": 28.8, + "sl7": 29.0 }, "ec": { "sl1": 14.0, @@ -2152,8 +2052,8 @@ "sl7": 16.67 }, "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols2", + "component": "Eutric vertisols", + "name": "Eutric vertisols4", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -2186,22 +2086,22 @@ }, "site": { "siteData": { - "componentID": 111641, - "distance": 63488.662, - "mapunitID": 17701, - "minCompDistance": 9861.4358, - "share": 100, + "componentID": 111193, + "distance": 47856.589, + "mapunitID": 17448, + "minCompDistance": 9085.2006, + "share": 70, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " } }, "texture": { @@ -2252,8 +2152,8 @@ "sl7": 0.67 }, "id": { - "component": "Ferric luvisols", - "name": "Ferric luvisols2", + "component": "Eutric vertisols", + "name": "Eutric vertisols5", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -2286,22 +2186,22 @@ }, "site": { "siteData": { - "componentID": 111335, - "distance": 41456.411, - "mapunitID": 17517, - "minCompDistance": 36837.7515, + "componentID": 111079, + "distance": 62588.145, + "mapunitID": 17378, + "minCompDistance": 9085.2006, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " } }, "texture": { @@ -2352,8 +2252,8 @@ "sl7": 0.67 }, "id": { - "component": "Ferric luvisols", - "name": "Ferric luvisols3", + "component": "Eutric vertisols", + "name": "Eutric vertisols6", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -2386,22 +2286,22 @@ }, "site": { "siteData": { - "componentID": 116201, + "componentID": 116200, "distance": 74794.646, "mapunitID": 27168, - "minCompDistance": 36837.7515, + "minCompDistance": 9085.2006, "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", + "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " } }, "texture": { @@ -2452,8 +2352,8 @@ "sl7": 1.17 }, "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz2", + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -2486,22 +2386,22 @@ }, "site": { "siteData": { - "componentID": 110985, - "distance": 55011.679, - "mapunitID": 17327, - "minCompDistance": 38961.9906, - "share": 40, + "componentID": 111641, + "distance": 63488.662, + "mapunitID": 17701, + "minCompDistance": 9861.4358, + "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", - "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", - "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -2525,22 +2425,22 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 11.2, - "sl5": 11.57, - "sl6": 12.2, - "sl7": 12.67 + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 41.0, + "sl5": 41.0, + "sl6": 41.0, + "sl7": 40.5 }, "clay": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 28.4, - "sl5": 29.86, - "sl6": 31.2, - "sl7": 31.83 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 56.8, + "sl5": 57.14, + "sl6": 57.0, + "sl7": 56.5 }, "ec": { "sl1": 0.0, @@ -2548,60 +2448,160 @@ "sl3": 0.0, "sl4": 0.2, "sl5": 0.43, - "sl6": 0.8, - "sl7": 1.0 + "sl6": 0.6, + "sl7": 0.67 }, "id": { - "component": "Gleyic solonchaks", - "name": "Gleyic solonchaks2", + "component": "Ferric luvisols", + "name": "Ferric luvisols2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 6.0, - "sl5": 6.03, - "sl6": 6.04, - "sl7": 6.08 + "sl1": 6.8, + "sl2": 6.8, + "sl3": 6.8, + "sl4": 7.02, + "sl5": 7.13, + "sl6": 7.26, + "sl7": 7.33 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 7.2, - "sl5": 9.71, - "sl6": 10.0, - "sl7": 8.83 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.14, + "sl6": 4.2, + "sl7": 4.0 }, "sand": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 34.2, - "sl5": 32.71, - "sl6": 31.0, - "sl7": 30.17 - }, - "site": { - "siteData": { - "componentID": 111103, - "distance": 60642.675, - "mapunitID": 17392, - "minCompDistance": 53068.3217, + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 12.4, + "sl5": 12.29, + "sl6": 12.4, + "sl7": 12.5 + }, + "site": { + "siteData": { + "componentID": 111335, + "distance": 41456.411, + "mapunitID": 17517, + "minCompDistance": 36837.7515, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", - "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", - "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." + "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + } + }, + "texture": { + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.2, + "sl5": 11.57, + "sl6": 12.2, + "sl7": 12.67 + }, + "clay": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 28.4, + "sl5": 29.86, + "sl6": 31.2, + "sl7": 31.83 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.8, + "sl7": 1.0 + }, + "id": { + "component": "Ferric luvisols", + "name": "Ferric luvisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 6.0, + "sl5": 6.03, + "sl6": 6.04, + "sl7": 6.08 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 7.2, + "sl5": 9.71, + "sl6": 10.0, + "sl7": 8.83 + }, + "sand": { + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 34.2, + "sl5": 32.71, + "sl6": 31.0, + "sl7": 30.17 + }, + "site": { + "siteData": { + "componentID": 116201, + "distance": 74794.646, + "mapunitID": 27168, + "minCompDistance": 36837.7515, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " } }, "texture": { @@ -2652,8 +2652,8 @@ "sl7": 0.83 }, "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols2", + "component": "Gleyic solonchaks", + "name": "Gleyic solonchaks2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -2686,22 +2686,22 @@ }, "site": { "siteData": { - "componentID": 110980, - "distance": 76138.236, - "mapunitID": 17324, - "minCompDistance": 70615.6896, + "componentID": 111103, + "distance": 60642.675, + "mapunitID": 17392, + "minCompDistance": 53068.3217, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", + "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." } }, "texture": { @@ -2753,7 +2753,7 @@ }, "id": { "component": "Eutric cambisols", - "name": "Eutric cambisols3", + "name": "Eutric cambisols2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -2784,6 +2784,106 @@ "sl6": 39.6, "sl7": 39.33 }, + "site": { + "siteData": { + "componentID": 110980, + "distance": 76138.236, + "mapunitID": 17324, + "minCompDistance": 70615.6896, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.6, + "sl5": 17.86, + "sl6": 18.4, + "sl7": 18.83 + }, + "clay": { + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 35.8, + "sl5": 36.71, + "sl6": 37.8, + "sl7": 38.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Eutric cambisols", + "name": "Eutric cambisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.96, + "sl5": 5.97, + "sl6": 6.02, + "sl7": 6.05 + }, + "rock_fragments": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 17.6, + "sl5": 17.14, + "sl6": 14.8, + "sl7": 15.83 + }, + "sand": { + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.6, + "sl5": 33.29, + "sl6": 32.8, + "sl7": 31.83 + }, "site": { "siteData": { "componentID": 110986, @@ -2823,51 +2923,75 @@ }, "soilRank": [ { - "component": "Humic cambisols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 111631, - "name": "Humic cambisols", + "componentID": 110986, + "name": "Eutric cambisols3", "rank_data": "1", "rank_data_loc": "1", - "rank_loc": "7", - "score_data": 0.747, + "rank_loc": "Not Displayed", + "score_data": 0.769, "score_data_loc": 1.0, "score_loc": 0.011 }, + { + "component": "Ferric luvisols", + "componentData": "Data Complete", + "componentID": 111336, + "name": "Ferric luvisols1", + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": "8", + "score_data": 0.749, + "score_data_loc": 0.974, + "score_loc": 0.011 + }, { "component": "Chromic cambisols", "componentData": "Data Complete", "componentID": 111105, "name": "Chromic cambisols1", - "rank_data": "2", - "rank_data_loc": "2", + "rank_data": "3", + "rank_data_loc": "3", "rank_loc": "4", "score_data": 0.724, - "score_data_loc": 0.973, + "score_data_loc": 0.945, "score_loc": 0.013 }, + { + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111101, + "name": "Eutric vertisols1", + "rank_data": "4", + "rank_data_loc": "4", + "rank_loc": "5", + "score_data": 0.724, + "score_data_loc": 0.942, + "score_loc": 0.011 + }, { "component": "Ferralic arenosols", "componentData": "Data Complete", "componentID": 111264, "name": "Ferralic arenosols2", - "rank_data": "5", - "rank_data_loc": "3", + "rank_data": "8", + "rank_data_loc": "5", "rank_loc": "Not Displayed", - "score_data": 0.705, - "score_data_loc": 0.971, + "score_data": 0.699, + "score_data_loc": 0.935, "score_loc": 0.03 }, { "component": "Haplic lixisols", "componentData": "Missing Data", - "componentID": 111208, + "componentID": 111240, "name": "Haplic lixisols1", - "rank_data": "7", - "rank_data_loc": "4", + "rank_data": "6", + "rank_data_loc": "6", "rank_loc": "3", - "score_data": 0.705, - "score_data_loc": 0.951, + "score_data": 0.713, + "score_data_loc": 0.934, "score_loc": 0.015 }, { @@ -2875,83 +2999,59 @@ "componentData": "Data Complete", "componentID": 111218, "name": "Calcic luvisols", - "rank_data": "3", - "rank_data_loc": "5", - "rank_loc": "10", - "score_data": 0.705, - "score_data_loc": 0.945, - "score_loc": 0.011 - }, - { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 111286, - "name": "Eutric vertisols2", - "rank_data": "4", - "rank_data_loc": "6", - "rank_loc": "Not Displayed", - "score_data": 0.705, - "score_data_loc": 0.945, - "score_loc": 0.011 - }, - { - "component": "Ferric luvisols", - "componentData": "Data Complete", - "componentID": 111336, - "name": "Ferric luvisols1", - "rank_data": "6", + "rank_data": "5", "rank_data_loc": "7", - "rank_loc": "8", - "score_data": 0.705, - "score_data_loc": 0.945, + "rank_loc": "9", + "score_data": 0.713, + "score_data_loc": 0.928, "score_loc": 0.011 }, { - "component": "Eutric cambisols", + "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 111337, - "name": "Eutric cambisols1", - "rank_data": "8", + "componentID": 111641, + "name": "Calcaric cambisols2", + "rank_data": "7", "rank_data_loc": "8", - "rank_loc": "12", - "score_data": 0.697, - "score_data_loc": 0.934, + "rank_loc": "Not Displayed", + "score_data": 0.699, + "score_data_loc": 0.91, "score_loc": 0.011 }, { - "component": "Gleyic solonchaks", + "component": "Humic cambisols", "componentData": "Data Complete", - "componentID": 111103, - "name": "Gleyic solonchaks2", + "componentID": 111631, + "name": "Humic cambisols", "rank_data": "9", "rank_data_loc": "9", - "rank_loc": "Not Displayed", - "score_data": 0.697, - "score_data_loc": 0.934, + "rank_loc": "7", + "score_data": 0.674, + "score_data_loc": 0.878, "score_loc": 0.011 }, { - "component": "Haplic solonetz", - "componentData": "Data Complete", - "componentID": 110985, - "name": "Haplic solonetz2", + "component": "Eutric gleysols", + "componentData": "Missing Data", + "componentID": 111314, + "name": "Eutric gleysols", "rank_data": "10", "rank_data_loc": "10", - "rank_loc": "Not Displayed", - "score_data": 0.697, - "score_data_loc": 0.934, + "rank_loc": "12", + "score_data": 0.657, + "score_data_loc": 0.857, "score_loc": 0.011 }, { - "component": "Calcaric cambisols", - "componentData": "Missing Data", - "componentID": 111282, - "name": "Calcaric cambisols1", + "component": "Gleyic solonchaks", + "componentData": "Data Complete", + "componentID": 111103, + "name": "Gleyic solonchaks2", "rank_data": "11", "rank_data_loc": "11", - "rank_loc": "6", - "score_data": 0.672, - "score_data_loc": 0.902, + "rank_loc": "Not Displayed", + "score_data": 0.594, + "score_data_loc": 0.776, "score_loc": 0.011 }, { @@ -2962,92 +3062,80 @@ "rank_data": "12", "rank_data_loc": "12", "rank_loc": "2", - "score_data": 0.125, - "score_data_loc": 0.196, + "score_data": 0.124, + "score_data_loc": 0.189, "score_loc": 0.024 }, { "component": "Haplic lixisols", - "componentData": "Data Complete", - "componentID": 111216, + "componentData": "Missing Data", + "componentID": 111208, "name": "Haplic lixisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.705, - "score_data_loc": 0.951, + "score_data": 0.713, + "score_data_loc": 0.934, "score_loc": 0.015 }, { - "component": "Ferric luvisols", - "componentData": "Data Complete", - "componentID": 111335, - "name": "Ferric luvisols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.705, - "score_data_loc": 0.945, - "score_loc": 0.011 - }, - { - "component": "Eutric cambisols", + "component": "Haplic lixisols", "componentData": "Data Complete", - "componentID": 110986, - "name": "Eutric cambisols3", + "componentID": 111216, + "name": "Haplic lixisols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.697, + "score_data": 0.713, "score_data_loc": 0.934, - "score_loc": 0.011 + "score_loc": 0.015 }, { - "component": "Calcaric cambisols", + "component": "Chromic cambisols", "componentData": "Data Complete", - "componentID": 111641, - "name": "Calcaric cambisols2", + "componentID": 111267, + "name": "Chromic cambisols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.665, - "score_data_loc": 0.893, - "score_loc": 0.011 + "score_data": 0.713, + "score_data_loc": 0.931, + "score_loc": 0.013 }, { - "component": "Gleyic solonchaks", - "componentData": "Missing Data", - "componentID": 111319, - "name": "Gleyic solonchaks1", + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 111337, + "name": "Eutric cambisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "11", - "score_data": 0.66, - "score_data_loc": 0.885, + "score_data": 0.713, + "score_data_loc": 0.928, "score_loc": 0.011 }, { - "component": "Chromic cambisols", - "componentData": "Missing Data", - "componentID": 111117, - "name": "Chromic cambisols2", + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111079, + "name": "Eutric vertisols5", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.633, - "score_data_loc": 0.853, - "score_loc": 0.013 + "score_data": 0.713, + "score_data_loc": 0.928, + "score_loc": 0.011 }, { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 111193, - "name": "Eutric vertisols4", + "component": "Ferric luvisols", + "componentData": "Data Complete", + "componentID": 111335, + "name": "Ferric luvisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.608, - "score_data_loc": 0.818, + "score_data": 0.713, + "score_data_loc": 0.928, "score_loc": 0.011 }, { @@ -3058,8 +3146,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.597, - "score_data_loc": 0.802, + "score_data": 0.699, + "score_data_loc": 0.91, "score_loc": 0.011 }, { @@ -3070,80 +3158,104 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.597, - "score_data_loc": 0.802, + "score_data": 0.699, + "score_data_loc": 0.91, "score_loc": 0.011 }, { - "component": "Haplic lixisols", - "componentData": "Data Complete", - "componentID": 116199, - "name": "Haplic lixisols3", + "component": "Eutric vertisols", + "componentData": "No Data", + "componentID": 111193, + "name": "Eutric vertisols4", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.583, - "score_data_loc": 0.79, - "score_loc": 0.015 + "score_data": 0.667, + "score_data_loc": 0.869, + "score_loc": 0.011 }, { "component": "Eutric vertisols", "componentData": "No Data", - "componentID": 111101, - "name": "Eutric vertisols1", + "componentID": 111202, + "name": "Eutric vertisols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "5", - "score_data": 0.587, - "score_data_loc": 0.789, + "rank_loc": "Not Displayed", + "score_data": 0.618, + "score_data_loc": 0.806, "score_loc": 0.011 }, { "component": "Eutric vertisols", "componentData": "No Data", - "componentID": 111202, - "name": "Eutric vertisols3", + "componentID": 116200, + "name": "Eutric vertisols6", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.587, - "score_data_loc": 0.789, + "score_data": 0.594, + "score_data_loc": 0.776, + "score_loc": 0.011 + }, + { + "component": "Haplic lixisols", + "componentData": "Data Complete", + "componentID": 116199, + "name": "Haplic lixisols4", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.585, + "score_data_loc": 0.77, + "score_loc": 0.015 + }, + { + "component": "Calcaric cambisols", + "componentData": "Missing Data", + "componentID": 111282, + "name": "Calcaric cambisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "6", + "score_data": 0.589, + "score_data_loc": 0.769, "score_loc": 0.011 }, { "component": "Eutric vertisols", "componentData": "No Data", - "componentID": 111079, - "name": "Eutric vertisols5", + "componentID": 111286, + "name": "Eutric vertisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.587, - "score_data_loc": 0.789, + "score_data": 0.589, + "score_data_loc": 0.769, "score_loc": 0.011 }, { - "component": "Haplic solonetz", - "componentData": "Data Complete", - "componentID": 111044, - "name": "Haplic solonetz1", + "component": "Gleyic solonchaks", + "componentData": "Missing Data", + "componentID": 111319, + "name": "Gleyic solonchaks1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "9", - "score_data": 0.587, - "score_data_loc": 0.789, + "rank_loc": "10", + "score_data": 0.589, + "score_data_loc": 0.769, "score_loc": 0.011 }, { "component": "Chromic cambisols", - "componentData": "Data Complete", - "componentID": 111267, - "name": "Chromic cambisols3", + "componentData": "Missing Data", + "componentID": 111117, + "name": "Chromic cambisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.583, - "score_data_loc": 0.787, + "score_data": 0.585, + "score_data_loc": 0.767, "score_loc": 0.013 }, { @@ -3154,8 +3266,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "1", - "score_data": 0.245, - "score_data_loc": 0.364, + "score_data": 0.243, + "score_data_loc": 0.351, "score_loc": 0.03 } ] diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json index 69dee36..2b33b56 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json @@ -1152,8 +1152,8 @@ "sl7": 0.0 }, "id": { - "component": "Umbric gleysols", - "name": "Umbric gleysols", + "component": "Haplic luvisols", + "name": "Haplic luvisols", "rank_loc": "12", "score_loc": 0.027 }, @@ -1186,22 +1186,22 @@ }, "site": { "siteData": { - "componentID": 112974, - "distance": 54381.47, - "mapunitID": 18406, - "minCompDistance": 54381.47, - "share": 60, + "componentID": 113128, + "distance": 95990.463, + "mapunitID": 18450, + "minCompDistance": 95990.4626, + "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ", - "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", - "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. " + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { @@ -1725,31 +1725,31 @@ "sl7": 120 }, "cec": { - "sl1": 28.0, - "sl2": 28.0, - "sl3": 28.0, - "sl4": 26.2, - "sl5": 24.71, - "sl6": 23.0, - "sl7": 21.5 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 13.8, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 13.83 }, "clay": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 49.0, - "sl5": 48.43, - "sl6": 46.8, - "sl7": 46.33 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.6, + "sl5": 20.14, + "sl6": 20.2, + "sl7": 20.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.4, - "sl7": 0.33 + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { "component": "Eutric planosols", @@ -1758,31 +1758,31 @@ "score_loc": 0.036 }, "ph": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 4.9, - "sl5": 4.91, - "sl6": 4.9, - "sl7": 4.9 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.14, + "sl5": 7.21, + "sl6": 7.34, + "sl7": 7.42 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 10.0, - "sl5": 11.43, - "sl6": 13.4, - "sl7": 14.33 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.71, + "sl6": 17.8, + "sl7": 17.83 }, "sand": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 25.0, - "sl5": 26.14, - "sl6": 27.6, - "sl7": 27.83 + "sl1": 64.0, + "sl2": 64.0, + "sl3": 64.0, + "sl4": 61.2, + "sl5": 60.86, + "sl6": 60.8, + "sl7": 60.83 }, "site": { "siteData": { @@ -1805,13 +1805,13 @@ } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } } ] @@ -1827,7 +1827,7 @@ "componentData": "Data Complete", "componentID": 113242, "name": "Salic fluvisols2", - "rank_data": "7", + "rank_data": "8", "rank_data_loc": "1", "rank_loc": "Not Displayed", "score_data": 0.9, @@ -1851,7 +1851,7 @@ "componentData": "Data Complete", "componentID": 113477, "name": "Mollic fluvisols", - "rank_data": "6", + "rank_data": "7", "rank_data_loc": "3", "rank_loc": "3", "score_data": 0.9, @@ -1875,20 +1875,32 @@ "componentData": "Data Complete", "componentID": 112871, "name": "Ferralic arenosols1", - "rank_data": "3", + "rank_data": "4", "rank_data_loc": "5", "rank_loc": "7", "score_data": 0.9, "score_data_loc": 0.947, "score_loc": 0.039 }, + { + "component": "Eutric planosols", + "componentData": "Missing Data", + "componentID": 113443, + "name": "Eutric planosols2", + "rank_data": "3", + "rank_data_loc": "6", + "rank_loc": "Not Displayed", + "score_data": 0.9, + "score_data_loc": 0.945, + "score_loc": 0.036 + }, { "component": "Haplic arenosols", "componentData": "Data Complete", "componentID": 113413, "name": "Haplic arenosols", - "rank_data": "5", - "rank_data_loc": "6", + "rank_data": "6", + "rank_data_loc": "7", "rank_loc": "9", "score_data": 0.9, "score_data_loc": 0.945, @@ -1899,31 +1911,19 @@ "componentData": "Data Complete", "componentID": 113054, "name": "Gleyic solonetz", - "rank_data": "4", - "rank_data_loc": "7", + "rank_data": "5", + "rank_data_loc": "8", "rank_loc": "11", "score_data": 0.9, "score_data_loc": 0.936, "score_loc": 0.027 }, - { - "component": "Eutric planosols", - "componentData": "Missing Data", - "componentID": 113443, - "name": "Eutric planosols2", - "rank_data": "8", - "rank_data_loc": "8", - "rank_loc": "Not Displayed", - "score_data": 0.833, - "score_data_loc": 0.877, - "score_loc": 0.036 - }, { "component": "Haplic solonetz", "componentData": "Data Complete", "componentID": 112902, "name": "Haplic solonetz2", - "rank_data": "10", + "rank_data": "11", "rank_data_loc": "9", "rank_loc": "Not Displayed", "score_data": 0.756, @@ -1943,11 +1943,11 @@ "score_loc": 0.045 }, { - "component": "Umbric gleysols", - "componentData": "Missing Data", - "componentID": 112974, - "name": "Umbric gleysols", - "rank_data": "11", + "component": "Haplic luvisols", + "componentData": "Data Complete", + "componentID": 113128, + "name": "Haplic luvisols", + "rank_data": "10", "rank_data_loc": "11", "rank_loc": "12", "score_data": 0.756, diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json index 30300a2..b41d304 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json @@ -414,6 +414,106 @@ "sl7": "Loam" } }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Rendzic leptosols", + "name": "Rendzic leptosols", + "rank_loc": "5", + "score_loc": 0.003 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 129097, + "distance": 47480.618, + "mapunitID": 33127, + "minCompDistance": 47480.6175, + "share": 82, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Description_es": "Los Leptosoles Rendzicos tienen un volumen de enraizamiento muy limitado debido a la roca continua, material altamente calcáreo, horizontes cementados, o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles Rendzic son altamente calcáreos en la superficie del suelo. ", + "Description_fr": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Description_ks": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo será alto (> 7,0) en estos suelos, y no será necesario el encalado.
Cualquier uso agrícola debe ser para el pastoreo o la agrosilvicultura, con el mantenimiento continuo de la cubierta.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, { "bottom_depth": { "sl1": 1, @@ -452,9 +552,9 @@ "sl7": 0.5 }, "id": { - "component": "Rendzic leptosols", - "name": "Rendzic leptosols", - "rank_loc": "5", + "component": "Calcaric arenosols", + "name": "Calcaric arenosols1", + "rank_loc": "6", "score_loc": 0.003 }, "ph": { @@ -486,22 +586,22 @@ }, "site": { "siteData": { - "componentID": 129097, - "distance": 47480.618, - "mapunitID": 33127, - "minCompDistance": 47480.6175, - "share": 82, - "soilDepth": 40 + "componentID": 130338, + "distance": 94026.373, + "mapunitID": 33860, + "minCompDistance": 94026.3732, + "share": 65, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", - "Description_es": "Los Leptosoles Rendzicos tienen un volumen de enraizamiento muy limitado debido a la roca continua, material altamente calcáreo, horizontes cementados, o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles Rendzic son altamente calcáreos en la superficie del suelo. ", - "Description_fr": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", - "Description_ks": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo será alto (> 7,0) en estos suelos, y no será necesario el encalado.
Cualquier uso agrícola debe ser para el pastoreo o la agrosilvicultura, con el mantenimiento continuo de la cubierta.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", + "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " } }, "texture": { @@ -552,9 +652,9 @@ "sl7": 1.83 }, "id": { - "component": "Calcaric arenosols", - "name": "Calcaric arenosols1", - "rank_loc": "6", + "component": "Calcic luvisols", + "name": "Calcic luvisols", + "rank_loc": "7", "score_loc": 0.003 }, "ph": { @@ -586,22 +686,22 @@ }, "site": { "siteData": { - "componentID": 130338, - "distance": 94026.373, - "mapunitID": 33860, - "minCompDistance": 94026.3732, - "share": 65, + "componentID": 129392, + "distance": 87650.254, + "mapunitID": 33303, + "minCompDistance": 87650.2544, + "share": 77, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", - "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " } }, "texture": { @@ -652,10 +752,10 @@ "sl7": 1.83 }, "id": { - "component": "Calcic luvisols", - "name": "Calcic luvisols", - "rank_loc": "7", - "score_loc": 0.003 + "component": "Calcaric fluvisols", + "name": "Calcaric fluvisols", + "rank_loc": "8", + "score_loc": 0.002 }, "ph": { "sl1": 8.2, @@ -686,22 +786,22 @@ }, "site": { "siteData": { - "componentID": 129392, - "distance": 87650.254, - "mapunitID": 33303, - "minCompDistance": 87650.2544, - "share": 77, + "componentID": 129425, + "distance": 51610.989, + "mapunitID": 33320, + "minCompDistance": 51610.9891, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", - "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { @@ -752,10 +852,10 @@ "sl7": 1.83 }, "id": { - "component": "Calcaric fluvisols", - "name": "Calcaric fluvisols", - "rank_loc": "8", - "score_loc": 0.002 + "component": "Regosols", + "name": "Regosols", + "rank_loc": "9", + "score_loc": 0.001 }, "ph": { "sl1": 8.2, @@ -786,22 +886,22 @@ }, "site": { "siteData": { - "componentID": 129425, - "distance": 51610.989, - "mapunitID": 33320, - "minCompDistance": 51610.9891, - "share": 10, + "componentID": 132579, + "distance": 93564.378, + "mapunitID": 3512, + "minCompDistance": 93564.3781, + "share": 33, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", - "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", - "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", - "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + "Description_en": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Description_es": "Los Regosoles son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad. ", + "Description_fr": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Description_ks": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { @@ -852,9 +952,9 @@ "sl7": 1.83 }, "id": { - "component": "Regosols", - "name": "Regosols", - "rank_loc": "9", + "component": "Umbric leptosols", + "name": "Umbric leptosols", + "rank_loc": "10", "score_loc": 0.001 }, "ph": { @@ -886,22 +986,22 @@ }, "site": { "siteData": { - "componentID": 132579, - "distance": 93564.378, - "mapunitID": 3512, - "minCompDistance": 93564.3781, - "share": 33, - "soilDepth": 200 + "componentID": 132400, + "distance": 84530.897, + "mapunitID": 3503, + "minCompDistance": 84530.8969, + "share": 25, + "soilDepth": 40 }, "siteDescription": { - "Description_en": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", - "Description_es": "Los Regosoles son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad. ", - "Description_fr": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", - "Description_ks": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + "Description_en": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", + "Description_es": "Los Leptosoles Úmbricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles umbrosos tienen un horizonte superficial grueso con un alto contenido de materia orgánica y una baja saturación de la base que se superpone a una capa que limita las raíces. ", + "Description_fr": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", + "Description_ks": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo del horizonte superficial será bajo (< 5,0) y se necesitará encalado para el uso de pastoreo o agroforestal.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cubierta.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " } }, "texture": { @@ -952,9 +1052,9 @@ "sl7": 1.5 }, "id": { - "component": "Umbric leptosols", - "name": "Umbric leptosols", - "rank_loc": "10", + "component": "Cambisols", + "name": "Cambisols", + "rank_loc": "11", "score_loc": 0.001 }, "ph": { @@ -986,22 +1086,22 @@ }, "site": { "siteData": { - "componentID": 132400, + "componentID": 132402, "distance": 84530.897, "mapunitID": 3503, "minCompDistance": 84530.8969, "share": 25, - "soilDepth": 40 + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", - "Description_es": "Los Leptosoles Úmbricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles umbrosos tienen un horizonte superficial grueso con un alto contenido de materia orgánica y una baja saturación de la base que se superpone a una capa que limita las raíces. ", - "Description_fr": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", - "Description_ks": "Umbric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Umbric Leptosols have a thick surface horizon with high organic matter and low base saturation overlying a root limiting layer. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo del horizonte superficial será bajo (< 5,0) y se necesitará encalado para el uso de pastoreo o agroforestal.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cubierta.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
The surface horizon soil pH will be low (< 5.0) and liming will be needed for grazing or agroforestry use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + "Description_en": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los cambisoles tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -1036,10 +1136,10 @@ "sl3": 1.0 }, "id": { - "component": "Cambisols", - "name": "Cambisols", - "rank_loc": "11", - "score_loc": 0.001 + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.007 }, "ph": { "sl1": 7.4, @@ -1058,22 +1158,22 @@ }, "site": { "siteData": { - "componentID": 132402, - "distance": 84530.897, - "mapunitID": 3503, - "minCompDistance": 84530.8969, - "share": 25, + "componentID": 128926, + "distance": 8501.441, + "mapunitID": 33019, + "minCompDistance": 3776.1698, + "share": 21, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los cambisoles tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -1105,7 +1205,7 @@ }, "id": { "component": "Calcaric cambisols", - "name": "Calcaric cambisols2", + "name": "Calcaric cambisols3", "rank_loc": "Not Displayed", "score_loc": 0.007 }, @@ -1126,11 +1226,11 @@ }, "site": { "siteData": { - "componentID": 128926, - "distance": 8501.441, - "mapunitID": 33019, + "componentID": 129002, + "distance": 17680.575, + "mapunitID": 33067, "minCompDistance": 3776.1698, - "share": 21, + "share": 90, "soilDepth": 200 }, "siteDescription": { @@ -1189,7 +1289,7 @@ }, "id": { "component": "Calcaric cambisols", - "name": "Calcaric cambisols3", + "name": "Calcaric cambisols4", "rank_loc": "Not Displayed", "score_loc": 0.007 }, @@ -1277,7 +1377,7 @@ }, "id": { "component": "Calcaric cambisols", - "name": "Calcaric cambisols4", + "name": "Calcaric cambisols5", "rank_loc": "Not Displayed", "score_loc": 0.007 }, @@ -1365,7 +1465,7 @@ }, "id": { "component": "Calcaric cambisols", - "name": "Calcaric cambisols5", + "name": "Calcaric cambisols6", "rank_loc": "Not Displayed", "score_loc": 0.007 }, @@ -2039,7 +2139,7 @@ "componentData": "Data Complete", "componentID": 133064, "name": "Histosols", - "rank_data": "4", + "rank_data": "5", "rank_data_loc": "3", "rank_loc": "4", "score_data": 1.0, @@ -2058,13 +2158,25 @@ "score_data_loc": 0.996, "score_loc": 0.003 }, + { + "component": "Cambisols", + "componentData": "Data Complete", + "componentID": 132402, + "name": "Cambisols", + "rank_data": "4", + "rank_data_loc": "5", + "rank_loc": "11", + "score_data": 1.0, + "score_data_loc": 0.994, + "score_loc": 0.001 + }, { "component": "Calcic luvisols", "componentData": "Data Complete", "componentID": 129392, "name": "Calcic luvisols", "rank_data": "9", - "rank_data_loc": "5", + "rank_data_loc": "6", "rank_loc": "7", "score_data": 0.613, "score_data_loc": 0.611, @@ -2076,7 +2188,7 @@ "componentID": 129425, "name": "Calcaric fluvisols", "rank_data": "8", - "rank_data_loc": "6", + "rank_data_loc": "7", "rank_loc": "8", "score_data": 0.613, "score_data_loc": 0.611, @@ -2087,21 +2199,9 @@ "componentData": "Data Complete", "componentID": 132579, "name": "Regosols", - "rank_data": "11", - "rank_data_loc": "7", - "rank_loc": "9", - "score_data": 0.613, - "score_data_loc": 0.609, - "score_loc": 0.001 - }, - { - "component": "Cambisols", - "componentData": "Data Complete", - "componentID": 132402, - "name": "Cambisols", "rank_data": "10", "rank_data_loc": "8", - "rank_loc": "11", + "rank_loc": "9", "score_data": 0.613, "score_data_loc": 0.609, "score_loc": 0.001 @@ -2109,11 +2209,11 @@ { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 128898, - "name": "Lithic leptosols1", - "rank_data": "5", + "componentID": 129499, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", "rank_data_loc": "9", - "rank_loc": "3", + "rank_loc": "Not Displayed", "score_data": 1.0, "score_data_loc": 0.002, "score_loc": 0.006 @@ -2126,7 +2226,7 @@ "rank_data": "7", "rank_data_loc": "10", "rank_loc": "5", - "score_data": 0.63, + "score_data": 1.0, "score_data_loc": 0.002, "score_loc": 0.003 }, @@ -2135,18 +2235,18 @@ "componentData": "Missing Data", "componentID": 132400, "name": "Umbric leptosols", - "rank_data": "6", + "rank_data": "11", "rank_data_loc": "11", "rank_loc": "10", - "score_data": 1.0, + "score_data": 0.613, "score_data_loc": 0.002, "score_loc": 0.001 }, { "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 128926, - "name": "Calcaric cambisols2", + "componentID": 129002, + "name": "Calcaric cambisols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2158,7 +2258,7 @@ "component": "Calcaric cambisols", "componentData": "Data Complete", "componentID": 128910, - "name": "Calcaric cambisols4", + "name": "Calcaric cambisols5", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2182,7 +2282,7 @@ "component": "Calcaric cambisols", "componentData": "Data Complete", "componentID": 128904, - "name": "Calcaric cambisols3", + "name": "Calcaric cambisols4", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2191,22 +2291,34 @@ "score_loc": 0.007 }, { - "component": "Calcaric regosols", + "component": "Calcaric arenosols", "componentData": "Data Complete", - "componentID": 128899, - "name": "Calcaric regosols3", + "componentID": 130338, + "name": "Calcaric arenosols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "6", + "score_data": 0.63, + "score_data_loc": 0.629, + "score_loc": 0.003 + }, + { + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 128926, + "name": "Calcaric cambisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", "score_data": 0.613, - "score_data_loc": 0.615, + "score_data_loc": 0.616, "score_loc": 0.007 }, { "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 129500, - "name": "Calcaric regosols5", + "componentID": 128899, + "name": "Calcaric regosols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2215,22 +2327,22 @@ "score_loc": 0.007 }, { - "component": "Calcaric arenosols", + "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 130338, - "name": "Calcaric arenosols1", + "componentID": 129500, + "name": "Calcaric regosols5", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "6", + "rank_loc": "Not Displayed", "score_data": 0.613, - "score_data_loc": 0.612, - "score_loc": 0.003 + "score_data_loc": 0.615, + "score_loc": 0.007 }, { "component": "Calcaric cambisols", "componentData": "Data Complete", "componentID": 129504, - "name": "Calcaric cambisols5", + "name": "Calcaric cambisols6", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2253,11 +2365,11 @@ { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 129499, - "name": "Lithic leptosols2", - "rank_data": "Not Displayed", + "componentID": 128898, + "name": "Lithic leptosols1", + "rank_data": "6", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", + "rank_loc": "3", "score_data": 1.0, "score_data_loc": 0.002, "score_loc": 0.006 diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json index b526170..eaeff9c 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json @@ -1004,8 +1004,8 @@ "sl3": 1.0 }, "id": { - "component": "Eutric planosols", - "name": "Eutric planosols", + "component": "Humic cambisols", + "name": "Humic cambisols", "rank_loc": "11", "score_loc": 0.018 }, @@ -1026,22 +1026,22 @@ }, "site": { "siteData": { - "componentID": 157545, - "distance": 65551.867, - "mapunitID": 9722, - "minCompDistance": 65551.8665, + "componentID": 157468, + "distance": 37691.376, + "mapunitID": 9697, + "minCompDistance": 37691.3759, "share": 50, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", - "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + "Description_en": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Description_es": "Los Cambisoles Húmicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos tienen más materia orgánica en los horizontes superficiales.
Cuando el clima y el paisaje son favorables, estos suelos pueden ser productivos. ", + "Description_fr": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Description_ks": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -1461,31 +1461,31 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 13.6, - "sl5": 15.0, - "sl6": 16.4, - "sl7": 16.83 + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 21.6, + "sl5": 19.86, + "sl6": 18.2, + "sl7": 17.17 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 24.4, - "sl5": 26.86, - "sl6": 29.2, - "sl7": 30.0 + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 22.0, + "sl5": 21.86, + "sl6": 21.4, + "sl7": 21.0 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 }, "id": { "component": "Chromic luvisols", @@ -1494,31 +1494,31 @@ "score_loc": 0.029 }, "ph": { - "sl1": 6.1, - "sl2": 6.1, - "sl3": 6.1, - "sl4": 6.26, - "sl5": 6.37, - "sl6": 6.52, - "sl7": 6.57 + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.18, + "sl5": 5.21, + "sl6": 5.26, + "sl7": 5.28 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.6, - "sl5": 2.57, - "sl6": 2.4, - "sl7": 2.33 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 18.4, + "sl5": 19.71, + "sl6": 22.0, + "sl7": 23.67 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 46.0, - "sl5": 44.14, - "sl6": 42.2, - "sl7": 42.0 + "sl1": 44.0, + "sl2": 44.0, + "sl3": 44.0, + "sl4": 44.2, + "sl5": 44.71, + "sl6": 45.8, + "sl7": 46.67 }, "site": { "siteData": { @@ -1546,8 +1546,8 @@ "sl3": "Loam", "sl4": "Loam", "sl5": "Loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -1683,10 +1683,10 @@ "score_loc": 0.021 }, { - "component": "Eutric planosols", + "component": "Humic cambisols", "componentData": "Data Complete", - "componentID": 157545, - "name": "Eutric planosols", + "componentID": 157468, + "name": "Humic cambisols", "rank_data": "3", "rank_data_loc": "3", "rank_loc": "11", @@ -1702,8 +1702,8 @@ "rank_data": "4", "rank_data_loc": "4", "rank_loc": "Not Displayed", - "score_data": 0.737, - "score_data_loc": 0.77, + "score_data": 0.753, + "score_data_loc": 0.787, "score_loc": 0.029 }, { @@ -1714,45 +1714,45 @@ "rank_data": "5", "rank_data_loc": "5", "rank_loc": "3", - "score_data": 0.731, - "score_data_loc": 0.769, + "score_data": 0.748, + "score_data_loc": 0.785, "score_loc": 0.033 }, { - "component": "Calcaric cambisols", + "component": "Chromic luvisols", "componentData": "Data Complete", - "componentID": 157401, - "name": "Calcaric cambisols1", - "rank_data": "11", + "componentID": 157477, + "name": "Chromic luvisols2", + "rank_data": "7", "rank_data_loc": "6", - "rank_loc": "2", - "score_data": 0.634, - "score_data_loc": 0.725, - "score_loc": 0.086 + "rank_loc": "Not Displayed", + "score_data": 0.711, + "score_data_loc": 0.744, + "score_loc": 0.029 }, { "component": "Calcaric fluvisols", "componentData": "Data Complete", "componentID": 157400, "name": "Calcaric fluvisols", - "rank_data": "7", + "rank_data": "8", "rank_data_loc": "7", "rank_loc": "6", - "score_data": 0.681, - "score_data_loc": 0.714, + "score_data": 0.697, + "score_data_loc": 0.73, "score_loc": 0.029 }, { - "component": "Chromic luvisols", - "componentData": "Missing Data", - "componentID": 157483, - "name": "Chromic luvisols1", - "rank_data": "8", + "component": "Calcaric cambisols", + "componentData": "Data Complete", + "componentID": 157401, + "name": "Calcaric cambisols1", + "rank_data": "11", "rank_data_loc": "8", - "rank_loc": "7", - "score_data": 0.681, - "score_data_loc": 0.714, - "score_loc": 0.029 + "rank_loc": "2", + "score_data": 0.614, + "score_data_loc": 0.704, + "score_loc": 0.086 }, { "component": "Calcic luvisols", @@ -1762,8 +1762,8 @@ "rank_data": "9", "rank_data_loc": "9", "rank_loc": "4", - "score_data": 0.643, - "score_data_loc": 0.676, + "score_data": 0.627, + "score_data_loc": 0.66, "score_loc": 0.029 }, { @@ -1774,8 +1774,8 @@ "rank_data": "10", "rank_data_loc": "10", "rank_loc": "12", - "score_data": 0.643, - "score_data_loc": 0.665, + "score_data": 0.627, + "score_data_loc": 0.649, "score_loc": 0.018 }, { @@ -1786,8 +1786,8 @@ "rank_data": "12", "rank_data_loc": "11", "rank_loc": "9", - "score_data": 0.634, - "score_data_loc": 0.664, + "score_data": 0.614, + "score_data_loc": 0.643, "score_loc": 0.025 }, { @@ -1798,20 +1798,20 @@ "rank_data": "6", "rank_data_loc": "12", "rank_loc": "8", - "score_data": 0.731, + "score_data": 0.748, "score_data_loc": 0.002, "score_loc": 0.029 }, { "component": "Chromic luvisols", - "componentData": "Data Complete", - "componentID": 157477, - "name": "Chromic luvisols2", + "componentData": "Missing Data", + "componentID": 157483, + "name": "Chromic luvisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.629, - "score_data_loc": 0.662, + "rank_loc": "7", + "score_data": 0.697, + "score_data_loc": 0.73, "score_loc": 0.029 }, { @@ -1822,8 +1822,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "5", - "score_data": 0.625, - "score_data_loc": 0.658, + "score_data": 0.62, + "score_data_loc": 0.652, "score_loc": 0.029 }, { @@ -1834,8 +1834,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.528, - "score_data_loc": 0.618, + "score_data": 0.548, + "score_data_loc": 0.638, "score_loc": 0.086 }, { @@ -1846,8 +1846,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.291, - "score_data_loc": 0.321, + "score_data": 0.311, + "score_data_loc": 0.342, "score_loc": 0.029 }, { @@ -1858,7 +1858,7 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.614, + "score_data": 0.594, "score_data_loc": 0.002, "score_loc": 0.029 } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json index c2f07a3..90782ea 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json @@ -625,89 +625,89 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 14.6, - "sl5": 13.57, - "sl6": 12.8, - "sl7": 12.33 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 28.4, + "sl5": 25.71, + "sl6": 22.6, + "sl7": 21.17 }, "clay": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 14.2, - "sl5": 14.43, - "sl6": 14.6, - "sl7": 14.5 + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 26.8, + "sl5": 26.57, + "sl6": 26.0, + "sl7": 25.67 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.29, - "sl6": 1.2, - "sl7": 1.17 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 1.0, + "sl7": 1.33 }, "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols", + "component": "Mollic gleysols", + "name": "Mollic gleysols", "rank_loc": "7", "score_loc": 0.035 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.36, - "sl5": 6.44, - "sl6": 6.54, - "sl7": 6.6 + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.98, + "sl5": 7.09, + "sl6": 7.2, + "sl7": 7.25 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 18.8, - "sl5": 20.71, - "sl6": 23.0, - "sl7": 24.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 2.2, + "sl5": 2.43, + "sl6": 2.8, + "sl7": 3.0 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 42.2, - "sl5": 43.43, - "sl6": 45.0, - "sl7": 46.0 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 34.0, + "sl5": 34.57, + "sl6": 35.8, + "sl7": 36.67 }, "site": { "siteData": { - "componentID": 104610, - "distance": 49566.694, - "mapunitID": 11920, - "minCompDistance": 49566.6944, + "componentID": 104132, + "distance": 31367.734, + "mapunitID": 11539, + "minCompDistance": 31367.734, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", + "Description_es": "Los Mollic Gleysols tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles móllicos tienen relativamente más materia orgánica y nutrientes en los horizontes superficiales.", + "Description_fr": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", + "Description_ks": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", "sl4": "Loam", "sl5": "Loam", "sl6": "Loam", @@ -1227,7 +1227,7 @@ "componentData": "Data Complete", "componentID": 103927, "name": "Haplic andosols", - "rank_data": "3", + "rank_data": "2", "rank_data_loc": "1", "rank_loc": 1, "score_data": 0.431, @@ -1239,7 +1239,7 @@ "componentData": "Data Complete", "componentID": 103604, "name": "Haplic phaeozems", - "rank_data": "4", + "rank_data": "3", "rank_data_loc": "2", "rank_loc": 2, "score_data": 0.431, @@ -1258,25 +1258,13 @@ "score_data_loc": 0.814, "score_loc": 0.035 }, - { - "component": "Eutric cambisols", - "componentData": "Data Complete", - "componentID": 104610, - "name": "Eutric cambisols", - "rank_data": "2", - "rank_data_loc": "4", - "rank_loc": 7, - "score_data": 0.431, - "score_data_loc": 0.814, - "score_loc": 0.035 - }, { "component": "Gleyic luvisols", "componentData": "Missing Data", "componentID": 104608, "name": "Gleyic luvisols", - "rank_data": "5", - "rank_data_loc": "5", + "rank_data": "4", + "rank_data_loc": "4", "rank_loc": 8, "score_data": 0.385, "score_data_loc": 0.733, @@ -1287,8 +1275,8 @@ "componentData": "Data Complete", "componentID": 104597, "name": "Haplic luvisols", - "rank_data": "6", - "rank_data_loc": "6", + "rank_data": "5", + "rank_data_loc": "5", "rank_loc": 6, "score_data": 0.385, "score_data_loc": 0.733, @@ -1299,8 +1287,8 @@ "componentData": "Data Complete", "componentID": 103928, "name": "Umbric andosols", - "rank_data": "7", - "rank_data_loc": "7", + "rank_data": "6", + "rank_data_loc": "6", "rank_loc": 3, "score_data": 0.385, "score_data_loc": 0.733, @@ -1311,8 +1299,8 @@ "componentData": "Data Complete", "componentID": 103635, "name": "Calcic chernozems", - "rank_data": "8", - "rank_data_loc": "8", + "rank_data": "7", + "rank_data_loc": "7", "rank_loc": 12, "score_data": 0.068, "score_data_loc": 0.181, @@ -1323,8 +1311,8 @@ "componentData": "Data Complete", "componentID": 104276, "name": "Eutric gleysols", - "rank_data": "9", - "rank_data_loc": "9", + "rank_data": "8", + "rank_data_loc": "8", "rank_loc": 5, "score_data": 0.068, "score_data_loc": 0.181, @@ -1335,8 +1323,8 @@ "componentData": "Data Complete", "componentID": 103642, "name": "Gleyic chernozems", - "rank_data": "10", - "rank_data_loc": "10", + "rank_data": "9", + "rank_data_loc": "9", "rank_loc": 11, "score_data": 0.068, "score_data_loc": 0.181, @@ -1347,9 +1335,21 @@ "componentData": "Missing Data", "componentID": 103605, "name": "Gleyic phaeozems", + "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": 4, + "score_data": 0.068, + "score_data_loc": 0.181, + "score_loc": 0.035 + }, + { + "component": "Mollic gleysols", + "componentData": "Data Complete", + "componentID": 104132, + "name": "Mollic gleysols", "rank_data": "11", "rank_data_loc": "11", - "rank_loc": 4, + "rank_loc": 7, "score_data": 0.068, "score_data_loc": 0.181, "score_loc": 0.035 diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json index 3f0a8ba..fb213d6 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json @@ -490,6 +490,106 @@ "sl4": "Loam" } }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 6.4, + "sl5": 6.29, + "sl6": 6.2, + "sl7": 6.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 28.8, + "sl5": 31.14, + "sl6": 33.4, + "sl7": 34.33 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Haplic acrisols", + "name": "Haplic acrisols1", + "rank_loc": "6", + "score_loc": 0.016 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.04, + "sl5": 5.03, + "sl6": 5.02, + "sl7": 5.02 + }, + "rock_fragments": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 14.0 + }, + "sand": { + "sl1": 59.0, + "sl2": 59.0, + "sl3": 59.0, + "sl4": 54.4, + "sl5": 52.29, + "sl6": 50.2, + "sl7": 49.17 + }, + "site": { + "siteData": { + "componentID": 134061, + "distance": 33211.766, + "mapunitID": 36185, + "minCompDistance": 33211.7658, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, { "bottom_depth": { "sl1": 1, @@ -514,7 +614,7 @@ "id": { "component": "Lithic leptosols", "name": "Lithic leptosols1", - "rank_loc": "6", + "rank_loc": "7", "score_loc": 0.016 }, "ph": { @@ -580,10 +680,10 @@ "sl3": 1.0 }, "id": { - "component": "Haplic acrisols", - "name": "Haplic acrisols", - "rank_loc": "7", - "score_loc": 0.016 + "component": "Ferric lixisols", + "name": "Ferric lixisols", + "rank_loc": "8", + "score_loc": 0.014 }, "ph": { "sl1": 6.7, @@ -602,22 +702,22 @@ }, "site": { "siteData": { - "componentID": 133287, - "distance": 49166.71, - "mapunitID": 36011, - "minCompDistance": 49166.7104, - "share": 20, + "componentID": 107928, + "distance": 34218.133, + "mapunitID": 1444, + "minCompDistance": 34218.1332, + "share": 50, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_es": "Los Lixisoles Férricos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta.
Los Lixisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", + "Description_fr": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Description_ks": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.
Estos suelos son especialmente sensibles a la erosión, por lo que se necesitan prácticas que trabajen para mantener una estructura fuerte del suelo (como los cultivos perennes).", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. " } }, "texture": { @@ -664,10 +764,10 @@ "sl7": 0.0 }, "id": { - "component": "Ferric lixisols", - "name": "Ferric lixisols", - "rank_loc": "8", - "score_loc": 0.014 + "component": "Dystric gleysols", + "name": "Dystric gleysols", + "rank_loc": "9", + "score_loc": 0.011 }, "ph": { "sl1": 5.1, @@ -698,22 +798,22 @@ }, "site": { "siteData": { - "componentID": 107928, - "distance": 34218.133, - "mapunitID": 1444, - "minCompDistance": 34218.1332, - "share": 50, + "componentID": 133232, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Lixisoles Férricos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta.
Los Lixisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.
Estos suelos son especialmente sensibles a la erosión, por lo que se necesitan prácticas que trabajen para mantener una estructura fuerte del suelo (como los cultivos perennes).", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. " + "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. " } }, "texture": { @@ -764,9 +864,9 @@ "sl7": 0.0 }, "id": { - "component": "Dystric gleysols", - "name": "Dystric gleysols", - "rank_loc": "9", + "component": "Dystric fluvisols", + "name": "Dystric fluvisols1", + "rank_loc": "10", "score_loc": 0.011 }, "ph": { @@ -798,7 +898,7 @@ }, "site": { "siteData": { - "componentID": 133232, + "componentID": 133237, "distance": 0.0, "mapunitID": 36001, "minCompDistance": 0.0, @@ -806,14 +906,14 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", - "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", - "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", - "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", - "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. " + "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " } }, "texture": { @@ -864,9 +964,9 @@ "sl7": 0.0 }, "id": { - "component": "Ferric acrisols", - "name": "Ferric acrisols1", - "rank_loc": "10", + "component": "Dystric leptosols", + "name": "Dystric leptosols", + "rank_loc": "11", "score_loc": 0.011 }, "ph": { @@ -898,22 +998,22 @@ }, "site": { "siteData": { - "componentID": 133233, - "distance": 0.0, - "mapunitID": 36001, - "minCompDistance": 0.0, - "share": 15, - "soilDepth": 200 + "componentID": 133329, + "distance": 48484.096, + "mapunitID": 36018, + "minCompDistance": 48484.0959, + "share": 5, + "soilDepth": 40 }, "siteDescription": { - "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", - "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Dístricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles dísticos tienen una baja saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Description_ks": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Este suelo prácticamente no tiene calcio disponible para el uso de las plantas.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " } }, "texture": { @@ -964,9 +1064,9 @@ "sl7": 0.33 }, "id": { - "component": "Dystric leptosols", - "name": "Dystric leptosols", - "rank_loc": "11", + "component": "Ferralic arenosols", + "name": "Ferralic arenosols", + "rank_loc": "12", "score_loc": 0.011 }, "ph": { @@ -998,22 +1098,22 @@ }, "site": { "siteData": { - "componentID": 133329, - "distance": 48484.096, - "mapunitID": 36018, - "minCompDistance": 48484.0959, + "componentID": 133291, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 49166.7104, "share": 5, - "soilDepth": 40 + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", - "Description_es": "Los Leptosoles Dístricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles dísticos tienen una baja saturación de la base sobre la capa limitante de las raíces poco profundas. ", - "Description_fr": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", - "Description_ks": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Este suelo prácticamente no tiene calcio disponible para el uso de las plantas.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { @@ -1037,93 +1137,93 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.57, - "sl6": 6.4, - "sl7": 6.33 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.4, + "sl5": 8.57, + "sl6": 7.8, + "sl7": 8.17 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 31.2, - "sl5": 34.0, - "sl6": 36.6, - "sl7": 37.67 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 24.2, + "sl5": 24.29, + "sl6": 24.2, + "sl7": 24.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols", - "rank_loc": "12", - "score_loc": 0.011 - }, - "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.18, - "sl5": 5.16, - "sl6": 5.14, - "sl7": 5.13 + "component": "Haplic lixisols", + "name": "Haplic lixisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.016 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.96, + "sl5": 4.99, + "sl6": 5.04, + "sl7": 5.08 }, "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.8, - "sl5": 28.29, - "sl6": 27.2, - "sl7": 26.33 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.8, + "sl5": 7.0, + "sl6": 9.4, + "sl7": 9.67 }, "sand": { - "sl1": 56.0, - "sl2": 56.0, - "sl3": 56.0, - "sl4": 50.2, - "sl5": 47.71, - "sl6": 45.2, - "sl7": 43.83 + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 49.2, + "sl5": 49.71, + "sl6": 50.8, + "sl7": 50.67 }, "site": { "siteData": { - "componentID": 133291, - "distance": 49166.71, - "mapunitID": 36011, - "minCompDistance": 49166.7104, - "share": 5, + "componentID": 134019, + "distance": 52599.161, + "mapunitID": 36178, + "minCompDistance": 15267.7017, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", - "sl6": "Sandy clay", - "sl7": "Clay loam" + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -1152,8 +1252,8 @@ "sl4": 0.5 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols2", + "component": "Haplic acrisols", + "name": "Haplic acrisols2", "rank_loc": "Not Displayed", "score_loc": 0.016 }, @@ -1177,22 +1277,22 @@ }, "site": { "siteData": { - "componentID": 134019, - "distance": 52599.161, - "mapunitID": 36178, - "minCompDistance": 15267.7017, + "componentID": 133287, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 33211.7658, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { @@ -1202,106 +1302,6 @@ "sl4": "Sandy clay loam" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.57, - "sl6": 6.4, - "sl7": 6.33 - }, - "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 31.2, - "sl5": 34.0, - "sl6": 36.6, - "sl7": 37.67 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.016 - }, - "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.18, - "sl5": 5.16, - "sl6": 5.14, - "sl7": 5.13 - }, - "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.8, - "sl5": 28.29, - "sl6": 27.2, - "sl7": 26.33 - }, - "sand": { - "sl1": 56.0, - "sl2": 56.0, - "sl3": 56.0, - "sl4": 50.2, - "sl5": 47.71, - "sl6": 45.2, - "sl7": 43.83 - }, - "site": { - "siteData": { - "componentID": 107931, - "distance": 34218.133, - "mapunitID": 1444, - "minCompDistance": 33726.7301, - "share": 10, - "soilDepth": 20 - }, - "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay", - "sl7": "Clay loam" - } - }, { "bottom_depth": { "sl1": 1, @@ -1340,10 +1340,10 @@ "sl7": 0.0 }, "id": { - "component": "Ferric acrisols", - "name": "Ferric acrisols2", + "component": "Lithic leptosols", + "name": "Lithic leptosols2", "rank_loc": "Not Displayed", - "score_loc": 0.011 + "score_loc": 0.016 }, "ph": { "sl1": 5.3, @@ -1374,22 +1374,22 @@ }, "site": { "siteData": { - "componentID": 133288, - "distance": 49166.71, - "mapunitID": 36011, - "minCompDistance": 0.0, + "componentID": 107931, + "distance": 34218.133, + "mapunitID": 1444, + "minCompDistance": 33726.7301, "share": 10, - "soilDepth": 200 + "soilDepth": 20 }, "siteDescription": { - "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", - "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " } }, "texture": { @@ -1413,193 +1413,93 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.57, - "sl6": 6.4, - "sl7": 6.33 - }, - "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 31.2, - "sl5": 34.0, - "sl6": 36.6, - "sl7": 37.67 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Ferric acrisols", - "name": "Ferric acrisols3", - "rank_loc": "Not Displayed", - "score_loc": 0.011 - }, - "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.18, - "sl5": 5.16, - "sl6": 5.14, - "sl7": 5.13 - }, - "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.8, - "sl5": 28.29, - "sl6": 27.2, - "sl7": 26.33 - }, - "sand": { - "sl1": 56.0, - "sl2": 56.0, - "sl3": 56.0, - "sl4": 50.2, - "sl5": 47.71, - "sl6": 45.2, - "sl7": 43.83 - }, - "site": { - "siteData": { - "componentID": 133557, - "distance": 52041.457, - "mapunitID": 36068, - "minCompDistance": 0.0, - "share": 50, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", - "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay", - "sl7": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.57, - "sl6": 6.4, - "sl7": 6.33 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.4, + "sl5": 8.57, + "sl6": 7.8, + "sl7": 8.17 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 31.2, - "sl5": 34.0, - "sl6": 36.6, - "sl7": 37.67 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 24.2, + "sl5": 24.29, + "sl6": 24.2, + "sl7": 24.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Ferric acrisols", - "name": "Ferric acrisols4", + "component": "Dystric fluvisols", + "name": "Dystric fluvisols2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.18, - "sl5": 5.16, - "sl6": 5.14, - "sl7": 5.13 + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.96, + "sl5": 4.99, + "sl6": 5.04, + "sl7": 5.08 }, "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.8, - "sl5": 28.29, - "sl6": 27.2, - "sl7": 26.33 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.8, + "sl5": 7.0, + "sl6": 9.4, + "sl7": 9.67 }, "sand": { - "sl1": 56.0, - "sl2": 56.0, - "sl3": 56.0, - "sl4": 50.2, - "sl5": 47.71, - "sl6": 45.2, - "sl7": 43.83 + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 49.2, + "sl5": 49.71, + "sl6": 50.8, + "sl7": 50.67 }, "site": { "siteData": { - "componentID": 133943, - "distance": 83016.795, - "mapunitID": 36160, + "componentID": 134011, + "distance": 57794.629, + "mapunitID": 36174, "minCompDistance": 0.0, - "share": 50, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", - "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", - "sl6": "Sandy clay", - "sl7": "Clay loam" + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } } ] @@ -1611,24 +1511,60 @@ }, "soilRank": [ { - "component": "Haplic acrisols", - "componentData": "Data Complete", - "componentID": 133287, - "name": "Haplic acrisols", - "rank_data": "3", + "component": "Haplic lixisols", + "componentData": "Missing Data", + "componentID": 134019, + "name": "Haplic lixisols2", + "rank_data": "5", "rank_data_loc": "1", - "rank_loc": "7", + "rank_loc": "Not Displayed", "score_data": 1.0, "score_data_loc": 1.0, "score_loc": 0.016 }, + { + "component": "Ferric lixisols", + "componentData": "Data Complete", + "componentID": 107928, + "name": "Ferric lixisols", + "rank_data": "4", + "rank_data_loc": "2", + "rank_loc": "8", + "score_data": 1.0, + "score_data_loc": 0.998, + "score_loc": 0.014 + }, + { + "component": "Dystric fluvisols", + "componentData": "Data Complete", + "componentID": 134011, + "name": "Dystric fluvisols2", + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": "Not Displayed", + "score_data": 1.0, + "score_data_loc": 0.995, + "score_loc": 0.011 + }, + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 133291, + "name": "Ferralic arenosols", + "rank_data": "3", + "rank_data_loc": "4", + "rank_loc": "12", + "score_data": 1.0, + "score_data_loc": 0.995, + "score_loc": 0.011 + }, { "component": "Eutric gleysols", "componentData": "Missing Data", "componentID": 133289, "name": "Eutric gleysols", - "rank_data": "4", - "rank_data_loc": "2", + "rank_data": "6", + "rank_data_loc": "5", "rank_loc": "1", "score_data": 0.63, "score_data_loc": 0.645, @@ -1639,8 +1575,8 @@ "componentData": "Data Complete", "componentID": 133231, "name": "Eutric plinthosols", - "rank_data": "6", - "rank_data_loc": "3", + "rank_data": "9", + "rank_data_loc": "6", "rank_loc": "2", "score_data": 0.613, "score_data_loc": 0.625, @@ -1651,69 +1587,33 @@ "componentData": "Missing Data", "componentID": 133240, "name": "Dystric planosols", - "rank_data": "5", - "rank_data_loc": "4", + "rank_data": "8", + "rank_data_loc": "7", "rank_loc": "3", "score_data": 0.613, "score_data_loc": 0.619, "score_loc": 0.016 }, { - "component": "Ferric acrisols", - "componentData": "Missing Data", - "componentID": 133233, - "name": "Ferric acrisols1", - "rank_data": "7", - "rank_data_loc": "5", - "rank_loc": "10", - "score_data": 0.613, - "score_data_loc": 0.614, - "score_loc": 0.011 - }, - { - "component": "Haplic lixisols", - "componentData": "Missing Data", - "componentID": 133488, - "name": "Haplic lixisols1", - "rank_data": "12", - "rank_data_loc": "6", - "rank_loc": "4", + "component": "Haplic acrisols", + "componentData": "Data Complete", + "componentID": 133287, + "name": "Haplic acrisols2", + "rank_data": "Not Displayed", + "rank_data_loc": "8", + "rank_loc": "Not Displayed", "score_data": 0.535, "score_data_loc": 0.542, "score_loc": 0.016 }, - { - "component": "Ferric lixisols", - "componentData": "Data Complete", - "componentID": 107928, - "name": "Ferric lixisols", - "rank_data": "11", - "rank_data_loc": "7", - "rank_loc": "8", - "score_data": 0.535, - "score_data_loc": 0.541, - "score_loc": 0.014 - }, { "component": "Dystric gleysols", "componentData": "Missing Data", "componentID": 133232, "name": "Dystric gleysols", - "rank_data": "9", - "rank_data_loc": "8", - "rank_loc": "9", - "score_data": 0.535, - "score_data_loc": 0.537, - "score_loc": 0.011 - }, - { - "component": "Ferralic arenosols", - "componentData": "Data Complete", - "componentID": 133291, - "name": "Ferralic arenosols", - "rank_data": "10", + "rank_data": "11", "rank_data_loc": "9", - "rank_loc": "12", + "rank_loc": "9", "score_data": 0.535, "score_data_loc": 0.537, "score_loc": 0.011 @@ -1723,10 +1623,10 @@ "componentData": "Missing Data", "componentID": 133329, "name": "Dystric leptosols", - "rank_data": "1", + "rank_data": "7", "rank_data_loc": "10", "rank_loc": "11", - "score_data": 1.0, + "score_data": 0.613, "score_data_loc": 0.002, "score_loc": 0.011 }, @@ -1747,61 +1647,49 @@ "componentData": "Missing Data", "componentID": 148823, "name": "Lithic leptosols1", - "rank_data": "8", + "rank_data": "10", "rank_data_loc": "12", - "rank_loc": "6", + "rank_loc": "7", "score_data": 0.613, "score_data_loc": 0.002, "score_loc": 0.016 }, { - "component": "Haplic lixisols", - "componentData": "Missing Data", - "componentID": 134019, - "name": "Haplic lixisols2", - "rank_data": "Not Displayed", + "component": "Haplic acrisols", + "componentData": "Data Complete", + "componentID": 134061, + "name": "Haplic acrisols1", + "rank_data": "12", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", + "rank_loc": "6", "score_data": 0.535, "score_data_loc": 0.542, "score_loc": 0.016 }, { - "component": "Ferric acrisols", + "component": "Haplic lixisols", "componentData": "Missing Data", - "componentID": 133557, - "name": "Ferric acrisols3", + "componentID": 133488, + "name": "Haplic lixisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", + "rank_loc": "4", "score_data": 0.535, - "score_data_loc": 0.537, - "score_loc": 0.011 + "score_data_loc": 0.542, + "score_loc": 0.016 }, { - "component": "Ferric acrisols", - "componentData": "Missing Data", - "componentID": 133943, - "name": "Ferric acrisols4", + "component": "Dystric fluvisols", + "componentData": "Data Complete", + "componentID": 133237, + "name": "Dystric fluvisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", + "rank_loc": "10", "score_data": 0.535, "score_data_loc": 0.537, "score_loc": 0.011 }, - { - "component": "Ferric acrisols", - "componentData": "Missing Data", - "componentID": 133288, - "name": "Ferric acrisols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.37, - "score_data_loc": 0.375, - "score_loc": 0.011 - }, { "component": "Lithic leptosols", "componentData": "Missing Data", @@ -1810,7 +1698,7 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.535, + "score_data": 0.37, "score_data_loc": 0.002, "score_loc": 0.016 } diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json index 8ce0e57..8080267 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json @@ -894,50 +894,50 @@ { "component": "Carrizo", "componentData": "Missing Data", - "componentID": 14185605, - "name": "Carrizo2", - "rank_data": "8", + "componentID": 14185597, + "name": "Carrizo3", + "rank_data": "6", "rank_data_loc": "1", "rank_loc": "Not Displayed", - "score_data": 0.724, - "score_data_loc": 0.544, + "score_data": 0.785, + "score_data_loc": 0.574, "score_loc": 0.363 }, { - "component": "Gunsight", + "component": "Rositas", "componentData": "Missing Data", - "componentID": 14185636, - "name": "Gunsight1", - "rank_data": "7", + "componentID": 14185600, + "name": "Rositas1", + "rank_data": "1", "rank_data_loc": "2", - "rank_loc": "2", - "score_data": 0.733, - "score_data_loc": 0.502, - "score_loc": 0.27 + "rank_loc": "4", + "score_data": 0.931, + "score_data_loc": 0.511, + "score_loc": 0.091 }, { "component": "Chuckawalla", "componentData": "Missing Data", "componentID": 14185601, "name": "Chuckawalla", - "rank_data": "1", + "rank_data": "2", "rank_data_loc": "3", "rank_loc": "5", - "score_data": 0.901, - "score_data_loc": 0.491, + "score_data": 0.931, + "score_data_loc": 0.505, "score_loc": 0.08 }, { - "component": "Cipriano", + "component": "Gunsight", "componentData": "Missing Data", - "componentID": 14185643, - "name": "Cipriano", - "rank_data": "2", + "componentID": 14185602, + "name": "Gunsight2", + "rank_data": "8", "rank_data_loc": "4", - "rank_loc": "10", - "score_data": 0.857, - "score_data_loc": 0.454, - "score_loc": 0.05 + "rank_loc": "Not Displayed", + "score_data": 0.717, + "score_data_loc": 0.494, + "score_loc": 0.27 }, { "component": "Denure", @@ -947,8 +947,8 @@ "rank_data": "3", "rank_data_loc": "5", "rank_loc": "12", - "score_data": 0.819, - "score_data_loc": 0.434, + "score_data": 0.922, + "score_data_loc": 0.486, "score_loc": 0.05 }, { @@ -959,56 +959,56 @@ "rank_data": "4", "rank_data_loc": "6", "rank_loc": "6", - "score_data": 0.817, - "score_data_loc": 0.434, + "score_data": 0.872, + "score_data_loc": 0.461, "score_loc": 0.05 }, { - "component": "Rositas", + "component": "Cipriano", "componentData": "Missing Data", - "componentID": 14185600, - "name": "Rositas1", + "componentID": 14185643, + "name": "Cipriano", "rank_data": "5", "rank_data_loc": "7", - "rank_loc": "4", - "score_data": 0.769, - "score_data_loc": 0.43, - "score_loc": 0.091 - }, - { - "component": "Rillito", - "componentData": "Missing Data", - "componentID": 14185645, - "name": "Rillito", - "rank_data": "9", - "rank_data_loc": "8", - "rank_loc": "3", - "score_data": 0.66, - "score_data_loc": 0.425, - "score_loc": 0.19 + "rank_loc": "10", + "score_data": 0.835, + "score_data_loc": 0.443, + "score_loc": 0.05 }, { "component": "Pinamt", "componentData": "Missing Data", "componentID": 14185641, "name": "Pinamt", - "rank_data": "6", - "rank_data_loc": "9", + "rank_data": "7", + "rank_data_loc": "8", "rank_loc": "11", - "score_data": 0.761, - "score_data_loc": 0.406, + "score_data": 0.748, + "score_data_loc": 0.399, "score_loc": 0.05 }, { - "component": "Momoli", + "component": "Rillito", "componentData": "Missing Data", - "componentID": 14185638, - "name": "Momoli", - "rank_data": "10", + "componentID": 14185645, + "name": "Rillito", + "rank_data": "12", + "rank_data_loc": "9", + "rank_loc": "3", + "score_data": 0.585, + "score_data_loc": 0.387, + "score_loc": 0.19 + }, + { + "component": "Gilman", + "componentData": "Missing Data", + "componentID": 14185646, + "name": "Gilman", + "rank_data": "9", "rank_data_loc": "10", - "rank_loc": "7", - "score_data": 0.652, - "score_data_loc": 0.351, + "rank_loc": "8", + "score_data": 0.616, + "score_data_loc": 0.333, "score_loc": 0.05 }, { @@ -1016,35 +1016,35 @@ "componentData": "Missing Data", "componentID": 14185644, "name": "Mohall", - "rank_data": "11", + "rank_data": "10", "rank_data_loc": "11", "rank_loc": "9", - "score_data": 0.636, - "score_data_loc": 0.343, + "score_data": 0.616, + "score_data_loc": 0.333, "score_loc": 0.05 }, { - "component": "Gilman", + "component": "Momoli", "componentData": "Missing Data", - "componentID": 14185646, - "name": "Gilman", - "rank_data": "12", + "componentID": 14185638, + "name": "Momoli", + "rank_data": "11", "rank_data_loc": "12", - "rank_loc": "8", - "score_data": 0.613, - "score_data_loc": 0.331, + "rank_loc": "7", + "score_data": 0.616, + "score_data_loc": 0.333, "score_loc": 0.05 }, { "component": "Carrizo", "componentData": "Missing Data", - "componentID": 14185597, - "name": "Carrizo3", + "componentID": 14185605, + "name": "Carrizo2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.719, - "score_data_loc": 0.541, + "score_data": 0.752, + "score_data_loc": 0.557, "score_loc": 0.363 }, { @@ -1055,20 +1055,20 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "1", - "score_data": 0.629, - "score_data_loc": 0.496, + "score_data": 0.653, + "score_data_loc": 0.508, "score_loc": 0.363 }, { "component": "Gunsight", "componentData": "Missing Data", - "componentID": 14185602, - "name": "Gunsight2", + "componentID": 14185636, + "name": "Gunsight1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.705, - "score_data_loc": 0.487, + "rank_loc": "2", + "score_data": 0.702, + "score_data_loc": 0.486, "score_loc": 0.27 }, { @@ -1079,8 +1079,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.671, - "score_data_loc": 0.381, + "score_data": 0.783, + "score_data_loc": 0.437, "score_loc": 0.091 }, { @@ -1091,8 +1091,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.582, - "score_data_loc": 0.337, + "score_data": 0.709, + "score_data_loc": 0.4, "score_loc": 0.091 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json index c9056d0..fc30087 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json @@ -433,40 +433,40 @@ "model": "v2" }, "soilRank": [ - { - "component": "Xerorthents", - "componentData": "Missing Data", - "componentID": 26038503, - "name": "Xerorthents1", - "rank_data": "1", - "rank_data_loc": "1", - "rank_loc": "2", - "score_data": 0.757, - "score_data_loc": 0.53, - "score_loc": 0.304 - }, { "component": "Hangerone", "componentData": "Data Complete", "componentID": 26038467, "name": "Hangerone", - "rank_data": "4", - "rank_data_loc": "2", + "rank_data": "1", + "rank_data_loc": "1", "rank_loc": "1", - "score_data": 0.709, - "score_data_loc": 0.51, + "score_data": 0.78, + "score_data_loc": 0.545, "score_loc": 0.311 }, + { + "component": "Xerorthents", + "componentData": "Missing Data", + "componentID": 26038503, + "name": "Xerorthents1", + "rank_data": "3", + "rank_data_loc": "2", + "rank_loc": "2", + "score_data": 0.764, + "score_data_loc": 0.534, + "score_loc": 0.304 + }, { "component": "Aquic xerorthents", "componentData": "Missing Data", "componentID": 26038456, "name": "Aquic xerorthents", - "rank_data": "3", + "rank_data": "4", "rank_data_loc": "3", "rank_loc": "3", - "score_data": 0.734, - "score_data_loc": 0.486, + "score_data": 0.764, + "score_data_loc": 0.501, "score_loc": 0.237 }, { @@ -477,8 +477,8 @@ "rank_data": "2", "rank_data_loc": "4", "rank_loc": "6", - "score_data": 0.735, - "score_data_loc": 0.372, + "score_data": 0.769, + "score_data_loc": 0.389, "score_loc": 0.01 }, { @@ -489,8 +489,8 @@ "rank_data": "5", "rank_data_loc": "5", "rank_loc": "4", - "score_data": 0.554, - "score_data_loc": 0.288, + "score_data": 0.548, + "score_data_loc": 0.285, "score_loc": 0.021 }, { @@ -501,8 +501,8 @@ "rank_data": "6", "rank_data_loc": "6", "rank_loc": "5", - "score_data": 0.478, - "score_data_loc": 0.249, + "score_data": 0.434, + "score_data_loc": 0.227, "score_loc": 0.02 }, { @@ -513,8 +513,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.56, - "score_data_loc": 0.432, + "score_data": 0.612, + "score_data_loc": 0.458, "score_loc": 0.304 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json index 487099a..8f6ae1c 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json @@ -1558,11 +1558,11 @@ "componentData": "Data Complete", "componentID": 25325349, "name": "Miami2", - "rank_data": "2", + "rank_data": "5", "rank_data_loc": "1", "rank_loc": "Not Displayed", - "score_data": 0.648, - "score_data_loc": 0.749, + "score_data": 0.542, + "score_data_loc": 0.696, "score_loc": 0.85 }, { @@ -1570,133 +1570,133 @@ "componentData": "Data Complete", "componentID": 25325354, "name": "Williamstown3", - "rank_data": "5", + "rank_data": "2", "rank_data_loc": "2", "rank_loc": "Not Displayed", - "score_data": 0.608, - "score_data_loc": 0.569, + "score_data": 0.588, + "score_data_loc": 0.559, "score_loc": 0.53 }, { "component": "Hennepin", "componentData": "Data Complete", - "componentID": 25325355, - "name": "Hennepin3", + "componentID": 25325325, + "name": "Hennepin2", "rank_data": "3", "rank_data_loc": "3", "rank_loc": "Not Displayed", - "score_data": 0.634, - "score_data_loc": 0.43, + "score_data": 0.569, + "score_data_loc": 0.397, "score_loc": 0.225 }, { - "component": "Fincastle", + "component": "Treaty", "componentData": "Data Complete", - "componentID": 25325308, - "name": "Fincastle", - "rank_data": "6", + "componentID": 25325401, + "name": "Treaty2", + "rank_data": "1", "rank_data_loc": "4", - "rank_loc": "4", - "score_data": 0.505, - "score_data_loc": 0.361, - "score_loc": 0.218 - }, - { - "component": "Crosby", - "componentData": "Data Complete", - "componentID": 25325344, - "name": "Crosby3", - "rank_data": "4", - "rank_data_loc": "5", "rank_loc": "Not Displayed", - "score_data": 0.619, - "score_data_loc": 0.354, - "score_loc": 0.09 + "score_data": 0.652, + "score_data_loc": 0.341, + "score_loc": 0.031 }, { "component": "Xenia", "componentData": "Data Complete", "componentID": 25325405, "name": "Xenia", - "rank_data": "8", - "rank_data_loc": "6", + "rank_data": "6", + "rank_data_loc": "5", "rank_loc": "6", - "score_data": 0.482, - "score_data_loc": 0.347, + "score_data": 0.448, + "score_data_loc": 0.33, "score_loc": 0.212 }, { - "component": "Treaty", + "component": "Crosby", "componentData": "Data Complete", - "componentID": 25325401, - "name": "Treaty2", - "rank_data": "1", - "rank_data_loc": "7", + "componentID": 25325351, + "name": "Crosby2", + "rank_data": "4", + "rank_data_loc": "6", "rank_loc": "Not Displayed", - "score_data": 0.66, - "score_data_loc": 0.345, - "score_loc": 0.031 + "score_data": 0.569, + "score_data_loc": 0.329, + "score_loc": 0.09 + }, + { + "component": "Fincastle", + "componentData": "Data Complete", + "componentID": 25325308, + "name": "Fincastle", + "rank_data": "7", + "rank_data_loc": "7", + "rank_loc": "4", + "score_data": 0.407, + "score_data_loc": 0.313, + "score_loc": 0.218 }, { "component": "Hickory", "componentData": "Data Complete", "componentID": 25325331, "name": "Hickory", - "rank_data": "12", + "rank_data": "8", "rank_data_loc": "8", "rank_loc": "5", - "score_data": 0.403, - "score_data_loc": 0.31, + "score_data": 0.407, + "score_data_loc": 0.312, "score_loc": 0.217 }, - { - "component": "Rainsville", - "componentData": "Data Complete", - "componentID": 25325345, - "name": "Rainsville", - "rank_data": "7", - "rank_data_loc": "9", - "rank_loc": "12", - "score_data": 0.502, - "score_data_loc": 0.258, - "score_loc": 0.013 - }, { "component": "Cyclone", "componentData": "Data Complete", "componentID": 25325310, "name": "Cyclone2", "rank_data": "9", - "rank_data_loc": "10", + "rank_data_loc": "9", "rank_loc": "Not Displayed", - "score_data": 0.472, - "score_data_loc": 0.249, + "score_data": 0.363, + "score_data_loc": 0.194, "score_loc": 0.026 }, { - "component": "Brookston", + "component": "Celina", "componentData": "Data Complete", - "componentID": 25325342, - "name": "Brookston", + "componentID": 25325406, + "name": "Celina", "rank_data": "10", - "rank_data_loc": "11", - "rank_loc": "8", - "score_data": 0.439, - "score_data_loc": 0.239, - "score_loc": 0.04 + "rank_data_loc": "10", + "rank_loc": "11", + "score_data": 0.333, + "score_data_loc": 0.173, + "score_loc": 0.013 }, { - "component": "Celina", + "component": "Rainsville", "componentData": "Data Complete", - "componentID": 25325406, - "name": "Celina", + "componentID": 25325345, + "name": "Rainsville", "rank_data": "11", - "rank_data_loc": "12", - "rank_loc": "11", - "score_data": 0.424, - "score_data_loc": 0.218, + "rank_data_loc": "11", + "rank_loc": "12", + "score_data": 0.333, + "score_data_loc": 0.173, "score_loc": 0.013 }, + { + "component": "Brookston", + "componentData": "Data Complete", + "componentID": 25325342, + "name": "Brookston", + "rank_data": "12", + "rank_data_loc": "12", + "rank_loc": "8", + "score_data": 0.3, + "score_data_loc": 0.17, + "score_loc": 0.04 + }, { "component": "Miami", "componentData": "Data Complete", @@ -1705,8 +1705,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.593, - "score_data_loc": 0.721, + "score_data": 0.447, + "score_data_loc": 0.648, "score_loc": 0.85 }, { @@ -1717,32 +1717,32 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.572, - "score_data_loc": 0.711, + "score_data": 0.437, + "score_data_loc": 0.644, "score_loc": 0.85 }, { "component": "Miami", "componentData": "Data Complete", - "componentID": 25325339, - "name": "Miami1", + "componentID": 25325326, + "name": "Miami4", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "1", - "score_data": 0.538, - "score_data_loc": 0.694, + "rank_loc": "Not Displayed", + "score_data": 0.433, + "score_data_loc": 0.641, "score_loc": 0.85 }, { "component": "Miami", "componentData": "Data Complete", - "componentID": 25325326, - "name": "Miami4", + "componentID": 25325339, + "name": "Miami1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.509, - "score_data_loc": 0.68, + "rank_loc": "1", + "score_data": 0.42, + "score_data_loc": 0.635, "score_loc": 0.85 }, { @@ -1753,8 +1753,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.483, - "score_data_loc": 0.667, + "score_data": 0.331, + "score_data_loc": 0.59, "score_loc": 0.85 }, { @@ -1765,8 +1765,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.548, - "score_data_loc": 0.539, + "score_data": 0.447, + "score_data_loc": 0.488, "score_loc": 0.53 }, { @@ -1777,32 +1777,44 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "2", - "score_data": 0.513, - "score_data_loc": 0.521, + "score_data": 0.407, + "score_data_loc": 0.469, "score_loc": 0.53 }, { "component": "Hennepin", "componentData": "Data Complete", - "componentID": 25325325, - "name": "Hennepin2", + "componentID": 25325355, + "name": "Hennepin3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.549, - "score_data_loc": 0.387, + "score_data": 0.569, + "score_data_loc": 0.397, "score_loc": 0.225 }, + { + "component": "Treaty", + "componentData": "Data Complete", + "componentID": 25325403, + "name": "Treaty3", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.652, + "score_data_loc": 0.341, + "score_loc": 0.031 + }, { "component": "Crosby", "componentData": "Data Complete", - "componentID": 25325351, - "name": "Crosby2", + "componentID": 25325344, + "name": "Crosby3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.597, - "score_data_loc": 0.344, + "score_data": 0.569, + "score_data_loc": 0.329, "score_loc": 0.09 }, { @@ -1813,20 +1825,20 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "3", - "score_data": 0.449, - "score_data_loc": 0.337, + "score_data": 0.407, + "score_data_loc": 0.316, "score_loc": 0.225 }, { "component": "Treaty", "componentData": "Data Complete", - "componentID": 25325403, - "name": "Treaty3", + "componentID": 25325343, + "name": "Treaty4", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.602, - "score_data_loc": 0.316, + "score_data": 0.398, + "score_data_loc": 0.214, "score_loc": 0.031 }, { @@ -1837,21 +1849,21 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "7", - "score_data": 0.447, - "score_data_loc": 0.269, + "score_data": 0.3, + "score_data_loc": 0.195, "score_loc": 0.09 }, { - "component": "Treaty", + "component": "Cyclone", "componentData": "Data Complete", - "componentID": 25325343, - "name": "Treaty4", + "componentID": 25325348, + "name": "Cyclone1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.501, - "score_data_loc": 0.266, - "score_loc": 0.031 + "rank_loc": "10", + "score_data": 0.333, + "score_data_loc": 0.18, + "score_loc": 0.026 }, { "component": "Treaty", @@ -1861,21 +1873,9 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "9", - "score_data": 0.439, - "score_data_loc": 0.235, + "score_data": 0.3, + "score_data_loc": 0.165, "score_loc": 0.031 - }, - { - "component": "Cyclone", - "componentData": "Data Complete", - "componentID": 25325348, - "name": "Cyclone1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "10", - "score_data": 0.428, - "score_data_loc": 0.227, - "score_loc": 0.026 } ] } From ee65da991e9b8f97d86652e4fb26e62251c85aac Mon Sep 17 00:00:00 2001 From: shrouxm Date: Thu, 14 Aug 2025 09:59:30 -0700 Subject: [PATCH 5/5] remove sort=False --- soil_id/global_soil.py | 14 +- soil_id/soil_sim.py | 2 +- .../test_soil_location[-1.75,13.6].json | 736 ++-- ...st_soil_location[-10.07856,15.107436].json | 2374 +++++------ ...t_soil_location[-10.950086,17.573093].json | 1858 ++++---- ...est_soil_location[-19.13333,145.5125].json | 3488 +++++++-------- .../test_soil_location[-2.06972,37.29].json | 3782 ++++++----------- ...est_soil_location[-24.53333,33.36667].json | 2184 +++++----- ...est_soil_location[15.73333,120.31667].json | 1390 +++--- ...test_soil_location[30.38333,35.53333].json | 1350 +++--- ...test_soil_location[32.11667,20.08333].json | 1050 ++--- .../test_soil_location[34.5,69.16667].json | 1470 +++---- .../test_soil_location[37.33333,-5.4].json | 2088 +++++---- ...est_soil_location[48.71667,126.13333].json | 1412 +++--- .../test_soil_location[7.3318,-1.4631].json | 2002 +++++---- .../test_soil_location[8.48333,76.95].json | 1514 ++++--- ...il_location[33.81246789,-101.9733687].json | 144 +- ...st_soil_location[34.92816,-114.80764].json | 536 +-- ...t_soil_location[35.59918,-120.491439].json | 206 +- .../test_soil_location[37.422,-122.084].json | 94 +- ...il_location[37.48216451,-99.55016693].json | 148 +- ...il_location[39.26009312,-85.50621214].json | 1466 ++----- ..._soil_location[42.494912,-123.064531].json | 482 +-- ...il_location[42.63413723,-94.31005777].json | 62 +- ...il_location[43.06450312,-119.4596489].json | 126 +- ...il_location[45.88932423,-121.0347381].json | 14 +- ...soil_location[47.213922,-69.28246582].json | 110 +- ...test_soil_location[48.6956,-121.8166].json | 1162 ----- ...il_location[60.42282639,-158.4018264].json | 60 +- ...il_location[62.32776717,-157.2767099].json | 94 +- ...il_location[63.52666854,-156.4422738].json | 348 +- soil_id/us_soil.py | 16 +- soil_id/utils.py | 6 +- 33 files changed, 13570 insertions(+), 18218 deletions(-) delete mode 100644 soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json diff --git a/soil_id/global_soil.py b/soil_id/global_soil.py index c55a90c..6a0aac8 100644 --- a/soil_id/global_soil.py +++ b/soil_id/global_soil.py @@ -105,7 +105,7 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000): ############################################################################################## ExpCoeff = -0.00036888 # Decays to 0.25 @ 10km loc_scores = [] - mucompdata_grouped = mucompdata_pd.groupby(["mukey", "cokey"], sort=False) + mucompdata_grouped = mucompdata_pd.groupby(["mukey", "cokey"]) for (mukey, cokey), group in mucompdata_grouped: loc_score = calculate_location_score(group, ExpCoeff) @@ -124,7 +124,7 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000): mucompdata_pd["Index"] = mucompdata_pd.index # Group by component name - mucompdata_grouped = mucompdata_pd.groupby("compname", sort=False) + mucompdata_grouped = mucompdata_pd.groupby("compname") # Take at most 12 groups mucompdata_comp_grps = [group for _, group in mucompdata_grouped][:12] @@ -234,7 +234,7 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000): ) # Group data by cokey for texture - muhorzdata_group_cokey = list(muhorzdata_pd.groupby("cokey", sort=False)) + muhorzdata_group_cokey = list(muhorzdata_pd.groupby("cokey")) pd.set_option("display.max_rows", None) pd.set_option("display.max_columns", None) pd.set_option("display.width", None) @@ -367,7 +367,7 @@ def list_soils_global(connection, lon, lat, buffer_dist=100000): # Create index for component instance display mucompdata_comp_grps_list = [] - mucompdata_comp_grps = [group for _, group in mucompdata_pd.groupby("compname_grp", sort=False)] + mucompdata_comp_grps = [group for _, group in mucompdata_pd.groupby("compname_grp")] for group in mucompdata_comp_grps: group = group.sort_values("distance").reset_index(drop=True) @@ -772,7 +772,7 @@ def rank_soils_global( # Horizon Data Similarity if soilIDRank_output_pd is not None: - cokey_groups = [group for _, group in soilIDRank_output_pd.groupby("compname", sort=False)] + cokey_groups = [group for _, group in soilIDRank_output_pd.groupby("compname")] # Create lists to store component statuses Comp_Rank_Status, Comp_Missing_Status, Comp_name = [], [], [] @@ -1087,7 +1087,7 @@ def normalize(arr): # Sorting and reindexing of Data-only score soilIDList_data = [] - D_final_comp_grps = [g for _, g in D_final_horz.groupby("compname_grp", sort=False)] + D_final_comp_grps = [g for _, g in D_final_horz.groupby("compname_grp")] for comp_grps_temp in D_final_comp_grps: comp_grps_temp = comp_grps_temp.sort_values("Score_Data", ascending=False).reset_index( @@ -1163,7 +1163,7 @@ def normalize(arr): soilIDList_out = [] # Group by 'compname_grp' - for _, comp_grps_temp in D_final_loc.groupby("compname_grp", sort=False): + for _, comp_grps_temp in D_final_loc.groupby("compname_grp"): comp_grps_temp = comp_grps_temp.sort_values("Score_Data_Loc", ascending=False).reset_index( drop=True ) diff --git a/soil_id/soil_sim.py b/soil_id/soil_sim.py index 78ce110..33cc323 100644 --- a/soil_id/soil_sim.py +++ b/soil_id/soil_sim.py @@ -128,7 +128,7 @@ def soil_sim(muhorzdata_pd): agg_data = [] # Group data by compname_grp - sim_group_compname = [group for _, group in sim.groupby("compname_grp", sort=False)] + sim_group_compname = [group for _, group in sim.groupby("compname_grp")] for index, group in enumerate(sim_group_compname): # aggregate data into 0-30 and 30-100 or bottom depth group_ag = slice_and_aggregate_soil_data(group[sim_data_columns]) diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json index f48e086..4eb38e5 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-1.75,13.6].json @@ -25,31 +25,31 @@ "sl7": 120 }, "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.29, - "sl6": 2.2, - "sl7": 2.0 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.14, + "sl6": 6.8, + "sl7": 6.67 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.2, - "sl5": 6.43, - "sl6": 6.8, - "sl7": 7.0 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 33.4, + "sl5": 33.86, + "sl6": 34.0, + "sl7": 33.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 }, "id": { "component": "Ferralic arenosols", @@ -58,31 +58,31 @@ "score_loc": 0.4 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.32, - "sl5": 5.34, - "sl6": 5.36, - "sl7": 5.37 + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.12, + "sl5": 5.14, + "sl6": 5.14, + "sl7": 5.13 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.2, - "sl5": 4.43, - "sl6": 4.6, - "sl7": 4.5 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.2, + "sl5": 11.43, + "sl6": 12.6, + "sl7": 12.83 }, "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 86.8, - "sl5": 86.57, - "sl6": 86.2, - "sl7": 86.0 + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 43.0, + "sl5": 42.43, + "sl6": 42.0, + "sl7": 42.0 }, "site": { "siteData": { @@ -105,113 +105,13 @@ } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 5.6, - "sl5": 5.14, - "sl6": 4.6, - "sl7": 4.33 - }, - "clay": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 39.2, - "sl5": 40.71, - "sl6": 42.0, - "sl7": 42.5 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Xanthic ferralsols", - "name": "Xanthic ferralsols", - "rank_loc": "2", - "score_loc": 0.133 - }, - "ph": { - "sl1": 4.5, - "sl2": 4.5, - "sl3": 4.5, - "sl4": 4.58, - "sl5": 4.63, - "sl6": 4.68, - "sl7": 4.72 - }, - "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.2, - "sl5": 3.57, - "sl6": 4.0, - "sl7": 5.0 - }, - "sand": { - "sl1": 53.0, - "sl2": 53.0, - "sl3": 53.0, - "sl4": 50.0, - "sl5": 48.71, - "sl6": 47.6, - "sl7": 47.17 - }, - "site": { - "siteData": { - "componentID": 156033, - "distance": 0.0, - "mapunitID": 918, - "minCompDistance": 0.0, - "share": 20, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", - "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." - } - }, - "texture": { - "sl1": "Sandy clay", - "sl2": "Sandy clay", - "sl3": "Sandy clay", - "sl4": "Sandy clay", - "sl5": "Sandy clay", - "sl6": "Sandy clay", - "sl7": "Sandy clay" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -254,7 +154,7 @@ "id": { "component": "Haplic ferralsols", "name": "Haplic ferralsols", - "rank_loc": "3", + "rank_loc": "2", "score_loc": 0.133 }, "ph": { @@ -325,31 +225,131 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 7.6, - "sl5": 7.14, + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 + }, + "clay": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, "sl6": 6.8, - "sl7": 6.67 + "sl7": 7.0 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Xanthic ferralsols", + "name": "Xanthic ferralsols", + "rank_loc": "3", + "score_loc": 0.133 + }, + "ph": { + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 + }, + "sand": { + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 + }, + "site": { + "siteData": { + "componentID": 156033, + "distance": 0.0, + "mapunitID": 918, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", + "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", + "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + } + }, + "texture": { + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 7.4, + "sl5": 7.43, + "sl6": 7.6, + "sl7": 7.67 }, "clay": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 33.4, - "sl5": 33.86, - "sl6": 34.0, - "sl7": 33.83 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 28.2, + "sl5": 30.57, + "sl6": 32.8, + "sl7": 34.0 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.5 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Ferralic cambisols", @@ -358,31 +358,31 @@ "score_loc": 0.083 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.12, - "sl5": 5.14, - "sl6": 5.14, - "sl7": 5.13 + "sl1": 4.8, + "sl2": 4.8, + "sl3": 4.8, + "sl4": 4.88, + "sl5": 4.93, + "sl6": 4.98, + "sl7": 4.98 }, "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 10.2, - "sl5": 11.43, - "sl6": 12.6, - "sl7": 12.83 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.6, + "sl5": 4.86, + "sl6": 5.4, + "sl7": 5.83 }, "sand": { "sl1": 45.0, "sl2": 45.0, "sl3": 45.0, - "sl4": 43.0, - "sl5": 42.43, - "sl6": 42.0, - "sl7": 42.0 + "sl4": 42.0, + "sl5": 40.57, + "sl6": 39.2, + "sl7": 37.67 }, "site": { "siteData": { @@ -405,9 +405,9 @@ } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", "sl4": "Clay loam", "sl5": "Clay loam", "sl6": "Clay loam", @@ -425,31 +425,31 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 9.4, - "sl5": 8.57, - "sl6": 7.8, - "sl7": 8.17 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 11.2, + "sl5": 10.57, + "sl6": 10.2, + "sl7": 10.5 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 24.2, - "sl5": 24.29, - "sl6": 24.2, - "sl7": 24.5 + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 30.0, + "sl5": 31.57, + "sl6": 33.0, + "sl7": 33.67 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 }, "id": { "component": "Dystric fluvisols", @@ -458,31 +458,31 @@ "score_loc": 0.017 }, "ph": { - "sl1": 4.9, - "sl2": 4.9, - "sl3": 4.9, - "sl4": 4.96, - "sl5": 4.99, - "sl6": 5.04, + "sl1": 4.8, + "sl2": 4.8, + "sl3": 4.8, + "sl4": 4.94, + "sl5": 5.0, + "sl6": 5.06, "sl7": 5.08 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, "sl4": 4.8, - "sl5": 7.0, - "sl6": 9.4, - "sl7": 9.67 + "sl5": 4.86, + "sl6": 5.4, + "sl7": 5.33 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 49.2, - "sl5": 49.71, - "sl6": 50.8, - "sl7": 50.67 + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 40.71, + "sl6": 40.6, + "sl7": 40.5 }, "site": { "siteData": { @@ -506,12 +506,12 @@ }, "texture": { "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -525,31 +525,31 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 11.2, - "sl5": 10.57, - "sl6": 10.2, - "sl7": 10.5 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.4, + "sl5": 8.57, + "sl6": 7.8, + "sl7": 8.17 }, "clay": { - "sl1": 27.0, - "sl2": 27.0, - "sl3": 27.0, - "sl4": 30.0, - "sl5": 31.57, - "sl6": 33.0, - "sl7": 33.67 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 24.2, + "sl5": 24.29, + "sl6": 24.2, + "sl7": 24.5 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.4, - "sl7": 0.33 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { "component": "Dystric gleysols", @@ -558,31 +558,31 @@ "score_loc": 0.017 }, "ph": { - "sl1": 4.8, - "sl2": 4.8, - "sl3": 4.8, - "sl4": 4.94, - "sl5": 5.0, - "sl6": 5.06, + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.96, + "sl5": 4.99, + "sl6": 5.04, "sl7": 5.08 }, "rock_fragments": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, "sl4": 4.8, - "sl5": 4.86, - "sl6": 5.4, - "sl7": 5.33 + "sl5": 7.0, + "sl6": 9.4, + "sl7": 9.67 }, "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 41.2, - "sl5": 40.71, - "sl6": 40.6, - "sl7": 40.5 + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 49.2, + "sl5": 49.71, + "sl6": 50.8, + "sl7": 50.67 }, "site": { "siteData": { @@ -608,10 +608,10 @@ "sl1": "Loam", "sl2": "Loam", "sl3": "Loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -625,22 +625,22 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 7.4, - "sl5": 7.43, - "sl6": 7.6, - "sl7": 7.67 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 5.6, + "sl5": 5.14, + "sl6": 4.6, + "sl7": 4.33 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 28.2, - "sl5": 30.57, - "sl6": 32.8, - "sl7": 34.0 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 39.2, + "sl5": 40.71, + "sl6": 42.0, + "sl7": 42.5 }, "ec": { "sl1": 0.0, @@ -658,31 +658,31 @@ "score_loc": 0.017 }, "ph": { - "sl1": 4.8, - "sl2": 4.8, - "sl3": 4.8, - "sl4": 4.88, - "sl5": 4.93, - "sl6": 4.98, - "sl7": 4.98 + "sl1": 4.5, + "sl2": 4.5, + "sl3": 4.5, + "sl4": 4.58, + "sl5": 4.63, + "sl6": 4.68, + "sl7": 4.72 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 3.6, - "sl5": 4.86, - "sl6": 5.4, - "sl7": 5.83 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.57, + "sl6": 4.0, + "sl7": 5.0 }, "sand": { - "sl1": 45.0, - "sl2": 45.0, - "sl3": 45.0, - "sl4": 42.0, - "sl5": 40.57, - "sl6": 39.2, - "sl7": 37.67 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 50.0, + "sl5": 48.71, + "sl6": 47.6, + "sl7": 47.17 }, "site": { "siteData": { @@ -705,13 +705,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sandy clay", + "sl2": "Sandy clay", + "sl3": "Sandy clay", + "sl4": "Sandy clay", + "sl5": "Sandy clay", + "sl6": "Sandy clay", + "sl7": "Sandy clay" } } ] @@ -722,16 +722,28 @@ "model": "v2" }, "soilRank": [ + { + "component": "Ferralic arenosols", + "componentData": "Data Complete", + "componentID": 144044, + "name": "Ferralic arenosols", + "rank_data": "6", + "rank_data_loc": "1", + "rank_loc": 1, + "score_data": 0.35, + "score_data_loc": 1.0, + "score_loc": 0.4 + }, { "component": "Ferralic cambisols", "componentData": "Data Complete", "componentID": 144042, "name": "Ferralic cambisols", "rank_data": "1", - "rank_data_loc": "1", + "rank_data_loc": "2", "rank_loc": 4, "score_data": 0.621, - "score_data_loc": 1.0, + "score_data_loc": 0.939, "score_loc": 0.083 }, { @@ -739,35 +751,35 @@ "componentData": "No Data", "componentID": 144043, "name": "Haplic ferralsols", - "rank_data": "4", - "rank_data_loc": "2", - "rank_loc": 3, - "score_data": 0.519, - "score_data_loc": 0.926, - "score_loc": 0.133 - }, - { - "component": "Xanthic ferralsols", - "componentData": "Missing Data", - "componentID": 156033, - "name": "Xanthic ferralsols", - "rank_data": "5", + "rank_data": "3", "rank_data_loc": "3", "rank_loc": 2, - "score_data": 0.517, - "score_data_loc": 0.924, + "score_data": 0.571, + "score_data_loc": 0.939, "score_loc": 0.133 }, + { + "component": "Dystric fluvisols", + "componentData": "Data Complete", + "componentID": 148190, + "name": "Dystric fluvisols", + "rank_data": "2", + "rank_data_loc": "4", + "rank_loc": 5, + "score_data": 0.571, + "score_data_loc": 0.783, + "score_loc": 0.017 + }, { "component": "Dystric gleysols", "componentData": "Missing Data", "componentID": 148189, "name": "Dystric gleysols", - "rank_data": "2", - "rank_data_loc": "4", + "rank_data": "4", + "rank_data_loc": "5", "rank_loc": 6, - "score_data": 0.571, - "score_data_loc": 0.834, + "score_data": 0.519, + "score_data_loc": 0.713, "score_loc": 0.017 }, { @@ -775,36 +787,24 @@ "componentData": "Missing Data", "componentID": 144045, "name": "Gleyic acrisols", - "rank_data": "3", - "rank_data_loc": "5", + "rank_data": "5", + "rank_data_loc": "6", "rank_loc": 7, - "score_data": 0.571, - "score_data_loc": 0.834, + "score_data": 0.517, + "score_data_loc": 0.712, "score_loc": 0.017 }, { - "component": "Ferralic arenosols", - "componentData": "Data Complete", - "componentID": 144044, - "name": "Ferralic arenosols", + "component": "Xanthic ferralsols", + "componentData": "Missing Data", + "componentID": 156033, + "name": "Xanthic ferralsols", "rank_data": "7", - "rank_data_loc": "6", - "rank_loc": 1, - "score_data": 0.0, - "score_data_loc": 0.568, - "score_loc": 0.4 - }, - { - "component": "Dystric fluvisols", - "componentData": "Data Complete", - "componentID": 148190, - "name": "Dystric fluvisols", - "rank_data": "6", "rank_data_loc": "7", - "rank_loc": 5, - "score_data": 0.35, - "score_data_loc": 0.521, - "score_loc": 0.017 + "rank_loc": 3, + "score_data": 0.0, + "score_data_loc": 0.178, + "score_loc": 0.133 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json index 0366726..22cedc9 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.07856,15.107436].json @@ -25,93 +25,93 @@ "sl7": 120 }, "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 6.4, - "sl5": 6.14, - "sl6": 5.8, - "sl7": 5.33 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.6, + "sl5": 13.57, + "sl6": 13.0, + "sl7": 13.17 }, "clay": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 25.8, - "sl5": 27.14, - "sl6": 28.6, - "sl7": 31.17 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.8, + "sl5": 18.86, + "sl6": 18.8, + "sl7": 18.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Xanthic ferralsols", - "name": "Xanthic ferralsols1", + "component": "Eutric leptosols", + "name": "Eutric leptosols1", "rank_loc": "1", - "score_loc": 0.067 + "score_loc": 0.033 }, "ph": { - "sl1": 4.5, - "sl2": 4.5, - "sl3": 4.5, - "sl4": 4.58, - "sl5": 4.63, - "sl6": 4.68, - "sl7": 4.72 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.62, + "sl5": 7.66, + "sl6": 7.68, + "sl7": 7.7 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.2, - "sl5": 3.57, - "sl6": 4.0, - "sl7": 5.0 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.57, + "sl6": 4.4, + "sl7": 5.5 }, "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0, - "sl4": 62.8, - "sl5": 61.71, - "sl6": 61.0, - "sl7": 58.5 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.2, + "sl5": 54.14, + "sl6": 54.6, + "sl7": 55.0 }, "site": { "siteData": { - "componentID": 105399, - "distance": 4468.846, - "mapunitID": 12207, - "minCompDistance": 4468.8459, - "share": 10, - "soilDepth": 200 + "componentID": 104801, + "distance": 31871.197, + "mapunitID": 12046, + "minCompDistance": 31871.1971, + "share": 15, + "soilDepth": 40 }, "siteDescription": { - "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", - "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -125,83 +125,83 @@ "sl7": 120 }, "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 6.4, - "sl5": 6.14, - "sl6": 5.8, - "sl7": 5.33 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 16.6, + "sl5": 16.14, + "sl6": 15.8, + "sl7": 15.5 }, "clay": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 25.8, - "sl5": 27.14, - "sl6": 28.6, - "sl7": 31.17 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 30.8, + "sl5": 30.57, + "sl6": 30.4, + "sl7": 30.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.83 }, "id": { - "component": "Haplic ferralsols", - "name": "Haplic ferralsols1", + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", "rank_loc": "2", - "score_loc": 0.042 + "score_loc": 0.029 }, "ph": { - "sl1": 4.5, - "sl2": 4.5, - "sl3": 4.5, - "sl4": 4.58, - "sl5": 4.63, - "sl6": 4.68, - "sl7": 4.72 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.52, + "sl5": 6.54, + "sl6": 6.6, + "sl7": 6.68 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.2, - "sl5": 3.57, - "sl6": 4.0, - "sl7": 5.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 7.6, + "sl5": 8.43, + "sl6": 8.6, + "sl7": 9.0 }, "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0, - "sl4": 62.8, - "sl5": 61.71, - "sl6": 61.0, - "sl7": 58.5 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 52.4, + "sl5": 53.0, + "sl6": 53.6, + "sl7": 54.5 }, "site": { "siteData": { - "componentID": 105398, - "distance": 4468.846, - "mapunitID": 12207, - "minCompDistance": 4468.8459, - "share": 15, + "componentID": 104657, + "distance": 86884.207, + "mapunitID": 12006, + "minCompDistance": 86884.2069, + "share": 70, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", - "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { @@ -225,22 +225,22 @@ "sl7": 120 }, "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 5.6, - "sl5": 5.14, - "sl6": 4.6, - "sl7": 4.33 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.6, + "sl5": 3.14, + "sl6": 3.0, + "sl7": 2.83 }, "clay": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 39.2, - "sl5": 40.71, - "sl6": 42.0, - "sl7": 42.5 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.0, + "sl6": 5.0, + "sl7": 5.17 }, "ec": { "sl1": 0.0, @@ -252,66 +252,66 @@ "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols1", + "component": "Eutric cambisols", + "name": "Eutric cambisols1", "rank_loc": "3", - "score_loc": 0.042 + "score_loc": 0.021 }, "ph": { - "sl1": 4.5, - "sl2": 4.5, - "sl3": 4.5, - "sl4": 4.58, - "sl5": 4.63, - "sl6": 4.68, - "sl7": 4.72 + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.72, + "sl5": 5.74, + "sl6": 5.76, + "sl7": 5.77 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.2, - "sl5": 3.57, - "sl6": 4.0, - "sl7": 5.0 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.8, + "sl5": 5.43, + "sl6": 5.0, + "sl7": 4.5 }, "sand": { - "sl1": 53.0, - "sl2": 53.0, - "sl3": 53.0, - "sl4": 50.0, - "sl5": 48.71, - "sl6": 47.6, - "sl7": 47.17 + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 88.0, + "sl5": 88.0, + "sl6": 88.2, + "sl7": 88.17 }, "site": { "siteData": { - "componentID": 104800, - "distance": 31871.197, - "mapunitID": 12046, - "minCompDistance": 31871.1971, - "share": 15, - "soilDepth": 20 + "componentID": 104809, + "distance": 75356.147, + "mapunitID": 12048, + "minCompDistance": 75356.1465, + "share": 20, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Sandy clay", - "sl2": "Sandy clay", - "sl3": "Sandy clay", - "sl4": "Sandy clay", - "sl5": "Sandy clay", - "sl6": "Sandy clay", - "sl7": "Sandy clay" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" } }, { @@ -319,167 +319,75 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl4": 40 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.6, - "sl5": 6.14, - "sl6": 5.8, - "sl7": 5.67 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.0 }, "clay": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0, - "sl4": 38.8, - "sl5": 39.86, - "sl6": 40.8, - "sl7": 41.5 + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 27.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 }, "id": { - "component": "Eutric leptosols", - "name": "Eutric leptosols1", + "component": "Haplic arenosols", + "name": "Haplic arenosols", "rank_loc": "4", - "score_loc": 0.033 + "score_loc": 0.021 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.16, - "sl5": 5.19, - "sl6": 5.24, - "sl7": 5.28 + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.55 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 3.4, - "sl5": 3.29, - "sl6": 3.2, - "sl7": 5.17 + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 30.5 }, "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 38.8, - "sl5": 37.86, - "sl6": 36.8, - "sl7": 36.0 + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 44.0 }, "site": { "siteData": { - "componentID": 104801, + "componentID": 104798, "distance": 31871.197, "mapunitID": 12046, "minCompDistance": 31871.1971, - "share": 15, - "soilDepth": 40 - }, - "siteDescription": { - "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", - "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Eutric fluvisols", - "name": "Eutric fluvisols", - "rank_loc": "5", - "score_loc": 0.029 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 - }, - "rock_fragments": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0 - }, - "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 - }, - "site": { - "siteData": { - "componentID": 104657, - "distance": 86884.207, - "mapunitID": 12006, - "minCompDistance": 86884.2069, - "share": 70, + "share": 50, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", - "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + "Description_en": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_es": "Los Arenosoles Háplicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.", + "Description_fr": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_ks": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " } }, "texture": { "sl1": "Loam", "sl2": "Loam", - "sl3": "Loam" + "sl3": "Loam", + "sl4": "Loam" } }, { @@ -493,22 +401,22 @@ "sl7": 120 }, "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 8.0, - "sl5": 7.43, - "sl6": 7.0, - "sl7": 6.83 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 }, "clay": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 46.4, - "sl5": 47.43, - "sl6": 48.2, - "sl7": 48.33 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 }, "ec": { "sl1": 0.0, @@ -520,286 +428,166 @@ "sl7": 0.0 }, "id": { - "component": "Rhodic ferralsols", - "name": "Rhodic ferralsols1", - "rank_loc": "6", - "score_loc": 0.025 + "component": "Ferralic arenosols", + "name": "Ferralic arenosols1", + "rank_loc": "5", + "score_loc": 0.017 }, "ph": { - "sl1": 4.9, - "sl2": 4.9, - "sl3": 4.9, - "sl4": 4.92, - "sl5": 4.96, - "sl6": 5.0, - "sl7": 5.02 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 }, "rock_fragments": { "sl1": 4.0, "sl2": 4.0, "sl3": 4.0, - "sl4": 4.6, - "sl5": 4.71, - "sl6": 5.0, - "sl7": 5.0 + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 37.4, - "sl5": 36.57, - "sl6": 35.8, - "sl7": 35.5 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 }, "site": { "siteData": { - "componentID": 105419, - "distance": 21840.312, - "mapunitID": 12213, - "minCompDistance": 21840.3117, + "componentID": 105472, + "distance": 40422.283, + "mapunitID": 12228, + "minCompDistance": 40422.2833, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", - "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20 + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.6, + "sl5": 14.71, + "sl6": 15.0, + "sl7": 15.17 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.6, + "sl5": 29.86, + "sl6": 30.6, + "sl7": 30.5 }, "ec": { "sl1": 1.0, "sl2": 1.0, - "sl3": 1.0 + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Luvic phaeozems", - "name": "Luvic phaeozems", - "rank_loc": "7", - "score_loc": 0.025 + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "6", + "score_loc": 0.017 }, "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.44, + "sl6": 6.44, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 9.29, + "sl6": 13.4, + "sl7": 12.5 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 - }, - "site": { - "siteData": { - "componentID": 104807, - "distance": 75356.147, - "mapunitID": 12048, - "minCompDistance": 75356.1465, - "share": 25, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", - "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 40 - }, - "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.0 - }, - "clay": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 27.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0 - }, - "id": { - "component": "Haplic arenosols", - "name": "Haplic arenosols", - "rank_loc": "8", - "score_loc": 0.021 - }, - "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.55 - }, - "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 30.5 - }, - "sand": { - "sl1": 45.0, - "sl2": 45.0, - "sl3": 45.0, - "sl4": 44.0 - }, - "site": { - "siteData": { - "componentID": 104798, - "distance": 31871.197, - "mapunitID": 12046, - "minCompDistance": 31871.1971, - "share": 50, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", - "Description_es": "Los Arenosoles Háplicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.", - "Description_fr": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", - "Description_ks": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 40 - }, - "cec": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 21.5 - }, - "clay": { - "sl1": 27.0, - "sl2": 27.0, - "sl3": 27.0, - "sl4": 34.5 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0 - }, - "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols1", - "rank_loc": "9", - "score_loc": 0.021 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7, - "sl4": 6.55 - }, - "rock_fragments": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 40.5 - }, - "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 36.5 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 49.0, + "sl5": 47.71, + "sl6": 46.6, + "sl7": 46.67 }, "site": { "siteData": { - "componentID": 104809, + "componentID": 104806, "distance": 75356.147, "mapunitID": 12048, "minCompDistance": 75356.1465, - "share": 20, + "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -807,49 +595,70 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 40 + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 12.5 + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.6, + "sl5": 21.86, + "sl6": 22.2, + "sl7": 22.67 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 18.0 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.0, + "sl5": 31.43, + "sl6": 31.4, + "sl7": 31.33 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 2.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 }, "id": { "component": "Ferralic cambisols", "name": "Ferralic cambisols1", - "rank_loc": "10", + "rank_loc": "7", "score_loc": 0.017 }, "ph": { - "sl1": 7.7, - "sl2": 7.7, - "sl3": 7.7, - "sl4": 7.65 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.47, + "sl6": 6.58, + "sl7": 6.65 }, "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.5 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.8, + "sl5": 16.57, + "sl6": 17.8, + "sl7": 16.0 }, "sand": { - "sl1": 61.0, - "sl2": 61.0, - "sl3": 61.0, - "sl4": 57.0 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.2, + "sl5": 39.14, + "sl6": 39.6, + "sl7": 39.33 }, "site": { "siteData": { @@ -872,110 +681,13 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.6, - "sl5": 13.57, - "sl6": 13.0, - "sl7": 13.17 - }, - "clay": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 18.8, - "sl5": 18.86, - "sl6": 18.8, - "sl7": 18.83 - }, - "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 - }, - "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols1", - "rank_loc": "11", - "score_loc": 0.017 - }, - "ph": { - "sl1": 7.5, - "sl2": 7.5, - "sl3": 7.5, - "sl4": 7.62, - "sl5": 7.66, - "sl6": 7.68, - "sl7": 7.7 - }, - "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.57, - "sl6": 4.4, - "sl7": 5.5 - }, - "sand": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 54.2, - "sl5": 54.14, - "sl6": 54.6, - "sl7": 55.0 - }, - "site": { - "siteData": { - "componentID": 105472, - "distance": 40422.283, - "mapunitID": 12228, - "minCompDistance": 40422.2833, - "share": 20, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -989,83 +701,83 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 7.6, - "sl5": 7.14, - "sl6": 6.6, - "sl7": 6.33 + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 39.6, + "sl5": 39.57, + "sl6": 39.2, + "sl7": 38.67 }, "clay": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 49.8, - "sl5": 50.71, - "sl6": 51.4, - "sl7": 51.67 + "sl1": 54.0, + "sl2": 54.0, + "sl3": 54.0, + "sl4": 55.4, + "sl5": 55.86, + "sl6": 55.8, + "sl7": 55.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.2, + "sl7": 1.5 }, "id": { - "component": "Chromic luvisols", - "name": "Chromic luvisols", - "rank_loc": "12", - "score_loc": 0.017 + "component": "Eutric gleysols", + "name": "Eutric gleysols", + "rank_loc": "8", + "score_loc": 0.012 }, "ph": { - "sl1": 5.5, - "sl2": 5.5, - "sl3": 5.5, - "sl4": 5.44, - "sl5": 5.44, - "sl6": 5.46, - "sl7": 5.48 + "sl1": 7.8, + "sl2": 7.8, + "sl3": 7.8, + "sl4": 7.94, + "sl5": 7.99, + "sl6": 8.04, + "sl7": 8.07 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 7.0, - "sl5": 5.29, - "sl6": 4.2, - "sl7": 4.67 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.4, + "sl5": 4.29, + "sl6": 4.0, + "sl7": 4.17 }, "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 34.4, - "sl5": 33.57, - "sl6": 32.8, - "sl7": 32.5 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.2, + "sl5": 16.86, + "sl6": 16.8, + "sl7": 16.67 }, "site": { "siteData": { - "componentID": 104806, - "distance": 75356.147, - "mapunitID": 12048, - "minCompDistance": 75356.1465, - "share": 35, + "componentID": 104658, + "distance": 86884.207, + "mapunitID": 12006, + "minCompDistance": 86884.2069, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", - "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { @@ -1089,93 +801,93 @@ "sl7": 120 }, "cec": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 23.0, - "sl5": 22.29, - "sl6": 21.8, - "sl7": 21.5 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.2, + "sl5": 12.43, + "sl6": 13.0, + "sl7": 13.33 }, "clay": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0, - "sl4": 40.2, - "sl5": 41.57, - "sl6": 42.0, - "sl7": 41.5 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 22.8, + "sl5": 23.29, + "sl6": 23.4, + "sl7": 23.17 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Xanthic ferralsols", - "name": "Xanthic ferralsols2", - "rank_loc": "Not Displayed", - "score_loc": 0.067 + "component": "Calcic vertisols", + "name": "Calcic vertisols", + "rank_loc": "9", + "score_loc": 0.008 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.26, - "sl5": 6.29, - "sl6": 6.32, - "sl7": 6.32 + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.9, + "sl5": 6.96, + "sl6": 7.06, + "sl7": 7.13 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 8.4, - "sl5": 8.43, - "sl6": 8.6, - "sl7": 12.33 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 8.6, + "sl5": 10.14, + "sl6": 10.8, + "sl7": 12.17 }, "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 34.4, - "sl5": 33.71, - "sl6": 33.8, - "sl7": 34.67 + "sl1": 61.0, + "sl2": 61.0, + "sl3": 61.0, + "sl4": 58.6, + "sl5": 58.43, + "sl6": 58.2, + "sl7": 58.5 }, "site": { "siteData": { - "componentID": 105417, - "distance": 21840.312, - "mapunitID": 12213, - "minCompDistance": 4468.8459, - "share": 30, + "componentID": 105227, + "distance": 99332.531, + "mapunitID": 12163, + "minCompDistance": 99332.5308, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", - "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.", + "Description_es": "Los Vertisoles Cálcicos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles cálcicos son calcáreos en una capa del suelo por debajo de la superficie. ", + "Description_fr": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.", + "Description_ks": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, sin embargo las características de la arcilla en este suelo pueden hacer que el manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -1183,99 +895,75 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl4": 40 }, "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 8.4, - "sl5": 7.71, - "sl6": 7.2, - "sl7": 7.0 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 12.5 }, "clay": { - "sl1": 48.0, - "sl2": 48.0, - "sl3": 48.0, - "sl4": 52.6, - "sl5": 53.86, - "sl6": 55.0, - "sl7": 55.67 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 18.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 2.0 }, "id": { - "component": "Xanthic ferralsols", - "name": "Xanthic ferralsols3", - "rank_loc": "Not Displayed", - "score_loc": 0.067 + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "10", + "score_loc": 0.008 }, "ph": { - "sl1": 5.6, - "sl2": 5.6, - "sl3": 5.6, - "sl4": 5.62, - "sl5": 5.63, - "sl6": 5.64, - "sl7": 5.65 + "sl1": 7.7, + "sl2": 7.7, + "sl3": 7.7, + "sl4": 7.65 }, "rock_fragments": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 17.0, - "sl5": 12.71, - "sl6": 10.0, - "sl7": 8.83 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.5 }, "sand": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 32.2, - "sl5": 31.29, - "sl6": 30.4, - "sl7": 29.83 + "sl1": 61.0, + "sl2": 61.0, + "sl3": 61.0, + "sl4": 57.0 }, "site": { "siteData": { - "componentID": 104818, - "distance": 96145.535, - "mapunitID": 12052, + "componentID": 105396, + "distance": 4468.846, + "mapunitID": 12207, "minCompDistance": 4468.8459, - "share": 30, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_es": "Los Ferralsoles Xánticos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos xánticos tienen subsuelos de color amarillo que indican una retención de humedad ligeramente superior. ", - "Description_fr": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Description_ks": "Xanthic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Xanthic Ferralsols have yellow colored subsoils indicating slightly higher moisture retention. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos. *Prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam" } }, { @@ -1289,93 +977,93 @@ "sl7": 120 }, "cec": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 3.6, - "sl5": 3.14, - "sl6": 3.0, - "sl7": 2.83 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.14, + "sl6": 6.8, + "sl7": 6.67 }, "clay": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0, - "sl5": 5.0, - "sl6": 5.0, - "sl7": 5.17 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 33.4, + "sl5": 33.86, + "sl6": 34.0, + "sl7": 33.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 }, "id": { - "component": "Haplic ferralsols", - "name": "Haplic ferralsols2", - "rank_loc": "Not Displayed", - "score_loc": 0.042 + "component": "Chromic cambisols", + "name": "Chromic cambisols", + "rank_loc": "11", + "score_loc": 0.006 }, "ph": { - "sl1": 5.7, - "sl2": 5.7, - "sl3": 5.7, - "sl4": 5.72, - "sl5": 5.74, - "sl6": 5.76, - "sl7": 5.77 + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.12, + "sl5": 5.14, + "sl6": 5.14, + "sl7": 5.13 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 4.8, - "sl5": 5.43, - "sl6": 5.0, - "sl7": 4.5 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.2, + "sl5": 11.43, + "sl6": 12.6, + "sl7": 12.83 }, "sand": { - "sl1": 88.0, - "sl2": 88.0, - "sl3": 88.0, - "sl4": 88.0, - "sl5": 88.0, - "sl6": 88.2, - "sl7": 88.17 + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 43.0, + "sl5": 42.43, + "sl6": 42.0, + "sl7": 42.0 }, "site": { "siteData": { - "componentID": 104799, - "distance": 31871.197, - "mapunitID": 12046, - "minCompDistance": 4468.8459, - "share": 20, + "componentID": 105228, + "distance": 99332.531, + "mapunitID": 12163, + "minCompDistance": 99332.5308, + "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", - "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Sand", - "sl2": "Sand", - "sl3": "Sand", - "sl4": "Sand", - "sl5": "Sand", - "sl6": "Sand", - "sl7": "Sand" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1383,99 +1071,75 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl4": 40 }, "cec": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 21.6, - "sl5": 21.86, - "sl6": 22.2, - "sl7": 22.67 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 21.5 }, "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 31.0, - "sl5": 31.43, - "sl6": 31.4, - "sl7": 31.33 + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 34.5 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.29, - "sl6": 1.2, - "sl7": 1.17 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.042 + "component": "Gleyic arenosols", + "name": "Gleyic arenosols1", + "rank_loc": "12", + "score_loc": 0.004 }, "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.42, - "sl5": 6.47, - "sl6": 6.58, - "sl7": 6.65 - }, - "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 15.8, - "sl5": 16.57, - "sl6": 17.8, - "sl7": 16.0 + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.55 + }, + "rock_fragments": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 40.5 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 39.2, - "sl5": 39.14, - "sl6": 39.6, - "sl7": 39.33 + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 36.5 }, "site": { "siteData": { - "componentID": 105352, - "distance": 99172.777, - "mapunitID": 12196, - "minCompDistance": 31871.1971, + "componentID": 105487, + "distance": 34740.199, + "mapunitID": 12231, + "minCompDistance": 34740.1989, "share": 10, - "soilDepth": 20 + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.", + "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam" } }, { @@ -1517,7 +1181,7 @@ }, "id": { "component": "Eutric leptosols", - "name": "Eutric leptosols2", + "name": "Eutric leptosols3", "rank_loc": "Not Displayed", "score_loc": 0.033 }, @@ -1550,11 +1214,11 @@ }, "site": { "siteData": { - "componentID": 105349, - "distance": 99172.777, - "mapunitID": 12196, + "componentID": 105229, + "distance": 99332.531, + "mapunitID": 12163, "minCompDistance": 31871.1971, - "share": 45, + "share": 10, "soilDepth": 40 }, "siteDescription": { @@ -1617,7 +1281,7 @@ }, "id": { "component": "Eutric leptosols", - "name": "Eutric leptosols3", + "name": "Eutric leptosols2", "rank_loc": "Not Displayed", "score_loc": 0.033 }, @@ -1650,11 +1314,11 @@ }, "site": { "siteData": { - "componentID": 105229, - "distance": 99332.531, - "mapunitID": 12163, + "componentID": 105349, + "distance": 99172.777, + "mapunitID": 12196, "minCompDistance": 31871.1971, - "share": 10, + "share": 45, "soilDepth": 40 }, "siteDescription": { @@ -1689,91 +1353,91 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 7.6, - "sl5": 7.14, - "sl6": 6.8, - "sl7": 6.67 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.0, + "sl5": 6.0, + "sl6": 6.0, + "sl7": 6.0 }, "clay": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 33.4, - "sl5": 33.86, - "sl6": 34.0, - "sl7": 33.83 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 25.6, + "sl5": 28.14, + "sl6": 30.0, + "sl7": 30.5 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.5 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Rhodic ferralsols", - "name": "Rhodic ferralsols2", + "component": "Eutric cambisols", + "name": "Eutric cambisols2", "rank_loc": "Not Displayed", - "score_loc": 0.025 + "score_loc": 0.021 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.12, - "sl5": 5.14, - "sl6": 5.14, + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.2, + "sl5": 5.19, + "sl6": 5.16, "sl7": 5.13 }, "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 10.2, - "sl5": 11.43, - "sl6": 12.6, - "sl7": 12.83 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.2, + "sl7": 5.83 }, "sand": { - "sl1": 45.0, - "sl2": 45.0, - "sl3": 45.0, - "sl4": 43.0, - "sl5": 42.43, - "sl6": 42.0, - "sl7": 42.0 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.8, + "sl5": 45.86, + "sl6": 44.8, + "sl7": 44.83 }, "site": { "siteData": { - "componentID": 104820, - "distance": 96145.535, - "mapunitID": 12052, - "minCompDistance": 21840.3117, - "share": 20, + "componentID": 105350, + "distance": 99172.777, + "mapunitID": 12196, + "minCompDistance": 75356.1465, + "share": 25, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", - "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", "sl6": "Clay loam", "sl7": "Clay loam" } @@ -1816,10 +1480,10 @@ "sl7": 0.0 }, "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols2", + "component": "Ferralic cambisols", + "name": "Ferralic cambisols2", "rank_loc": "Not Displayed", - "score_loc": 0.021 + "score_loc": 0.017 }, "ph": { "sl1": 5.5, @@ -1850,22 +1514,22 @@ }, "site": { "siteData": { - "componentID": 105350, - "distance": 99172.777, - "mapunitID": 12196, - "minCompDistance": 75356.1465, - "share": 25, + "componentID": 105247, + "distance": 28892.433, + "mapunitID": 12167, + "minCompDistance": 4468.8459, + "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " } }, "texture": { @@ -1889,22 +1553,22 @@ "sl7": 120 }, "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.29, - "sl6": 2.2, - "sl7": 2.0 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.6, + "sl5": 3.14, + "sl6": 2.8, + "sl7": 2.67 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.2, - "sl5": 6.43, - "sl6": 6.8, - "sl7": 7.0 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.14, + "sl6": 5.2, + "sl7": 5.33 }, "ec": { "sl1": 0.0, @@ -1916,56 +1580,56 @@ "sl7": 0.0 }, "id": { - "component": "Ferralic cambisols", - "name": "Ferralic cambisols2", + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", "rank_loc": "Not Displayed", "score_loc": 0.017 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.32, - "sl5": 5.34, - "sl6": 5.36, - "sl7": 5.37 + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.8, + "sl5": 5.8, + "sl6": 5.8, + "sl7": 5.82 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.2, - "sl5": 4.43, - "sl6": 4.6, - "sl7": 4.5 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 10.4, + "sl5": 11.0, + "sl6": 10.0, + "sl7": 8.83 }, "sand": { "sl1": 87.0, "sl2": 87.0, "sl3": 87.0, - "sl4": 86.8, - "sl5": 86.57, - "sl6": 86.2, - "sl7": 86.0 + "sl4": 87.2, + "sl5": 87.29, + "sl6": 87.4, + "sl7": 86.83 }, "site": { "siteData": { - "componentID": 105247, - "distance": 28892.433, - "mapunitID": 12167, - "minCompDistance": 4468.8459, + "componentID": 104805, + "distance": 63317.634, + "mapunitID": 12047, + "minCompDistance": 40422.2833, "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", - "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { @@ -1989,93 +1653,93 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 14.6, - "sl5": 14.71, - "sl6": 15.0, - "sl7": 15.17 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.2, + "sl5": 2.86, + "sl6": 2.6, + "sl7": 2.5 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 28.6, - "sl5": 29.86, - "sl6": 30.6, - "sl7": 30.5 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.6, + "sl5": 5.71, + "sl6": 6.0, + "sl7": 6.67 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols2", + "component": "Gleyic arenosols", + "name": "Gleyic arenosols2", "rank_loc": "Not Displayed", - "score_loc": 0.017 + "score_loc": 0.004 }, "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.42, - "sl5": 6.44, - "sl6": 6.44, - "sl7": 6.43 + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.64, + "sl5": 5.63, + "sl6": 5.64, + "sl7": 5.63 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.8, - "sl5": 9.29, - "sl6": 13.4, - "sl7": 12.5 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 11.6, + "sl5": 11.86, + "sl6": 10.6, + "sl7": 9.33 }, "sand": { - "sl1": 53.0, - "sl2": 53.0, - "sl3": 53.0, - "sl4": 49.0, - "sl5": 47.71, - "sl6": 46.6, - "sl7": 46.67 + "sl1": 84.0, + "sl2": 84.0, + "sl3": 84.0, + "sl4": 84.6, + "sl5": 84.71, + "sl6": 84.2, + "sl7": 82.33 }, "site": { "siteData": { - "componentID": 104805, - "distance": 63317.634, - "mapunitID": 12047, - "minCompDistance": 40422.2833, - "share": 15, + "componentID": 105474, + "distance": 40422.283, + "mapunitID": 12228, + "minCompDistance": 34740.1989, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.", + "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } } ] @@ -2087,184 +1751,148 @@ }, "soilRank": [ { - "component": "Eutric fluvisols", + "component": "Ferralic arenosols", "componentData": "Data Complete", - "componentID": 104657, - "name": "Eutric fluvisols", - "rank_data": "2", + "componentID": 105472, + "name": "Ferralic arenosols1", + "rank_data": "3", "rank_data_loc": "1", "rank_loc": "5", "score_data": 1.0, "score_data_loc": 1.0, - "score_loc": 0.029 + "score_loc": 0.017 }, { - "component": "Luvic phaeozems", - "componentData": "Missing Data", - "componentID": 104807, - "name": "Luvic phaeozems", - "rank_data": "5", + "component": "Eutric gleysols", + "componentData": "Data Complete", + "componentID": 104658, + "name": "Eutric gleysols", + "rank_data": "2", "rank_data_loc": "2", - "rank_loc": "7", + "rank_loc": "8", "score_data": 1.0, "score_data_loc": 0.996, - "score_loc": 0.025 + "score_loc": 0.012 }, { - "component": "Eutric cambisols", - "componentData": "Data Complete", - "componentID": 104809, - "name": "Eutric cambisols1", + "component": "Calcic vertisols", + "componentData": "No Data", + "componentID": 105227, + "name": "Calcic vertisols", "rank_data": "1", "rank_data_loc": "3", "rank_loc": "9", "score_data": 1.0, "score_data_loc": 0.992, - "score_loc": 0.021 + "score_loc": 0.008 }, { - "component": "Haplic arenosols", + "component": "Eutric fluvisols", "componentData": "Data Complete", - "componentID": 104798, - "name": "Haplic arenosols", - "rank_data": "4", + "componentID": 104657, + "name": "Eutric fluvisols", + "rank_data": "6", "rank_data_loc": "4", - "rank_loc": "8", - "score_data": 1.0, - "score_data_loc": 0.992, - "score_loc": 0.021 + "rank_loc": "2", + "score_data": 0.676, + "score_data_loc": 0.693, + "score_loc": 0.029 }, { - "component": "Xanthic ferralsols", - "componentData": "Missing Data", - "componentID": 104818, - "name": "Xanthic ferralsols3", - "rank_data": "8", + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 104806, + "name": "Chromic luvisols", + "rank_data": "5", "rank_data_loc": "5", - "rank_loc": "Not Displayed", - "score_data": 0.829, - "score_data_loc": 0.87, - "score_loc": 0.067 + "rank_loc": "6", + "score_data": 0.676, + "score_data_loc": 0.681, + "score_loc": 0.017 }, { - "component": "Rhodic ferralsols", - "componentData": "No Data", - "componentID": 105419, - "name": "Rhodic ferralsols1", - "rank_data": "7", + "component": "Haplic arenosols", + "componentData": "Data Complete", + "componentID": 104798, + "name": "Haplic arenosols", + "rank_data": "8", "rank_data_loc": "6", - "rank_loc": "6", - "score_data": 0.829, - "score_data_loc": 0.83, - "score_loc": 0.025 + "rank_loc": "4", + "score_data": 0.669, + "score_data_loc": 0.678, + "score_loc": 0.021 }, { - "component": "Chromic luvisols", + "component": "Haplic acrisols", "componentData": "Data Complete", - "componentID": 104806, - "name": "Chromic luvisols", - "rank_data": "6", + "componentID": 105396, + "name": "Haplic acrisols", + "rank_data": "7", "rank_data_loc": "7", - "rank_loc": "12", - "score_data": 0.829, - "score_data_loc": 0.821, - "score_loc": 0.017 + "rank_loc": "10", + "score_data": 0.676, + "score_data_loc": 0.673, + "score_loc": 0.008 }, { - "component": "Ferralic arenosols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 105472, - "name": "Ferralic arenosols1", - "rank_data": "10", + "componentID": 104809, + "name": "Eutric cambisols1", + "rank_data": "9", "rank_data_loc": "8", - "rank_loc": "11", - "score_data": 0.711, - "score_data_loc": 0.707, - "score_loc": 0.017 + "rank_loc": "3", + "score_data": 0.606, + "score_data_loc": 0.616, + "score_loc": 0.021 }, { "component": "Ferralic cambisols", "componentData": "Data Complete", "componentID": 105395, "name": "Ferralic cambisols1", - "rank_data": "11", + "rank_data": "10", "rank_data_loc": "9", - "rank_loc": "10", - "score_data": 0.711, - "score_data_loc": 0.707, + "rank_loc": "7", + "score_data": 0.606, + "score_data_loc": 0.612, "score_loc": 0.017 }, { - "component": "Haplic ferralsols", - "componentData": "Missing Data", - "componentID": 105398, - "name": "Haplic ferralsols1", - "rank_data": "12", + "component": "Gleyic arenosols", + "componentData": "Data Complete", + "componentID": 105487, + "name": "Gleyic arenosols1", + "rank_data": "11", "rank_data_loc": "10", - "rank_loc": "2", - "score_data": 0.659, - "score_data_loc": 0.68, - "score_loc": 0.042 + "rank_loc": "12", + "score_data": 0.476, + "score_data_loc": 0.472, + "score_loc": 0.004 }, { - "component": "Eutric leptosols", - "componentData": "Missing Data", - "componentID": 105349, - "name": "Eutric leptosols2", - "rank_data": "3", + "component": "Chromic cambisols", + "componentData": "Data Complete", + "componentID": 105228, + "name": "Chromic cambisols", + "rank_data": "12", "rank_data_loc": "11", - "rank_loc": "Not Displayed", - "score_data": 1.0, - "score_data_loc": 0.002, - "score_loc": 0.033 + "rank_loc": "11", + "score_data": 0.331, + "score_data_loc": 0.332, + "score_loc": 0.006 }, { - "component": "Lithic leptosols", + "component": "Eutric leptosols", "componentData": "Missing Data", - "componentID": 105352, - "name": "Lithic leptosols2", - "rank_data": "9", + "componentID": 105229, + "name": "Eutric leptosols3", + "rank_data": "Not Displayed", "rank_data_loc": "12", "rank_loc": "Not Displayed", - "score_data": 0.752, + "score_data": 0.669, "score_data_loc": 0.002, - "score_loc": 0.042 - }, - { - "component": "Xanthic ferralsols", - "componentData": "Missing Data", - "componentID": 105417, - "name": "Xanthic ferralsols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.752, - "score_data_loc": 0.795, - "score_loc": 0.067 - }, - { - "component": "Rhodic ferralsols", - "componentData": "No Data", - "componentID": 104820, - "name": "Rhodic ferralsols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.752, - "score_data_loc": 0.755, - "score_loc": 0.025 - }, - { - "component": "Xanthic ferralsols", - "componentData": "Missing Data", - "componentID": 105399, - "name": "Xanthic ferralsols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "1", - "score_data": 0.659, - "score_data_loc": 0.705, - "score_loc": 0.067 + "score_loc": 0.033 }, { "component": "Ferralic arenosols", @@ -2274,81 +1902,69 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.659, - "score_data_loc": 0.656, + "score_data": 0.676, + "score_data_loc": 0.681, "score_loc": 0.017 }, { - "component": "Ferralic cambisols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 105247, - "name": "Ferralic cambisols2", + "componentID": 105350, + "name": "Eutric cambisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.524, - "score_data_loc": 0.525, - "score_loc": 0.017 + "score_data": 0.476, + "score_data_loc": 0.489, + "score_loc": 0.021 }, { - "component": "Haplic ferralsols", - "componentData": "No Data", - "componentID": 104799, - "name": "Haplic ferralsols2", + "component": "Ferralic cambisols", + "componentData": "Data Complete", + "componentID": 105247, + "name": "Ferralic cambisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.392, - "score_data_loc": 0.421, - "score_loc": 0.042 + "score_data": 0.476, + "score_data_loc": 0.485, + "score_loc": 0.017 }, { - "component": "Eutric cambisols", + "component": "Gleyic arenosols", "componentData": "Data Complete", - "componentID": 105350, - "name": "Eutric cambisols2", + "componentID": 105474, + "name": "Gleyic arenosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.392, - "score_data_loc": 0.401, - "score_loc": 0.021 + "score_data": 0.331, + "score_data_loc": 0.33, + "score_loc": 0.004 }, { "component": "Eutric leptosols", "componentData": "Missing Data", "componentID": 104801, "name": "Eutric leptosols1", - "rank_data": "Not Displayed", + "rank_data": "4", "rank_data_loc": "Not Displayed", - "rank_loc": "4", - "score_data": 0.752, + "rank_loc": "1", + "score_data": 0.819, "score_data_loc": 0.002, "score_loc": 0.033 }, { "component": "Eutric leptosols", "componentData": "Missing Data", - "componentID": 105229, - "name": "Eutric leptosols3", + "componentID": 105349, + "name": "Eutric leptosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.752, + "score_data": 0.669, "score_data_loc": 0.002, "score_loc": 0.033 - }, - { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 104800, - "name": "Lithic leptosols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "3", - "score_data": 0.503, - "score_data_loc": 0.002, - "score_loc": 0.042 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json index 8bb8a9c..968dd67 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-10.950086,17.573093].json @@ -25,22 +25,22 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 10.2, - "sl5": 10.43, - "sl6": 10.4, - "sl7": 10.33 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.14, + "sl6": 1.8, + "sl7": 1.67 }, "clay": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 19.4, - "sl5": 21.43, - "sl6": 22.2, - "sl7": 22.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.86, + "sl6": 7.2, + "sl7": 7.33 }, "ec": { "sl1": 0.0, @@ -58,31 +58,31 @@ "score_loc": 0.127 }, "ph": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 4.92, - "sl5": 4.89, - "sl6": 4.86, - "sl7": 4.83 + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.5, + "sl5": 5.5, + "sl6": 5.5, + "sl7": 5.48 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 4.8, - "sl5": 4.29, - "sl6": 3.6, - "sl7": 3.83 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.71, + "sl6": 4.4, + "sl7": 6.0 }, "sand": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 28.0, - "sl5": 28.43, - "sl6": 31.4, - "sl7": 33.83 + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 89.0, + "sl5": 88.86, + "sl6": 88.4, + "sl7": 88.17 }, "site": { "siteData": { @@ -105,13 +105,13 @@ } }, "texture": { - "sl1": "Silt loam", - "sl2": "Silt loam", - "sl3": "Silt loam", - "sl4": "Silt loam", - "sl5": "Silt loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -128,19 +128,19 @@ "sl1": 11.0, "sl2": 11.0, "sl3": 11.0, - "sl4": 10.4, + "sl4": 10.2, "sl5": 10.43, "sl6": 10.4, - "sl7": 10.5 + "sl7": 10.33 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 23.2, - "sl5": 24.57, - "sl6": 25.6, - "sl7": 25.83 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 19.4, + "sl5": 21.43, + "sl6": 22.2, + "sl7": 22.0 }, "ec": { "sl1": 0.0, @@ -158,31 +158,31 @@ "score_loc": 0.029 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.24, - "sl5": 5.21, - "sl6": 5.18, - "sl7": 5.17 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.92, + "sl5": 4.89, + "sl6": 4.86, + "sl7": 4.83 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 11.4, - "sl5": 12.14, - "sl6": 13.4, - "sl7": 14.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 4.8, + "sl5": 4.29, + "sl6": 3.6, + "sl7": 3.83 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 37.4, - "sl5": 36.86, - "sl6": 36.8, - "sl7": 37.33 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 28.0, + "sl5": 28.43, + "sl6": 31.4, + "sl7": 33.83 }, "site": { "siteData": { @@ -205,11 +205,11 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Silt loam", + "sl5": "Silt loam", "sl6": "Loam", "sl7": "Loam" } @@ -219,37 +219,25 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl4": 40 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.4, - "sl5": 14.0, - "sl6": 14.6, - "sl7": 14.67 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 21.5 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 28.2, - "sl5": 30.71, - "sl6": 33.0, - "sl7": 33.83 + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 34.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 }, "id": { "component": "Ferralic arenosols", @@ -258,31 +246,22 @@ "score_loc": 0.027 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.24, - "sl5": 5.23, - "sl6": 5.22, - "sl7": 5.15 + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.55 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 3.4, - "sl5": 3.86, - "sl6": 4.6, - "sl7": 5.5 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 40.5 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0, - "sl4": 48.6, - "sl5": 46.43, - "sl6": 44.2, - "sl7": 42.5 + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 36.5 }, "site": { "siteData": { @@ -305,13 +284,10 @@ } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam" } }, { @@ -325,22 +301,22 @@ "sl7": 120 }, "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.14, - "sl6": 1.8, - "sl7": 1.67 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.6, + "sl5": 3.14, + "sl6": 2.8, + "sl7": 2.67 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.6, - "sl5": 6.86, - "sl6": 7.2, - "sl7": 7.33 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.14, + "sl6": 5.2, + "sl7": 5.33 }, "ec": { "sl1": 0.0, @@ -358,31 +334,31 @@ "score_loc": 0.023 }, "ph": { - "sl1": 5.5, - "sl2": 5.5, - "sl3": 5.5, - "sl4": 5.5, - "sl5": 5.5, - "sl6": 5.5, - "sl7": 5.48 + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.8, + "sl5": 5.8, + "sl6": 5.8, + "sl7": 5.82 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.2, - "sl5": 3.71, - "sl6": 4.4, - "sl7": 6.0 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 10.4, + "sl5": 11.0, + "sl6": 10.0, + "sl7": 8.83 }, "sand": { - "sl1": 89.0, - "sl2": 89.0, - "sl3": 89.0, - "sl4": 89.0, - "sl5": 88.86, - "sl6": 88.4, - "sl7": 88.17 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 87.2, + "sl5": 87.29, + "sl6": 87.4, + "sl7": 86.83 }, "site": { "siteData": { @@ -404,106 +380,6 @@ "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " } }, - "texture": { - "sl1": "Sand", - "sl2": "Sand", - "sl3": "Sand", - "sl4": "Sand", - "sl5": "Sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.29, - "sl6": 2.2, - "sl7": 2.0 - }, - "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.2, - "sl5": 6.43, - "sl6": 6.8, - "sl7": 7.0 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols1", - "rank_loc": "5", - "score_loc": 0.023 - }, - "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.32, - "sl5": 5.34, - "sl6": 5.36, - "sl7": 5.37 - }, - "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.2, - "sl5": 4.43, - "sl6": 4.6, - "sl7": 4.5 - }, - "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 86.8, - "sl5": 86.57, - "sl6": 86.2, - "sl7": 86.0 - }, - "site": { - "siteData": { - "componentID": 105466, - "distance": 61918.695, - "mapunitID": 12226, - "minCompDistance": 61918.6954, - "share": 25, - "soilDepth": 20 - }, - "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " - } - }, "texture": { "sl1": "Loamy sand", "sl2": "Loamy sand", @@ -514,218 +390,6 @@ "sl7": "Loamy sand" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 40 - }, - "cec": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 21.5 - }, - "clay": { - "sl1": 27.0, - "sl2": 27.0, - "sl3": 27.0, - "sl4": 34.5 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0 - }, - "id": { - "component": "Haplic ferralsols", - "name": "Haplic ferralsols1", - "rank_loc": "6", - "score_loc": 0.02 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7, - "sl4": 6.55 - }, - "rock_fragments": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 40.5 - }, - "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 36.5 - }, - "site": { - "siteData": { - "componentID": 104785, - "distance": 58618.178, - "mapunitID": 12042, - "minCompDistance": 58618.178, - "share": 40, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", - "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Rhodic ferralsols", - "name": "Rhodic ferralsols1", - "rank_loc": "7", - "score_loc": 0.02 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 - }, - "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0 - }, - "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 - }, - "site": { - "siteData": { - "componentID": 104784, - "distance": 58618.178, - "mapunitID": 12042, - "minCompDistance": 58618.178, - "share": 40, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", - "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Luvic phaeozems", - "name": "Luvic phaeozems1", - "rank_loc": "8", - "score_loc": 0.02 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 - }, - "rock_fragments": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0 - }, - "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 - }, - "site": { - "siteData": { - "componentID": 104946, - "distance": 88902.515, - "mapunitID": 12084, - "minCompDistance": 88902.5153, - "share": 15, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", - "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" - } - }, { "bottom_depth": { "sl1": 1, @@ -737,64 +401,64 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.6, - "sl5": 6.14, - "sl6": 5.8, - "sl7": 5.67 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.4, + "sl7": 16.83 }, "clay": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0, - "sl4": 38.8, - "sl5": 39.86, - "sl6": 40.8, - "sl7": 41.5 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 21.6, + "sl5": 21.57, + "sl6": 21.6, + "sl7": 22.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.29, + "sl6": 2.4, + "sl7": 2.33 }, "id": { "component": "Gleyic arenosols", "name": "Gleyic arenosols", - "rank_loc": "9", + "rank_loc": "5", "score_loc": 0.018 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.16, - "sl5": 5.19, - "sl6": 5.24, - "sl7": 5.28 + "sl1": 6.8, + "sl2": 6.8, + "sl3": 6.8, + "sl4": 7.0, + "sl5": 7.07, + "sl6": 7.16, + "sl7": 7.2 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 3.4, - "sl5": 3.29, - "sl6": 3.2, - "sl7": 5.17 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 4.2, + "sl5": 4.0, + "sl6": 3.4, + "sl7": 4.83 }, "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 38.8, - "sl5": 37.86, - "sl6": 36.8, - "sl7": 36.0 + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.4, + "sl5": 36.43, + "sl6": 36.4, + "sl7": 35.5 }, "site": { "siteData": { @@ -817,13 +481,13 @@ } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -837,93 +501,93 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 7.6, - "sl5": 7.14, - "sl6": 6.6, - "sl7": 6.33 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 5.8, + "sl5": 5.71, + "sl6": 5.8, + "sl7": 6.0 }, "clay": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 49.8, - "sl5": 50.71, - "sl6": 51.4, - "sl7": 51.67 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 12.6, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.29, + "sl6": 2.4, + "sl7": 2.33 }, "id": { - "component": "Umbric gleysols", - "name": "Umbric gleysols", - "rank_loc": "10", - "score_loc": 0.018 + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "6", + "score_loc": 0.016 }, "ph": { - "sl1": 5.5, - "sl2": 5.5, - "sl3": 5.5, - "sl4": 5.44, - "sl5": 5.44, - "sl6": 5.46, - "sl7": 5.48 + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.98, + "sl5": 5.03, + "sl6": 5.08, + "sl7": 5.12 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 7.0, - "sl5": 5.29, - "sl6": 4.2, - "sl7": 4.67 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.2, + "sl5": 12.29, + "sl6": 14.0, + "sl7": 13.83 }, "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 34.4, - "sl5": 33.57, - "sl6": 32.8, - "sl7": 32.5 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 47.2, + "sl5": 48.57, + "sl6": 48.8, + "sl7": 48.17 }, "site": { "siteData": { - "componentID": 104792, - "distance": 0.0, - "mapunitID": 12044, - "minCompDistance": 0.0, - "share": 10, + "componentID": 105457, + "distance": 53803.703, + "mapunitID": 12224, + "minCompDistance": 53803.703, + "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Description_es": "Los Gleysoles Úmbricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles úmbricos tienen una materia orgánica relativamente alta, pero menos nutrientes en los horizontes superficiales. ", - "Description_fr": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Description_ks": "Umbric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Umbric Gleysols have relatively higher organic matter but lower nutrients in surface horizons.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", - "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
El pH superficial del suelo es bajo en estos suelos, y es probable que sea necesario el encalado.", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
The surface soil pH is low in these soils, and liming will likely be required. " + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -937,93 +601,93 @@ "sl7": 120 }, "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 8.0, - "sl5": 7.43, - "sl6": 7.0, - "sl7": 6.83 + "sl1": 78.0, + "sl2": 78.0, + "sl3": 78.0, + "sl4": 77.2, + "sl5": 75.86, + "sl6": 73.8, + "sl7": 72.0 }, "clay": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 46.4, - "sl5": 47.43, - "sl6": 48.2, - "sl7": 48.33 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 34.4, + "sl5": 34.29, + "sl6": 33.4, + "sl7": 32.67 }, "ec": { "sl1": 0.0, "sl2": 0.0, "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl4": 0.6, + "sl5": 0.71, + "sl6": 0.8, + "sl7": 0.83 }, "id": { - "component": "Haplic acrisols", - "name": "Haplic acrisols", - "rank_loc": "11", + "component": "Ferralic cambisols", + "name": "Ferralic cambisols", + "rank_loc": "7", "score_loc": 0.016 }, "ph": { - "sl1": 4.9, - "sl2": 4.9, - "sl3": 4.9, - "sl4": 4.92, - "sl5": 4.96, - "sl6": 5.0, - "sl7": 5.02 + "sl1": 4.4, + "sl2": 4.4, + "sl3": 4.4, + "sl4": 4.3, + "sl5": 4.31, + "sl6": 4.34, + "sl7": 4.37 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.6, - "sl5": 4.71, - "sl6": 5.0, - "sl7": 5.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.2, + "sl5": 11.29, + "sl6": 10.6, + "sl7": 10.67 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 37.4, - "sl5": 36.57, - "sl6": 35.8, - "sl7": 35.5 + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 28.6, + "sl5": 29.0, + "sl6": 31.8, + "sl7": 33.83 }, "site": { "siteData": { - "componentID": 105457, - "distance": 53803.703, - "mapunitID": 12224, - "minCompDistance": 53803.703, + "componentID": 105461, + "distance": 82783.427, + "mapunitID": 12225, + "minCompDistance": 82783.4266, "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1037,22 +701,22 @@ "sl7": 120 }, "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 8.4, - "sl5": 7.71, - "sl6": 7.2, - "sl7": 7.0 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 }, "clay": { - "sl1": 48.0, - "sl2": 48.0, - "sl3": 48.0, - "sl4": 52.6, - "sl5": 53.86, - "sl6": 55.0, - "sl7": 55.67 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 }, "ec": { "sl1": 0.0, @@ -1064,66 +728,66 @@ "sl7": 0.0 }, "id": { - "component": "Ferralic cambisols", - "name": "Ferralic cambisols", - "rank_loc": "12", - "score_loc": 0.016 + "component": "Dystric fluvisols", + "name": "Dystric fluvisols", + "rank_loc": "8", + "score_loc": 0.014 }, "ph": { - "sl1": 5.6, - "sl2": 5.6, - "sl3": 5.6, - "sl4": 5.62, - "sl5": 5.63, - "sl6": 5.64, - "sl7": 5.65 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 }, "rock_fragments": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 17.0, - "sl5": 12.71, - "sl6": 10.0, - "sl7": 8.83 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 }, "sand": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 32.2, - "sl5": 31.29, - "sl6": 30.4, - "sl7": 29.83 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 }, "site": { "siteData": { - "componentID": 105461, - "distance": 82783.427, - "mapunitID": 12225, - "minCompDistance": 82783.4266, - "share": 35, + "componentID": 104796, + "distance": 26247.791, + "mapunitID": 12045, + "minCompDistance": 26247.7907, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", - "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " + "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -1137,93 +801,93 @@ "sl7": 120 }, "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.6, + "sl5": 14.71, + "sl6": 15.0, + "sl7": 15.17 + }, + "clay": { "sl1": 24.0, "sl2": 24.0, "sl3": 24.0, - "sl4": 23.0, - "sl5": 22.29, - "sl6": 21.8, - "sl7": 21.5 - }, - "clay": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0, - "sl4": 40.2, - "sl5": 41.57, - "sl6": 42.0, - "sl7": 41.5 + "sl4": 28.6, + "sl5": 29.86, + "sl6": 30.6, + "sl7": 30.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Haplic alisols", - "name": "Haplic alisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.029 + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "9", + "score_loc": 0.014 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.26, - "sl5": 6.29, - "sl6": 6.32, - "sl7": 6.32 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.44, + "sl6": 6.44, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 8.4, - "sl5": 8.43, - "sl6": 8.6, - "sl7": 12.33 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 9.29, + "sl6": 13.4, + "sl7": 12.5 }, "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 34.4, - "sl5": 33.71, - "sl6": 33.8, - "sl7": 34.67 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 49.0, + "sl5": 47.71, + "sl6": 46.6, + "sl7": 46.67 }, "site": { "siteData": { - "componentID": 104944, - "distance": 88902.515, - "mapunitID": 12084, - "minCompDistance": 66876.8882, - "share": 65, + "componentID": 104795, + "distance": 26247.791, + "mapunitID": 12045, + "minCompDistance": 26247.7907, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", - "Description_es": "Los Alisoles Háplicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua. ", - "Description_fr": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", - "Description_ks": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", - "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", - "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
Debido a su poca profundidad, estos suelos no son adecuados para el cultivo, por lo que debe considerarse su uso para el pastoreo.
La preservación de la superficie del suelo con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua. ", - "Management_fr": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", - "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. " + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -1237,22 +901,22 @@ "sl7": 120 }, "cec": { + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.4, + "sl5": 10.43, + "sl6": 10.4, + "sl7": 10.5 + }, + "clay": { "sl1": 19.0, "sl2": 19.0, "sl3": 19.0, - "sl4": 21.4, - "sl5": 22.43, - "sl6": 23.0, - "sl7": 22.83 - }, - "clay": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 31.2, - "sl5": 33.71, - "sl6": 35.2, - "sl7": 35.33 + "sl4": 23.2, + "sl5": 24.57, + "sl6": 25.6, + "sl7": 25.83 }, "ec": { "sl1": 0.0, @@ -1264,66 +928,66 @@ "sl7": 0.0 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.027 + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "10", + "score_loc": 0.009 }, "ph": { - "sl1": 6.1, - "sl2": 6.1, - "sl3": 6.1, - "sl4": 6.26, - "sl5": 6.37, - "sl6": 6.52, - "sl7": 6.62 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.24, + "sl5": 5.21, + "sl6": 5.18, + "sl7": 5.17 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 5.8, - "sl5": 6.71, - "sl6": 7.6, - "sl7": 9.83 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.4, + "sl5": 12.14, + "sl6": 13.4, + "sl7": 14.0 }, "sand": { - "sl1": 33.0, - "sl2": 33.0, - "sl3": 33.0, - "sl4": 30.0, - "sl5": 28.86, - "sl6": 28.0, - "sl7": 28.0 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 37.4, + "sl5": 36.86, + "sl6": 36.8, + "sl7": 37.33 }, "site": { "siteData": { - "componentID": 104894, - "distance": 68854.944, - "mapunitID": 12071, - "minCompDistance": 58618.178, - "share": 10, + "componentID": 104896, + "distance": 93153.994, + "mapunitID": 12072, + "minCompDistance": 93153.994, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { "sl1": "Loam", "sl2": "Loam", "sl3": "Loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -1337,22 +1001,22 @@ "sl7": 120 }, "cec": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 3.6, - "sl5": 3.14, - "sl6": 2.8, - "sl7": 2.67 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.4, + "sl5": 14.0, + "sl6": 14.6, + "sl7": 14.67 }, "clay": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0, - "sl5": 5.14, - "sl6": 5.2, - "sl7": 5.33 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.2, + "sl5": 30.71, + "sl6": 33.0, + "sl7": 33.83 }, "ec": { "sl1": 0.0, @@ -1364,66 +1028,66 @@ "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.023 + "component": "Haplic arenosols", + "name": "Haplic arenosols", + "rank_loc": "11", + "score_loc": 0.007 }, "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 5.8, - "sl5": 5.8, - "sl6": 5.8, - "sl7": 5.82 - }, - "rock_fragments": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 10.4, - "sl5": 11.0, - "sl6": 10.0, - "sl7": 8.83 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.24, + "sl5": 5.23, + "sl6": 5.22, + "sl7": 5.15 + }, + "rock_fragments": { + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.4, + "sl5": 3.86, + "sl6": 4.6, + "sl7": 5.5 }, "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 87.2, - "sl5": 87.29, - "sl6": 87.4, - "sl7": 86.83 + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 48.6, + "sl5": 46.43, + "sl6": 44.2, + "sl7": 42.5 }, "site": { "siteData": { - "componentID": 104895, - "distance": 93153.994, - "mapunitID": 12072, - "minCompDistance": 61918.6954, - "share": 50, - "soilDepth": 20 + "componentID": 105094, + "distance": 46698.183, + "mapunitID": 12127, + "minCompDistance": 46698.1828, + "share": 15, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_es": "Los Arenosoles Háplicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.", + "Description_fr": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_ks": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1437,93 +1101,93 @@ "sl7": 120 }, "cec": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 19.6, - "sl5": 17.14, - "sl6": 14.6, - "sl7": 13.5 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.4, + "sl5": 3.29, + "sl6": 3.2, + "sl7": 3.0 }, "clay": { - "sl1": 27.0, - "sl2": 27.0, - "sl3": 27.0, - "sl4": 26.4, - "sl5": 26.29, - "sl6": 26.2, - "sl7": 25.5 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.2, + "sl7": 4.33 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.4, - "sl7": 0.33 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Haplic ferralsols", - "name": "Haplic ferralsols2", - "rank_loc": "Not Displayed", - "score_loc": 0.02 + "component": "Fibric histosols", + "name": "Fibric histosols", + "rank_loc": "12", + "score_loc": 0.005 }, "ph": { - "sl1": 4.7, - "sl2": 4.7, - "sl3": 4.7, - "sl4": 4.86, - "sl5": 4.94, - "sl6": 5.02, - "sl7": 5.07 + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.84, + "sl5": 5.87, + "sl6": 5.88, + "sl7": 5.88 }, "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 11.8, - "sl5": 11.86, - "sl6": 13.6, - "sl7": 14.67 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 12.8, + "sl5": 13.43, + "sl6": 13.4, + "sl7": 13.0 }, "sand": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 42.0, - "sl5": 43.43, - "sl6": 45.0, - "sl7": 47.17 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 87.6, + "sl5": 87.57, + "sl6": 87.4, + "sl7": 87.33 }, "site": { "siteData": { - "componentID": 104892, - "distance": 68854.944, - "mapunitID": 12071, - "minCompDistance": 58618.178, - "share": 30, + "componentID": 104797, + "distance": 26247.791, + "mapunitID": 12045, + "minCompDistance": 26247.7907, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_es": "Los Ferralsoles Háplicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada de retener nutrientes. ", - "Description_fr": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Description_ks": "Haplic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.", - "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "Estos suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Fibric Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges.
Fibric Histosols have relatively undecomposed organic soil materials.
Thus, they have a slightly lower bulk density and higher water content. ", + "Description_es": "Los Histosoles Fíbricos son suelos orgánicos que se forman típicamente en ambientes húmedos.
Sus propiedades dependen en gran medida del tipo y el grado de descomposición de los materiales orgánicos del suelo.
Los suelos pueden ser productivos con una gestión intensiva que incluya el drenaje del suelo, pero su naturaleza frágil y su hábitat sugieren que se garantice la preservación de estos suelos cuando sea posible.
Cuando se cultivan, el hundimiento y la oxidación de los sulfuros plantean problemas de gestión.
Los Histosoles Fíbricos tienen materiales orgánicos relativamente poco descompuestos.
Por lo tanto, tienen una densidad aparente ligeramente inferior y un mayor contenido de agua. ", + "Description_fr": "Fibric Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges.
Fibric Histosols have relatively undecomposed organic soil materials.
Thus, they have a slightly lower bulk density and higher water content. ", + "Description_ks": "Fibric Histosols are organic soils that typically form in wet environments.
Their properties are largely dependent on the type and degree of decomposition of the organic soil materials.
The soils can be productive with intensive management including soil drainage but their fragile nature and habitat suggests preservation of these soils is warranted where possible.
When cultivated, subsidence and sulfide oxidation present management challenges.
Fibric Histosols have relatively undecomposed organic soil materials.
Thus, they have a slightly lower bulk density and higher water content. ", + "Management_en": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regularliming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority. ", + "Management_es": "Estos suelos pueden ser algunos de los más productivos, especialmente para cultivos especiales como las hortalizas.
Sin embargo, deben ser drenados para su uso, y esto conducirá al hundimiento del suelo, ya que la turba expuesta se mineraliza rápidamente, y el contenido de materia orgánica disminuye rápidamente.
Esto hará que los suelos se vuelvan cada vez más ácidos, por lo que será necesario un tratamiento regular.
Estos suelos orgánicos deben gestionarse de forma diferente a los suelos minerales, y las técnicas que minimizan la degradación de la materia orgánica son una prioridad.", + "Management_fr": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regularliming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority. ", + "Management_ks": "These soils can be some of our most productive soils, especially for specialty crops such as vegetables.
However, they must be drained for use, and this will lead to subsidence of the soil, as exposed peat is rapidly mineralized, and organic matter content quickly drops.
This will lead to increasingly acid soils, and thus regularliming will be needed.
These organic soils must be managed differently from mineral soils, and techniques that minimize organic matter degradation are a priority. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Sandy clay loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" } }, { @@ -1564,10 +1228,10 @@ "sl7": 0.0 }, "id": { - "component": "Rhodic ferralsols", - "name": "Rhodic ferralsols2", + "component": "Haplic alisols", + "name": "Haplic alisols2", "rank_loc": "Not Displayed", - "score_loc": 0.02 + "score_loc": 0.029 }, "ph": { "sl1": 5.2, @@ -1598,22 +1262,22 @@ }, "site": { "siteData": { - "componentID": 104891, - "distance": 68854.944, - "mapunitID": 12071, - "minCompDistance": 58618.178, - "share": 40, + "componentID": 104944, + "distance": 88902.515, + "mapunitID": 12084, + "minCompDistance": 66876.8882, + "share": 65, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_es": "Los Ferralsoles Ródicos son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes.
Los ferraliscos ródicos tienen subsuelos de color rojo oscuro con una buena estructura de suelo. ", - "Description_fr": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Description_ks": "Rhodic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Rhodic Ferralsols have dark red subsoils with good soil structure. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_es": "Los Alisoles Háplicos son suelos ácidos que suelen encontrarse en zonas de colinas, por lo que son propensos a la erosión.
También tienen altos niveles de aluminio soluble, que es tóxico para las plantas.
Son suelos poco profundos y, por lo general, poco productivos para el cultivo, por lo que su uso debe limitarse al pastoreo de bajo volumen o a otros usos con cobertura vegetal continua. ", + "Description_fr": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Description_ks": "Haplic Alisols are acidic soils that are often found on hilly areas, and are thus prone to erosion.
They also have high levels of soluble aluminum, which is toxic to plants.
They are shallow soils and usually unproductive for cropping, and so their use should be limited to low volume grazing or other uses with continuous plant cover. ", + "Management_en": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_es": "La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el Al de la solución, puede ayudar a reducir la toxicidad del aluminio.
Debido a su poca profundidad, estos suelos no son adecuados para el cultivo, por lo que debe considerarse su uso para el pastoreo.
La preservación de la superficie del suelo con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. *Aunque no suele recomendarse, si el suelo se utiliza para cultivos, la fertilización debe combinarse con la rotación de cultivos y/o los cultivos de cobertura, u otros medios de adición de materia orgánica para el desarrollo de una mayor fertilidad y capacidad de retención de agua. ", + "Management_fr": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. ", + "Management_ks": "Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which takes Al out of solution, can help to reduce aluminum toxicity.
Because they are shallow these soils are not well suited for cultivation for crops, and so use for grazing should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Although not usually recommended, if the soil is used for cultivated cropping then fertilization should be combined with crop rotations andcover crops, or other means of organic matter addition for the development of improved fertility and water holding capacity. " } }, "texture": { @@ -1664,10 +1328,10 @@ "sl7": 0.17 }, "id": { - "component": "Luvic phaeozems", - "name": "Luvic phaeozems2", + "component": "Ferralic arenosols", + "name": "Ferralic arenosols2", "rank_loc": "Not Displayed", - "score_loc": 0.02 + "score_loc": 0.027 }, "ph": { "sl1": 5.2, @@ -1698,22 +1362,22 @@ }, "site": { "siteData": { - "componentID": 105449, - "distance": 91158.288, - "mapunitID": 12222, - "minCompDistance": 88902.5153, - "share": 45, + "componentID": 104894, + "distance": 68854.944, + "mapunitID": 12071, + "minCompDistance": 58618.178, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_es": "Los Phaeozemss Lúvicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems lúvicos tienen un contenido de arcilla relativamente alto en el subsuelo.", - "Description_fr": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Description_ks": "Luvic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Luvic Phaeozems have relatively higher clay content in subsoils.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
El mayor contenido de arcilla en este suelo puede ayudar a retener el agua para la producción de cultivos.", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. ", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
The increased clay content in this soil may assist with water holding for crop production. " + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { @@ -1739,7 +1403,7 @@ "componentData": "Data Complete", "componentID": 104943, "name": "Haplic alisols1", - "rank_data": "2", + "rank_data": "4", "rank_data_loc": "1", "rank_loc": "2", "score_data": 1.0, @@ -1749,50 +1413,38 @@ { "component": "Ferralic arenosols", "componentData": "Data Complete", - "componentID": 104894, - "name": "Ferralic arenosols2", - "rank_data": "1", + "componentID": 104786, + "name": "Ferralic arenosols1", + "rank_data": "2", "rank_data_loc": "2", - "rank_loc": "Not Displayed", + "rank_loc": "3", "score_data": 1.0, "score_data_loc": 0.998, "score_loc": 0.027 }, { - "component": "Haplic ferralsols", - "componentData": "Missing Data", - "componentID": 104785, - "name": "Haplic ferralsols1", + "component": "Fibric histosols", + "componentData": "Data Complete", + "componentID": 104797, + "name": "Fibric histosols", "rank_data": "3", "rank_data_loc": "3", - "rank_loc": "6", - "score_data": 1.0, - "score_data_loc": 0.991, - "score_loc": 0.02 - }, - { - "component": "Luvic phaeozems", - "componentData": "Missing Data", - "componentID": 104946, - "name": "Luvic phaeozems1", - "rank_data": "4", - "rank_data_loc": "4", - "rank_loc": "8", + "rank_loc": "12", "score_data": 1.0, - "score_data_loc": 0.991, - "score_loc": 0.02 + "score_data_loc": 0.976, + "score_loc": 0.005 }, { - "component": "Rhodic ferralsols", - "componentData": "No Data", - "componentID": 104784, - "name": "Rhodic ferralsols1", + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 104795, + "name": "Eutric fluvisols", "rank_data": "5", - "rank_data_loc": "5", - "rank_loc": "7", - "score_data": 1.0, - "score_data_loc": 0.991, - "score_loc": 0.02 + "rank_data_loc": "4", + "rank_loc": "9", + "score_data": 0.845, + "score_data_loc": 0.834, + "score_loc": 0.014 }, { "component": "Gleyic alisols", @@ -1800,108 +1452,96 @@ "componentID": 104790, "name": "Gleyic alisols", "rank_data": "9", - "rank_data_loc": "6", + "rank_data_loc": "5", "rank_loc": "1", - "score_data": 0.845, - "score_data_loc": 0.945, + "score_data": 0.629, + "score_data_loc": 0.735, "score_loc": 0.127 }, { - "component": "Umbric gleysols", + "component": "Haplic arenosols", "componentData": "Data Complete", - "componentID": 104792, - "name": "Umbric gleysols", - "rank_data": "8", - "rank_data_loc": "7", - "rank_loc": "10", - "score_data": 0.905, - "score_data_loc": 0.896, - "score_loc": 0.018 + "componentID": 105094, + "name": "Haplic arenosols", + "rank_data": "6", + "rank_data_loc": "6", + "rank_loc": "11", + "score_data": 0.698, + "score_data_loc": 0.685, + "score_loc": 0.007 }, { "component": "Ferralic cambisols", "componentData": "Data Complete", "componentID": 105461, "name": "Ferralic cambisols", - "rank_data": "6", - "rank_data_loc": "8", - "rank_loc": "12", - "score_data": 0.905, - "score_data_loc": 0.894, + "rank_data": "8", + "rank_data_loc": "7", + "rank_loc": "7", + "score_data": 0.673, + "score_data_loc": 0.669, "score_loc": 0.016 }, + { + "component": "Dystric fluvisols", + "componentData": "Data Complete", + "componentID": 104796, + "name": "Dystric fluvisols", + "rank_data": "7", + "rank_data_loc": "8", + "rank_loc": "8", + "score_data": 0.673, + "score_data_loc": 0.667, + "score_loc": 0.014 + }, { "component": "Haplic acrisols", "componentData": "Data Complete", "componentID": 105457, "name": "Haplic acrisols", - "rank_data": "7", + "rank_data": "11", "rank_data_loc": "9", - "rank_loc": "11", - "score_data": 0.905, - "score_data_loc": 0.894, + "rank_loc": "6", + "score_data": 0.516, + "score_data_loc": 0.517, "score_loc": 0.016 }, { - "component": "Gleyic arenosols", + "component": "Chromic luvisols", "componentData": "Data Complete", - "componentID": 104793, - "name": "Gleyic arenosols", + "componentID": 104896, + "name": "Chromic luvisols", "rank_data": "10", "rank_data_loc": "10", - "rank_loc": "9", - "score_data": 0.673, - "score_data_loc": 0.672, - "score_loc": 0.018 + "rank_loc": "10", + "score_data": 0.516, + "score_data_loc": 0.51, + "score_loc": 0.009 }, { - "component": "Eutric leptosols", - "componentData": "Missing Data", - "componentID": 104791, - "name": "Eutric leptosols", + "component": "Gleyic arenosols", + "componentData": "Data Complete", + "componentID": 104793, + "name": "Gleyic arenosols", "rank_data": "12", "rank_data_loc": "11", - "rank_loc": "4", + "rank_loc": "5", "score_data": 0.383, - "score_data_loc": 0.002, - "score_loc": 0.023 + "score_data_loc": 0.389, + "score_loc": 0.018 }, { - "component": "Lithic leptosols", + "component": "Eutric leptosols", "componentData": "Missing Data", - "componentID": 105466, - "name": "Lithic leptosols1", - "rank_data": "11", + "componentID": 104791, + "name": "Eutric leptosols", + "rank_data": "1", "rank_data_loc": "12", - "rank_loc": "5", - "score_data": 0.516, + "rank_loc": "4", + "score_data": 1.0, "score_data_loc": 0.002, "score_loc": 0.023 }, - { - "component": "Haplic ferralsols", - "componentData": "No Data", - "componentID": 104892, - "name": "Haplic ferralsols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 1.0, - "score_data_loc": 0.991, - "score_loc": 0.02 - }, - { - "component": "Rhodic ferralsols", - "componentData": "No Data", - "componentID": 104891, - "name": "Rhodic ferralsols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.698, - "score_data_loc": 0.698, - "score_loc": 0.02 - }, { "component": "Haplic alisols", "componentData": "Data Complete", @@ -1910,45 +1550,21 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.673, - "score_data_loc": 0.683, + "score_data": 0.629, + "score_data_loc": 0.64, "score_loc": 0.029 }, - { - "component": "Luvic phaeozems", - "componentData": "Missing Data", - "componentID": 105449, - "name": "Luvic phaeozems2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.673, - "score_data_loc": 0.674, - "score_loc": 0.02 - }, { "component": "Ferralic arenosols", "componentData": "Data Complete", - "componentID": 104786, - "name": "Ferralic arenosols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "3", - "score_data": 0.629, - "score_data_loc": 0.638, - "score_loc": 0.027 - }, - { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 104895, - "name": "Lithic leptosols2", + "componentID": 104894, + "name": "Ferralic arenosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", "score_data": 0.516, - "score_data_loc": 0.002, - "score_loc": 0.023 + "score_data_loc": 0.528, + "score_loc": 0.027 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json index bf01167..4c70ad9 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-19.13333,145.5125].json @@ -25,91 +25,91 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 16.0, - "sl5": 16.71, - "sl6": 17.4, + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.2, + "sl5": 18.43, + "sl6": 18.4, "sl7": 17.83 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 25.2, - "sl5": 26.57, - "sl6": 27.8, - "sl7": 28.0 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 34.2, + "sl5": 35.86, + "sl6": 37.2, + "sl7": 37.5 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz1", + "component": "Eutric planosols", + "name": "Eutric planosols1", "rank_loc": "1", - "score_loc": 0.05 + "score_loc": 0.038 }, "ph": { - "sl1": 7.1, - "sl2": 7.1, - "sl3": 7.1, - "sl4": 7.56, - "sl5": 7.74, - "sl6": 7.94, - "sl7": 8.0 + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.56, + "sl5": 6.57, + "sl6": 6.58, + "sl7": 6.55 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.8, - "sl5": 6.14, - "sl6": 8.8, - "sl7": 10.67 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.6, + "sl5": 10.14, + "sl6": 9.8, + "sl7": 11.33 }, "sand": { - "sl1": 50.0, - "sl2": 50.0, - "sl3": 50.0, - "sl4": 43.8, - "sl5": 42.43, - "sl6": 41.0, - "sl7": 40.33 + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.43, + "sl6": 32.6, + "sl7": 33.0 }, "site": { "siteData": { - "componentID": 148584, + "componentID": 148582, "distance": 7539.61, "mapunitID": 5933, "minCompDistance": 7539.6102, - "share": 10, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", - "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", - "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", "sl6": "Clay loam", "sl7": "Clay loam" } @@ -125,93 +125,93 @@ "sl7": 120 }, "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 19.2, - "sl5": 19.29, - "sl6": 19.0, - "sl7": 18.67 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.6, + "sl5": 14.71, + "sl6": 15.0, + "sl7": 15.17 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 26.0, - "sl5": 26.29, - "sl6": 25.6, - "sl7": 24.67 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.6, + "sl5": 29.86, + "sl6": 30.6, + "sl7": 30.5 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Eutric planosols", - "name": "Eutric planosols1", + "component": "Cambic arenosols", + "name": "Cambic arenosols", "rank_loc": "2", - "score_loc": 0.038 + "score_loc": 0.032 }, "ph": { - "sl1": 8.3, - "sl2": 8.3, - "sl3": 8.3, - "sl4": 8.56, - "sl5": 8.63, - "sl6": 8.66, - "sl7": 8.65 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.44, + "sl6": 6.44, + "sl7": 6.43 }, "rock_fragments": { "sl1": 6.0, "sl2": 6.0, "sl3": 6.0, - "sl4": 5.0, - "sl5": 5.29, - "sl6": 7.4, - "sl7": 9.0 + "sl4": 6.8, + "sl5": 9.29, + "sl6": 13.4, + "sl7": 12.5 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 44.6, - "sl5": 44.57, - "sl6": 45.4, - "sl7": 46.17 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 49.0, + "sl5": 47.71, + "sl6": 46.6, + "sl7": 46.67 }, "site": { "siteData": { - "componentID": 148582, - "distance": 7539.61, - "mapunitID": 5933, - "minCompDistance": 7539.6102, - "share": 20, + "componentID": 148403, + "distance": 29716.363, + "mapunitID": 5876, + "minCompDistance": 29716.3626, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", - "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -225,68 +225,68 @@ "sl7": 120 }, "cec": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 15.0, - "sl5": 16.14, - "sl6": 17.2, - "sl7": 17.33 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 16.0, + "sl5": 16.0, + "sl6": 16.0, + "sl7": 15.83 }, "clay": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 21.6, - "sl5": 23.57, - "sl6": 25.2, - "sl7": 25.17 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 22.2, + "sl5": 23.0, + "sl6": 23.6, + "sl7": 23.67 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Cambic arenosols", - "name": "Cambic arenosols", + "component": "Chromic luvisols", + "name": "Chromic luvisols1", "rank_loc": "3", - "score_loc": 0.032 + "score_loc": 0.022 }, "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.86, - "sl5": 7.09, - "sl6": 7.36, - "sl7": 7.47 + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4, + "sl4": 7.56, + "sl5": 7.64, + "sl6": 7.74, + "sl7": 7.82 }, "rock_fragments": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0, - "sl5": 5.29, - "sl6": 7.2, - "sl7": 9.0 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 19.0, + "sl5": 21.0, + "sl6": 22.6, + "sl7": 22.83 }, "sand": { - "sl1": 63.0, - "sl2": 63.0, - "sl3": 63.0, - "sl4": 60.0, - "sl5": 58.14, - "sl6": 56.4, - "sl7": 56.17 + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 55.0, + "sl5": 54.57, + "sl6": 54.2, + "sl7": 54.17 }, "site": { "siteData": { - "componentID": 148403, + "componentID": 148401, "distance": 29716.363, "mapunitID": 5876, "minCompDistance": 29716.3626, @@ -294,14 +294,14 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", - "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { @@ -325,93 +325,93 @@ "sl7": 120 }, "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 19.2, - "sl5": 19.29, - "sl6": 19.0, - "sl7": 18.67 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.8, + "sl5": 3.57, + "sl6": 3.8, + "sl7": 3.5 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 26.0, - "sl5": 26.29, - "sl6": 25.6, - "sl7": 24.67 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.0, + "sl5": 7.14, + "sl6": 7.6, + "sl7": 7.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols1", + "component": "Dystric regosols", + "name": "Dystric regosols1", "rank_loc": "4", - "score_loc": 0.032 + "score_loc": 0.021 }, "ph": { - "sl1": 8.3, - "sl2": 8.3, - "sl3": 8.3, - "sl4": 8.56, - "sl5": 8.63, - "sl6": 8.66, - "sl7": 8.65 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.46, + "sl6": 6.54, + "sl7": 6.55 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 5.0, - "sl5": 5.29, - "sl6": 7.4, - "sl7": 9.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.4, + "sl5": 2.86, + "sl6": 2.8, + "sl7": 5.33 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 44.6, - "sl5": 44.57, - "sl6": 45.4, - "sl7": 46.17 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.29, + "sl6": 85.2, + "sl7": 86.0 }, "site": { "siteData": { - "componentID": 148388, - "distance": 50714.61, - "mapunitID": 5874, - "minCompDistance": 50714.6101, + "componentID": 148956, + "distance": 438.366, + "mapunitID": 6037, + "minCompDistance": 438.3662, "share": 20, - "soilDepth": 20 + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", + "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -425,22 +425,22 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 13.6, - "sl5": 15.0, - "sl6": 16.4, - "sl7": 16.83 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 24.4, - "sl5": 26.86, - "sl6": 29.2, - "sl7": 30.0 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 }, "ec": { "sl1": 1.0, @@ -452,66 +452,66 @@ "sl7": 1.0 }, "id": { - "component": "Vertisols", - "name": "Vertisols1", + "component": "Albic arenosols", + "name": "Albic arenosols1", "rank_loc": "5", - "score_loc": 0.032 + "score_loc": 0.021 }, "ph": { - "sl1": 6.1, - "sl2": 6.1, - "sl3": 6.1, - "sl4": 6.26, - "sl5": 6.37, - "sl6": 6.52, - "sl7": 6.57 + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.6, - "sl5": 2.57, - "sl6": 2.4, - "sl7": 2.33 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 46.0, - "sl5": 44.14, - "sl6": 42.2, - "sl7": 42.0 + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 }, "site": { "siteData": { - "componentID": 148452, - "distance": 74511.638, - "mapunitID": 5890, - "minCompDistance": 74511.6383, - "share": 30, + "componentID": 148894, + "distance": 32877.453, + "mapunitID": 6017, + "minCompDistance": 32877.4526, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", - "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.", + "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -525,68 +525,68 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 10.6, - "sl5": 12.29, - "sl6": 14.2, - "sl7": 15.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 8.8, + "sl5": 10.0, + "sl6": 10.8, + "sl7": 11.33 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 23.2, - "sl5": 27.0, - "sl6": 30.8, - "sl7": 32.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 18.4, + "sl5": 20.86, + "sl6": 22.2, + "sl7": 22.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.83 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.2, + "sl7": 1.33 }, "id": { - "component": "Chromic luvisols", - "name": "Chromic luvisols1", + "component": "Calcic luvisols", + "name": "Calcic luvisols1", "rank_loc": "6", - "score_loc": 0.022 + "score_loc": 0.013 }, "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 5.98, - "sl5": 6.11, - "sl6": 6.28, - "sl7": 6.42 - }, - "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 9.0, - "sl5": 10.14, - "sl6": 11.0, - "sl7": 11.5 + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.36, + "sl5": 6.46, + "sl6": 6.64, + "sl7": 6.73 + }, + "rock_fragments": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 13.6, + "sl5": 11.29, + "sl6": 9.6, + "sl7": 8.83 }, "sand": { - "sl1": 58.0, - "sl2": 58.0, - "sl3": 58.0, - "sl4": 52.8, - "sl5": 49.57, - "sl6": 46.0, - "sl7": 44.33 + "sl1": 80.0, + "sl2": 80.0, + "sl3": 80.0, + "sl4": 72.0, + "sl5": 70.0, + "sl6": 69.0, + "sl7": 68.0 }, "site": { "siteData": { - "componentID": 148401, + "componentID": 148402, "distance": 29716.363, "mapunitID": 5876, "minCompDistance": 29716.3626, @@ -594,24 +594,24 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", - "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Sandy loam", "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", - "sl7": "Clay loam" + "sl7": "Sandy clay loam" } }, { @@ -625,93 +625,93 @@ "sl7": 120 }, "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 8.8, - "sl5": 10.0, - "sl6": 10.8, - "sl7": 11.33 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.0, + "sl5": 11.29, + "sl6": 12.4, + "sl7": 12.33 }, "clay": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 18.4, - "sl5": 20.86, - "sl6": 22.2, - "sl7": 22.83 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 21.8, + "sl5": 26.86, + "sl6": 31.2, + "sl7": 32.33 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.2, - "sl7": 1.33 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Dystric regosols", - "name": "Dystric regosols1", + "component": "Acrisols", + "name": "Acrisols1", "rank_loc": "7", - "score_loc": 0.021 + "score_loc": 0.011 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.36, - "sl5": 6.46, - "sl6": 6.64, - "sl7": 6.73 + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.92, + "sl5": 4.94, + "sl6": 5.0, + "sl7": 5.07 }, "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 13.6, - "sl5": 11.29, - "sl6": 9.6, - "sl7": 8.83 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 7.6, + "sl5": 7.14, + "sl6": 7.4, + "sl7": 10.33 }, "sand": { - "sl1": 80.0, - "sl2": 80.0, - "sl3": 80.0, - "sl4": 72.0, - "sl5": 70.0, - "sl6": 69.0, - "sl7": 68.0 + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 50.2, + "sl5": 46.71, + "sl6": 44.0, + "sl7": 43.67 }, "site": { "siteData": { - "componentID": 148956, - "distance": 438.366, - "mapunitID": 6037, - "minCompDistance": 438.3662, + "componentID": 148895, + "distance": 32877.453, + "mapunitID": 6017, + "minCompDistance": 32877.4526, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", - "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", - "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", - "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", - "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " + "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Sandy loam", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Loam", "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -752,10 +752,10 @@ "sl7": 1.0 }, "id": { - "component": "Albic arenosols", - "name": "Albic arenosols1", + "component": "Ferralsols", + "name": "Ferralsols1", "rank_loc": "8", - "score_loc": 0.021 + "score_loc": 0.011 }, "ph": { "sl1": 6.1, @@ -786,22 +786,22 @@ }, "site": { "siteData": { - "componentID": 148894, + "componentID": 148898, "distance": 32877.453, "mapunitID": 6017, "minCompDistance": 32877.4526, - "share": 20, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", - "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.", - "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", - "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", - "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. " + "Description_en": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Description_es": "Los Ferralisoles son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad, como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes. ", + "Description_fr": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Description_ks": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por parte de los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." } }, "texture": { @@ -825,22 +825,22 @@ "sl7": 120 }, "cec": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 3.8, - "sl5": 3.57, - "sl6": 3.8, - "sl7": 3.5 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 13.2, + "sl5": 14.71, + "sl6": 15.8, + "sl7": 15.67 }, "clay": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 7.0, - "sl5": 7.14, - "sl6": 7.6, - "sl7": 7.17 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 25.6, + "sl5": 31.86, + "sl6": 36.2, + "sl7": 36.33 }, "ec": { "sl1": 0.0, @@ -852,370 +852,166 @@ "sl7": 0.0 }, "id": { - "component": "Haplic luvisols", - "name": "Haplic luvisols1", + "component": "Dystric planosols", + "name": "Dystric planosols1", "rank_loc": "9", - "score_loc": 0.016 + "score_loc": 0.009 }, "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.42, - "sl5": 6.46, - "sl6": 6.54, - "sl7": 6.55 + "sl1": 4.7, + "sl2": 4.7, + "sl3": 4.7, + "sl4": 4.78, + "sl5": 4.76, + "sl6": 4.74, + "sl7": 4.87 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.4, - "sl5": 2.86, - "sl6": 2.8, - "sl7": 5.33 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 13.2, + "sl5": 11.14, + "sl6": 10.2, + "sl7": 12.67 }, "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 86.8, - "sl5": 86.29, - "sl6": 85.2, - "sl7": 86.0 + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 43.0, + "sl5": 38.14, + "sl6": 35.2, + "sl7": 36.33 }, "site": { "siteData": { - "componentID": 148583, + "componentID": 148585, "distance": 7539.61, "mapunitID": 5933, "minCompDistance": 7539.6102, - "share": 20, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", - "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.", + "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed." } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20 + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { "sl1": 16.0, "sl2": 16.0, - "sl3": 16.0 + "sl3": 16.0, + "sl4": 14.8, + "sl5": 14.57, + "sl6": 14.2, + "sl7": 14.0 }, "clay": { "sl1": 20.0, "sl2": 20.0, - "sl3": 20.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Calcic luvisols", - "name": "Calcic luvisols1", - "rank_loc": "10", - "score_loc": 0.013 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 - }, - "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0 - }, - "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 - }, - "site": { - "siteData": { - "componentID": 148402, - "distance": 29716.363, - "mapunitID": 5876, - "minCompDistance": 29716.3626, - "share": 10, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", - "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 39.6, - "sl5": 39.57, - "sl6": 39.4, - "sl7": 39.17 - }, - "clay": { - "sl1": 54.0, - "sl2": 54.0, - "sl3": 54.0, - "sl4": 55.2, - "sl5": 55.43, - "sl6": 55.4, - "sl7": 55.17 + "sl3": 20.0, + "sl4": 20.6, + "sl5": 20.86, + "sl6": 21.0, + "sl7": 20.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 1.0, - "sl6": 1.4, - "sl7": 1.5 - }, - "id": { - "component": "Rhodic nitisols", - "name": "Rhodic nitisols", - "rank_loc": "11", - "score_loc": 0.013 - }, - "ph": { - "sl1": 7.5, - "sl2": 7.5, - "sl3": 7.5, - "sl4": 7.64, - "sl5": 7.7, - "sl6": 7.76, - "sl7": 7.8 - }, - "rock_fragments": { "sl1": 2.0, "sl2": 2.0, "sl3": 2.0, - "sl4": 2.2, - "sl5": 2.57, - "sl6": 3.0, - "sl7": 3.33 - }, - "sand": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 18.8, - "sl5": 18.57, - "sl6": 18.6, - "sl7": 18.5 - }, - "site": { - "siteData": { - "componentID": 148454, - "distance": 74511.638, - "mapunitID": 5890, - "minCompDistance": 74511.6383, - "share": 20, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", - "Description_es": "Los Nitisoles Ródicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes. *Los Nitisoles Ródicos tienen subsuelos de color rojo oscuro con alta sorción de P.", - "Description_fr": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", - "Description_ks": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", - "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", - "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la absorción de las plantas durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
Es especialmente importante que la fertilización con P se utilice en estos suelos, que se destacan específicamente por tener una alta sorción de P.", - "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", - "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. " - } - }, - "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0 - }, - "clay": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Haplic podzols", - "name": "Haplic podzols1", - "rank_loc": "12", - "score_loc": 0.011 - }, - "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4 - }, - "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0 - }, - "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0 - }, - "site": { - "siteData": { - "componentID": 148915, - "distance": 3068.563, - "mapunitID": 6024, - "minCompDistance": 3068.5627, - "share": 20, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", - "Description_es": "Los Podzoles Háplicos son suelos de textura gruesa, ácidos e improductivos, con horizontes superficiales muy lixiviados sobre los que se asientan subsuelos que contienen materia orgánica acumulada y metales (aluminio y hierro).*En los paisajes de llanura costera plana, estos suelos también son húmedos.", - "Description_fr": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", - "Description_ks": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", - "Management_en": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", - "Management_es": "Los podzoles están muy lixiviados y, como tales, tienen una baja fertilidad.
Las capas superficiales suelen ser bastante ácidas (pH < 4,5), por lo que es necesario el encalado.
Debido al alto grado de meteorización, los suelos también tienen un alto contenido de aluminio soluble y fijan el fósforo, creando deficiencias de P. Aunque no se recomienda, si estos suelos se utilizan para el cultivo necesitarán un arado profundo (para romper las capas del subsuelo), encalado y fertilización.
Será necesario un cuidado específico con la fertilización de P, y se recomienda el uso de banda en la colocación de P en la semilla.", - "Management_fr": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", - "Management_ks": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended." - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 + "sl4": 0.8, + "sl5": 0.71, + "sl6": 0.8, + "sl7": 0.83 }, "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz2", - "rank_loc": "Not Displayed", - "score_loc": 0.05 + "component": "Calcaric regosols", + "name": "Calcaric regosols", + "rank_loc": "10", + "score_loc": 0.006 }, "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.54, + "sl5": 6.6, + "sl6": 6.66, + "sl7": 6.7 }, "rock_fragments": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 15.0, + "sl5": 16.57, + "sl6": 18.8, + "sl7": 19.17 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.8, + "sl5": 41.14, + "sl6": 41.8, + "sl7": 42.17 }, "site": { "siteData": { - "componentID": 149438, + "componentID": 149436, "distance": 50505.675, "mapunitID": 6189, - "minCompDistance": 7539.6102, - "share": 10, + "minCompDistance": 50505.675, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", - "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", - "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { "sl1": "Loam", "sl2": "Loam", - "sl3": "Loam" + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -1229,393 +1025,93 @@ "sl7": 120 }, "cec": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 40.4, - "sl5": 40.29, - "sl6": 40.2, - "sl7": 39.67 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 20.2, + "sl5": 20.14, + "sl6": 19.8, + "sl7": 19.0 }, "clay": { - "sl1": 53.0, - "sl2": 53.0, - "sl3": 53.0, - "sl4": 54.8, - "sl5": 55.29, - "sl6": 55.6, - "sl7": 55.33 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 26.8, + "sl5": 27.86, + "sl6": 29.2, + "sl7": 28.83 }, "ec": { "sl1": 0.0, "sl2": 0.0, "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.14, - "sl6": 0.4, - "sl7": 0.67 + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.8, + "sl7": 0.83 }, "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz3", - "rank_loc": "Not Displayed", - "score_loc": 0.05 + "component": "Ferralic arenosols", + "name": "Ferralic arenosols", + "rank_loc": "11", + "score_loc": 0.006 }, "ph": { - "sl1": 6.9, - "sl2": 6.9, - "sl3": 6.9, - "sl4": 7.06, - "sl5": 7.14, - "sl6": 7.3, - "sl7": 7.37 + "sl1": 7.6, + "sl2": 7.6, + "sl3": 7.6, + "sl4": 7.68, + "sl5": 7.74, + "sl6": 7.82, + "sl7": 7.88 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.2, - "sl5": 2.43, - "sl6": 2.4, - "sl7": 2.33 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.0, + "sl5": 18.0, + "sl6": 21.2, + "sl7": 21.67 }, "sand": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.4, - "sl5": 13.14, - "sl6": 13.0, - "sl7": 13.0 + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 39.0, + "sl5": 38.29, + "sl6": 36.8, + "sl7": 36.83 }, "site": { "siteData": { - "componentID": 148772, - "distance": 57897.214, - "mapunitID": 5986, - "minCompDistance": 7539.6102, - "share": 30, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", - "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", - "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " - } - }, - "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 14.6, - "sl5": 14.71, - "sl6": 15.0, - "sl7": 15.17 - }, - "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 28.6, - "sl5": 29.86, - "sl6": 30.6, - "sl7": 30.5 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 - }, - "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz4", - "rank_loc": "Not Displayed", - "score_loc": 0.05 - }, - "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.42, - "sl5": 6.44, - "sl6": 6.44, - "sl7": 6.43 - }, - "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.8, - "sl5": 9.29, - "sl6": 13.4, - "sl7": 12.5 - }, - "sand": { - "sl1": 53.0, - "sl2": 53.0, - "sl3": 53.0, - "sl4": 49.0, - "sl5": 47.71, - "sl6": 46.6, - "sl7": 46.67 - }, - "site": { - "siteData": { - "componentID": 148560, - "distance": 63106.737, - "mapunitID": 5929, - "minCompDistance": 7539.6102, - "share": 10, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", - "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", - "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 18.2, - "sl5": 18.43, - "sl6": 18.4, - "sl7": 17.83 - }, - "clay": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 34.2, - "sl5": 35.86, - "sl6": 37.2, - "sl7": 37.5 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 - }, - "id": { - "component": "Eutric planosols", - "name": "Eutric planosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.038 - }, - "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.56, - "sl5": 6.57, - "sl6": 6.58, - "sl7": 6.55 - }, - "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 10.6, - "sl5": 10.14, - "sl6": 9.8, - "sl7": 11.33 - }, - "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 34.4, - "sl5": 33.43, - "sl6": 32.6, - "sl7": 33.0 - }, - "site": { - "siteData": { - "componentID": 148773, - "distance": 57897.214, - "mapunitID": 5986, - "minCompDistance": 7539.6102, - "share": 10, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", - "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 11.8, - "sl5": 12.14, - "sl6": 12.2, - "sl7": 12.17 - }, - "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 24.2, - "sl5": 25.43, - "sl6": 26.2, - "sl7": 26.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 - }, - "id": { - "component": "Eutric planosols", - "name": "Eutric planosols3", - "rank_loc": "Not Displayed", - "score_loc": 0.038 - }, - "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.62, - "sl5": 6.66, - "sl6": 6.76, - "sl7": 6.83 - }, - "rock_fragments": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 12.0, - "sl5": 12.71, - "sl6": 16.0, - "sl7": 18.0 - }, - "sand": { - "sl1": 67.0, - "sl2": 67.0, - "sl3": 67.0, - "sl4": 62.6, - "sl5": 61.71, - "sl6": 61.0, - "sl7": 61.17 - }, - "site": { - "siteData": { - "componentID": 148558, - "distance": 63106.737, - "mapunitID": 5929, - "minCompDistance": 7539.6102, - "share": 20, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", - "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + "componentID": 149437, + "distance": 50505.675, + "mapunitID": 6189, + "minCompDistance": 50505.675, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1632,90 +1128,90 @@ "sl1": 9.0, "sl2": 9.0, "sl3": 9.0, - "sl4": 7.6, - "sl5": 7.0, - "sl6": 6.4, - "sl7": 6.0 + "sl4": 10.6, + "sl5": 12.29, + "sl6": 14.2, + "sl7": 15.0 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 18.0, - "sl5": 17.14, - "sl6": 16.0, - "sl7": 15.67 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 23.2, + "sl5": 27.0, + "sl6": 30.8, + "sl7": 32.0 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.14, - "sl6": 1.2, - "sl7": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 }, "id": { - "component": "Eutric planosols", - "name": "Eutric planosols4", - "rank_loc": "Not Displayed", - "score_loc": 0.038 + "component": "Eutric cambisols", + "name": "Eutric cambisols", + "rank_loc": "12", + "score_loc": 0.003 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.08, - "sl5": 5.13, - "sl6": 5.16, - "sl7": 5.18 + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.98, + "sl5": 6.11, + "sl6": 6.28, + "sl7": 6.42 }, "rock_fragments": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 30.6, - "sl5": 31.14, - "sl6": 35.2, - "sl7": 36.67 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.0, + "sl5": 10.14, + "sl6": 11.0, + "sl7": 11.5 }, "sand": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 57.6, - "sl5": 58.71, - "sl6": 60.2, - "sl7": 60.17 + "sl1": 58.0, + "sl2": 58.0, + "sl3": 58.0, + "sl4": 52.8, + "sl5": 49.57, + "sl6": 46.0, + "sl7": 44.33 }, "site": { "siteData": { - "componentID": 149078, - "distance": 95465.543, - "mapunitID": 6079, + "componentID": 148586, + "distance": 7539.61, + "mapunitID": 5933, "minCompDistance": 7539.6102, - "share": 30, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", - "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { "sl1": "Sandy loam", "sl2": "Sandy loam", "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Clay loam" } }, { @@ -1756,10 +1252,10 @@ "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", + "component": "Eutric planosols", + "name": "Eutric planosols2", "rank_loc": "Not Displayed", - "score_loc": 0.032 + "score_loc": 0.038 }, "ph": { "sl1": 5.3, @@ -1790,22 +1286,22 @@ }, "site": { "siteData": { - "componentID": 148481, - "distance": 75034.597, - "mapunitID": 5896, - "minCompDistance": 50714.6101, - "share": 100, - "soilDepth": 20 + "componentID": 148773, + "distance": 57897.214, + "mapunitID": 5986, + "minCompDistance": 7539.6102, + "share": 10, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." } }, "texture": { @@ -1829,22 +1325,22 @@ "sl7": 120 }, "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.14, - "sl6": 1.8, - "sl7": 1.67 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.6, + "sl7": 6.67 }, "clay": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.0, - "sl5": 4.0, - "sl6": 4.0, - "sl7": 4.0 + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 30.8, + "sl5": 33.14, + "sl6": 35.6, + "sl7": 36.67 }, "ec": { "sl1": 0.0, @@ -1856,66 +1352,66 @@ "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols3", + "component": "Eutric planosols", + "name": "Eutric planosols3", "rank_loc": "Not Displayed", - "score_loc": 0.032 + "score_loc": 0.038 }, "ph": { - "sl1": 5.5, - "sl2": 5.5, - "sl3": 5.5, - "sl4": 5.5, - "sl5": 5.53, - "sl6": 5.58, - "sl7": 5.6 + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.04, + "sl5": 5.03, + "sl6": 5.02, + "sl7": 5.02 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.0, - "sl5": 3.14, - "sl6": 3.4, - "sl7": 4.17 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 17.8, + "sl5": 19.14, + "sl6": 19.6, + "sl7": 20.0 }, "sand": { - "sl1": 88.0, - "sl2": 88.0, - "sl3": 88.0, - "sl4": 88.6, - "sl5": 88.57, - "sl6": 88.4, - "sl7": 88.33 + "sl1": 54.0, + "sl2": 54.0, + "sl3": 54.0, + "sl4": 49.6, + "sl5": 47.71, + "sl6": 45.6, + "sl7": 44.5 }, "site": { "siteData": { - "componentID": 148386, - "distance": 85053.285, - "mapunitID": 5873, - "minCompDistance": 50714.6101, - "share": 10, - "soilDepth": 20 + "componentID": 148558, + "distance": 63106.737, + "mapunitID": 5929, + "minCompDistance": 7539.6102, + "share": 20, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." } }, "texture": { - "sl1": "Sand", - "sl2": "Sand", - "sl3": "Sand", - "sl4": "Sand", - "sl5": "Sand", - "sl6": "Sand", - "sl7": "Sand" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" } }, { @@ -1929,93 +1425,93 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.8, - "sl5": 14.43, - "sl6": 13.2, - "sl7": 12.17 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.0, + "sl6": 6.4, + "sl7": 6.17 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 25.4, - "sl5": 25.86, - "sl6": 24.0, - "sl7": 22.67 + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 46.4, + "sl5": 47.43, + "sl6": 48.2, + "sl7": 48.67 }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.6, - "sl5": 1.71, - "sl6": 1.6, - "sl7": 1.33 + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Vertisols", - "name": "Vertisols2", + "component": "Eutric planosols", + "name": "Eutric planosols4", "rank_loc": "Not Displayed", - "score_loc": 0.032 + "score_loc": 0.038 }, "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 5.54, - "sl5": 5.44, - "sl6": 5.42, - "sl7": 5.45 + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.92, + "sl5": 4.94, + "sl6": 4.98, + "sl7": 5.0 }, "rock_fragments": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 20.6, - "sl5": 21.14, - "sl6": 22.4, - "sl7": 23.67 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.8, + "sl7": 5.0 }, "sand": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 40.2, - "sl5": 39.0, - "sl6": 42.4, - "sl7": 44.5 + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 38.8, + "sl5": 38.0, + "sl6": 37.4, + "sl7": 37.0 }, "site": { "siteData": { - "componentID": 148225, - "distance": 98631.899, - "mapunitID": 5688, - "minCompDistance": 74511.6383, - "share": 100, + "componentID": 149078, + "distance": 95465.543, + "mapunitID": 6079, + "minCompDistance": 7539.6102, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", - "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" } }, { @@ -2029,70 +1525,70 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 14.0, - "sl5": 14.71, - "sl6": 15.2, - "sl7": 15.33 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.14, + "sl6": 1.8, + "sl7": 1.67 }, "clay": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 22.8, - "sl5": 24.86, - "sl6": 26.2, - "sl7": 26.17 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.0, + "sl7": 4.0 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.2, - "sl7": 1.33 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Chromic luvisols", - "name": "Chromic luvisols2", + "name": "Chromic luvisols3", "rank_loc": "Not Displayed", "score_loc": 0.022 }, "ph": { - "sl1": 5.9, - "sl2": 5.9, - "sl3": 5.9, - "sl4": 5.96, - "sl5": 5.97, - "sl6": 6.0, - "sl7": 6.03 + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.5, + "sl5": 5.53, + "sl6": 5.58, + "sl7": 5.6 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 11.2, - "sl5": 11.71, - "sl6": 12.8, - "sl7": 13.33 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.0, + "sl5": 3.14, + "sl6": 3.4, + "sl7": 4.17 }, "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 37.6, - "sl5": 36.57, - "sl6": 36.2, - "sl7": 36.67 + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 88.6, + "sl5": 88.57, + "sl6": 88.4, + "sl7": 88.33 }, "site": { "siteData": { - "componentID": 148392, - "distance": 50714.61, - "mapunitID": 5874, + "componentID": 148455, + "distance": 74511.638, + "mapunitID": 5890, "minCompDistance": 29716.3626, "share": 10, "soilDepth": 200 @@ -2109,13 +1605,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" } }, { @@ -2129,70 +1625,70 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.6, - "sl5": 16.71, - "sl6": 16.6, - "sl7": 16.5 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.43, + "sl6": 6.0, + "sl7": 5.83 }, "clay": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 30.2, - "sl5": 31.57, - "sl6": 32.4, - "sl7": 32.33 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 33.4, + "sl5": 34.57, + "sl6": 35.4, + "sl7": 36.0 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Chromic luvisols", - "name": "Chromic luvisols3", + "name": "Chromic luvisols2", "rank_loc": "Not Displayed", "score_loc": 0.022 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.22, - "sl5": 6.26, - "sl6": 6.32, - "sl7": 6.37 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.04, + "sl5": 4.99, + "sl6": 4.96, + "sl7": 5.0 }, "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 14.8, - "sl5": 15.29, - "sl6": 15.2, - "sl7": 14.67 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.6, + "sl5": 3.86, + "sl6": 4.2, + "sl7": 5.0 }, "sand": { - "sl1": 47.0, - "sl2": 47.0, - "sl3": 47.0, - "sl4": 43.6, - "sl5": 42.71, - "sl6": 42.4, - "sl7": 42.67 + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 53.8, + "sl5": 52.86, + "sl6": 52.2, + "sl7": 51.33 }, "site": { "siteData": { - "componentID": 148455, - "distance": 74511.638, - "mapunitID": 5890, + "componentID": 148392, + "distance": 50714.61, + "mapunitID": 5874, "minCompDistance": 29716.3626, "share": 10, "soilDepth": 200 @@ -2209,13 +1705,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Sandy clay" } }, { @@ -2229,31 +1725,31 @@ "sl7": 120 }, "cec": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 13.8, - "sl5": 14.0, - "sl6": 14.0, - "sl7": 13.83 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 3.6, + "sl5": 3.71, + "sl6": 3.8, + "sl7": 3.83 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 19.6, - "sl5": 20.14, - "sl6": 20.2, - "sl7": 20.17 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.4, + "sl5": 17.14, + "sl6": 18.6, + "sl7": 19.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Dystric regosols", @@ -2262,31 +1758,31 @@ "score_loc": 0.021 }, "ph": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 7.14, - "sl5": 7.21, - "sl6": 7.34, - "sl7": 7.42 + "sl1": 5.4, + "sl2": 5.4, + "sl3": 5.4, + "sl4": 5.22, + "sl5": 5.19, + "sl6": 5.16, + "sl7": 5.17 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.8, - "sl5": 16.71, - "sl6": 17.8, - "sl7": 17.83 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.0, + "sl5": 9.14, + "sl6": 8.4, + "sl7": 9.17 }, "sand": { - "sl1": 64.0, - "sl2": 64.0, - "sl3": 64.0, - "sl4": 61.2, - "sl5": 60.86, - "sl6": 60.8, - "sl7": 60.83 + "sl1": 77.0, + "sl2": 77.0, + "sl3": 77.0, + "sl4": 72.6, + "sl5": 71.0, + "sl6": 70.0, + "sl7": 69.33 }, "site": { "siteData": { @@ -2309,13 +1805,13 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", "sl4": "Sandy loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -2329,30 +1825,30 @@ "sl7": 120 }, "cec": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 16.0, - "sl5": 16.0, - "sl6": 16.0, - "sl7": 15.83 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.0, + "sl6": 6.4, + "sl7": 6.0 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 22.2, - "sl5": 23.0, - "sl6": 23.6, - "sl7": 23.67 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.0, + "sl5": 17.14, + "sl6": 16.0, + "sl7": 15.67 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, + "sl5": 1.14, + "sl6": 1.2, "sl7": 1.0 }, "id": { @@ -2362,31 +1858,31 @@ "score_loc": 0.021 }, "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4, - "sl4": 7.56, - "sl5": 7.64, - "sl6": 7.74, - "sl7": 7.82 + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.08, + "sl5": 5.13, + "sl6": 5.16, + "sl7": 5.18 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 19.0, - "sl5": 21.0, - "sl6": 22.6, - "sl7": 22.83 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 30.6, + "sl5": 31.14, + "sl6": 35.2, + "sl7": 36.67 }, "sand": { - "sl1": 57.0, - "sl2": 57.0, - "sl3": 57.0, - "sl4": 55.0, - "sl5": 54.57, - "sl6": 54.2, - "sl7": 54.17 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 57.6, + "sl5": 58.71, + "sl6": 60.2, + "sl7": 60.17 }, "site": { "siteData": { @@ -2412,10 +1908,10 @@ "sl1": "Sandy loam", "sl2": "Sandy loam", "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -2429,83 +1925,83 @@ "sl7": 120 }, "cec": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 20.2, - "sl5": 20.14, - "sl6": 19.8, - "sl7": 19.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 13.6, + "sl5": 15.0, + "sl6": 16.4, + "sl7": 16.83 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 26.8, - "sl5": 27.86, + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 24.4, + "sl5": 26.86, "sl6": 29.2, - "sl7": 28.83 + "sl7": 30.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.8, - "sl7": 0.83 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Haplic luvisols", - "name": "Haplic luvisols2", + "component": "Calcic luvisols", + "name": "Calcic luvisols2", "rank_loc": "Not Displayed", - "score_loc": 0.016 + "score_loc": 0.013 }, "ph": { - "sl1": 7.6, - "sl2": 7.6, - "sl3": 7.6, - "sl4": 7.68, - "sl5": 7.74, - "sl6": 7.82, - "sl7": 7.88 + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.26, + "sl5": 6.37, + "sl6": 6.52, + "sl7": 6.57 }, "rock_fragments": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.0, - "sl5": 18.0, - "sl6": 21.2, - "sl7": 21.67 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.57, + "sl6": 2.4, + "sl7": 2.33 }, "sand": { - "sl1": 42.0, - "sl2": 42.0, - "sl3": 42.0, - "sl4": 39.0, - "sl5": 38.29, - "sl6": 36.8, - "sl7": 36.83 + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 46.0, + "sl5": 44.14, + "sl6": 42.2, + "sl7": 42.0 }, "site": { "siteData": { - "componentID": 148399, - "distance": 29716.363, - "mapunitID": 5876, - "minCompDistance": 7539.6102, + "componentID": 148589, + "distance": 46063.093, + "mapunitID": 5935, + "minCompDistance": 29716.3626, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", - "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " } }, "texture": { @@ -2513,7 +2009,7 @@ "sl2": "Loam", "sl3": "Loam", "sl4": "Loam", - "sl5": "Clay loam", + "sl5": "Loam", "sl6": "Clay loam", "sl7": "Clay loam" } @@ -2529,93 +2025,93 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 14.0, - "sl5": 14.0, - "sl6": 14.0, - "sl7": 14.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 }, "clay": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 20.2, - "sl5": 20.86, - "sl6": 21.2, - "sl7": 21.33 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 }, "id": { - "component": "Haplic luvisols", - "name": "Haplic luvisols3", + "component": "Calcic luvisols", + "name": "Calcic luvisols3", "rank_loc": "Not Displayed", - "score_loc": 0.016 - }, - "ph": { - "sl1": 7.5, - "sl2": 7.5, - "sl3": 7.5, - "sl4": 7.72, - "sl5": 7.81, - "sl6": 7.92, - "sl7": 8.0 + "score_loc": 0.013 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 24.8, - "sl5": 27.86, - "sl6": 29.8, - "sl7": 30.17 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 }, "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 62.4, - "sl5": 62.0, - "sl6": 62.0, - "sl7": 61.83 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 }, "site": { "siteData": { - "componentID": 148456, - "distance": 74511.638, - "mapunitID": 5890, - "minCompDistance": 7539.6102, + "componentID": 149440, + "distance": 50505.675, + "mapunitID": 6189, + "minCompDistance": 29716.3626, "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", - "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " } }, "texture": { "sl1": "Sandy loam", "sl2": "Sandy loam", "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -2629,22 +2125,22 @@ "sl7": 120 }, "cec": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 13.2, - "sl5": 12.86, - "sl6": 12.4, - "sl7": 12.17 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.0, + "sl6": 2.0, + "sl7": 2.0 }, "clay": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 52.8, - "sl5": 55.14, - "sl6": 57.4, - "sl7": 58.5 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 }, "ec": { "sl1": 0.0, @@ -2656,17 +2152,17 @@ "sl7": 0.0 }, "id": { - "component": "Calcic luvisols", - "name": "Calcic luvisols2", + "component": "Acrisols", + "name": "Acrisols2", "rank_loc": "Not Displayed", - "score_loc": 0.013 + "score_loc": 0.011 }, "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 5.74, - "sl5": 5.73, + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.82, + "sl5": 5.77, "sl6": 5.72, "sl7": 5.72 }, @@ -2674,48 +2170,48 @@ "sl1": 2.0, "sl2": 2.0, "sl3": 2.0, - "sl4": 2.4, - "sl5": 2.71, - "sl6": 3.0, - "sl7": 3.33 + "sl4": 3.2, + "sl5": 3.71, + "sl6": 4.4, + "sl7": 8.83 }, "sand": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 25.0, - "sl5": 23.86, - "sl6": 22.8, - "sl7": 22.17 + "sl1": 90.0, + "sl2": 90.0, + "sl3": 90.0, + "sl4": 89.4, + "sl5": 89.29, + "sl6": 89.4, + "sl7": 89.5 }, "site": { "siteData": { - "componentID": 148589, - "distance": 46063.093, - "mapunitID": 5935, - "minCompDistance": 29716.3626, + "componentID": 148909, + "distance": 35586.855, + "mapunitID": 6020, + "minCompDistance": 32877.4526, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", - "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + "Description_en": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" } }, { @@ -2729,93 +2225,93 @@ "sl7": 120 }, "cec": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 17.4, - "sl5": 14.57, - "sl6": 11.8, - "sl7": 10.67 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.8, + "sl5": 14.43, + "sl6": 13.2, + "sl7": 12.17 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 5.4, - "sl5": 5.43, - "sl6": 5.6, - "sl7": 5.67 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 25.4, + "sl5": 25.86, + "sl6": 24.0, + "sl7": 22.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.33 }, "id": { - "component": "Calcic luvisols", - "name": "Calcic luvisols3", + "component": "Ferralsols", + "name": "Ferralsols2", "rank_loc": "Not Displayed", - "score_loc": 0.013 + "score_loc": 0.011 }, "ph": { - "sl1": 4.6, - "sl2": 4.6, - "sl3": 4.6, - "sl4": 4.88, - "sl5": 4.99, - "sl6": 5.1, - "sl7": 5.17 + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.54, + "sl5": 5.44, + "sl6": 5.42, + "sl7": 5.45 }, "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 16.8, - "sl5": 18.71, - "sl6": 20.6, - "sl7": 21.5 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.6, + "sl5": 21.14, + "sl6": 22.4, + "sl7": 23.67 }, "sand": { - "sl1": 58.0, - "sl2": 58.0, - "sl3": 58.0, - "sl4": 60.4, - "sl5": 61.57, - "sl6": 63.2, - "sl7": 64.17 + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 40.2, + "sl5": 39.0, + "sl6": 42.4, + "sl7": 44.5 }, "site": { "siteData": { - "componentID": 149440, - "distance": 50505.675, - "mapunitID": 6189, - "minCompDistance": 29716.3626, - "share": 10, + "componentID": 148908, + "distance": 35586.855, + "mapunitID": 6020, + "minCompDistance": 32877.4526, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", - "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " + "Description_en": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Description_es": "Los Ferralisoles son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad, como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes. ", + "Description_fr": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Description_ks": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por parte de los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -2829,93 +2325,93 @@ "sl7": 120 }, "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 3.8, - "sl5": 3.86, - "sl6": 3.6, - "sl7": 3.83 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 14.0 }, "clay": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.8, - "sl5": 3.29, - "sl6": 3.8, - "sl7": 4.17 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.2, + "sl5": 20.86, + "sl6": 21.2, + "sl7": 21.33 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Haplic podzols", - "name": "Haplic podzols2", + "component": "Dystric planosols", + "name": "Dystric planosols2", "rank_loc": "Not Displayed", - "score_loc": 0.011 + "score_loc": 0.009 }, "ph": { - "sl1": 4.7, - "sl2": 4.7, - "sl3": 4.7, - "sl4": 4.92, - "sl5": 4.94, - "sl6": 4.96, - "sl7": 4.95 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.72, + "sl5": 7.81, + "sl6": 7.92, + "sl7": 8.0 }, "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 16.8, - "sl5": 18.71, - "sl6": 20.6, - "sl7": 19.5 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.8, + "sl5": 27.86, + "sl6": 29.8, + "sl7": 30.17 }, "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 88.6, - "sl5": 88.57, - "sl6": 88.4, - "sl7": 88.33 + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 62.4, + "sl5": 62.0, + "sl6": 62.0, + "sl7": 61.83 }, "site": { "siteData": { - "componentID": 148893, - "distance": 32877.453, - "mapunitID": 6017, - "minCompDistance": 3068.5627, - "share": 30, + "componentID": 148559, + "distance": 63106.737, + "mapunitID": 5929, + "minCompDistance": 7539.6102, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", - "Description_es": "Los Podzoles Háplicos son suelos de textura gruesa, ácidos e improductivos, con horizontes superficiales muy lixiviados sobre los que se asientan subsuelos que contienen materia orgánica acumulada y metales (aluminio y hierro).*En los paisajes de llanura costera plana, estos suelos también son húmedos.", - "Description_fr": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", - "Description_ks": "Haplic Podzols are coarse textured, acidic, unproductive soils with highly leached surface horizons overlying subsoils containing accumulated organic matter and metals (aluminum and iron).
In flat coastal plain landscapes, these soils are also wet.", - "Management_en": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", - "Management_es": "Los podzoles están muy lixiviados y, como tales, tienen una baja fertilidad.
Las capas superficiales suelen ser bastante ácidas (pH < 4,5), por lo que es necesario el encalado.
Debido al alto grado de meteorización, los suelos también tienen un alto contenido de aluminio soluble y fijan el fósforo, creando deficiencias de P. Aunque no se recomienda, si estos suelos se utilizan para el cultivo necesitarán un arado profundo (para romper las capas del subsuelo), encalado y fertilización.
Será necesario un cuidado específico con la fertilización de P, y se recomienda el uso de banda en la colocación de P en la semilla.", - "Management_fr": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended.", - "Management_ks": "Podzols are highly leached, and as such are low in soil fertility.
The surface layers are usually quite acidic (pH < 4.5) and thus liming is needed.
Because of the high degree of weathering the soils are also high in soluble aluminum and will fix phosphorus, creating P deficiencies. Although not recommended, if these soils are used for cultivation they will need deep plowing (to break subsoil layers), liming and fertilization.
Specific care with P fertilization will be needed, and use of band on on-seed placement of P is recommended." + "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.", + "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed." } }, "texture": { - "sl1": "Sand", - "sl2": "Sand", - "sl3": "Sand", - "sl4": "Sand", - "sl5": "Sand", - "sl6": "Sand", - "sl7": "Sand" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } } ] @@ -2927,207 +2423,159 @@ }, "soilRank": [ { - "component": "Vertisols", - "componentData": "No Data", - "componentID": 148225, - "name": "Vertisols2", + "component": "Eutric planosols", + "componentData": "Data Complete", + "componentID": 148558, + "name": "Eutric planosols3", "rank_data": "Not Displayed", "rank_data_loc": "1", "rank_loc": "Not Displayed", "score_data": 0.919, "score_data_loc": 1.0, - "score_loc": 0.032 + "score_loc": 0.038 }, { "component": "Chromic luvisols", "componentData": "Missing Data", "componentID": 148392, "name": "Chromic luvisols2", - "rank_data": "2", + "rank_data": "Not Displayed", "rank_data_loc": "2", "rank_loc": "Not Displayed", "score_data": 0.919, - "score_data_loc": 0.99, + "score_data_loc": 0.984, "score_loc": 0.022 }, { - "component": "Albic arenosols", + "component": "Dystric regosols", "componentData": "Data Complete", - "componentID": 148894, - "name": "Albic arenosols1", - "rank_data": "1", + "componentID": 149439, + "name": "Dystric regosols2", + "rank_data": "3", "rank_data_loc": "3", - "rank_loc": "8", + "rank_loc": "Not Displayed", "score_data": 0.919, - "score_data_loc": 0.989, + "score_data_loc": 0.983, "score_loc": 0.021 }, { - "component": "Haplic solonetz", + "component": "Calcic luvisols", "componentData": "Data Complete", - "componentID": 148772, - "name": "Haplic solonetz3", - "rank_data": "5", + "componentID": 149440, + "name": "Calcic luvisols3", + "rank_data": "1", "rank_data_loc": "4", "rank_loc": "Not Displayed", - "score_data": 0.808, - "score_data_loc": 0.904, - "score_loc": 0.05 + "score_data": 0.919, + "score_data_loc": 0.974, + "score_loc": 0.013 }, { - "component": "Calcic luvisols", - "componentData": "Data Complete", - "componentID": 148589, - "name": "Calcic luvisols2", - "rank_data": "4", + "component": "Ferralsols", + "componentData": "Missing Data", + "componentID": 148908, + "name": "Ferralsols2", + "rank_data": "5", "rank_data_loc": "5", "rank_loc": "Not Displayed", - "score_data": 0.808, - "score_data_loc": 0.864, - "score_loc": 0.013 + "score_data": 0.825, + "score_data_loc": 0.874, + "score_loc": 0.011 }, { - "component": "Rhodic nitisols", - "componentData": "No Data", - "componentID": 148454, - "name": "Rhodic nitisols", + "component": "Acrisols", + "componentData": "Missing Data", + "componentID": 148895, + "name": "Acrisols1", "rank_data": "6", "rank_data_loc": "6", - "rank_loc": "11", - "score_data": 0.808, - "score_data_loc": 0.864, - "score_loc": 0.013 + "rank_loc": "7", + "score_data": 0.795, + "score_data_loc": 0.842, + "score_loc": 0.011 }, { - "component": "Haplic podzols", + "component": "Albic arenosols", "componentData": "Data Complete", - "componentID": 148915, - "name": "Haplic podzols1", + "componentID": 148894, + "name": "Albic arenosols1", "rank_data": "7", "rank_data_loc": "7", - "rank_loc": "12", - "score_data": 0.805, - "score_data_loc": 0.859, - "score_loc": 0.011 + "rank_loc": "5", + "score_data": 0.774, + "score_data_loc": 0.832, + "score_loc": 0.021 }, { - "component": "Eutric planosols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 149078, - "name": "Eutric planosols4", + "componentID": 148586, + "name": "Eutric cambisols", "rank_data": "8", "rank_data_loc": "8", - "rank_loc": "Not Displayed", - "score_data": 0.757, - "score_data_loc": 0.836, - "score_loc": 0.038 + "rank_loc": "12", + "score_data": 0.748, + "score_data_loc": 0.785, + "score_loc": 0.003 }, { - "component": "Haplic luvisols", + "component": "Cambic arenosols", "componentData": "Data Complete", - "componentID": 148399, - "name": "Haplic luvisols2", + "componentID": 148403, + "name": "Cambic arenosols", "rank_data": "9", "rank_data_loc": "9", - "rank_loc": "Not Displayed", - "score_data": 0.753, - "score_data_loc": 0.809, - "score_loc": 0.016 + "rank_loc": "2", + "score_data": 0.675, + "score_data_loc": 0.739, + "score_loc": 0.032 }, { - "component": "Cambic arenosols", + "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 148403, - "name": "Cambic arenosols", - "rank_data": "11", + "componentID": 149436, + "name": "Calcaric regosols", + "rank_data": "10", "rank_data_loc": "10", - "rank_loc": "3", - "score_data": 0.722, - "score_data_loc": 0.793, - "score_loc": 0.032 + "rank_loc": "10", + "score_data": 0.652, + "score_data_loc": 0.688, + "score_loc": 0.006 }, { - "component": "Dystric regosols", + "component": "Ferralic arenosols", "componentData": "Data Complete", - "componentID": 149439, - "name": "Dystric regosols2", - "rank_data": "12", + "componentID": 149437, + "name": "Ferralic arenosols", + "rank_data": "11", "rank_data_loc": "11", - "rank_loc": "Not Displayed", - "score_data": 0.722, - "score_data_loc": 0.782, - "score_loc": 0.021 + "rank_loc": "11", + "score_data": 0.629, + "score_data_loc": 0.664, + "score_loc": 0.006 }, { - "component": "Lithic leptosols", + "component": "Dystric planosols", "componentData": "Missing Data", - "componentID": 148388, - "name": "Lithic leptosols1", - "rank_data": "10", + "componentID": 148585, + "name": "Dystric planosols1", + "rank_data": "12", "rank_data_loc": "12", - "rank_loc": "4", - "score_data": 0.753, - "score_data_loc": 0.002, - "score_loc": 0.032 + "rank_loc": "9", + "score_data": 0.581, + "score_data_loc": 0.617, + "score_loc": 0.009 }, { - "component": "Vertisols", - "componentData": "No Data", - "componentID": 148452, - "name": "Vertisols1", - "rank_data": "3", + "component": "Eutric planosols", + "componentData": "Missing Data", + "componentID": 148773, + "name": "Eutric planosols2", + "rank_data": "4", "rank_data_loc": "Not Displayed", - "rank_loc": "5", + "rank_loc": "Not Displayed", "score_data": 0.919, "score_data_loc": 1.0, - "score_loc": 0.032 - }, - { - "component": "Haplic solonetz", - "componentData": "Data Complete", - "componentID": 149438, - "name": "Haplic solonetz2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.805, - "score_data_loc": 0.901, - "score_loc": 0.05 - }, - { - "component": "Calcic luvisols", - "componentData": "Data Complete", - "componentID": 148402, - "name": "Calcic luvisols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "10", - "score_data": 0.805, - "score_data_loc": 0.861, - "score_loc": 0.013 - }, - { - "component": "Haplic solonetz", - "componentData": "Data Complete", - "componentID": 148584, - "name": "Haplic solonetz1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "1", - "score_data": 0.753, - "score_data_loc": 0.846, - "score_loc": 0.05 - }, - { - "component": "Eutric planosols", - "componentData": "Data Complete", - "componentID": 148582, - "name": "Eutric planosols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "2", - "score_data": 0.753, - "score_data_loc": 0.832, "score_loc": 0.038 }, { @@ -3135,49 +2583,25 @@ "componentData": "Data Complete", "componentID": 148455, "name": "Chromic luvisols3", - "rank_data": "Not Displayed", + "rank_data": "2", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.753, - "score_data_loc": 0.816, + "score_data": 0.919, + "score_data_loc": 0.984, "score_loc": 0.022 }, - { - "component": "Calcic luvisols", - "componentData": "Data Complete", - "componentID": 149440, - "name": "Calcic luvisols3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.757, - "score_data_loc": 0.809, - "score_loc": 0.013 - }, { "component": "Eutric planosols", "componentData": "Data Complete", - "componentID": 148558, - "name": "Eutric planosols3", + "componentID": 149078, + "name": "Eutric planosols4", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.722, - "score_data_loc": 0.799, + "score_data": 0.774, + "score_data_loc": 0.849, "score_loc": 0.038 }, - { - "component": "Chromic luvisols", - "componentData": "Data Complete", - "componentID": 148401, - "name": "Chromic luvisols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "6", - "score_data": 0.722, - "score_data_loc": 0.783, - "score_loc": 0.022 - }, { "component": "Albic arenosols", "componentData": "Data Complete", @@ -3186,105 +2610,105 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.722, - "score_data_loc": 0.782, + "score_data": 0.748, + "score_data_loc": 0.804, "score_loc": 0.021 }, { - "component": "Haplic luvisols", + "component": "Calcic luvisols", "componentData": "Data Complete", - "componentID": 148456, - "name": "Haplic luvisols3", + "componentID": 148402, + "name": "Calcic luvisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.722, - "score_data_loc": 0.776, - "score_loc": 0.016 + "rank_loc": "6", + "score_data": 0.748, + "score_data_loc": 0.795, + "score_loc": 0.013 }, { - "component": "Haplic solonetz", - "componentData": "Data Complete", - "componentID": 148560, - "name": "Haplic solonetz4", + "component": "Ferralsols", + "componentData": "No Data", + "componentID": 148898, + "name": "Ferralsols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.625, - "score_data_loc": 0.711, - "score_loc": 0.05 + "rank_loc": "8", + "score_data": 0.748, + "score_data_loc": 0.793, + "score_loc": 0.011 }, { - "component": "Dystric regosols", + "component": "Eutric planosols", "componentData": "Data Complete", - "componentID": 148956, - "name": "Dystric regosols1", + "componentID": 148582, + "name": "Eutric planosols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "7", - "score_data": 0.622, - "score_data_loc": 0.677, - "score_loc": 0.021 + "rank_loc": "1", + "score_data": 0.652, + "score_data_loc": 0.721, + "score_loc": 0.038 }, { - "component": "Eutric planosols", - "componentData": "Missing Data", - "componentID": 148773, - "name": "Eutric planosols2", + "component": "Calcic luvisols", + "componentData": "Data Complete", + "componentID": 148589, + "name": "Calcic luvisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.587, - "score_data_loc": 0.658, - "score_loc": 0.038 + "score_data": 0.649, + "score_data_loc": 0.691, + "score_loc": 0.013 }, { - "component": "Haplic luvisols", + "component": "Chromic luvisols", "componentData": "Data Complete", - "componentID": 148583, - "name": "Haplic luvisols1", + "componentID": 148401, + "name": "Chromic luvisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "9", - "score_data": 0.557, - "score_data_loc": 0.603, - "score_loc": 0.016 + "rank_loc": "3", + "score_data": 0.581, + "score_data_loc": 0.631, + "score_loc": 0.022 }, { - "component": "Haplic podzols", - "componentData": "Data Complete", - "componentID": 148893, - "name": "Haplic podzols2", + "component": "Dystric planosols", + "componentData": "Missing Data", + "componentID": 148559, + "name": "Dystric planosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.413, - "score_data_loc": 0.445, - "score_loc": 0.011 + "score_data": 0.574, + "score_data_loc": 0.61, + "score_loc": 0.009 }, { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 148481, - "name": "Lithic leptosols2", + "component": "Dystric regosols", + "componentData": "Data Complete", + "componentID": 148956, + "name": "Dystric regosols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.557, - "score_data_loc": 0.002, - "score_loc": 0.032 + "rank_loc": "4", + "score_data": 0.443, + "score_data_loc": 0.485, + "score_loc": 0.021 }, { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 148386, - "name": "Lithic leptosols3", + "component": "Acrisols", + "componentData": "Data Complete", + "componentID": 148909, + "name": "Acrisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.413, - "score_data_loc": 0.002, - "score_loc": 0.032 + "score_data": 0.443, + "score_data_loc": 0.474, + "score_loc": 0.011 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json index a5f0846..6af3483 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-2.06972,37.29].json @@ -25,93 +25,93 @@ "sl7": 120 }, "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.29, - "sl6": 2.2, - "sl7": 2.0 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.43, + "sl6": 16.6, + "sl7": 16.17 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.2, - "sl5": 6.43, - "sl6": 6.8, - "sl7": 7.0 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.6, + "sl5": 25.0, + "sl6": 25.4, + "sl7": 25.17 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.5 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols1", + "component": "Chromic cambisols", + "name": "Chromic cambisols1", "rank_loc": "1", - "score_loc": 0.03 + "score_loc": 0.013 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.32, - "sl5": 5.34, - "sl6": 5.36, - "sl7": 5.37 + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 7.98, + "sl5": 8.01, + "sl6": 8.06, + "sl7": 8.03 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.2, - "sl5": 4.43, - "sl6": 4.6, - "sl7": 4.5 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 13.4, + "sl5": 12.86, + "sl6": 12.4, + "sl7": 12.5 }, "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 86.8, - "sl5": 86.57, - "sl6": 86.2, - "sl7": 86.0 + "sl1": 44.0, + "sl2": 44.0, + "sl3": 44.0, + "sl4": 42.8, + "sl5": 42.14, + "sl6": 41.2, + "sl7": 41.0 }, "site": { "siteData": { - "componentID": 111242, - "distance": 45915.675, - "mapunitID": 17468, - "minCompDistance": 45915.6746, - "share": 100, + "componentID": 111105, + "distance": 54718.541, + "mapunitID": 17393, + "minCompDistance": 54718.5415, + "share": 50, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -125,93 +125,93 @@ "sl7": 120 }, "cec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.0, - "sl5": 2.0, - "sl6": 2.0, - "sl7": 2.0 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.2, + "sl5": 18.43, + "sl6": 18.4, + "sl7": 17.83 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.6, - "sl5": 6.71, - "sl6": 6.8, - "sl7": 6.83 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 34.2, + "sl5": 35.86, + "sl6": 37.2, + "sl7": 37.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Humic nitisols", - "name": "Humic nitisols", + "component": "Calcaric cambisols", + "name": "Calcaric cambisols1", "rank_loc": "2", - "score_loc": 0.024 + "score_loc": 0.011 }, "ph": { - "sl1": 5.9, - "sl2": 5.9, - "sl3": 5.9, - "sl4": 5.82, - "sl5": 5.77, - "sl6": 5.72, - "sl7": 5.72 + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.56, + "sl5": 6.57, + "sl6": 6.58, + "sl7": 6.55 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.2, - "sl5": 3.71, - "sl6": 4.4, - "sl7": 8.83 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.6, + "sl5": 10.14, + "sl6": 9.8, + "sl7": 11.33 }, "sand": { - "sl1": 90.0, - "sl2": 90.0, - "sl3": 90.0, - "sl4": 89.4, - "sl5": 89.29, - "sl6": 89.4, - "sl7": 89.5 + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 34.4, + "sl5": 33.43, + "sl6": 32.6, + "sl7": 33.0 }, "site": { "siteData": { - "componentID": 111081, - "distance": 85305.924, - "mapunitID": 17379, - "minCompDistance": 85305.9237, - "share": 30, + "componentID": 111282, + "distance": 9861.436, + "mapunitID": 17486, + "minCompDistance": 9861.4358, + "share": 85, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Humic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Humic Nitisols have relatively higher organic matter in surface horizons.", - "Description_es": "Los Nitisoles Húmicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes. *Los Nitisoles Húmicos tienen relativamente más materia orgánica en los horizontes superficiales.", - "Description_fr": "Humic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Humic Nitisols have relatively higher organic matter in surface horizons.", - "Description_ks": "Humic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Humic Nitisols have relatively higher organic matter in surface horizons.", - "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", - "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la planta durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación de fertilizantes fosfatados en banda (directamente sobre la semilla o a un lado y abajo de la semilla), ayudarán a reducir la fijación de P.", - "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", - "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation." + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Sand", - "sl2": "Sand", - "sl3": "Sand", - "sl4": "Sand", - "sl5": "Sand", - "sl6": "Sand", - "sl7": "Sand" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -225,93 +225,93 @@ "sl7": 120 }, "cec": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 19.6, - "sl5": 18.43, - "sl6": 17.4, - "sl7": 16.67 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 14.8, + "sl5": 14.57, + "sl6": 14.2, + "sl7": 14.0 }, "clay": { - "sl1": 45.0, - "sl2": 45.0, - "sl3": 45.0, - "sl4": 49.0, - "sl5": 51.14, - "sl6": 54.0, - "sl7": 56.0 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.6, + "sl5": 20.86, + "sl6": 21.0, + "sl7": 20.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 0.8, + "sl5": 0.71, + "sl6": 0.8, + "sl7": 0.83 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols1", + "component": "Eutric cambisols", + "name": "Eutric cambisols1", "rank_loc": "3", - "score_loc": 0.015 + "score_loc": 0.011 }, "ph": { - "sl1": 5.2, - "sl2": 5.2, - "sl3": 5.2, - "sl4": 5.24, - "sl5": 5.31, - "sl6": 5.4, - "sl7": 5.43 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.54, + "sl5": 6.6, + "sl6": 6.66, + "sl7": 6.7 }, "rock_fragments": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 7.0, - "sl5": 6.71, - "sl6": 7.6, - "sl7": 8.33 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 15.0, + "sl5": 16.57, + "sl6": 18.8, + "sl7": 19.17 }, "sand": { - "sl1": 28.0, - "sl2": 28.0, - "sl3": 28.0, - "sl4": 25.4, - "sl5": 24.14, - "sl6": 22.6, - "sl7": 21.33 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 40.8, + "sl5": 41.14, + "sl6": 41.8, + "sl7": 42.17 }, "site": { "siteData": { - "componentID": 111240, - "distance": 9468.474, - "mapunitID": 17466, - "minCompDistance": 9468.4741, - "share": 10, + "componentID": 111337, + "distance": 70615.69, + "mapunitID": 17519, + "minCompDistance": 70615.6896, + "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -325,983 +325,83 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.71, - "sl6": 6.8, - "sl7": 6.83 + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.6, + "sl5": 21.86, + "sl6": 22.2, + "sl7": 22.67 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.2, - "sl5": 30.29, - "sl6": 33.2, - "sl7": 34.33 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.0, + "sl5": 31.43, + "sl6": 31.4, + "sl7": 31.33 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 }, "id": { - "component": "Chromic cambisols", - "name": "Chromic cambisols1", + "component": "Calcic luvisols", + "name": "Calcic luvisols", "rank_loc": "4", - "score_loc": 0.013 + "score_loc": 0.011 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.12, - "sl5": 6.07, - "sl6": 6.02, - "sl7": 6.02 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.47, + "sl6": 6.58, + "sl7": 6.65 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 9.8, - "sl5": 10.43, - "sl6": 10.6, - "sl7": 10.5 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.8, + "sl5": 16.57, + "sl6": 17.8, + "sl7": 16.0 }, "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 60.2, - "sl5": 57.57, - "sl6": 54.8, - "sl7": 53.0 - }, - "site": { - "siteData": { - "componentID": 111105, - "distance": 54718.541, - "mapunitID": 17393, - "minCompDistance": 54718.5415, - "share": 50, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", - "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.71, - "sl6": 6.8, - "sl7": 6.83 - }, - "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.2, - "sl5": 30.29, - "sl6": 33.2, - "sl7": 34.33 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols1", - "rank_loc": "5", - "score_loc": 0.011 - }, - "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.12, - "sl5": 6.07, - "sl6": 6.02, - "sl7": 6.02 - }, - "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 9.8, - "sl5": 10.43, - "sl6": 10.6, - "sl7": 10.5 - }, - "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 60.2, - "sl5": 57.57, - "sl6": 54.8, - "sl7": 53.0 - }, - "site": { - "siteData": { - "componentID": 111101, - "distance": 9085.201, - "mapunitID": 17390, - "minCompDistance": 9085.2006, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0, - "sl5": 5.14, - "sl6": 5.2, - "sl7": 5.33 - }, - "clay": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 18.8, - "sl5": 20.43, - "sl6": 22.2, - "sl7": 22.83 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols1", - "rank_loc": "6", - "score_loc": 0.011 - }, - "ph": { - "sl1": 6.1, - "sl2": 6.1, - "sl3": 6.1, - "sl4": 6.0, - "sl5": 5.99, - "sl6": 6.0, - "sl7": 6.02 - }, - "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.8, - "sl5": 5.86, - "sl6": 9.2, - "sl7": 9.5 - }, - "sand": { - "sl1": 76.0, - "sl2": 76.0, - "sl3": 76.0, - "sl4": 71.4, - "sl5": 69.86, - "sl6": 68.2, - "sl7": 67.67 - }, - "site": { - "siteData": { - "componentID": 111282, - "distance": 9861.436, - "mapunitID": 17486, - "minCompDistance": 9861.4358, - "share": 85, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.0, - "sl5": 6.14, - "sl6": 6.4, - "sl7": 6.5 - }, - "clay": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 25.0, - "sl5": 28.14, - "sl6": 30.6, - "sl7": 31.17 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Humic cambisols", - "name": "Humic cambisols", - "rank_loc": "7", - "score_loc": 0.011 - }, - "ph": { - "sl1": 5.6, - "sl2": 5.6, - "sl3": 5.6, - "sl4": 5.68, - "sl5": 5.71, - "sl6": 5.74, - "sl7": 5.73 - }, - "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 10.8, - "sl5": 10.29, - "sl6": 11.4, - "sl7": 11.17 - }, - "sand": { - "sl1": 63.0, - "sl2": 63.0, - "sl3": 63.0, - "sl4": 56.8, - "sl5": 54.14, - "sl6": 52.2, - "sl7": 51.67 - }, - "site": { - "siteData": { - "componentID": 111631, - "distance": 26306.421, - "mapunitID": 17694, - "minCompDistance": 26306.4211, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Description_es": "Los Cambisoles Húmicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos tienen más materia orgánica en los horizontes superficiales.
Cuando el clima y el paisaje son favorables, estos suelos pueden ser productivos. ", - "Description_fr": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Description_ks": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 18.2, - "sl5": 18.29, - "sl6": 18.2, - "sl7": 17.67 - }, - "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 31.4, - "sl5": 31.71, - "sl6": 31.4, - "sl7": 31.5 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.5 - }, - "id": { - "component": "Ferric luvisols", - "name": "Ferric luvisols1", - "rank_loc": "8", - "score_loc": 0.011 - }, - "ph": { - "sl1": 6.6, - "sl2": 6.6, - "sl3": 6.6, - "sl4": 6.56, - "sl5": 6.6, - "sl6": 6.68, - "sl7": 6.77 - }, - "rock_fragments": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 12.0, - "sl5": 14.14, - "sl6": 12.6, - "sl7": 10.83 - }, - "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 41.8, - "sl5": 41.57, - "sl6": 42.0, - "sl7": 42.67 - }, - "site": { - "siteData": { - "componentID": 111336, - "distance": 36837.751, - "mapunitID": 17518, - "minCompDistance": 36837.7515, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 19.6, - "sl5": 19.0, - "sl6": 17.8, - "sl7": 17.67 - }, - "clay": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0, - "sl4": 39.0, - "sl5": 39.57, - "sl6": 40.0, - "sl7": 40.33 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.4, - "sl5": 0.29, - "sl6": 0.2, - "sl7": 0.17 - }, - "id": { - "component": "Calcic luvisols", - "name": "Calcic luvisols", - "rank_loc": "9", - "score_loc": 0.011 - }, - "ph": { - "sl1": 6.1, - "sl2": 6.1, - "sl3": 6.1, - "sl4": 6.18, - "sl5": 6.2, - "sl6": 6.2, - "sl7": 6.28 - }, - "rock_fragments": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 9.4, - "sl5": 11.29, - "sl6": 16.4, - "sl7": 19.5 - }, - "sand": { - "sl1": 33.0, - "sl2": 33.0, - "sl3": 33.0, - "sl4": 31.4, - "sl5": 31.57, - "sl6": 32.4, - "sl7": 32.33 - }, - "site": { - "siteData": { - "componentID": 111218, - "distance": 52061.241, - "mapunitID": 17457, - "minCompDistance": 52061.2413, - "share": 70, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", - "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 12.2, - "sl5": 12.43, - "sl6": 13.0, - "sl7": 13.33 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 22.8, - "sl5": 23.29, - "sl6": 23.4, - "sl7": 23.17 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 - }, - "id": { - "component": "Gleyic solonchaks", - "name": "Gleyic solonchaks1", - "rank_loc": "10", - "score_loc": 0.011 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7, - "sl4": 6.9, - "sl5": 6.96, - "sl6": 7.06, - "sl7": 7.13 - }, - "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 8.6, - "sl5": 10.14, - "sl6": 10.8, - "sl7": 12.17 - }, - "sand": { - "sl1": 61.0, - "sl2": 61.0, - "sl3": 61.0, - "sl4": 58.6, - "sl5": 58.43, - "sl6": 58.2, - "sl7": 58.5 - }, - "site": { - "siteData": { - "componentID": 111319, - "distance": 53068.322, - "mapunitID": 17507, - "minCompDistance": 53068.3217, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", - "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", - "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 39.8, - "sl5": 40.0, - "sl6": 39.8, - "sl7": 39.5 - }, - "clay": { - "sl1": 52.0, - "sl2": 52.0, - "sl3": 52.0, - "sl4": 54.6, - "sl5": 55.14, - "sl6": 55.4, - "sl7": 54.67 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.83 - }, - "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols1", - "rank_loc": "11", - "score_loc": 0.011 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7, - "sl4": 6.78, - "sl5": 6.84, - "sl6": 6.94, - "sl7": 7.05 - }, - "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 3.6, - "sl5": 3.71, - "sl6": 4.0, - "sl7": 4.0 - }, - "sand": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 19.8, - "sl5": 19.71, - "sl6": 19.8, - "sl7": 20.17 - }, - "site": { - "siteData": { - "componentID": 111337, - "distance": 70615.69, - "mapunitID": 17519, - "minCompDistance": 70615.6896, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " - } - }, - "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 37.4, - "sl5": 36.0, - "sl6": 33.2, - "sl7": 32.0 - }, - "clay": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 42.4, - "sl5": 40.14, - "sl6": 36.4, - "sl7": 34.33 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.67 - }, - "id": { - "component": "Eutric gleysols", - "name": "Eutric gleysols", - "rank_loc": "12", - "score_loc": 0.011 - }, - "ph": { - "sl1": 7.6, - "sl2": 7.6, - "sl3": 7.6, - "sl4": 7.76, - "sl5": 7.83, - "sl6": 7.94, - "sl7": 8.02 - }, - "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 21.8, - "sl5": 24.0, - "sl6": 22.8, - "sl7": 22.83 - }, - "sand": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 29.4, - "sl5": 30.43, - "sl6": 32.4, - "sl7": 33.5 - }, - "site": { - "siteData": { - "componentID": 111314, - "distance": 95128.611, - "mapunitID": 17504, - "minCompDistance": 95128.6114, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", - "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " - } - }, - "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Clay loam", - "sl7": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 21.6, - "sl5": 20.29, - "sl6": 18.8, - "sl7": 18.17 - }, - "clay": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 34.4, - "sl5": 34.14, - "sl6": 33.6, - "sl7": 33.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.5 - }, - "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.03 - }, - "ph": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.06, - "sl5": 5.09, - "sl6": 5.12, - "sl7": 5.13 - }, - "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 10.8, - "sl5": 11.14, - "sl6": 14.0, - "sl7": 16.17 - }, - "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 38.2, - "sl5": 38.57, - "sl6": 39.0, + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.2, + "sl5": 39.14, + "sl6": 39.6, "sl7": 39.33 }, "site": { "siteData": { - "componentID": 111264, - "distance": 72257.485, - "mapunitID": 17476, - "minCompDistance": 45915.6746, - "share": 30, + "componentID": 111218, + "distance": 52061.241, + "mapunitID": 17457, + "minCompDistance": 52061.2413, + "share": 70, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " } }, "texture": { @@ -1325,193 +425,93 @@ "sl7": 120 }, "cec": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 40.0, - "sl5": 40.14, - "sl6": 40.2, - "sl7": 40.17 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 }, "clay": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 55.8, - "sl5": 55.86, - "sl6": 55.6, - "sl7": 55.17 + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 28.4, + "sl5": 28.86, + "sl6": 28.6, + "sl7": 27.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.83 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.015 + "component": "Chromic luvisols", + "name": "Chromic luvisols1", + "rank_loc": "5", + "score_loc": 0.011 }, "ph": { - "sl1": 7.3, - "sl2": 7.3, - "sl3": 7.3, - "sl4": 7.46, - "sl5": 7.53, - "sl6": 7.58, - "sl7": 7.62 + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.36, + "sl5": 8.37, + "sl6": 8.38, + "sl7": 8.38 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.6, - "sl5": 2.71, - "sl6": 3.0, - "sl7": 3.0 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 18.0, + "sl5": 21.29, + "sl6": 26.4, + "sl7": 28.17 }, "sand": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 20.2, - "sl5": 20.0, - "sl6": 20.0, - "sl7": 20.17 - }, - "site": { - "siteData": { - "componentID": 111208, - "distance": 36128.047, - "mapunitID": 17453, - "minCompDistance": 9468.4741, - "share": 30, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " - } - }, - "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 39.8, + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 40.0, "sl5": 40.0, - "sl6": 39.8, - "sl7": 39.5 - }, - "clay": { - "sl1": 52.0, - "sl2": 52.0, - "sl3": 52.0, - "sl4": 54.6, - "sl5": 55.14, - "sl6": 55.4, - "sl7": 54.67 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.83 - }, - "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols3", - "rank_loc": "Not Displayed", - "score_loc": 0.015 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7, - "sl4": 6.78, - "sl5": 6.84, - "sl6": 6.94, - "sl7": 7.05 - }, - "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 3.6, - "sl5": 3.71, - "sl6": 4.0, - "sl7": 4.0 - }, - "sand": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 19.8, - "sl5": 19.71, - "sl6": 19.8, - "sl7": 20.17 + "sl6": 40.4, + "sl7": 41.0 }, "site": { "siteData": { - "componentID": 111216, - "distance": 41935.929, - "mapunitID": 17456, - "minCompDistance": 9468.4741, - "share": 30, + "componentID": 111097, + "distance": 14199.569, + "mapunitID": 17389, + "minCompDistance": 14199.5688, + "share": 25, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1525,93 +525,93 @@ "sl7": 120 }, "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 7.8, - "sl5": 8.29, - "sl6": 9.0, - "sl7": 9.17 - }, - "clay": { "sl1": 16.0, "sl2": 16.0, "sl3": 16.0, - "sl4": 18.4, - "sl5": 19.71, - "sl6": 21.2, - "sl7": 21.67 + "sl4": 16.4, + "sl5": 16.14, + "sl6": 16.0, + "sl7": 15.83 }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.0, + "sl5": 20.0, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols4", - "rank_loc": "Not Displayed", - "score_loc": 0.015 + "component": "Dystric regosols", + "name": "Dystric regosols", + "rank_loc": "6", + "score_loc": 0.009 }, "ph": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.06, - "sl5": 6.07, - "sl6": 6.08, - "sl7": 6.03 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.2, + "sl5": 8.2, + "sl6": 8.2, + "sl7": 8.2 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.4, - "sl5": 6.29, - "sl6": 6.0, - "sl7": 5.83 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.2, + "sl5": 5.0, + "sl6": 5.2, + "sl7": 5.33 }, "sand": { - "sl1": 72.0, - "sl2": 72.0, - "sl3": 72.0, - "sl4": 69.6, - "sl5": 68.43, - "sl6": 67.0, - "sl7": 66.67 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.6, + "sl5": 39.86, + "sl6": 39.8, + "sl7": 39.67 }, "site": { "siteData": { - "componentID": 116199, - "distance": 74794.646, - "mapunitID": 27168, - "minCompDistance": 9468.4741, - "share": 20, + "componentID": 111300, + "distance": 3832.725, + "mapunitID": 17496, + "minCompDistance": 3832.7247, + "share": 85, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", + "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -1625,22 +625,22 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 9.4, - "sl5": 10.29, - "sl6": 11.6, - "sl7": 12.33 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 }, "clay": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 19.0, - "sl5": 22.0, - "sl6": 25.4, - "sl7": 26.67 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 }, "ec": { "sl1": 1.0, @@ -1652,63 +652,63 @@ "sl7": 1.0 }, "id": { - "component": "Chromic cambisols", - "name": "Chromic cambisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.013 + "component": "Calcaric fluvisols", + "name": "Calcaric fluvisols", + "rank_loc": "7", + "score_loc": 0.008 }, "ph": { "sl1": 6.5, "sl2": 6.5, "sl3": 6.5, - "sl4": 6.44, - "sl5": 6.43, - "sl6": 6.4, - "sl7": 6.4 + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 }, "rock_fragments": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.43, - "sl6": 5.6, - "sl7": 5.17 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 }, "sand": { "sl1": 67.0, "sl2": 67.0, "sl3": 67.0, - "sl4": 63.2, - "sl5": 60.43, - "sl6": 56.8, - "sl7": 55.0 + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 }, "site": { "siteData": { - "componentID": 111117, - "distance": 72048.113, - "mapunitID": 17400, - "minCompDistance": 54718.5415, - "share": 100, + "componentID": 111096, + "distance": 14199.569, + "mapunitID": 17389, + "minCompDistance": 14199.5688, + "share": 75, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", - "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { "sl1": "Sandy loam", "sl2": "Sandy loam", "sl3": "Sandy loam", - "sl4": "Sandy loam", + "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", "sl7": "Sandy clay loam" @@ -1725,193 +725,93 @@ "sl7": 120 }, "cec": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 41.0, - "sl5": 41.0, - "sl6": 41.0, - "sl7": 40.5 - }, - "clay": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 56.8, - "sl5": 57.14, - "sl6": 57.0, - "sl7": 56.5 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.67 - }, - "id": { - "component": "Chromic cambisols", - "name": "Chromic cambisols3", - "rank_loc": "Not Displayed", - "score_loc": 0.013 - }, - "ph": { - "sl1": 6.8, - "sl2": 6.8, - "sl3": 6.8, - "sl4": 7.02, - "sl5": 7.13, - "sl6": 7.26, - "sl7": 7.33 - }, - "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.0, - "sl5": 4.14, - "sl6": 4.2, - "sl7": 4.0 - }, - "sand": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 12.4, - "sl5": 12.29, - "sl6": 12.4, - "sl7": 12.5 - }, - "site": { - "siteData": { - "componentID": 111267, - "distance": 73282.727, - "mapunitID": 17478, - "minCompDistance": 54718.5415, - "share": 40, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", - "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " - } - }, - "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 16.0, - "sl5": 16.0, - "sl6": 16.0, - "sl7": 15.83 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.2, + "sl5": 18.29, + "sl6": 18.2, + "sl7": 17.67 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 22.2, - "sl5": 23.0, - "sl6": 23.6, - "sl7": 23.67 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.4, + "sl5": 31.71, + "sl6": 31.4, + "sl7": 31.5 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.011 + "component": "Calcic vertisols", + "name": "Calcic vertisols", + "rank_loc": "8", + "score_loc": 0.008 }, "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4, - "sl4": 7.56, - "sl5": 7.64, - "sl6": 7.74, - "sl7": 7.82 + "sl1": 6.6, + "sl2": 6.6, + "sl3": 6.6, + "sl4": 6.56, + "sl5": 6.6, + "sl6": 6.68, + "sl7": 6.77 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 19.0, - "sl5": 21.0, - "sl6": 22.6, - "sl7": 22.83 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 12.0, + "sl5": 14.14, + "sl6": 12.6, + "sl7": 10.83 }, "sand": { - "sl1": 57.0, - "sl2": 57.0, - "sl3": 57.0, - "sl4": 55.0, - "sl5": 54.57, - "sl6": 54.2, - "sl7": 54.17 + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.8, + "sl5": 41.57, + "sl6": 42.0, + "sl7": 42.67 }, "site": { "siteData": { - "componentID": 111286, - "distance": 34446.462, - "mapunitID": 17488, - "minCompDistance": 9085.2006, - "share": 85, + "componentID": 111275, + "distance": 337.622, + "mapunitID": 17482, + "minCompDistance": 337.6222, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.", + "Description_es": "Los Vertisoles Cálcicos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles cálcicos son calcáreos en una capa del suelo por debajo de la superficie. ", + "Description_fr": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.", + "Description_ks": "Calcic Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Calcic Vertisols are calcareous in a soil layer below the surface.", + "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, sin embargo las características de la arcilla en este suelo pueden hacer que el manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", + "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", + "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1925,83 +825,83 @@ "sl7": 120 }, "cec": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 26.0, - "sl5": 25.43, - "sl6": 25.2, - "sl7": 24.17 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 19.6, + "sl5": 19.0, + "sl6": 17.8, + "sl7": 17.67 }, "clay": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 37.6, - "sl5": 38.71, - "sl6": 39.6, - "sl7": 39.0 + "sl1": 36.0, + "sl2": 36.0, + "sl3": 36.0, + "sl4": 39.0, + "sl5": 39.57, + "sl6": 40.0, + "sl7": 40.33 }, "ec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.2, - "sl5": 16.86, - "sl6": 17.4, - "sl7": 17.5 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols3", - "rank_loc": "Not Displayed", - "score_loc": 0.011 + "component": "Dystric cambisols", + "name": "Dystric cambisols1", + "rank_loc": "9", + "score_loc": 0.006 }, "ph": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 8.96, - "sl5": 8.96, - "sl6": 8.94, - "sl7": 9.0 + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.18, + "sl5": 6.2, + "sl6": 6.2, + "sl7": 6.28 }, "rock_fragments": { "sl1": 5.0, "sl2": 5.0, "sl3": 5.0, - "sl4": 11.4, - "sl5": 13.14, - "sl6": 10.4, - "sl7": 9.0 + "sl4": 9.4, + "sl5": 11.29, + "sl6": 16.4, + "sl7": 19.5 }, "sand": { - "sl1": 32.0, - "sl2": 32.0, - "sl3": 32.0, - "sl4": 30.6, - "sl5": 31.14, - "sl6": 30.8, - "sl7": 30.33 + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 31.4, + "sl5": 31.57, + "sl6": 32.4, + "sl7": 32.33 }, "site": { "siteData": { - "componentID": 111202, - "distance": 35027.212, - "mapunitID": 17450, - "minCompDistance": 9085.2006, - "share": 100, + "componentID": 111211, + "distance": 4944.944, + "mapunitID": 17454, + "minCompDistance": 4944.9441, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", + "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " } }, "texture": { @@ -2010,8 +910,8 @@ "sl3": "Clay loam", "sl4": "Clay loam", "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl6": "Unknown", + "sl7": "Unknown" } }, { @@ -2025,93 +925,93 @@ "sl7": 120 }, "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 16.6, - "sl5": 16.29, - "sl6": 16.4, - "sl7": 16.33 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 14.2, + "sl5": 13.14, + "sl6": 12.2, + "sl7": 11.83 }, "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 29.0, - "sl5": 28.57, - "sl6": 28.8, - "sl7": 29.0 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.4, + "sl5": 20.29, + "sl6": 20.2, + "sl7": 19.83 }, "ec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 15.2, - "sl5": 16.14, - "sl6": 16.8, - "sl7": 16.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols4", - "rank_loc": "Not Displayed", - "score_loc": 0.011 + "component": "Calcic solonchaks", + "name": "Calcic solonchaks", + "rank_loc": "10", + "score_loc": 0.005 }, "ph": { - "sl1": 8.5, - "sl2": 8.5, - "sl3": 8.5, - "sl4": 8.56, - "sl5": 8.51, - "sl6": 8.52, - "sl7": 8.52 + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.26, + "sl5": 5.27, + "sl6": 5.3, + "sl7": 5.32 }, "rock_fragments": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 21.6, - "sl5": 22.29, - "sl6": 17.8, - "sl7": 18.17 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.0, + "sl5": 21.57, + "sl6": 23.4, + "sl7": 23.83 }, "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 42.6, - "sl5": 43.0, - "sl6": 42.8, - "sl7": 42.5 + "sl1": 44.0, + "sl2": 44.0, + "sl3": 44.0, + "sl4": 44.0, + "sl5": 44.57, + "sl6": 45.0, + "sl7": 45.83 }, "site": { "siteData": { - "componentID": 111193, - "distance": 47856.589, - "mapunitID": 17448, - "minCompDistance": 9085.2006, - "share": 70, + "componentID": 111008, + "distance": 4355.807, + "mapunitID": 17338, + "minCompDistance": 4355.8073, + "share": 50, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Calcic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
Calcic Solonchaks are calcareous in a soil layer below the surface.", + "Description_es": "Los Solonchaks Cálcicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Los Solonchaks cálcicos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
Calcic Solonchaks are calcareous in a soil layer below the surface.", + "Description_ks": "Calcic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
Calcic Solonchaks are calcareous in a soil layer below the surface.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.
The soil pH in the upper soil layer will be high (> 7.0) ", + "Management_es": "Estos suelos son típicamente altos en sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.
El pH del suelo en la capa superior será alto (> 7,0).", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.
The soil pH in the upper soil layer will be high (> 7.0) ", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.
The soil pH in the upper soil layer will be high (> 7.0) " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -2125,93 +1025,93 @@ "sl7": 120 }, "cec": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 41.0, - "sl5": 41.0, - "sl6": 41.0, - "sl7": 40.5 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 16.0, + "sl5": 16.0, + "sl6": 16.0, + "sl7": 15.83 }, "clay": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 56.8, - "sl5": 57.14, - "sl6": 57.0, - "sl7": 56.5 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 22.2, + "sl5": 23.0, + "sl6": 23.6, + "sl7": 23.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols5", - "rank_loc": "Not Displayed", - "score_loc": 0.011 + "component": "Calcic chernozems", + "name": "Calcic chernozems", + "rank_loc": "11", + "score_loc": 0.003 }, "ph": { - "sl1": 6.8, - "sl2": 6.8, - "sl3": 6.8, - "sl4": 7.02, - "sl5": 7.13, - "sl6": 7.26, - "sl7": 7.33 + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4, + "sl4": 7.56, + "sl5": 7.64, + "sl6": 7.74, + "sl7": 7.82 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.0, - "sl5": 4.14, - "sl6": 4.2, - "sl7": 4.0 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 19.0, + "sl5": 21.0, + "sl6": 22.6, + "sl7": 22.83 }, "sand": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 12.4, - "sl5": 12.29, - "sl6": 12.4, - "sl7": 12.5 + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 55.0, + "sl5": 54.57, + "sl6": 54.2, + "sl7": 54.17 }, "site": { "siteData": { - "componentID": 111079, - "distance": 62588.145, - "mapunitID": 17378, - "minCompDistance": 9085.2006, - "share": 100, + "componentID": 116079, + "distance": 78421.421, + "mapunitID": 27135, + "minCompDistance": 78421.4209, + "share": 25, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Chernozems Cálcicos son suelos altamente productivos con buenas propiedades físicas y químicas.
Tienen una alta calidad de suelo y capas superficiales oscuras y ricas.
Los Chernozems Cálcicos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Management_en": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", + "Management_es": "Son, en general, suelos excelentes para la producción de cultivos.
Tienen una excelente porosidad y retención de agua, y son adecuados para una amplia gama de sistemas de producción de cultivos.
Algunos cultivos especiales pueden ser sensibles a los suelos con pH más alto, y puede ser necesario un suplemento de hierro.
Puede ser necesario el uso de fertilizantes.
Al tener un subsuelo calcáreo, pueden fijar el fósforo, por lo que puede ser necesaria una fertilización adecuada de P.", + "Management_fr": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", + "Management_ks": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -2225,93 +1125,93 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.4, - "sl5": 16.29, - "sl6": 16.0, - "sl7": 15.67 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.2, + "sl5": 12.43, + "sl6": 13.0, + "sl7": 13.33 }, "clay": { "sl1": 20.0, "sl2": 20.0, "sl3": 20.0, - "sl4": 21.2, - "sl5": 21.29, - "sl6": 21.0, - "sl7": 20.83 + "sl4": 22.8, + "sl5": 23.29, + "sl6": 23.4, + "sl7": 23.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.67 + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols6", - "rank_loc": "Not Displayed", - "score_loc": 0.011 + "component": "Calcaric regosols", + "name": "Calcaric regosols", + "rank_loc": "12", + "score_loc": 0.002 }, "ph": { - "sl1": 8.2, - "sl2": 8.2, - "sl3": 8.2, - "sl4": 8.22, - "sl5": 8.24, - "sl6": 8.26, - "sl7": 8.27 - }, - "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 5.0, - "sl5": 6.14, - "sl6": 7.4, - "sl7": 7.17 + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.9, + "sl5": 6.96, + "sl6": 7.06, + "sl7": 7.13 + }, + "rock_fragments": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 8.6, + "sl5": 10.14, + "sl6": 10.8, + "sl7": 12.17 }, "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 41.2, - "sl5": 41.14, - "sl6": 41.6, - "sl7": 41.83 + "sl1": 61.0, + "sl2": 61.0, + "sl3": 61.0, + "sl4": 58.6, + "sl5": 58.43, + "sl6": 58.2, + "sl7": 58.5 }, "site": { "siteData": { - "componentID": 116200, - "distance": 74794.646, - "mapunitID": 27168, - "minCompDistance": 9085.2006, - "share": 15, + "componentID": 110978, + "distance": 78521.447, + "mapunitID": 17323, + "minCompDistance": 78521.4474, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -2325,93 +1225,93 @@ "sl7": 120 }, "cec": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 21.6, - "sl5": 21.86, - "sl6": 22.2, - "sl7": 22.67 + "sl1": 52.0, + "sl2": 52.0, + "sl3": 52.0, + "sl4": 51.2, + "sl5": 50.86, + "sl6": 50.0, + "sl7": 49.17 }, "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 31.0, - "sl5": 31.43, - "sl6": 31.4, - "sl7": 31.33 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 54.6, + "sl5": 55.0, + "sl6": 54.2, + "sl7": 53.67 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.29, + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, "sl6": 1.2, - "sl7": 1.17 + "sl7": 1.5 }, "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols2", + "component": "Chromic cambisols", + "name": "Chromic cambisols3", "rank_loc": "Not Displayed", - "score_loc": 0.011 + "score_loc": 0.013 }, "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.42, - "sl5": 6.47, - "sl6": 6.58, - "sl7": 6.65 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.7, + "sl5": 7.8, + "sl6": 7.96, + "sl7": 8.05 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 15.8, - "sl5": 16.57, - "sl6": 17.8, - "sl7": 16.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.0, + "sl5": 6.0, + "sl6": 7.8, + "sl7": 7.83 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 39.2, - "sl5": 39.14, - "sl6": 39.6, - "sl7": 39.33 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 20.2, + "sl5": 20.14, + "sl6": 20.8, + "sl7": 21.17 }, "site": { "siteData": { - "componentID": 111641, - "distance": 63488.662, - "mapunitID": 17701, - "minCompDistance": 9861.4358, - "share": 100, + "componentID": 111267, + "distance": 73282.727, + "mapunitID": 17478, + "minCompDistance": 54718.5415, + "share": 40, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" } }, { @@ -2425,83 +1325,83 @@ "sl7": 120 }, "cec": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 41.0, - "sl5": 41.0, - "sl6": 41.0, - "sl7": 40.5 + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 37.4, + "sl5": 36.0, + "sl6": 33.2, + "sl7": 32.0 }, "clay": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 56.8, - "sl5": 57.14, - "sl6": 57.0, - "sl7": 56.5 + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 42.4, + "sl5": 40.14, + "sl6": 36.4, + "sl7": 34.33 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, "sl6": 0.6, "sl7": 0.67 }, "id": { - "component": "Ferric luvisols", - "name": "Ferric luvisols2", + "component": "Chromic cambisols", + "name": "Chromic cambisols2", "rank_loc": "Not Displayed", - "score_loc": 0.011 + "score_loc": 0.013 }, "ph": { - "sl1": 6.8, - "sl2": 6.8, - "sl3": 6.8, - "sl4": 7.02, - "sl5": 7.13, - "sl6": 7.26, - "sl7": 7.33 + "sl1": 7.6, + "sl2": 7.6, + "sl3": 7.6, + "sl4": 7.76, + "sl5": 7.83, + "sl6": 7.94, + "sl7": 8.02 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.0, - "sl5": 4.14, - "sl6": 4.2, - "sl7": 4.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 21.8, + "sl5": 24.0, + "sl6": 22.8, + "sl7": 22.83 }, "sand": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 12.4, - "sl5": 12.29, - "sl6": 12.4, - "sl7": 12.5 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 29.4, + "sl5": 30.43, + "sl6": 32.4, + "sl7": 33.5 }, "site": { "siteData": { - "componentID": 111335, - "distance": 41456.411, - "mapunitID": 17517, - "minCompDistance": 36837.7515, + "componentID": 111117, + "distance": 72048.113, + "mapunitID": 17400, + "minCompDistance": 54718.5415, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -2510,8 +1410,8 @@ "sl3": "Unknown", "sl4": "Unknown", "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -2525,93 +1425,93 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 11.2, - "sl5": 11.57, - "sl6": 12.2, - "sl7": 12.67 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.0, + "sl6": 6.4, + "sl7": 6.0 }, "clay": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 28.4, - "sl5": 29.86, - "sl6": 31.2, - "sl7": 31.83 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.0, + "sl5": 17.14, + "sl6": 16.0, + "sl7": 15.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.8, + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, "sl7": 1.0 }, "id": { - "component": "Ferric luvisols", - "name": "Ferric luvisols3", + "component": "Eutric cambisols", + "name": "Eutric cambisols3", "rank_loc": "Not Displayed", "score_loc": 0.011 }, "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 6.0, - "sl5": 6.03, - "sl6": 6.04, - "sl7": 6.08 + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.08, + "sl5": 5.13, + "sl6": 5.16, + "sl7": 5.18 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 7.2, - "sl5": 9.71, - "sl6": 10.0, - "sl7": 8.83 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 30.6, + "sl5": 31.14, + "sl6": 35.2, + "sl7": 36.67 }, "sand": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 34.2, - "sl5": 32.71, - "sl6": 31.0, - "sl7": 30.17 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 57.6, + "sl5": 58.71, + "sl6": 60.2, + "sl7": 60.17 }, "site": { "siteData": { - "componentID": 116201, - "distance": 74794.646, - "mapunitID": 27168, - "minCompDistance": 36837.7515, - "share": 15, + "componentID": 110986, + "distance": 78053.869, + "mapunitID": 17328, + "minCompDistance": 70615.6896, + "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Luvisoles Férricos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Ferric Luvisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, puede ser más adecuado para el pastoreo y/o los cultivos arbóreos.
Los suelos con una estructura poco desarrollada pueden verse favorecidos por la inclusión de cultivos de raíces profundas y perennes.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Soils with poorly developed structure may be further aided by the inclusion of deep rooted and perennial crops. " + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -2625,35 +1525,35 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 14.8, - "sl5": 14.57, - "sl6": 14.2, - "sl7": 14.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.6, + "sl5": 14.71, + "sl6": 15.0, + "sl7": 15.17 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 20.6, - "sl5": 20.86, - "sl6": 21.0, - "sl7": 20.83 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.6, + "sl5": 29.86, + "sl6": 30.6, + "sl7": 30.5 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 0.8, - "sl5": 0.71, - "sl6": 0.8, - "sl7": 0.83 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Gleyic solonchaks", - "name": "Gleyic solonchaks2", + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", "rank_loc": "Not Displayed", "score_loc": 0.011 }, @@ -2661,57 +1561,57 @@ "sl1": 6.4, "sl2": 6.4, "sl3": 6.4, - "sl4": 6.54, - "sl5": 6.6, - "sl6": 6.66, - "sl7": 6.7 + "sl4": 6.42, + "sl5": 6.44, + "sl6": 6.44, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 15.0, - "sl5": 16.57, - "sl6": 18.8, - "sl7": 19.17 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 9.29, + "sl6": 13.4, + "sl7": 12.5 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 40.8, - "sl5": 41.14, - "sl6": 41.8, - "sl7": 42.17 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 49.0, + "sl5": 47.71, + "sl6": 46.6, + "sl7": 46.67 }, "site": { "siteData": { - "componentID": 111103, - "distance": 60642.675, - "mapunitID": 17392, - "minCompDistance": 53068.3217, + "componentID": 111641, + "distance": 63488.662, + "mapunitID": 17701, + "minCompDistance": 9861.4358, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_es": "Los Solonchaks Gléyicos son suelos que contienen sales en la superficie del suelo o cerca de ella y que se forman en los desiertos o cerca de las costas.
Estos suelos están saturados con aguas subterráneas poco profundas a un metro de la superficie del suelo.", - "Description_fr": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Description_ks": "Gleyic Solonchaks are soils that contain salts at or near the soil surface that form in either deserts or close to coastlines.
These soils are saturated with shallow groundwater within one meter of the soil surface.", - "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy baja y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas.
Será necesario el drenaje de estos suelos, tanto para eliminar el agua estancada como para remediar los problemas de salinidad. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", - "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow.", - "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
Drainage of these soils will be needed, both to eliminate standing water and remediate salinity issues.
These soils are not well suited for agriculture and are best used for grazing, or left fallow." + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -2805,13 +1705,213 @@ } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 17.0, + "sl5": 16.29, + "sl6": 15.6, + "sl7": 15.33 + }, + "clay": { + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.8, + "sl5": 30.14, + "sl6": 30.0, + "sl7": 29.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols3", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.02, + "sl5": 5.06, + "sl6": 5.12, + "sl7": 5.13 + }, + "rock_fragments": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.4, + "sl5": 14.43, + "sl6": 15.2, + "sl7": 16.67 + }, + "sand": { + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 42.6, + "sl5": 42.57, + "sl6": 42.6, + "sl7": 43.0 + }, + "site": { + "siteData": { + "componentID": 110979, + "distance": 78521.447, + "mapunitID": 17323, + "minCompDistance": 14199.5688, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 + }, + "id": { + "component": "Chromic luvisols", + "name": "Chromic luvisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.011 + }, + "ph": { + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 + }, + "site": { + "siteData": { + "componentID": 111328, + "distance": 67101.164, + "mapunitID": 17512, + "minCompDistance": 14199.5688, + "share": 65, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -2825,83 +1925,83 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 17.6, - "sl5": 17.86, - "sl6": 18.4, - "sl7": 18.83 + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 24.2, + "sl5": 23.0, + "sl6": 21.4, + "sl7": 20.5 }, "clay": { - "sl1": 33.0, - "sl2": 33.0, - "sl3": 33.0, - "sl4": 35.8, - "sl5": 36.71, - "sl6": 37.8, - "sl7": 38.5 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.6, + "sl5": 29.57, + "sl6": 28.8, + "sl7": 28.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.6, - "sl7": 0.67 + "sl4": 1.0, + "sl5": 1.29, + "sl6": 1.8, + "sl7": 2.0 }, "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols3", + "component": "Dystric cambisols", + "name": "Dystric cambisols2", "rank_loc": "Not Displayed", - "score_loc": 0.011 + "score_loc": 0.006 }, "ph": { - "sl1": 5.9, - "sl2": 5.9, - "sl3": 5.9, - "sl4": 5.96, - "sl5": 5.97, - "sl6": 6.02, - "sl7": 6.05 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.66, + "sl5": 7.76, + "sl6": 7.88, + "sl7": 7.95 }, "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 17.6, - "sl5": 17.14, - "sl6": 14.8, - "sl7": 15.83 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 6.2, + "sl5": 8.14, + "sl6": 10.4, + "sl7": 11.5 }, "sand": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 33.6, - "sl5": 33.29, - "sl6": 32.8, - "sl7": 31.83 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 28.4, + "sl5": 28.43, + "sl6": 29.2, + "sl7": 29.67 }, "site": { "siteData": { - "componentID": 110986, - "distance": 78053.869, - "mapunitID": 17328, - "minCompDistance": 70615.6896, - "share": 100, + "componentID": 111624, + "distance": 18090.354, + "mapunitID": 17691, + "minCompDistance": 4944.9441, + "share": 60, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", + "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " } }, "texture": { @@ -2923,352 +2023,244 @@ }, "soilRank": [ { - "component": "Eutric cambisols", - "componentData": "Data Complete", - "componentID": 110986, - "name": "Eutric cambisols3", - "rank_data": "1", + "component": "Calcic vertisols", + "componentData": "No Data", + "componentID": 111275, + "name": "Calcic vertisols", + "rank_data": "2", "rank_data_loc": "1", - "rank_loc": "Not Displayed", - "score_data": 0.769, + "rank_loc": "8", + "score_data": 0.647, "score_data_loc": 1.0, - "score_loc": 0.011 + "score_loc": 0.008 }, { - "component": "Ferric luvisols", + "component": "Calcic solonchaks", "componentData": "Data Complete", - "componentID": 111336, - "name": "Ferric luvisols1", - "rank_data": "2", + "componentID": 111008, + "name": "Calcic solonchaks", + "rank_data": "1", "rank_data_loc": "2", - "rank_loc": "8", - "score_data": 0.749, - "score_data_loc": 0.974, - "score_loc": 0.011 + "rank_loc": "10", + "score_data": 0.647, + "score_data_loc": 0.997, + "score_loc": 0.005 }, { - "component": "Chromic cambisols", + "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 111105, - "name": "Chromic cambisols1", + "componentID": 111641, + "name": "Calcaric cambisols2", "rank_data": "3", "rank_data_loc": "3", - "rank_loc": "4", - "score_data": 0.724, - "score_data_loc": 0.945, - "score_loc": 0.013 + "rank_loc": "Not Displayed", + "score_data": 0.605, + "score_data_loc": 0.94, + "score_loc": 0.011 }, { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 111101, - "name": "Eutric vertisols1", + "component": "Chromic luvisols", + "componentData": "Missing Data", + "componentID": 110979, + "name": "Chromic luvisols3", "rank_data": "4", "rank_data_loc": "4", - "rank_loc": "5", - "score_data": 0.724, - "score_data_loc": 0.942, + "rank_loc": "Not Displayed", + "score_data": 0.605, + "score_data_loc": 0.94, "score_loc": 0.011 }, { - "component": "Ferralic arenosols", + "component": "Dystric cambisols", "componentData": "Data Complete", - "componentID": 111264, - "name": "Ferralic arenosols2", - "rank_data": "8", + "componentID": 111624, + "name": "Dystric cambisols2", + "rank_data": "5", "rank_data_loc": "5", "rank_loc": "Not Displayed", - "score_data": 0.699, - "score_data_loc": 0.935, - "score_loc": 0.03 + "score_data": 0.605, + "score_data_loc": 0.934, + "score_loc": 0.006 }, { - "component": "Haplic lixisols", - "componentData": "Missing Data", - "componentID": 111240, - "name": "Haplic lixisols1", - "rank_data": "6", + "component": "Chromic cambisols", + "componentData": "Data Complete", + "componentID": 111267, + "name": "Chromic cambisols3", + "rank_data": "7", "rank_data_loc": "6", - "rank_loc": "3", - "score_data": 0.713, - "score_data_loc": 0.934, - "score_loc": 0.015 + "rank_loc": "Not Displayed", + "score_data": 0.592, + "score_data_loc": 0.924, + "score_loc": 0.013 }, { - "component": "Calcic luvisols", + "component": "Calcaric fluvisols", "componentData": "Data Complete", - "componentID": 111218, - "name": "Calcic luvisols", - "rank_data": "5", + "componentID": 111096, + "name": "Calcaric fluvisols", + "rank_data": "6", "rank_data_loc": "7", - "rank_loc": "9", - "score_data": 0.713, - "score_data_loc": 0.928, - "score_loc": 0.011 + "rank_loc": "7", + "score_data": 0.592, + "score_data_loc": 0.917, + "score_loc": 0.008 }, { - "component": "Calcaric cambisols", + "component": "Calcic luvisols", "componentData": "Data Complete", - "componentID": 111641, - "name": "Calcaric cambisols2", - "rank_data": "7", + "componentID": 111218, + "name": "Calcic luvisols", + "rank_data": "8", "rank_data_loc": "8", - "rank_loc": "Not Displayed", - "score_data": 0.699, - "score_data_loc": 0.91, + "rank_loc": "4", + "score_data": 0.509, + "score_data_loc": 0.794, "score_loc": 0.011 }, { - "component": "Humic cambisols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 111631, - "name": "Humic cambisols", + "componentID": 111337, + "name": "Eutric cambisols1", "rank_data": "9", "rank_data_loc": "9", - "rank_loc": "7", - "score_data": 0.674, - "score_data_loc": 0.878, + "rank_loc": "3", + "score_data": 0.509, + "score_data_loc": 0.794, "score_loc": 0.011 }, { - "component": "Eutric gleysols", - "componentData": "Missing Data", - "componentID": 111314, - "name": "Eutric gleysols", - "rank_data": "10", + "component": "Dystric regosols", + "componentData": "Data Complete", + "componentID": 111300, + "name": "Dystric regosols", + "rank_data": "12", "rank_data_loc": "10", - "rank_loc": "12", - "score_data": 0.657, - "score_data_loc": 0.857, - "score_loc": 0.011 + "rank_loc": "6", + "score_data": 0.346, + "score_data_loc": 0.542, + "score_loc": 0.009 }, { - "component": "Gleyic solonchaks", + "component": "Calcic chernozems", "componentData": "Data Complete", - "componentID": 111103, - "name": "Gleyic solonchaks2", + "componentID": 116079, + "name": "Calcic chernozems", "rank_data": "11", "rank_data_loc": "11", - "rank_loc": "Not Displayed", - "score_data": 0.594, - "score_data_loc": 0.776, - "score_loc": 0.011 + "rank_loc": "11", + "score_data": 0.346, + "score_data_loc": 0.533, + "score_loc": 0.003 }, { - "component": "Humic nitisols", - "componentData": "No Data", - "componentID": 111081, - "name": "Humic nitisols", - "rank_data": "12", + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 110978, + "name": "Calcaric regosols", + "rank_data": "10", "rank_data_loc": "12", - "rank_loc": "2", - "score_data": 0.124, - "score_data_loc": 0.189, - "score_loc": 0.024 + "rank_loc": "12", + "score_data": 0.346, + "score_data_loc": 0.532, + "score_loc": 0.002 }, { - "component": "Haplic lixisols", - "componentData": "Missing Data", - "componentID": 111208, - "name": "Haplic lixisols2", + "component": "Dystric cambisols", + "componentData": "Data Complete", + "componentID": 111211, + "name": "Dystric cambisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.713, - "score_data_loc": 0.934, - "score_loc": 0.015 + "rank_loc": "9", + "score_data": 0.605, + "score_data_loc": 0.933, + "score_loc": 0.006 }, { - "component": "Haplic lixisols", + "component": "Chromic luvisols", "componentData": "Data Complete", - "componentID": 111216, - "name": "Haplic lixisols3", + "componentID": 111097, + "name": "Chromic luvisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.713, - "score_data_loc": 0.934, - "score_loc": 0.015 + "rank_loc": "5", + "score_data": 0.592, + "score_data_loc": 0.921, + "score_loc": 0.011 }, { "component": "Chromic cambisols", "componentData": "Data Complete", - "componentID": 111267, - "name": "Chromic cambisols3", + "componentID": 111105, + "name": "Chromic cambisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.713, - "score_data_loc": 0.931, + "rank_loc": "1", + "score_data": 0.588, + "score_data_loc": 0.918, "score_loc": 0.013 }, { - "component": "Eutric cambisols", - "componentData": "Data Complete", - "componentID": 111337, - "name": "Eutric cambisols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "11", - "score_data": 0.713, - "score_data_loc": 0.928, - "score_loc": 0.011 - }, - { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 111079, - "name": "Eutric vertisols5", + "component": "Chromic cambisols", + "componentData": "Missing Data", + "componentID": 111117, + "name": "Chromic cambisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.713, - "score_data_loc": 0.928, - "score_loc": 0.011 + "score_data": 0.533, + "score_data_loc": 0.835, + "score_loc": 0.013 }, { - "component": "Ferric luvisols", - "componentData": "Data Complete", - "componentID": 111335, - "name": "Ferric luvisols2", + "component": "Calcaric cambisols", + "componentData": "Missing Data", + "componentID": 111282, + "name": "Calcaric cambisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.713, - "score_data_loc": 0.928, + "rank_loc": "2", + "score_data": 0.509, + "score_data_loc": 0.794, "score_loc": 0.011 }, { - "component": "Eutric cambisols", + "component": "Chromic luvisols", "componentData": "Data Complete", - "componentID": 110980, - "name": "Eutric cambisols2", + "componentID": 111328, + "name": "Chromic luvisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.699, - "score_data_loc": 0.91, + "score_data": 0.509, + "score_data_loc": 0.794, "score_loc": 0.011 }, { - "component": "Ferric luvisols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 116201, - "name": "Ferric luvisols3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.699, - "score_data_loc": 0.91, - "score_loc": 0.011 - }, - { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 111193, - "name": "Eutric vertisols4", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.667, - "score_data_loc": 0.869, - "score_loc": 0.011 - }, - { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 111202, - "name": "Eutric vertisols3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.618, - "score_data_loc": 0.806, - "score_loc": 0.011 - }, - { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 116200, - "name": "Eutric vertisols6", + "componentID": 110986, + "name": "Eutric cambisols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.594, - "score_data_loc": 0.776, + "score_data": 0.509, + "score_data_loc": 0.794, "score_loc": 0.011 }, { - "component": "Haplic lixisols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 116199, - "name": "Haplic lixisols4", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.585, - "score_data_loc": 0.77, - "score_loc": 0.015 - }, - { - "component": "Calcaric cambisols", - "componentData": "Missing Data", - "componentID": 111282, - "name": "Calcaric cambisols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "6", - "score_data": 0.589, - "score_data_loc": 0.769, - "score_loc": 0.011 - }, - { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 111286, - "name": "Eutric vertisols2", + "componentID": 110980, + "name": "Eutric cambisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.589, - "score_data_loc": 0.769, - "score_loc": 0.011 - }, - { - "component": "Gleyic solonchaks", - "componentData": "Missing Data", - "componentID": 111319, - "name": "Gleyic solonchaks1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "10", - "score_data": 0.589, - "score_data_loc": 0.769, + "score_data": 0.165, + "score_data_loc": 0.269, "score_loc": 0.011 - }, - { - "component": "Chromic cambisols", - "componentData": "Missing Data", - "componentID": 111117, - "name": "Chromic cambisols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.585, - "score_data_loc": 0.767, - "score_loc": 0.013 - }, - { - "component": "Ferralic arenosols", - "componentData": "Data Complete", - "componentID": 111242, - "name": "Ferralic arenosols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "1", - "score_data": 0.243, - "score_data_loc": 0.351, - "score_loc": 0.03 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json index 2b33b56..12f1151 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[-24.53333,33.36667].json @@ -25,164 +25,64 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.2, - "sl5": 12.71, - "sl6": 12.4, - "sl7": 12.5 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 }, "clay": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 26.2, - "sl5": 25.57, - "sl6": 25.2, - "sl7": 25.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Salic fluvisols", - "name": "Salic fluvisols1", + "component": "Haplic solonetz", + "name": "Haplic solonetz1", "rank_loc": "1", - "score_loc": 0.091 + "score_loc": 0.064 }, "ph": { - "sl1": 8.4, - "sl2": 8.4, - "sl3": 8.4, - "sl4": 8.4, - "sl5": 8.41, - "sl6": 8.44, - "sl7": 8.45 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 }, "rock_fragments": { "sl1": 4.0, "sl2": 4.0, "sl3": 4.0, - "sl4": 6.0, - "sl5": 7.71, - "sl6": 10.4, - "sl7": 10.67 - }, - "sand": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 39.4, - "sl5": 40.43, - "sl6": 41.0, - "sl7": 41.5 - }, - "site": { - "siteData": { - "componentID": 113476, - "distance": 0.5, - "mapunitID": 18586, - "minCompDistance": 0.5004, - "share": 50, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", - "Description_es": "Los Fluvisoles Sálicos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles salinos tienen una alta salinidad en la parte superior del suelo.", - "Description_fr": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", - "Description_ks": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
La lixiviación con una fuente de agua de alta calidad (baja salinidad) será necesaria para desplazar las sales fuera de la zona de enraizamiento.
También se recomienda el uso de cultivos y variedades tolerantes a la sal.
Por último, es necesario gestionar los programas de fertilización para evitar la sobreaplicación y la acumulación de sales.", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 14.8, - "sl5": 13.71, - "sl6": 13.0, - "sl7": 12.67 - }, - "clay": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 26.8, - "sl5": 26.0, - "sl6": 25.2, - "sl7": 25.0 - }, - "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 - }, - "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz1", - "rank_loc": "2", - "score_loc": 0.064 - }, - "ph": { - "sl1": 8.5, - "sl2": 8.5, - "sl3": 8.5, - "sl4": 8.5, - "sl5": 8.5, - "sl6": 8.52, - "sl7": 8.53 - }, - "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 5.2, - "sl5": 7.14, - "sl6": 10.0, - "sl7": 8.83 + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 }, "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 41.0, - "sl5": 42.43, - "sl6": 43.4, - "sl7": 44.33 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 }, "site": { "siteData": { @@ -205,113 +105,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 15.0, - "sl5": 16.14, - "sl6": 17.2, - "sl7": 17.33 - }, - "clay": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 21.6, - "sl5": 23.57, - "sl6": 25.2, - "sl7": 25.17 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 - }, - "id": { - "component": "Mollic fluvisols", - "name": "Mollic fluvisols", - "rank_loc": "3", - "score_loc": 0.055 - }, - "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.86, - "sl5": 7.09, - "sl6": 7.36, - "sl7": 7.47 - }, - "rock_fragments": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0, - "sl5": 5.29, - "sl6": 7.2, - "sl7": 9.0 - }, - "sand": { - "sl1": 63.0, - "sl2": 63.0, - "sl3": 63.0, - "sl4": 60.0, - "sl5": 58.14, - "sl6": 56.4, - "sl7": 56.17 - }, - "site": { - "siteData": { - "componentID": 113477, - "distance": 0.5, - "mapunitID": 18586, - "minCompDistance": 0.5004, - "share": 30, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.", - "Description_es": "Los Fluvisoles Mólicos se encuentran principalmente en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles móllicos tienen una materia orgánica y nutrientes relativamente altos en los horizontes superficiales.", - "Description_fr": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.", - "Description_ks": "Mollic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Mollic Fluvisols have relatively higher organic matter and nutrients in surface horizons.", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -325,64 +125,64 @@ "sl7": 120 }, "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 19.2, - "sl5": 19.29, - "sl6": 19.0, - "sl7": 18.67 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.2, + "sl5": 2.86, + "sl6": 2.6, + "sl7": 2.5 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 26.0, - "sl5": 26.29, - "sl6": 25.6, - "sl7": 24.67 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.6, + "sl5": 5.71, + "sl6": 6.0, + "sl7": 6.67 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.8, - "sl5": 2.57, - "sl6": 3.8, - "sl7": 3.83 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Cambic arenosols", "name": "Cambic arenosols1", - "rank_loc": "4", + "rank_loc": "2", "score_loc": 0.055 }, "ph": { - "sl1": 8.3, - "sl2": 8.3, - "sl3": 8.3, - "sl4": 8.56, - "sl5": 8.63, - "sl6": 8.66, - "sl7": 8.65 + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.64, + "sl5": 5.63, + "sl6": 5.64, + "sl7": 5.63 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 5.0, - "sl5": 5.29, - "sl6": 7.4, - "sl7": 9.0 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 11.6, + "sl5": 11.86, + "sl6": 10.6, + "sl7": 9.33 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 44.6, - "sl5": 44.57, - "sl6": 45.4, - "sl7": 46.17 + "sl1": 84.0, + "sl2": 84.0, + "sl3": 84.0, + "sl4": 84.6, + "sl5": 84.71, + "sl6": 84.2, + "sl7": 82.33 }, "site": { "siteData": { @@ -405,13 +205,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -425,92 +225,92 @@ "sl7": 120 }, "cec": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 21.4, - "sl5": 21.0, - "sl6": 20.2, - "sl7": 18.67 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 }, "clay": { - "sl1": 32.0, - "sl2": 32.0, - "sl3": 32.0, - "sl4": 33.4, - "sl5": 32.86, - "sl6": 31.4, - "sl7": 29.83 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Eutric fluvisols", - "name": "Eutric fluvisols1", - "rank_loc": "5", + "component": "Eutric cambisols", + "name": "Eutric cambisols", + "rank_loc": "3", "score_loc": 0.045 }, "ph": { "sl1": 6.5, "sl2": 6.5, "sl3": 6.5, - "sl4": 6.52, - "sl5": 6.56, - "sl6": 6.62, - "sl7": 6.7 + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 17.6, - "sl5": 16.43, - "sl6": 17.4, + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, "sl7": 18.0 }, "sand": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 40.0, - "sl5": 41.29, - "sl6": 43.8, - "sl7": 45.33 + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 }, "site": { "siteData": { - "componentID": 113479, - "distance": 0.5, - "mapunitID": 18586, - "minCompDistance": 0.5004, - "share": 10, + "componentID": 113157, + "distance": 91670.472, + "mapunitID": 18461, + "minCompDistance": 91670.4723, + "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", - "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", "sl7": "Sandy clay loam" } }, @@ -525,93 +325,93 @@ "sl7": 120 }, "cec": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.0, - "sl5": 4.0, - "sl6": 4.0, - "sl7": 4.0 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 19.2, + "sl5": 19.29, + "sl6": 19.0, + "sl7": 18.67 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 5.8, - "sl5": 5.57, - "sl6": 5.4, - "sl7": 5.33 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 26.0, + "sl5": 26.29, + "sl6": 25.6, + "sl7": 24.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 }, "id": { - "component": "Eutric cambisols", - "name": "Eutric cambisols", - "rank_loc": "6", + "component": "Eutric fluvisols", + "name": "Eutric fluvisols1", + "rank_loc": "4", "score_loc": 0.045 }, "ph": { - "sl1": 6.9, - "sl2": 6.9, - "sl3": 6.9, - "sl4": 6.82, - "sl5": 6.8, - "sl6": 6.8, - "sl7": 6.82 + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.56, + "sl5": 8.63, + "sl6": 8.66, + "sl7": 8.65 }, "rock_fragments": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 14.4, - "sl5": 16.57, - "sl6": 21.2, - "sl7": 20.67 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.4, + "sl7": 9.0 }, "sand": { - "sl1": 89.0, - "sl2": 89.0, - "sl3": 89.0, - "sl4": 89.2, - "sl5": 89.29, - "sl6": 89.2, - "sl7": 89.17 + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 44.6, + "sl5": 44.57, + "sl6": 45.4, + "sl7": 46.17 }, "site": { "siteData": { - "componentID": 113157, - "distance": 91670.472, - "mapunitID": 18461, - "minCompDistance": 91670.4723, - "share": 15, + "componentID": 113479, + "distance": 0.5, + "mapunitID": 18586, + "minCompDistance": 0.5004, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { - "sl1": "Sand", - "sl2": "Sand", - "sl3": "Sand", - "sl4": "Sand", - "sl5": "Sand", - "sl6": "Sand", - "sl7": "Sand" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -654,7 +454,7 @@ "id": { "component": "Ferralic arenosols", "name": "Ferralic arenosols1", - "rank_loc": "7", + "rank_loc": "5", "score_loc": 0.039 }, "ph": { @@ -725,93 +525,93 @@ "sl7": 120 }, "cec": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 18.4, - "sl5": 18.14, - "sl6": 17.6, - "sl7": 17.5 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.0, + "sl7": 4.0 }, "clay": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 32.2, - "sl5": 32.14, - "sl6": 31.6, - "sl7": 31.33 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 5.8, + "sl5": 5.57, + "sl6": 5.4, + "sl7": 5.33 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Eutric planosols", - "name": "Eutric planosols1", - "rank_loc": "8", + "component": "Haplic arenosols", + "name": "Haplic arenosols", + "rank_loc": "6", "score_loc": 0.036 }, "ph": { - "sl1": 6.1, - "sl2": 6.1, - "sl3": 6.1, - "sl4": 6.24, - "sl5": 6.3, - "sl6": 6.38, - "sl7": 6.43 + "sl1": 6.9, + "sl2": 6.9, + "sl3": 6.9, + "sl4": 6.82, + "sl5": 6.8, + "sl6": 6.8, + "sl7": 6.82 }, "rock_fragments": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 11.6, - "sl5": 9.86, - "sl6": 10.2, - "sl7": 10.33 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 14.4, + "sl5": 16.57, + "sl6": 21.2, + "sl7": 20.67 }, "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 36.2, - "sl5": 36.86, - "sl6": 38.4, - "sl7": 38.83 + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 89.2, + "sl5": 89.29, + "sl6": 89.2, + "sl7": 89.17 }, "site": { "siteData": { - "componentID": 113053, - "distance": 0.0, - "mapunitID": 18428, - "minCompDistance": 0.0, - "share": 20, + "componentID": 113413, + "distance": 70158.54, + "mapunitID": 18564, + "minCompDistance": 70158.5404, + "share": 80, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", - "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + "Description_en": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_es": "Los Arenosoles Háplicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.", + "Description_fr": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Description_ks": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" } }, { @@ -825,93 +625,93 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.6, - "sl5": 13.57, - "sl6": 13.0, - "sl7": 13.17 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.2, + "sl5": 5.43, + "sl6": 5.8, + "sl7": 5.17 }, "clay": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 18.8, - "sl5": 18.86, - "sl6": 18.8, - "sl7": 18.83 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 6.0, + "sl5": 6.71, + "sl6": 7.0, + "sl7": 6.67 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Haplic arenosols", - "name": "Haplic arenosols", - "rank_loc": "9", + "component": "Eutric planosols", + "name": "Eutric planosols1", + "rank_loc": "7", "score_loc": 0.036 }, "ph": { - "sl1": 7.5, - "sl2": 7.5, - "sl3": 7.5, - "sl4": 7.62, - "sl5": 7.66, - "sl6": 7.68, - "sl7": 7.7 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.36, + "sl5": 6.47, + "sl6": 6.62, + "sl7": 6.5 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.57, - "sl6": 4.4, - "sl7": 5.5 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 10.4, + "sl5": 11.0, + "sl6": 10.0, + "sl7": 8.83 }, "sand": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 54.2, - "sl5": 54.14, - "sl6": 54.6, - "sl7": 55.0 + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 87.8, + "sl5": 86.86, + "sl6": 86.6, + "sl7": 87.0 }, "site": { "siteData": { - "componentID": 113413, - "distance": 70158.54, - "mapunitID": 18564, - "minCompDistance": 70158.5404, - "share": 80, + "componentID": 113053, + "distance": 0.0, + "mapunitID": 18428, + "minCompDistance": 0.0, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", - "Description_es": "Los Arenosoles Háplicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.", - "Description_fr": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", - "Description_ks": "Haplic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -925,64 +725,64 @@ "sl7": 120 }, "cec": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.8, - "sl5": 16.0, - "sl6": 15.8, - "sl7": 15.67 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 8.8, + "sl5": 10.0, + "sl6": 10.8, + "sl7": 11.33 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 20.8, - "sl5": 21.14, - "sl6": 21.2, - "sl7": 21.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 18.4, + "sl5": 20.86, + "sl6": 22.2, + "sl7": 22.83 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.29, + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, "sl6": 1.2, - "sl7": 1.17 + "sl7": 1.33 }, "id": { "component": "Chromic luvisols", "name": "Chromic luvisols", - "rank_loc": "10", + "rank_loc": "8", "score_loc": 0.029 }, "ph": { - "sl1": 7.5, - "sl2": 7.5, - "sl3": 7.5, - "sl4": 7.64, - "sl5": 7.69, - "sl6": 7.72, - "sl7": 7.77 + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.36, + "sl5": 6.46, + "sl6": 6.64, + "sl7": 6.73 }, "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 12.4, - "sl5": 14.0, - "sl6": 16.0, - "sl7": 16.0 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 13.6, + "sl5": 11.29, + "sl6": 9.6, + "sl7": 8.83 }, "sand": { - "sl1": 52.0, - "sl2": 52.0, - "sl3": 52.0, - "sl4": 51.2, - "sl5": 50.86, - "sl6": 51.0, - "sl7": 51.0 + "sl1": 80.0, + "sl2": 80.0, + "sl3": 80.0, + "sl4": 72.0, + "sl5": 70.0, + "sl6": 69.0, + "sl7": 68.0 }, "site": { "siteData": { @@ -1005,13 +805,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", - "sl7": "Loam" + "sl7": "Sandy clay loam" } }, { @@ -1025,64 +825,64 @@ "sl7": 120 }, "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.29, - "sl6": 2.2, - "sl7": 2.0 - }, - "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.2, - "sl5": 6.43, - "sl6": 6.8, - "sl7": 7.0 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.0, + "sl5": 16.14, + "sl6": 16.6, + "sl7": 17.0 + }, + "clay": { + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 29.2, + "sl5": 30.14, + "sl6": 30.8, + "sl7": 31.33 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.86, + "sl6": 5.0, + "sl7": 5.17 }, "id": { "component": "Gleyic solonetz", "name": "Gleyic solonetz", - "rank_loc": "11", + "rank_loc": "9", "score_loc": 0.027 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.32, - "sl5": 5.34, - "sl6": 5.36, - "sl7": 5.37 + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 8.26, + "sl5": 8.41, + "sl6": 8.6, + "sl7": 8.7 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.2, - "sl5": 4.43, - "sl6": 4.6, + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.2, "sl7": 4.5 }, "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 86.8, - "sl5": 86.57, - "sl6": 86.2, - "sl7": 86.0 + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 38.4, + "sl5": 37.14, + "sl6": 35.6, + "sl7": 35.0 }, "site": { "siteData": { @@ -1105,13 +905,13 @@ } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1154,7 +954,7 @@ "id": { "component": "Haplic luvisols", "name": "Haplic luvisols", - "rank_loc": "12", + "rank_loc": "10", "score_loc": 0.027 }, "ph": { @@ -1225,93 +1025,293 @@ "sl7": 120 }, "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 8.8, - "sl5": 10.0, - "sl6": 10.8, - "sl7": 11.33 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 13.8, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 13.83 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.6, + "sl5": 20.14, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Gleyic arenosols", + "name": "Gleyic arenosols1", + "rank_loc": "11", + "score_loc": 0.018 + }, + "ph": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.14, + "sl5": 7.21, + "sl6": 7.34, + "sl7": 7.42 + }, + "rock_fragments": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.71, + "sl6": 17.8, + "sl7": 17.83 + }, + "sand": { + "sl1": 64.0, + "sl2": 64.0, + "sl3": 64.0, + "sl4": 61.2, + "sl5": 60.86, + "sl6": 60.8, + "sl7": 60.83 + }, + "site": { + "siteData": { + "componentID": 112872, + "distance": 14598.857, + "mapunitID": 18373, + "minCompDistance": 14598.8574, + "share": 15, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.", + "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.0, + "sl6": 15.8, + "sl7": 15.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.8, + "sl5": 21.14, + "sl6": 21.2, + "sl7": 21.0 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 + }, + "id": { + "component": "Haplic lixisols", + "name": "Haplic lixisols", + "rank_loc": "12", + "score_loc": 0.011 + }, + "ph": { + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.64, + "sl5": 7.69, + "sl6": 7.72, + "sl7": 7.77 + }, + "rock_fragments": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 12.4, + "sl5": 14.0, + "sl6": 16.0, + "sl7": 16.0 + }, + "sand": { + "sl1": 52.0, + "sl2": 52.0, + "sl3": 52.0, + "sl4": 51.2, + "sl5": 50.86, + "sl6": 51.0, + "sl7": 51.0 + }, + "site": { + "siteData": { + "componentID": 113445, + "distance": 78150.205, + "mapunitID": 18575, + "minCompDistance": 78150.2053, + "share": 25, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", + "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", + "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", + "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", + "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Sandy clay loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.6, + "sl5": 13.57, + "sl6": 13.0, + "sl7": 13.17 }, "clay": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 18.4, - "sl5": 20.86, - "sl6": 22.2, - "sl7": 22.83 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.8, + "sl5": 18.86, + "sl6": 18.8, + "sl7": 18.83 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.2, - "sl7": 1.33 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Salic fluvisols", - "name": "Salic fluvisols2", + "component": "Haplic solonetz", + "name": "Haplic solonetz2", "rank_loc": "Not Displayed", - "score_loc": 0.091 + "score_loc": 0.064 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.36, - "sl5": 6.46, - "sl6": 6.64, - "sl7": 6.73 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.62, + "sl5": 7.66, + "sl6": 7.68, + "sl7": 7.7 }, "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 13.6, - "sl5": 11.29, - "sl6": 9.6, - "sl7": 8.83 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.57, + "sl6": 4.4, + "sl7": 5.5 }, "sand": { - "sl1": 80.0, - "sl2": 80.0, - "sl3": 80.0, - "sl4": 72.0, - "sl5": 70.0, - "sl6": 69.0, - "sl7": 68.0 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.2, + "sl5": 54.14, + "sl6": 54.6, + "sl7": 55.0 }, "site": { "siteData": { - "componentID": 113242, - "distance": 39959.704, - "mapunitID": 18495, - "minCompDistance": 0.5004, - "share": 100, + "componentID": 112902, + "distance": 86897.899, + "mapunitID": 18384, + "minCompDistance": 78150.2053, + "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", - "Description_es": "Los Fluvisoles Sálicos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles salinos tienen una alta salinidad en la parte superior del suelo.", - "Description_fr": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", - "Description_ks": "Salic Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Salic Fluvisols have high salinity in the upper portion of soil.", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
La lixiviación con una fuente de agua de alta calidad (baja salinidad) será necesaria para desplazar las sales fuera de la zona de enraizamiento.
También se recomienda el uso de cultivos y variedades tolerantes a la sal.
Por último, es necesario gestionar los programas de fertilización para evitar la sobreaplicación y la acumulación de sales.", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. ", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
Leaching with a high quality (low salinity) water source will be needed to move salts out of the rooting zone.
Use of salt tolerant crops and varieties is also recommended.
Last, management of fertilization programs to avoid overapplication and accumulation of salts is needed. " + "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", + "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", + "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", + "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", + "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", "sl4": "Sandy loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -1352,10 +1352,10 @@ "sl7": 0.0 }, "id": { - "component": "Haplic solonetz", - "name": "Haplic solonetz2", + "component": "Cambic arenosols", + "name": "Cambic arenosols2", "rank_loc": "Not Displayed", - "score_loc": 0.064 + "score_loc": 0.055 }, "ph": { "sl1": 5.7, @@ -1386,22 +1386,22 @@ }, "site": { "siteData": { - "componentID": 112902, - "distance": 86897.899, - "mapunitID": 18384, - "minCompDistance": 78150.2053, - "share": 35, + "componentID": 112938, + "distance": 45507.906, + "mapunitID": 18395, + "minCompDistance": 35390.0171, + "share": 85, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_es": "Los Solonetz Háplicos tienen subsuelos ricos en arcilla fuertemente estructurados con un alto nivel de sodio intercambiable.
La productividad de estos suelos depende de la profundidad de los horizontes superficiales por encima de estos subsuelos.", - "Description_fr": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Description_ks": "Haplic Solonetzs have strongly structured clay rich subsoils with high exchangeable sodium.
Productivity of these soils depends on the depth of surface horizons above these subsoils.", - "Management_en": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_es": "Es probable que tengan un alto nivel de sodio en los horizontes subsuperficiales, lo que da lugar a una mala estructura del suelo y a una mala infiltración.
Los suelos parecerán húmedos, pero las plantas se marchitarán.
Para mejorar el drenaje interno, debe aplicarse yeso para desplazar el sodio, seguido de una lixiviación con agua de mayor calidad para desplazar el sodio desplazado de la zona de enraizamiento.
Si los suelos pueden recuperarse mediante la aplicación de yeso y la lixiviación del sodio, pueden ser aptos para el pastoreo o el cultivo.
La selección de cultivos tolerantes al sodio también es una opción, y debería utilizarse para el mantenimiento.
El cultivo es más adecuado cuando estos suelos están situados en regiones templadas, y el suelo superficial es más rico en materia orgánica.", - "Management_fr": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. ", - "Management_ks": "These are likely to have high sodium in subsurface horizons which results in poor soil structure and poor infiltration.
The soils will appear wet, but plants will wilt.
To improve internal drainage, gypsum should be applied to displace the sodium, followed by leaching with higher quality water to move the displaced sodium from the rooting zone.
If the soils can be reclaimed by the application of gypsum and leaching of sodium, they may be suitable for grazing or cultivation.
Selection of sodium tolerant crops is also an option, and should be used for maintenance.
Cultivation is more suited when these soils are located in temperate regions, and the surface soil is higher in organic matter. " + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " } }, "texture": { @@ -1445,111 +1445,11 @@ "ec": { "sl1": 0.0, "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.83 - }, - "id": { - "component": "Cambic arenosols", - "name": "Cambic arenosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.055 - }, - "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 5.98, - "sl5": 6.11, - "sl6": 6.28, - "sl7": 6.42 - }, - "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 9.0, - "sl5": 10.14, - "sl6": 11.0, - "sl7": 11.5 - }, - "sand": { - "sl1": 58.0, - "sl2": 58.0, - "sl3": 58.0, - "sl4": 52.8, - "sl5": 49.57, - "sl6": 46.0, - "sl7": 44.33 - }, - "site": { - "siteData": { - "componentID": 112938, - "distance": 45507.906, - "mapunitID": 18395, - "minCompDistance": 35390.0171, - "share": 85, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", - "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 11.8, - "sl5": 12.14, - "sl6": 12.2, - "sl7": 12.17 - }, - "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 24.2, - "sl5": 25.43, - "sl6": 26.2, - "sl7": 26.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl3": 0.0, + "sl4": 0.2, + "sl5": 0.43, + "sl6": 0.6, + "sl7": 0.83 }, "id": { "component": "Eutric fluvisols", @@ -1558,31 +1458,31 @@ "score_loc": 0.045 }, "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.62, - "sl5": 6.66, - "sl6": 6.76, - "sl7": 6.83 + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.98, + "sl5": 6.11, + "sl6": 6.28, + "sl7": 6.42 }, "rock_fragments": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 12.0, - "sl5": 12.71, - "sl6": 16.0, - "sl7": 18.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.0, + "sl5": 10.14, + "sl6": 11.0, + "sl7": 11.5 }, "sand": { - "sl1": 67.0, - "sl2": 67.0, - "sl3": 67.0, - "sl4": 62.6, - "sl5": 61.71, - "sl6": 61.0, - "sl7": 61.17 + "sl1": 58.0, + "sl2": 58.0, + "sl3": 58.0, + "sl4": 52.8, + "sl5": 49.57, + "sl6": 46.0, + "sl7": 44.33 }, "site": { "siteData": { @@ -1611,7 +1511,7 @@ "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl7": "Clay loam" } }, { @@ -1625,31 +1525,31 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.0, + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.0, "sl5": 16.14, - "sl6": 16.6, - "sl7": 17.0 + "sl6": 17.2, + "sl7": 17.33 }, "clay": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 29.2, - "sl5": 30.14, - "sl6": 30.8, - "sl7": 31.33 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 21.6, + "sl5": 23.57, + "sl6": 25.2, + "sl7": 25.17 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.2, - "sl5": 3.86, - "sl6": 5.0, - "sl7": 5.17 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.8, + "sl5": 2.57, + "sl6": 3.8, + "sl7": 3.83 }, "id": { "component": "Ferralic arenosols", @@ -1658,31 +1558,31 @@ "score_loc": 0.039 }, "ph": { - "sl1": 7.9, - "sl2": 7.9, - "sl3": 7.9, - "sl4": 8.26, - "sl5": 8.41, - "sl6": 8.6, - "sl7": 8.7 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.86, + "sl5": 7.09, + "sl6": 7.36, + "sl7": 7.47 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 4.0, - "sl5": 4.0, - "sl6": 4.2, - "sl7": 4.5 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0, + "sl5": 5.29, + "sl6": 7.2, + "sl7": 9.0 }, "sand": { - "sl1": 42.0, - "sl2": 42.0, - "sl3": 42.0, - "sl4": 38.4, - "sl5": 37.14, - "sl6": 35.6, - "sl7": 35.0 + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 60.0, + "sl5": 58.14, + "sl6": 56.4, + "sl7": 56.17 }, "site": { "siteData": { @@ -1705,13 +1605,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -1725,93 +1625,193 @@ "sl7": 120 }, "cec": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 13.8, - "sl5": 14.0, - "sl6": 14.0, - "sl7": 13.83 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.8, + "sl7": 6.83 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 19.6, - "sl5": 20.14, - "sl6": 20.2, - "sl7": 20.17 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.2, + "sl5": 30.29, + "sl6": 33.2, + "sl7": 34.33 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Eutric planosols", + "name": "Eutric planosols2", + "rank_loc": "Not Displayed", + "score_loc": 0.036 + }, + "ph": { + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.12, + "sl5": 6.07, + "sl6": 6.02, + "sl7": 6.02 + }, + "rock_fragments": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.8, + "sl5": 10.43, + "sl6": 10.6, + "sl7": 10.5 + }, + "sand": { + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 60.2, + "sl5": 57.57, + "sl6": 54.8, + "sl7": 53.0 + }, + "site": { + "siteData": { + "componentID": 113443, + "distance": 78150.205, + "mapunitID": 18575, + "minCompDistance": 0.0, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", + "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + } + }, + "texture": { + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.14, + "sl6": 17.6, + "sl7": 17.5 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.2, + "sl5": 32.14, + "sl6": 31.6, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Eutric planosols", - "name": "Eutric planosols2", + "component": "Gleyic arenosols", + "name": "Gleyic arenosols2", "rank_loc": "Not Displayed", - "score_loc": 0.036 + "score_loc": 0.018 }, "ph": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 7.14, - "sl5": 7.21, - "sl6": 7.34, - "sl7": 7.42 + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.24, + "sl5": 6.3, + "sl6": 6.38, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.8, - "sl5": 16.71, - "sl6": 17.8, - "sl7": 17.83 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.6, + "sl5": 9.86, + "sl6": 10.2, + "sl7": 10.33 }, "sand": { - "sl1": 64.0, - "sl2": 64.0, - "sl3": 64.0, - "sl4": 61.2, - "sl5": 60.86, - "sl6": 60.8, - "sl7": 60.83 + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.2, + "sl5": 36.86, + "sl6": 38.4, + "sl7": 38.83 }, "site": { "siteData": { - "componentID": 113443, - "distance": 78150.205, - "mapunitID": 18575, - "minCompDistance": 0.0, - "share": 50, + "componentID": 113016, + "distance": 35390.017, + "mapunitID": 18417, + "minCompDistance": 14598.8574, + "share": 40, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Planosoles Éutricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren drenaje para la producción de cultivos.
Los Planosoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo.", - "Description_fr": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Eutric Planosols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_es": "Ubicados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requieren una fertilización adicional.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization." + "Description_en": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_es": "Los Arenosoles Gleyicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están saturados con aguas subterráneas poco profundas por encima de un metro.", + "Description_fr": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Description_ks": "Gleyic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are saturated with shallow groundwater above one meter.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación por aguas subterráneas puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
En estos suelos se puede conseguir un uso más eficiente del N por parte de los cultivos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Drainage of these soils may be needed.
However, since this is saturation from groundwater installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained the loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } } ] @@ -1823,220 +1823,220 @@ }, "soilRank": [ { - "component": "Salic fluvisols", + "component": "Cambic arenosols", "componentData": "Data Complete", - "componentID": 113242, - "name": "Salic fluvisols2", - "rank_data": "8", + "componentID": 113015, + "name": "Cambic arenosols1", + "rank_data": "1", "rank_data_loc": "1", - "rank_loc": "Not Displayed", + "rank_loc": "2", "score_data": 0.9, "score_data_loc": 1.0, - "score_loc": 0.091 + "score_loc": 0.055 }, { - "component": "Cambic arenosols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 112938, - "name": "Cambic arenosols2", - "rank_data": "1", + "componentID": 113157, + "name": "Eutric cambisols", + "rank_data": "3", "rank_data_loc": "2", - "rank_loc": "Not Displayed", + "rank_loc": "3", "score_data": 0.9, - "score_data_loc": 0.963, - "score_loc": 0.055 + "score_data_loc": 0.99, + "score_loc": 0.045 }, { - "component": "Mollic fluvisols", + "component": "Ferralic arenosols", "componentData": "Data Complete", - "componentID": 113477, - "name": "Mollic fluvisols", - "rank_data": "7", + "componentID": 113127, + "name": "Ferralic arenosols2", + "rank_data": "5", "rank_data_loc": "3", - "rank_loc": "3", + "rank_loc": "Not Displayed", "score_data": 0.9, - "score_data_loc": 0.963, - "score_loc": 0.055 + "score_data_loc": 0.983, + "score_loc": 0.039 }, { - "component": "Eutric fluvisols", + "component": "Eutric planosols", "componentData": "Data Complete", - "componentID": 113211, - "name": "Eutric fluvisols2", - "rank_data": "2", + "componentID": 113053, + "name": "Eutric planosols1", + "rank_data": "4", "rank_data_loc": "4", - "rank_loc": "Not Displayed", + "rank_loc": "7", "score_data": 0.9, - "score_data_loc": 0.954, - "score_loc": 0.045 + "score_data_loc": 0.981, + "score_loc": 0.036 }, { - "component": "Ferralic arenosols", + "component": "Haplic arenosols", "componentData": "Data Complete", - "componentID": 112871, - "name": "Ferralic arenosols1", - "rank_data": "4", + "componentID": 113413, + "name": "Haplic arenosols", + "rank_data": "8", "rank_data_loc": "5", - "rank_loc": "7", + "rank_loc": "6", "score_data": 0.9, - "score_data_loc": 0.947, - "score_loc": 0.039 + "score_data_loc": 0.981, + "score_loc": 0.036 }, { - "component": "Eutric planosols", - "componentData": "Missing Data", - "componentID": 113443, - "name": "Eutric planosols2", - "rank_data": "3", + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 112901, + "name": "Chromic luvisols", + "rank_data": "2", "rank_data_loc": "6", - "rank_loc": "Not Displayed", + "rank_loc": "8", "score_data": 0.9, - "score_data_loc": 0.945, - "score_loc": 0.036 + "score_data_loc": 0.974, + "score_loc": 0.029 }, { - "component": "Haplic arenosols", + "component": "Gleyic solonetz", "componentData": "Data Complete", - "componentID": 113413, - "name": "Haplic arenosols", - "rank_data": "6", + "componentID": 113054, + "name": "Gleyic solonetz", + "rank_data": "7", "rank_data_loc": "7", "rank_loc": "9", "score_data": 0.9, - "score_data_loc": 0.945, - "score_loc": 0.036 + "score_data_loc": 0.971, + "score_loc": 0.027 }, { - "component": "Gleyic solonetz", + "component": "Gleyic arenosols", "componentData": "Data Complete", - "componentID": 113054, - "name": "Gleyic solonetz", - "rank_data": "5", + "componentID": 112872, + "name": "Gleyic arenosols1", + "rank_data": "6", "rank_data_loc": "8", "rank_loc": "11", "score_data": 0.9, - "score_data_loc": 0.936, - "score_loc": 0.027 + "score_data_loc": 0.962, + "score_loc": 0.018 }, { "component": "Haplic solonetz", "componentData": "Data Complete", - "componentID": 112902, - "name": "Haplic solonetz2", + "componentID": 113444, + "name": "Haplic solonetz1", "rank_data": "11", "rank_data_loc": "9", - "rank_loc": "Not Displayed", + "rank_loc": "1", "score_data": 0.756, - "score_data_loc": 0.827, + "score_data_loc": 0.858, "score_loc": 0.064 }, - { - "component": "Eutric cambisols", - "componentData": "Data Complete", - "componentID": 113157, - "name": "Eutric cambisols", - "rank_data": "9", - "rank_data_loc": "10", - "rank_loc": "6", - "score_data": 0.756, - "score_data_loc": 0.808, - "score_loc": 0.045 - }, { "component": "Haplic luvisols", "componentData": "Data Complete", "componentID": 113128, "name": "Haplic luvisols", "rank_data": "10", + "rank_data_loc": "10", + "rank_loc": "10", + "score_data": 0.756, + "score_data_loc": 0.82, + "score_loc": 0.027 + }, + { + "component": "Haplic lixisols", + "componentData": "Missing Data", + "componentID": 113445, + "name": "Haplic lixisols", + "rank_data": "9", "rank_data_loc": "11", "rank_loc": "12", "score_data": 0.756, - "score_data_loc": 0.79, - "score_loc": 0.027 + "score_data_loc": 0.803, + "score_loc": 0.011 }, { - "component": "Chromic luvisols", + "component": "Eutric fluvisols", "componentData": "Data Complete", - "componentID": 112901, - "name": "Chromic luvisols", + "componentID": 113211, + "name": "Eutric fluvisols2", "rank_data": "12", "rank_data_loc": "12", - "rank_loc": "10", - "score_data": 0.576, - "score_data_loc": 0.611, - "score_loc": 0.029 + "rank_loc": "Not Displayed", + "score_data": 0.593, + "score_data_loc": 0.669, + "score_loc": 0.045 + }, + { + "component": "Eutric planosols", + "componentData": "Missing Data", + "componentID": 113443, + "name": "Eutric planosols2", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "Not Displayed", + "score_data": 0.9, + "score_data_loc": 0.981, + "score_loc": 0.036 }, { - "component": "Salic fluvisols", + "component": "Cambic arenosols", "componentData": "Data Complete", - "componentID": 113476, - "name": "Salic fluvisols1", + "componentID": 112938, + "name": "Cambic arenosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "1", - "score_data": 0.576, - "score_data_loc": 0.673, - "score_loc": 0.091 + "rank_loc": "Not Displayed", + "score_data": 0.756, + "score_data_loc": 0.848, + "score_loc": 0.055 }, { "component": "Haplic solonetz", "componentData": "Data Complete", - "componentID": 113444, - "name": "Haplic solonetz1", + "componentID": 112902, + "name": "Haplic solonetz2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "2", + "rank_loc": "Not Displayed", "score_data": 0.576, - "score_data_loc": 0.645, + "score_data_loc": 0.67, "score_loc": 0.064 }, { - "component": "Cambic arenosols", + "component": "Eutric fluvisols", "componentData": "Data Complete", - "componentID": 113015, - "name": "Cambic arenosols1", + "componentID": 113479, + "name": "Eutric fluvisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "4", "score_data": 0.576, - "score_data_loc": 0.636, - "score_loc": 0.055 + "score_data_loc": 0.651, + "score_loc": 0.045 }, { - "component": "Ferralic arenosols", + "component": "Gleyic arenosols", "componentData": "Data Complete", - "componentID": 113127, - "name": "Ferralic arenosols2", + "componentID": 113016, + "name": "Gleyic arenosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", "score_data": 0.576, - "score_data_loc": 0.62, - "score_loc": 0.039 + "score_data_loc": 0.622, + "score_loc": 0.018 }, { - "component": "Eutric fluvisols", + "component": "Ferralic arenosols", "componentData": "Data Complete", - "componentID": 113479, - "name": "Eutric fluvisols1", + "componentID": 112871, + "name": "Ferralic arenosols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "5", "score_data": 0.244, - "score_data_loc": 0.292, - "score_loc": 0.045 - }, - { - "component": "Eutric planosols", - "componentData": "Data Complete", - "componentID": 113053, - "name": "Eutric planosols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "8", - "score_data": 0.244, - "score_data_loc": 0.283, - "score_loc": 0.036 + "score_data_loc": 0.296, + "score_loc": 0.039 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json index 8d5a2f1..19331ed 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[15.73333,120.31667].json @@ -25,22 +25,22 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 11.0, - "sl5": 11.0, - "sl6": 11.0, - "sl7": 10.83 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 6.4, + "sl5": 6.29, + "sl6": 6.2, + "sl7": 6.17 }, "clay": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 37.6, - "sl5": 41.0, - "sl6": 44.2, - "sl7": 45.17 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 28.8, + "sl5": 31.14, + "sl6": 33.4, + "sl7": 34.33 }, "ec": { "sl1": 0.0, @@ -51,138 +51,38 @@ "sl6": 0.0, "sl7": 0.0 }, - "id": { - "component": "Haplic nitisols", - "name": "Haplic nitisols", - "rank_loc": "1", - "score_loc": 0.094 - }, - "ph": { - "sl1": 5.5, - "sl2": 5.5, - "sl3": 5.5, - "sl4": 5.36, - "sl5": 5.31, - "sl6": 5.28, - "sl7": 5.27 - }, - "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 13.2, - "sl5": 14.14, - "sl6": 13.0, - "sl7": 11.5 - }, - "sand": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 40.6, - "sl5": 38.0, - "sl6": 35.4, - "sl7": 34.67 - }, - "site": { - "siteData": { - "componentID": 141607, - "distance": 0.357, - "mapunitID": 4413, - "minCompDistance": 0.3573, - "share": 40, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", - "Description_es": "Los Nitisoles Háplicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes.", - "Description_fr": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", - "Description_ks": "Haplic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.", - "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", - "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la planta durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación de fertilizantes fosfatados en banda (directamente sobre la semilla o a un lado y abajo de la semilla), ayudarán a reducir la fijación de P.", - "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.", - "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation." - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Clay loam", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.0, - "sl5": 16.14, - "sl6": 16.6, - "sl7": 16.83 - }, - "clay": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 33.8, - "sl5": 35.57, - "sl6": 37.4, - "sl7": 38.33 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.5 - }, "id": { "component": "Gleyic cambisols", "name": "Gleyic cambisols", - "rank_loc": "2", + "rank_loc": "1", "score_loc": 0.071 }, "ph": { - "sl1": 5.7, - "sl2": 5.7, - "sl3": 5.7, - "sl4": 5.78, - "sl5": 5.83, - "sl6": 5.9, - "sl7": 5.93 + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.04, + "sl5": 5.03, + "sl6": 5.02, + "sl7": 5.02 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 7.6, - "sl5": 8.29, - "sl6": 8.0, - "sl7": 8.17 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 14.0 }, "sand": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 39.0, - "sl5": 37.57, - "sl6": 35.8, - "sl7": 35.0 + "sl1": 59.0, + "sl2": 59.0, + "sl3": 59.0, + "sl4": 54.4, + "sl5": 52.29, + "sl6": 50.2, + "sl7": 49.17 }, "site": { "siteData": { @@ -205,13 +105,13 @@ } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -225,93 +125,93 @@ "sl7": 120 }, "cec": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 41.6, - "sl5": 41.57, - "sl6": 41.2, - "sl7": 40.83 + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 21.6, + "sl5": 21.86, + "sl6": 22.2, + "sl7": 22.67 }, "clay": { - "sl1": 52.0, - "sl2": 52.0, - "sl3": 52.0, - "sl4": 54.6, - "sl5": 55.14, - "sl6": 55.2, - "sl7": 54.67 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 31.0, + "sl5": 31.43, + "sl6": 31.4, + "sl7": 31.33 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.83 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 }, "id": { - "component": "Vertisols", - "name": "Vertisols", - "rank_loc": "3", + "component": "Dystric cambisols", + "name": "Dystric cambisols", + "rank_loc": "2", "score_loc": 0.047 }, "ph": { - "sl1": 6.8, - "sl2": 6.8, - "sl3": 6.8, - "sl4": 6.88, - "sl5": 6.94, - "sl6": 7.04, - "sl7": 7.17 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.47, + "sl6": 6.58, + "sl7": 6.65 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.6, - "sl5": 4.71, - "sl6": 4.8, - "sl7": 5.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 15.8, + "sl5": 16.57, + "sl6": 17.8, + "sl7": 16.0 }, "sand": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 19.8, - "sl5": 19.71, - "sl6": 20.0, - "sl7": 20.33 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.2, + "sl5": 39.14, + "sl6": 39.6, + "sl7": 39.33 }, "site": { "siteData": { - "componentID": 142292, - "distance": 0.0, - "mapunitID": 4478, - "minCompDistance": 0.0, - "share": 5, + "componentID": 142153, + "distance": 9267.434, + "mapunitID": 4465, + "minCompDistance": 9267.4336, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", - "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", + "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -325,64 +225,64 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 10.8, - "sl5": 11.86, - "sl6": 13.0, - "sl7": 13.5 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 17.0, + "sl5": 16.29, + "sl6": 15.6, + "sl7": 15.33 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 22.2, - "sl5": 25.57, - "sl6": 28.6, - "sl7": 29.83 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.8, + "sl5": 30.14, + "sl6": 30.0, + "sl7": 29.67 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 1.14, - "sl6": 1.4, - "sl7": 1.67 + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 }, "id": { "component": "Gleyic luvisols", "name": "Gleyic luvisols", - "rank_loc": "4", + "rank_loc": "3", "score_loc": 0.047 }, "ph": { - "sl1": 6.3, - "sl2": 6.3, - "sl3": 6.3, - "sl4": 6.34, - "sl5": 6.41, - "sl6": 6.54, - "sl7": 6.62 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.02, + "sl5": 5.06, + "sl6": 5.12, + "sl7": 5.13 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 8.4, - "sl5": 13.14, - "sl6": 17.8, - "sl7": 15.67 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.4, + "sl5": 14.43, + "sl6": 15.2, + "sl7": 16.67 }, "sand": { - "sl1": 62.0, - "sl2": 62.0, - "sl3": 62.0, - "sl4": 57.4, - "sl5": 54.57, - "sl6": 51.4, - "sl7": 49.83 + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 42.6, + "sl5": 42.57, + "sl6": 42.6, + "sl7": 43.0 }, "site": { "siteData": { @@ -405,13 +305,13 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -425,64 +325,64 @@ "sl7": 120 }, "cec": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 21.6, - "sl5": 21.86, - "sl6": 22.2, - "sl7": 22.67 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.0, + "sl5": 16.14, + "sl6": 16.6, + "sl7": 16.83 }, "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 31.0, - "sl5": 31.43, - "sl6": 31.4, - "sl7": 31.33 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 33.8, + "sl5": 35.57, + "sl6": 37.4, + "sl7": 38.33 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.29, - "sl6": 1.2, - "sl7": 1.17 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 }, "id": { "component": "Eutric cambisols", "name": "Eutric cambisols", - "rank_loc": "5", + "rank_loc": "4", "score_loc": 0.047 }, "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.42, - "sl5": 6.47, - "sl6": 6.58, - "sl7": 6.65 + "sl1": 5.7, + "sl2": 5.7, + "sl3": 5.7, + "sl4": 5.78, + "sl5": 5.83, + "sl6": 5.9, + "sl7": 5.93 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 15.8, - "sl5": 16.57, - "sl6": 17.8, - "sl7": 16.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 7.6, + "sl5": 8.29, + "sl6": 8.0, + "sl7": 8.17 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 39.2, - "sl5": 39.14, - "sl6": 39.6, - "sl7": 39.33 + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 39.0, + "sl5": 37.57, + "sl6": 35.8, + "sl7": 35.0 }, "site": { "siteData": { @@ -525,64 +425,64 @@ "sl7": 120 }, "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 6.4, - "sl5": 6.29, - "sl6": 6.2, - "sl7": 6.17 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 10.8, + "sl5": 11.86, + "sl6": 13.0, + "sl7": 13.5 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 28.8, - "sl5": 31.14, - "sl6": 33.4, - "sl7": 34.33 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 22.2, + "sl5": 25.57, + "sl6": 28.6, + "sl7": 29.83 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.4, + "sl7": 1.67 }, "id": { "component": "Haplic acrisols", "name": "Haplic acrisols", - "rank_loc": "6", + "rank_loc": "5", "score_loc": 0.047 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.04, - "sl5": 5.03, - "sl6": 5.02, - "sl7": 5.02 + "sl1": 6.3, + "sl2": 6.3, + "sl3": 6.3, + "sl4": 6.34, + "sl5": 6.41, + "sl6": 6.54, + "sl7": 6.62 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 12.4, - "sl5": 13.29, - "sl6": 13.0, - "sl7": 14.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 8.4, + "sl5": 13.14, + "sl6": 17.8, + "sl7": 15.67 }, "sand": { - "sl1": 59.0, - "sl2": 59.0, - "sl3": 59.0, - "sl4": 54.4, - "sl5": 52.29, - "sl6": 50.2, - "sl7": 49.17 + "sl1": 62.0, + "sl2": 62.0, + "sl3": 62.0, + "sl4": 57.4, + "sl5": 54.57, + "sl6": 51.4, + "sl7": 49.83 }, "site": { "siteData": { @@ -605,9 +505,9 @@ } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", @@ -625,93 +525,93 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 12.8, - "sl5": 12.57, - "sl6": 12.2, - "sl7": 11.83 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.29, + "sl6": 18.4, + "sl7": 18.5 }, "clay": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 50.4, - "sl5": 52.86, - "sl6": 55.2, - "sl7": 56.17 + "sl1": 34.0, + "sl2": 34.0, + "sl3": 34.0, + "sl4": 36.6, + "sl5": 37.29, + "sl6": 38.0, + "sl7": 38.33 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 }, "id": { - "component": "Rhodic nitisols", - "name": "Rhodic nitisols", - "rank_loc": "7", - "score_loc": 0.047 + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "6", + "score_loc": 0.041 }, "ph": { - "sl1": 5.7, - "sl2": 5.7, - "sl3": 5.7, - "sl4": 5.64, - "sl5": 5.63, - "sl6": 5.64, - "sl7": 5.65 + "sl1": 5.6, + "sl2": 5.6, + "sl3": 5.6, + "sl4": 5.66, + "sl5": 5.69, + "sl6": 5.74, + "sl7": 5.77 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.2, - "sl5": 2.86, - "sl6": 3.4, - "sl7": 3.67 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 9.6, + "sl5": 10.43, + "sl6": 10.8, + "sl7": 11.83 }, "sand": { - "sl1": 32.0, - "sl2": 32.0, - "sl3": 32.0, - "sl4": 27.0, - "sl5": 25.71, - "sl6": 24.6, - "sl7": 24.17 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.8, + "sl5": 33.71, + "sl6": 33.6, + "sl7": 33.17 }, "site": { "siteData": { - "componentID": 141608, - "distance": 0.357, - "mapunitID": 4413, - "minCompDistance": 0.3573, + "componentID": 142595, + "distance": 92425.303, + "mapunitID": 4503, + "minCompDistance": 92425.3027, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", - "Description_es": "Los Nitisoles Ródicos son los suelos subtropicales y tropicales húmedos más productivos.
Tienen una estructura bien desarrollada con subsuelos relativamente arcillosos y enriquecidos en hierro que retienen agua y nutrientes. *Los Nitisoles Ródicos tienen subsuelos de color rojo oscuro con alta sorción de P.", - "Description_fr": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", - "Description_ks": "Rhodic Nitisols are the most productive humid subtropical and tropical soils.
They have well developed structure with relatively clayey and iron enriched subsoils which retain water and nutrients.
Rhodic Nitisols have dark red subsoils with high P sorption.", - "Management_en": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", - "Management_es": "Son suelos productivos y pueden utilizarse para la producción de cultivos.
Tienen un excelente drenaje interno y una buena capacidad de retención de agua.
Estos suelos tienen un alto grado de absorción de fósforo y fijan el fósforo, por lo que no está disponible para la absorción de las plantas durante la temporada de cultivo.
La fertilización con fósforo será necesaria para obtener la mejor productividad.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
Es especialmente importante que la fertilización con P se utilice en estos suelos, que se destacan específicamente por tener una alta sorción de P.", - "Management_fr": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. ", - "Management_ks": "These are productive soils, and can be used for crop production.
They have excellent internal drainage and good water holding capacity.
These soils do have a high degree of phosphorus sorption, and will fix phosphorus, making it unavailable for plant uptake during the cropping season.
Phosphorus fertilization will be needed for best productivity.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
It is especially important that P fertilization be used on these soils, which are specifically noted for having high P sorption. " + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -725,83 +625,83 @@ "sl7": 120 }, "cec": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 17.0, - "sl5": 16.29, - "sl6": 15.6, - "sl7": 15.33 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.6, + "sl5": 17.86, + "sl6": 18.4, + "sl7": 18.83 }, "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 29.8, - "sl5": 30.14, - "sl6": 30.0, - "sl7": 29.67 + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 35.8, + "sl5": 36.71, + "sl6": 37.8, + "sl7": 38.5 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, + "sl4": 0.8, + "sl5": 0.57, "sl6": 0.6, - "sl7": 0.5 + "sl7": 0.67 }, "id": { - "component": "Dystric cambisols", - "name": "Dystric cambisols", - "rank_loc": "8", - "score_loc": 0.047 + "component": "Eutric gleysols", + "name": "Eutric gleysols", + "rank_loc": "7", + "score_loc": 0.035 }, "ph": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.02, - "sl5": 5.06, - "sl6": 5.12, - "sl7": 5.13 + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.96, + "sl5": 5.97, + "sl6": 6.02, + "sl7": 6.05 }, "rock_fragments": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 14.4, - "sl5": 14.43, - "sl6": 15.2, - "sl7": 16.67 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 17.6, + "sl5": 17.14, + "sl6": 14.8, + "sl7": 15.83 }, "sand": { - "sl1": 42.0, - "sl2": 42.0, - "sl3": 42.0, - "sl4": 42.6, - "sl5": 42.57, - "sl6": 42.6, - "sl7": 43.0 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.6, + "sl5": 33.29, + "sl6": 32.8, + "sl7": 31.83 }, "site": { "siteData": { - "componentID": 142153, - "distance": 9267.434, - "mapunitID": 4465, - "minCompDistance": 9267.4336, - "share": 20, + "componentID": 142594, + "distance": 92425.303, + "mapunitID": 4503, + "minCompDistance": 92425.3027, + "share": 60, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", - "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", - "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", - "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { @@ -852,10 +752,10 @@ "sl7": 1.67 }, "id": { - "component": "Eutric fluvisols", - "name": "Eutric fluvisols", - "rank_loc": "9", - "score_loc": 0.041 + "component": "Cambic arenosols", + "name": "Cambic arenosols", + "rank_loc": "8", + "score_loc": 0.029 }, "ph": { "sl1": 6.1, @@ -886,32 +786,132 @@ }, "site": { "siteData": { - "componentID": 142595, - "distance": 92425.303, - "mapunitID": 4503, - "minCompDistance": 92425.3027, - "share": 20, + "componentID": 143286, + "distance": 57428.221, + "mapunitID": 4564, + "minCompDistance": 57428.2213, + "share": 50, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.0, + "sl6": 6.4, + "sl7": 6.17 + }, + "clay": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 46.4, + "sl5": 47.43, + "sl6": 48.2, + "sl7": 48.67 + }, + "ec": { + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 + }, + "id": { + "component": "Gleysols", + "name": "Gleysols", + "rank_loc": "9", + "score_loc": 0.012 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.92, + "sl5": 4.94, + "sl6": 4.98, + "sl7": 5.0 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.8, + "sl7": 5.0 + }, + "sand": { + "sl1": 41.0, + "sl2": 41.0, + "sl3": 41.0, + "sl4": 38.8, + "sl5": 38.0, + "sl6": 37.4, + "sl7": 37.0 + }, + "site": { + "siteData": { + "componentID": 142293, + "distance": 0.0, + "mapunitID": 4478, + "minCompDistance": 0.0, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", - "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + "Description_en": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los Gleysoles tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los gleysoles son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" } }, { @@ -925,83 +925,83 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 17.6, - "sl5": 17.86, - "sl6": 18.4, - "sl7": 18.83 + "sl1": 38.0, + "sl2": 38.0, + "sl3": 38.0, + "sl4": 36.6, + "sl5": 36.43, + "sl6": 36.8, + "sl7": 36.83 }, "clay": { "sl1": 33.0, "sl2": 33.0, "sl3": 33.0, - "sl4": 35.8, - "sl5": 36.71, - "sl6": 37.8, - "sl7": 38.5 + "sl4": 31.2, + "sl5": 30.43, + "sl6": 30.2, + "sl7": 30.0 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.6, - "sl7": 0.67 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.2, + "sl7": 0.33 }, "id": { - "component": "Eutric gleysols", - "name": "Eutric gleysols", + "component": "Fluvisols", + "name": "Fluvisols", "rank_loc": "10", - "score_loc": 0.035 + "score_loc": 0.012 }, "ph": { - "sl1": 5.9, - "sl2": 5.9, - "sl3": 5.9, - "sl4": 5.96, - "sl5": 5.97, - "sl6": 6.02, - "sl7": 6.05 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.42, + "sl5": 5.51, + "sl6": 5.64, + "sl7": 5.72 }, "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 17.6, - "sl5": 17.14, - "sl6": 14.8, - "sl7": 15.83 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.2, + "sl5": 12.71, + "sl6": 13.6, + "sl7": 13.67 }, "sand": { "sl1": 35.0, "sl2": 35.0, "sl3": 35.0, - "sl4": 33.6, - "sl5": 33.29, - "sl6": 32.8, - "sl7": 31.83 + "sl4": 37.0, + "sl5": 38.0, + "sl6": 38.4, + "sl7": 38.67 }, "site": { "siteData": { - "componentID": 142594, - "distance": 92425.303, - "mapunitID": 4503, - "minCompDistance": 92425.3027, - "share": 60, + "componentID": 143287, + "distance": 57428.221, + "mapunitID": 4564, + "minCompDistance": 57428.2213, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", - "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " + "Description_en": "Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles se encuentran sobre todo en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { @@ -1052,10 +1052,10 @@ "sl7": 0.0 }, "id": { - "component": "Cambic arenosols", - "name": "Cambic arenosols", + "component": "Haplic andosols", + "name": "Haplic andosols", "rank_loc": "11", - "score_loc": 0.029 + "score_loc": 0.012 }, "ph": { "sl1": 6.4, @@ -1086,22 +1086,22 @@ }, "site": { "siteData": { - "componentID": 143286, - "distance": 57428.221, - "mapunitID": 4564, - "minCompDistance": 57428.2213, - "share": 50, + "componentID": 143082, + "distance": 56276.866, + "mapunitID": 4546, + "minCompDistance": 56276.8656, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", - "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + "Description_en": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Description_es": "Los Andosoles Háplicos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas. ", + "Description_fr": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Description_ks": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", + "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Debido a que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.", + "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", + "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. " } }, "texture": { @@ -1125,89 +1125,89 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.6, - "sl5": 16.71, + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.2, + "sl5": 16.86, "sl6": 16.6, "sl7": 16.5 }, "clay": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 30.2, - "sl5": 31.57, + "sl1": 32.0, + "sl2": 32.0, + "sl3": 32.0, + "sl4": 32.8, + "sl5": 32.86, "sl6": 32.4, - "sl7": 32.33 + "sl7": 31.83 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Haplic luvisols", - "name": "Haplic luvisols", + "component": "Ferralsols", + "name": "Ferralsols", "rank_loc": "12", - "score_loc": 0.024 + "score_loc": 0.006 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.22, - "sl5": 6.26, - "sl6": 6.32, - "sl7": 6.37 + "sl1": 5.6, + "sl2": 5.6, + "sl3": 5.6, + "sl4": 5.68, + "sl5": 5.71, + "sl6": 5.74, + "sl7": 5.77 }, "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 14.8, - "sl5": 15.29, - "sl6": 15.2, - "sl7": 14.67 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 6.6, + "sl5": 7.0, + "sl6": 8.4, + "sl7": 9.5 }, "sand": { - "sl1": 47.0, - "sl2": 47.0, - "sl3": 47.0, - "sl4": 43.6, - "sl5": 42.71, - "sl6": 42.4, - "sl7": 42.67 + "sl1": 38.0, + "sl2": 38.0, + "sl3": 38.0, + "sl4": 38.0, + "sl5": 38.57, + "sl6": 39.8, + "sl7": 40.5 }, "site": { "siteData": { - "componentID": 141610, - "distance": 0.357, - "mapunitID": 4413, - "minCompDistance": 0.3573, + "componentID": 142977, + "distance": 54080.223, + "mapunitID": 4537, + "minCompDistance": 54080.2228, "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", - "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Description_es": "Los Ferralisoles son suelos bien desarrollados en climas húmedos y cálidos en los que predominan los minerales de baja actividad, como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas, pero son ácidos, relativamente infértiles, tienen una alta fijación de P y una capacidad limitada para retener nutrientes. ", + "Description_fr": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Description_ks": "Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients. ", + "Management_en": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_es": "suelos son propensos a la fijación de fósforo, y la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por parte de los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", + "Management_fr": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", + "Management_ks": "soils are prone to phosphorus fixation, and most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", "sl4": "Clay loam", "sl5": "Clay loam", "sl6": "Clay loam", @@ -1223,39 +1223,39 @@ }, "soilRank": [ { - "component": "Vertisols", - "componentData": "No Data", - "componentID": 142292, - "name": "Vertisols", - "rank_data": "1", + "component": "Fluvisols", + "componentData": "Data Complete", + "componentID": 143287, + "name": "Fluvisols", + "rank_data": "2", "rank_data_loc": "1", - "rank_loc": 3, - "score_data": 0.69, + "rank_loc": 10, + "score_data": 0.723, "score_data_loc": 1.0, - "score_loc": 0.047 + "score_loc": 0.012 }, { - "component": "Gleyic cambisols", - "componentData": "Missing Data", - "componentID": 142288, - "name": "Gleyic cambisols", - "rank_data": "4", + "component": "Ferralsols", + "componentData": "No Data", + "componentID": 142977, + "name": "Ferralsols", + "rank_data": "1", "rank_data_loc": "2", - "rank_loc": 2, - "score_data": 0.605, - "score_data_loc": 0.916, - "score_loc": 0.071 + "rank_loc": 12, + "score_data": 0.723, + "score_data_loc": 0.992, + "score_loc": 0.006 }, { "component": "Dystric cambisols", "componentData": "Data Complete", "componentID": 142153, "name": "Dystric cambisols", - "rank_data": "2", + "rank_data": "3", "rank_data_loc": "3", - "rank_loc": 8, + "rank_loc": 2, "score_data": 0.605, - "score_data_loc": 0.884, + "score_data_loc": 0.887, "score_loc": 0.047 }, { @@ -1263,11 +1263,11 @@ "componentData": "Data Complete", "componentID": 141611, "name": "Eutric cambisols", - "rank_data": "3", + "rank_data": "4", "rank_data_loc": "4", - "rank_loc": 5, + "rank_loc": 4, "score_data": 0.605, - "score_data_loc": 0.884, + "score_data_loc": 0.887, "score_loc": 0.047 }, { @@ -1277,94 +1277,94 @@ "name": "Eutric gleysols", "rank_data": "5", "rank_data_loc": "5", - "rank_loc": 10, + "rank_loc": 7, "score_data": 0.597, - "score_data_loc": 0.857, + "score_data_loc": 0.86, "score_loc": 0.035 }, { - "component": "Haplic nitisols", - "componentData": "Missing Data", - "componentID": 141607, - "name": "Haplic nitisols", - "rank_data": "9", + "component": "Gleyic luvisols", + "componentData": "Data Complete", + "componentID": 142289, + "name": "Gleyic luvisols", + "rank_data": "6", "rank_data_loc": "6", - "rank_loc": 1, - "score_data": 0.516, - "score_data_loc": 0.828, - "score_loc": 0.094 + "rank_loc": 3, + "score_data": 0.569, + "score_data_loc": 0.839, + "score_loc": 0.047 }, { - "component": "Eutric fluvisols", + "component": "Cambic arenosols", "componentData": "Data Complete", - "componentID": 142595, - "name": "Eutric fluvisols", - "rank_data": "6", + "componentID": 143286, + "name": "Cambic arenosols", + "rank_data": "7", "rank_data_loc": "7", - "rank_loc": 9, - "score_data": 0.554, - "score_data_loc": 0.807, - "score_loc": 0.041 + "rank_loc": 8, + "score_data": 0.557, + "score_data_loc": 0.798, + "score_loc": 0.029 }, { - "component": "Rhodic nitisols", - "componentData": "No Data", - "componentID": 141608, - "name": "Rhodic nitisols", - "rank_data": "7", + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 142595, + "name": "Eutric fluvisols", + "rank_data": "8", "rank_data_loc": "8", - "rank_loc": 7, - "score_data": 0.533, - "score_data_loc": 0.787, - "score_loc": 0.047 + "rank_loc": 6, + "score_data": 0.532, + "score_data_loc": 0.78, + "score_loc": 0.041 }, { - "component": "Haplic luvisols", + "component": "Haplic acrisols", "componentData": "Data Complete", - "componentID": 141610, - "name": "Haplic luvisols", - "rank_data": "8", + "componentID": 141609, + "name": "Haplic acrisols", + "rank_data": "10", "rank_data_loc": "9", - "rank_loc": 12, - "score_data": 0.52, - "score_data_loc": 0.737, - "score_loc": 0.024 + "rank_loc": 5, + "score_data": 0.492, + "score_data_loc": 0.734, + "score_loc": 0.047 }, { - "component": "Gleyic luvisols", - "componentData": "Data Complete", - "componentID": 142289, - "name": "Gleyic luvisols", - "rank_data": "10", + "component": "Gleysols", + "componentData": "Missing Data", + "componentID": 142293, + "name": "Gleysols", + "rank_data": "9", "rank_data_loc": "10", - "rank_loc": 4, - "score_data": 0.36, - "score_data_loc": 0.552, - "score_loc": 0.047 + "rank_loc": 9, + "score_data": 0.514, + "score_data_loc": 0.715, + "score_loc": 0.012 }, { - "component": "Haplic acrisols", + "component": "Haplic andosols", "componentData": "Data Complete", - "componentID": 141609, - "name": "Haplic acrisols", + "componentID": 143082, + "name": "Haplic andosols", "rank_data": "11", "rank_data_loc": "11", - "rank_loc": 6, - "score_data": 0.329, - "score_data_loc": 0.51, - "score_loc": 0.047 + "rank_loc": 11, + "score_data": 0.41, + "score_data_loc": 0.574, + "score_loc": 0.012 }, { - "component": "Cambic arenosols", - "componentData": "Data Complete", - "componentID": 143286, - "name": "Cambic arenosols", + "component": "Gleyic cambisols", + "componentData": "Missing Data", + "componentID": 142288, + "name": "Gleyic cambisols", "rank_data": "12", "rank_data_loc": "12", - "rank_loc": 11, - "score_data": 0.267, - "score_data_loc": 0.401, - "score_loc": 0.029 + "rank_loc": 1, + "score_data": 0.314, + "score_data_loc": 0.523, + "score_loc": 0.071 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json index c7b06c1..19830df 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[30.38333,35.53333].json @@ -25,31 +25,31 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.8, - "sl5": 13.43, - "sl6": 13.0, - "sl7": 12.67 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 4.4, + "sl5": 4.29, + "sl6": 4.2, + "sl7": 4.17 }, "clay": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 20.0, - "sl5": 20.43, - "sl6": 20.4, - "sl7": 20.17 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.6, + "sl5": 6.71, + "sl6": 7.0, + "sl7": 7.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.4, - "sl5": 1.71, - "sl6": 1.8, - "sl7": 1.83 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Haplic calcisols", @@ -58,31 +58,31 @@ "score_loc": 0.094 }, "ph": { - "sl1": 8.2, - "sl2": 8.2, - "sl3": 8.2, - "sl4": 8.28, - "sl5": 8.31, - "sl6": 8.34, - "sl7": 8.35 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.2, + "sl5": 8.26, + "sl6": 8.3, + "sl7": 8.33 }, "rock_fragments": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 14.2, - "sl5": 15.29, - "sl6": 16.6, - "sl7": 17.33 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 17.6, + "sl5": 19.0, + "sl6": 20.2, + "sl7": 19.83 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 46.8, - "sl5": 46.14, - "sl6": 46.0, - "sl7": 46.5 + "sl1": 88.0, + "sl2": 88.0, + "sl3": 88.0, + "sl4": 87.6, + "sl5": 87.71, + "sl6": 87.6, + "sl7": 87.33 }, "site": { "siteData": { @@ -105,13 +105,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { @@ -125,35 +125,35 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.4, - "sl5": 13.29, - "sl6": 13.0, - "sl7": 12.67 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.14, + "sl6": 16.0, + "sl7": 15.83 }, "clay": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.4, - "sl5": 15.43, - "sl6": 15.8, - "sl7": 16.17 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.0, + "sl5": 20.0, + "sl6": 20.2, + "sl7": 20.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.6, - "sl5": 1.71, + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, "sl6": 1.6, - "sl7": 1.83 + "sl7": 1.67 }, "id": { - "component": "Calcaric regosols", - "name": "Calcaric regosols", + "component": "Calcaric arenosols", + "name": "Calcaric arenosols", "rank_loc": "2", "score_loc": 0.059 }, @@ -161,57 +161,57 @@ "sl1": 8.2, "sl2": 8.2, "sl3": 8.2, - "sl4": 8.26, - "sl5": 8.27, - "sl6": 8.28, - "sl7": 8.28 + "sl4": 8.2, + "sl5": 8.2, + "sl6": 8.2, + "sl7": 8.2 }, "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 9.4, - "sl5": 8.0, - "sl6": 7.4, - "sl7": 7.83 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.2, + "sl5": 5.0, + "sl6": 5.2, + "sl7": 5.33 }, "sand": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 54.0, - "sl5": 53.71, - "sl6": 52.8, - "sl7": 52.5 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.6, + "sl5": 39.86, + "sl6": 39.8, + "sl7": 39.67 }, "site": { "siteData": { - "componentID": 132966, - "distance": 41734.66, - "mapunitID": 3534, - "minCompDistance": 41734.66, - "share": 10, + "componentID": 128772, + "distance": 92104.211, + "mapunitID": 32109, + "minCompDistance": 92104.2105, + "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", - "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", + "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -240,8 +240,8 @@ "sl4": 2.0 }, "id": { - "component": "Eutric leptosols", - "name": "Eutric leptosols", + "component": "Calcaric regosols", + "name": "Calcaric regosols", "rank_loc": "3", "score_loc": 0.059 }, @@ -265,22 +265,22 @@ }, "site": { "siteData": { - "componentID": 128778, - "distance": 84403.702, - "mapunitID": 32116, - "minCompDistance": 84403.7016, - "share": 100, - "soilDepth": 40 + "componentID": 132966, + "distance": 41734.66, + "mapunitID": 3534, + "minCompDistance": 41734.66, + "share": 10, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", - "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { @@ -294,38 +294,22 @@ "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl3": 20 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.4, - "sl5": 16.14, - "sl6": 16.0, - "sl7": 15.83 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 20.0, - "sl5": 20.0, - "sl6": 20.2, - "sl7": 20.17 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 }, "id": { "component": "Calcaric fluvisols", @@ -334,31 +318,19 @@ "score_loc": 0.059 }, "ph": { - "sl1": 8.2, - "sl2": 8.2, - "sl3": 8.2, - "sl4": 8.2, - "sl5": 8.2, - "sl6": 8.2, - "sl7": 8.2 + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 4.2, - "sl5": 5.0, - "sl6": 5.2, - "sl7": 5.33 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 39.6, - "sl5": 39.86, - "sl6": 39.8, - "sl7": 39.67 + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 }, "site": { "siteData": { @@ -381,13 +353,9 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" } }, { @@ -401,161 +369,93 @@ "sl7": 120 }, "cec": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 4.4, - "sl5": 4.29, - "sl6": 4.2, - "sl7": 4.17 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.8, + "sl5": 13.43, + "sl6": 13.0, + "sl7": 12.67 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.6, - "sl5": 6.71, - "sl6": 7.0, - "sl7": 7.17 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 20.0, + "sl5": 20.43, + "sl6": 20.4, + "sl7": 20.17 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.4, + "sl5": 1.71, + "sl6": 1.8, + "sl7": 1.83 }, "id": { - "component": "Calcaric arenosols", - "name": "Calcaric arenosols", + "component": "Eutric leptosols", + "name": "Eutric leptosols", "rank_loc": "5", "score_loc": 0.059 }, "ph": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 8.2, - "sl5": 8.26, - "sl6": 8.3, - "sl7": 8.33 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.28, + "sl5": 8.31, + "sl6": 8.34, + "sl7": 8.35 }, "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 17.6, - "sl5": 19.0, - "sl6": 20.2, - "sl7": 19.83 - }, - "sand": { - "sl1": 88.0, - "sl2": 88.0, - "sl3": 88.0, - "sl4": 87.6, - "sl5": 87.71, - "sl6": 87.6, - "sl7": 87.33 - }, - "site": { - "siteData": { - "componentID": 128772, - "distance": 92104.211, - "mapunitID": 32109, - "minCompDistance": 92104.2105, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", - "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " - } - }, - "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0 - }, - "clay": { "sl1": 12.0, "sl2": 12.0, - "sl3": 12.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols", - "rank_loc": "6", - "score_loc": 0.047 - }, - "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4 - }, - "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0 + "sl3": 12.0, + "sl4": 14.2, + "sl5": 15.29, + "sl6": 16.6, + "sl7": 17.33 }, "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0 + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 46.8, + "sl5": 46.14, + "sl6": 46.0, + "sl7": 46.5 }, "site": { "siteData": { - "componentID": 132626, - "distance": 3698.05, - "mapunitID": 3515, - "minCompDistance": 3698.0496, - "share": 50, - "soilDepth": 20 + "componentID": 128778, + "distance": 84403.702, + "mapunitID": 32116, + "minCompDistance": 84403.7016, + "share": 100, + "soilDepth": 40 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -569,64 +469,64 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 17.0, - "sl5": 16.86, - "sl6": 16.8, - "sl7": 16.17 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 14.0 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 24.4, - "sl5": 24.29, - "sl6": 24.0, - "sl7": 23.17 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.2, + "sl5": 20.86, + "sl6": 21.2, + "sl7": 21.33 }, "ec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 15.2, - "sl5": 16.14, - "sl6": 16.8, - "sl7": 16.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { "component": "Haplic solonchaks", "name": "Haplic solonchaks", - "rank_loc": "7", + "rank_loc": "6", "score_loc": 0.047 }, "ph": { - "sl1": 8.1, - "sl2": 8.1, - "sl3": 8.1, - "sl4": 8.16, - "sl5": 8.17, - "sl6": 8.2, - "sl7": 8.23 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.72, + "sl5": 7.81, + "sl6": 7.92, + "sl7": 8.0 }, "rock_fragments": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 16.4, - "sl5": 16.57, - "sl6": 14.0, - "sl7": 14.0 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.8, + "sl5": 27.86, + "sl6": 29.8, + "sl7": 30.17 }, "sand": { - "sl1": 50.0, - "sl2": 50.0, - "sl3": 50.0, - "sl4": 50.0, - "sl5": 49.86, - "sl6": 50.2, - "sl7": 51.5 + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 62.4, + "sl5": 62.0, + "sl6": 62.0, + "sl7": 61.83 }, "site": { "siteData": { @@ -649,9 +549,9 @@ } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", @@ -669,93 +569,93 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.2, - "sl5": 13.43, - "sl6": 13.8, - "sl7": 14.0 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.6, - "sl5": 16.71, - "sl6": 17.0, - "sl7": 17.5 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.6, - "sl5": 1.71, - "sl6": 1.6, - "sl7": 1.83 + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Regosols", - "name": "Regosols", - "rank_loc": "8", - "score_loc": 0.03 + "component": "Lithic leptosols", + "name": "Lithic leptosols", + "rank_loc": "7", + "score_loc": 0.047 }, "ph": { - "sl1": 7.8, - "sl2": 7.8, - "sl3": 7.8, - "sl4": 7.86, - "sl5": 7.93, - "sl6": 7.98, - "sl7": 8.02 + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 }, "rock_fragments": { "sl1": 12.0, "sl2": 12.0, "sl3": 12.0, - "sl4": 15.6, - "sl5": 16.57, - "sl6": 17.0, - "sl7": 17.17 + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 }, "sand": { - "sl1": 57.0, - "sl2": 57.0, - "sl3": 57.0, - "sl4": 56.2, - "sl5": 55.57, - "sl6": 54.4, - "sl7": 53.5 + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 }, "site": { "siteData": { - "componentID": 132625, + "componentID": 132626, "distance": 3698.05, "mapunitID": 3515, "minCompDistance": 3698.0496, "share": 50, - "soilDepth": 200 + "soilDepth": 20 }, "siteDescription": { - "Description_en": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", - "Description_es": "Los Regosoles son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad. ", - "Description_fr": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", - "Description_ks": "Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " } }, "texture": { "sl1": "Sandy loam", "sl2": "Sandy loam", "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -769,83 +669,83 @@ "sl7": 120 }, "cec": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 13.8, - "sl5": 14.0, - "sl6": 14.0, - "sl7": 13.83 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 19.6, - "sl5": 20.14, - "sl6": 20.2, - "sl7": 20.17 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 }, "id": { - "component": "Haplic luvisols", - "name": "Haplic luvisols", - "rank_loc": "9", + "component": "Cambic arenosols", + "name": "Cambic arenosols", + "rank_loc": "8", "score_loc": 0.029 }, "ph": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 7.14, - "sl5": 7.21, - "sl6": 7.34, - "sl7": 7.42 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 }, "rock_fragments": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.8, - "sl5": 16.71, - "sl6": 17.8, - "sl7": 17.83 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 }, "sand": { - "sl1": 64.0, - "sl2": 64.0, - "sl3": 64.0, - "sl4": 61.2, - "sl5": 60.86, - "sl6": 60.8, - "sl7": 60.83 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 }, "site": { "siteData": { - "componentID": 133773, - "distance": 16922.699, - "mapunitID": 3612, - "minCompDistance": 16922.6993, + "componentID": 133053, + "distance": 66261.442, + "mapunitID": 3539, + "minCompDistance": 66261.4422, "share": 50, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", - "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " } }, "texture": { @@ -853,9 +753,9 @@ "sl2": "Sandy loam", "sl3": "Sandy loam", "sl4": "Sandy loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -896,9 +796,9 @@ "sl7": 0.0 }, "id": { - "component": "Cambic arenosols", - "name": "Cambic arenosols", - "rank_loc": "10", + "component": "Haplic luvisols", + "name": "Haplic luvisols", + "rank_loc": "9", "score_loc": 0.029 }, "ph": { @@ -930,22 +830,22 @@ }, "site": { "siteData": { - "componentID": 133053, - "distance": 66261.442, - "mapunitID": 3539, - "minCompDistance": 66261.4422, + "componentID": 133773, + "distance": 16922.699, + "mapunitID": 3612, + "minCompDistance": 16922.6993, "share": 50, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", - "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { @@ -969,93 +869,193 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.0, - "sl5": 12.86, - "sl6": 12.6, - "sl7": 12.17 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.8, + "sl5": 8.43, + "sl6": 8.0, + "sl7": 7.83 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 23.6, - "sl5": 23.71, - "sl6": 23.8, - "sl7": 23.67 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 18.2, + "sl5": 18.29, + "sl6": 18.0, + "sl7": 17.67 }, "ec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 15.2, - "sl5": 16.14, - "sl6": 16.8, - "sl7": 16.67 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.71, + "sl6": 2.8, + "sl7": 3.0 }, "id": { - "component": "Solonchaks", - "name": "Solonchaks", - "rank_loc": "11", + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "10", "score_loc": 0.023 }, "ph": { - "sl1": 8.3, - "sl2": 8.3, - "sl3": 8.3, - "sl4": 8.36, - "sl5": 8.37, - "sl6": 8.38, - "sl7": 8.38 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.06, + "sl5": 8.07, + "sl6": 8.08, + "sl7": 8.07 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 3.4, + "sl5": 3.86, + "sl6": 7.2, + "sl7": 9.5 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 45.8, + "sl5": 45.86, + "sl6": 46.0, + "sl7": 46.33 + }, + "site": { + "siteData": { + "componentID": 132963, + "distance": 41734.66, + "mapunitID": 3534, + "minCompDistance": 41734.66, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 13.8, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 13.83 + }, + "clay": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.6, + "sl5": 20.14, + "sl6": 20.2, + "sl7": 20.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Calcic luvisols", + "name": "Calcic luvisols", + "rank_loc": "11", + "score_loc": 0.018 + }, + "ph": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 7.14, + "sl5": 7.21, + "sl6": 7.34, + "sl7": 7.42 }, "rock_fragments": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 19.0, - "sl5": 21.14, - "sl6": 22.8, - "sl7": 23.33 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.71, + "sl6": 17.8, + "sl7": 17.83 }, "sand": { - "sl1": 47.0, - "sl2": 47.0, - "sl3": 47.0, - "sl4": 47.6, - "sl5": 47.57, - "sl6": 47.6, - "sl7": 47.67 + "sl1": 64.0, + "sl2": 64.0, + "sl3": 64.0, + "sl4": 61.2, + "sl5": 60.86, + "sl6": 60.8, + "sl7": 60.83 }, "site": { "siteData": { - "componentID": 132965, + "componentID": 132962, "distance": 41734.66, "mapunitID": 3534, "minCompDistance": 41734.66, - "share": 10, + "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Description_es": "Los Solonchaks son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", - "Description_fr": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Description_ks": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", - "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", - "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", - "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " + "Description_en": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_es": "Los Luvisoles Cálcicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles cálcicos tienen subsuelos calcáreos.", + "Description_fr": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Description_ks": "Calcic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Calcic Luvisols have calcareous subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Estos suelos tendrán grandes cantidades de carbonato de calcio libre en la submuestra, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
These soils will have large amounts of free calcium carbonate in the subsample, and thus the soil pH will be > 7.0. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -1069,89 +1069,89 @@ "sl7": 120 }, "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 11.8, - "sl5": 12.14, - "sl6": 12.2, - "sl7": 12.17 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.0, + "sl5": 16.86, + "sl6": 16.8, + "sl7": 16.17 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 24.2, - "sl5": 25.43, - "sl6": 26.2, - "sl7": 26.0 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.4, + "sl5": 24.29, + "sl6": 24.0, + "sl7": 23.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 }, "id": { - "component": "Chromic luvisols", - "name": "Chromic luvisols", + "component": "Gypsisols", + "name": "Gypsisols", "rank_loc": "12", - "score_loc": 0.023 + "score_loc": 0.006 }, "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.62, - "sl5": 6.66, - "sl6": 6.76, - "sl7": 6.83 + "sl1": 8.1, + "sl2": 8.1, + "sl3": 8.1, + "sl4": 8.16, + "sl5": 8.17, + "sl6": 8.2, + "sl7": 8.23 }, "rock_fragments": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 12.0, - "sl5": 12.71, - "sl6": 16.0, - "sl7": 18.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 16.4, + "sl5": 16.57, + "sl6": 14.0, + "sl7": 14.0 }, "sand": { - "sl1": 67.0, - "sl2": 67.0, - "sl3": 67.0, - "sl4": 62.6, - "sl5": 61.71, - "sl6": 61.0, - "sl7": 61.17 + "sl1": 50.0, + "sl2": 50.0, + "sl3": 50.0, + "sl4": 50.0, + "sl5": 49.86, + "sl6": 50.2, + "sl7": 51.5 }, "site": { "siteData": { - "componentID": 132963, - "distance": 41734.66, - "mapunitID": 3534, - "minCompDistance": 41734.66, - "share": 20, + "componentID": 133188, + "distance": 67164.278, + "mapunitID": 3586, + "minCompDistance": 67164.278, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", - "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": NaN, + "Description_es": NaN, + "Description_fr": NaN, + "Description_ks": NaN, + "Management_en": NaN, + "Management_es": NaN, + "Management_fr": NaN, + "Management_ks": NaN } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", "sl6": "Sandy clay loam", @@ -1167,134 +1167,134 @@ }, "soilRank": [ { - "component": "Haplic calcisols", + "component": "Calcaric arenosols", "componentData": "Data Complete", - "componentID": 132718, - "name": "Haplic calcisols", - "rank_data": "2", + "componentID": 128772, + "name": "Calcaric arenosols", + "rank_data": "1", "rank_data_loc": "1", - "rank_loc": 1, + "rank_loc": 2, "score_data": 1.0, "score_data_loc": 1.0, - "score_loc": 0.094 + "score_loc": 0.059 }, { - "component": "Calcaric fluvisols", + "component": "Cambic arenosols", "componentData": "Data Complete", - "componentID": 128775, - "name": "Calcaric fluvisols", - "rank_data": "1", + "componentID": 133053, + "name": "Cambic arenosols", + "rank_data": "2", "rank_data_loc": "2", - "rank_loc": 4, + "rank_loc": 8, "score_data": 1.0, - "score_data_loc": 0.968, - "score_loc": 0.059 + "score_data_loc": 0.972, + "score_loc": 0.029 }, { - "component": "Solonchaks", + "component": "Haplic luvisols", "componentData": "Data Complete", - "componentID": 132965, - "name": "Solonchaks", + "componentID": 133773, + "name": "Haplic luvisols", "rank_data": "3", "rank_data_loc": "3", - "rank_loc": 11, + "rank_loc": 9, "score_data": 1.0, - "score_data_loc": 0.936, - "score_loc": 0.023 + "score_data_loc": 0.972, + "score_loc": 0.029 }, { - "component": "Calcaric regosols", + "component": "Calcaric fluvisols", "componentData": "Data Complete", - "componentID": 132966, - "name": "Calcaric regosols", + "componentID": 128775, + "name": "Calcaric fluvisols", "rank_data": "4", "rank_data_loc": "4", - "rank_loc": 2, + "rank_loc": 4, "score_data": 0.624, - "score_data_loc": 0.624, + "score_data_loc": 0.645, "score_loc": 0.059 }, { - "component": "Regosols", + "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 132625, - "name": "Regosols", - "rank_data": "9", + "componentID": 132966, + "name": "Calcaric regosols", + "rank_data": "5", "rank_data_loc": "5", - "rank_loc": 8, + "rank_loc": 3, "score_data": 0.624, - "score_data_loc": 0.598, - "score_loc": 0.03 + "score_data_loc": 0.645, + "score_loc": 0.059 }, { - "component": "Haplic luvisols", + "component": "Haplic solonchaks", "componentData": "Data Complete", - "componentID": 133773, - "name": "Haplic luvisols", - "rank_data": "7", + "componentID": 134183, + "name": "Haplic solonchaks", + "rank_data": "8", "rank_data_loc": "6", - "rank_loc": 9, + "rank_loc": 6, "score_data": 0.624, - "score_data_loc": 0.597, - "score_loc": 0.029 + "score_data_loc": 0.634, + "score_loc": 0.047 }, { "component": "Chromic luvisols", "componentData": "Data Complete", "componentID": 132963, "name": "Chromic luvisols", - "rank_data": "5", + "rank_data": "6", "rank_data_loc": "7", - "rank_loc": 12, + "rank_loc": 10, "score_data": 0.624, - "score_data_loc": 0.592, + "score_data_loc": 0.612, "score_loc": 0.023 }, { - "component": "Haplic solonchaks", + "component": "Gypsisols", "componentData": "Data Complete", - "componentID": 134183, - "name": "Haplic solonchaks", - "rank_data": "10", + "componentID": 133188, + "name": "Gypsisols", + "rank_data": "7", "rank_data_loc": "8", - "rank_loc": 7, - "score_data": 0.537, - "score_data_loc": 0.534, - "score_loc": 0.047 + "rank_loc": 12, + "score_data": 0.624, + "score_data_loc": 0.595, + "score_loc": 0.006 }, { - "component": "Calcaric arenosols", + "component": "Calcic luvisols", "componentData": "Data Complete", - "componentID": 128772, - "name": "Calcaric arenosols", - "rank_data": "11", + "componentID": 132962, + "name": "Calcic luvisols", + "rank_data": "10", "rank_data_loc": "9", - "rank_loc": 5, - "score_data": 0.399, - "score_data_loc": 0.418, - "score_loc": 0.059 + "rank_loc": 11, + "score_data": 0.537, + "score_data_loc": 0.524, + "score_loc": 0.018 }, { - "component": "Cambic arenosols", + "component": "Haplic calcisols", "componentData": "Data Complete", - "componentID": 133053, - "name": "Cambic arenosols", - "rank_data": "12", + "componentID": 132718, + "name": "Haplic calcisols", + "rank_data": "11", "rank_data_loc": "10", - "rank_loc": 10, - "score_data": 0.233, - "score_data_loc": 0.24, - "score_loc": 0.029 + "rank_loc": 1, + "score_data": 0.399, + "score_data_loc": 0.466, + "score_loc": 0.094 }, { "component": "Eutric leptosols", "componentData": "Missing Data", "componentID": 128778, "name": "Eutric leptosols", - "rank_data": "6", + "rank_data": "12", "rank_data_loc": "11", - "rank_loc": 3, - "score_data": 0.624, + "rank_loc": 5, + "score_data": 0.233, "score_data_loc": 0.002, "score_loc": 0.059 }, @@ -1303,9 +1303,9 @@ "componentData": "Missing Data", "componentID": 132626, "name": "Lithic leptosols", - "rank_data": "8", + "rank_data": "9", "rank_data_loc": "12", - "rank_loc": 6, + "rank_loc": 7, "score_data": 0.624, "score_data_loc": 0.002, "score_loc": 0.047 diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json index 345001a..273d560 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[32.11667,20.08333].json @@ -114,6 +114,106 @@ "sl7": "Loam" } }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.0, + "sl5": 12.86, + "sl6": 12.6, + "sl7": 12.17 + }, + "clay": { + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 23.6, + "sl5": 23.71, + "sl6": 23.8, + "sl7": 23.67 + }, + "ec": { + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 + }, + "id": { + "component": "Chromic cambisols", + "name": "Chromic cambisols", + "rank_loc": "2", + "score_loc": 0.114 + }, + "ph": { + "sl1": 8.3, + "sl2": 8.3, + "sl3": 8.3, + "sl4": 8.36, + "sl5": 8.37, + "sl6": 8.38, + "sl7": 8.38 + }, + "rock_fragments": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 19.0, + "sl5": 21.14, + "sl6": 22.8, + "sl7": 23.33 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 47.6, + "sl5": 47.57, + "sl6": 47.6, + "sl7": 47.67 + }, + "site": { + "siteData": { + "componentID": 101344, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", + "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, { "bottom_depth": { "sl1": 1, @@ -152,9 +252,9 @@ "sl7": 1.0 }, "id": { - "component": "Chromic cambisols", - "name": "Chromic cambisols", - "rank_loc": "2", + "component": "Haplic calcisols", + "name": "Haplic calcisols", + "rank_loc": "3", "score_loc": 0.114 }, "ph": { @@ -186,7 +286,7 @@ }, "site": { "siteData": { - "componentID": 101344, + "componentID": 101345, "distance": 0.0, "mapunitID": 103, "minCompDistance": 0.0, @@ -194,14 +294,14 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_es": "Los Cambisoles Crómicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos bien drenados, con un color intenso.
Cuando el clima y el paisaje son favorables, pueden ser suelos productivos. ", - "Description_fr": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Description_ks": "Chromic Cambisols are widely occurring soils with limited soil development.
These are well drained soils, with intense color.
When climate and landscape are favorable, they can be productive soils. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Description_es": "Los Calcisoles Háplicos se dan principalmente en climas semiáridos y áridos. Son suelos calcáreos, con alta saturación de bases, pH y fijación de P.
Muchos tienen horizontes superficiales de grava. ", + "Description_fr": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Description_ks": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", + "Management_en": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", + "Management_es": "Estos suelos tienen un bajo contenido en materia orgánica, son secos y a menudo pedregosos.
Son calcáreos, y tendrán una alta saturación de bases (Ca, Mg y K) y un alto pH del suelo.
Si se utilizan, los suelos son más adecuados para el pastoreo o para un uso limitado con cultivos tolerantes a la sequía.
En el mejor de los casos, podrían cultivarse cada dos o tres años, con barbecho en los años en que no se utilicen los suelos para cultivos.
Si se riega, hay que tener cuidado para que los suelos no se vuelvan altos en sales (salinos). Para evitar la salinización sería necesario un agua de riego de alta calidad y bajo contenido en sales.", + "Management_fr": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", + "Management_ks": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization." } }, "texture": { @@ -252,9 +352,9 @@ "sl7": 1.83 }, "id": { - "component": "Haplic calcisols", - "name": "Haplic calcisols", - "rank_loc": "3", + "component": "Solonchaks", + "name": "Solonchaks", + "rank_loc": "4", "score_loc": 0.114 }, "ph": { @@ -286,7 +386,7 @@ }, "site": { "siteData": { - "componentID": 101345, + "componentID": 101343, "distance": 0.0, "mapunitID": 103, "minCompDistance": 0.0, @@ -294,14 +394,14 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", - "Description_es": "Los Calcisoles Háplicos se dan principalmente en climas semiáridos y áridos. Son suelos calcáreos, con alta saturación de bases, pH y fijación de P.
Muchos tienen horizontes superficiales de grava. ", - "Description_fr": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", - "Description_ks": "Haplic Calcisols mostly occur in semiarid and arid climates. They are calcareous soils, with high base saturation, pH, and P fixation.
Many have gravelly surface horizons. ", - "Management_en": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", - "Management_es": "Estos suelos tienen un bajo contenido en materia orgánica, son secos y a menudo pedregosos.
Son calcáreos, y tendrán una alta saturación de bases (Ca, Mg y K) y un alto pH del suelo.
Si se utilizan, los suelos son más adecuados para el pastoreo o para un uso limitado con cultivos tolerantes a la sequía.
En el mejor de los casos, podrían cultivarse cada dos o tres años, con barbecho en los años en que no se utilicen los suelos para cultivos.
Si se riega, hay que tener cuidado para que los suelos no se vuelvan altos en sales (salinos). Para evitar la salinización sería necesario un agua de riego de alta calidad y bajo contenido en sales.", - "Management_fr": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization.", - "Management_ks": "These soils have low organic matter content, are dry, and often stony.
They are calcareous, and will have high base saturation (Ca, Mg and K) and high soil pH.
If used, the soils are best suited for grazing or limited use with drought tolerant crops.
At best they could be cultivated every-other or every-third year, with fallow in the years in which the soils are not used for crops.
If irrigated, care must be taken so that the soils do not become high in salts (saline). High quality irrigation water that is low in salts would be needed to prevent salinization." + "Description_en": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_es": "Los Solonchaks son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", + "Description_fr": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_ks": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " } }, "texture": { @@ -325,93 +425,93 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.0, - "sl5": 12.86, - "sl6": 12.6, - "sl7": 12.17 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 23.6, - "sl5": 23.71, - "sl6": 23.8, - "sl7": 23.67 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 }, "ec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 15.2, - "sl5": 16.14, - "sl6": 16.8, - "sl7": 16.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 }, "id": { - "component": "Solonchaks", - "name": "Solonchaks", - "rank_loc": "4", - "score_loc": 0.114 + "component": "Lithic leptosols", + "name": "Lithic leptosols1", + "rank_loc": "5", + "score_loc": 0.049 }, "ph": { - "sl1": 8.3, - "sl2": 8.3, - "sl3": 8.3, - "sl4": 8.36, - "sl5": 8.37, - "sl6": 8.38, - "sl7": 8.38 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 }, "rock_fragments": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 19.0, - "sl5": 21.14, - "sl6": 22.8, - "sl7": 23.33 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 }, "sand": { - "sl1": 47.0, - "sl2": 47.0, - "sl3": 47.0, - "sl4": 47.6, - "sl5": 47.57, - "sl6": 47.6, - "sl7": 47.67 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 }, "site": { "siteData": { - "componentID": 101343, + "componentID": 101347, "distance": 0.0, "mapunitID": 103, "minCompDistance": 0.0, - "share": 20, - "soilDepth": 200 + "share": 5, + "soilDepth": 20 }, "siteDescription": { - "Description_en": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Description_es": "Los Solonchaks son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", - "Description_fr": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Description_ks": "Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", - "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", - "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", - "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " - } - }, + "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", + "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + } + }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -436,10 +536,10 @@ "sl3": 1.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols1", - "rank_loc": "5", - "score_loc": 0.049 + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "6", + "score_loc": 0.047 }, "ph": { "sl1": 7.4, @@ -458,22 +558,22 @@ }, "site": { "siteData": { - "componentID": 101347, - "distance": 0.0, - "mapunitID": 103, - "minCompDistance": 0.0, - "share": 5, - "soilDepth": 20 + "componentID": 150227, + "distance": 72409.687, + "mapunitID": 67, + "minCompDistance": 72409.6869, + "share": 33, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { @@ -486,43 +586,71 @@ "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20 + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.0, + "sl5": 16.86, + "sl6": 16.8, + "sl7": 16.17 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.4, + "sl5": 24.29, + "sl6": 24.0, + "sl7": 23.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 15.2, + "sl5": 16.14, + "sl6": 16.8, + "sl7": 16.67 }, "id": { "component": "Vertic cambisols", "name": "Vertic cambisols", - "rank_loc": "6", + "rank_loc": "7", "score_loc": 0.047 }, "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 + "sl1": 8.1, + "sl2": 8.1, + "sl3": 8.1, + "sl4": 8.16, + "sl5": 8.17, + "sl6": 8.2, + "sl7": 8.23 }, "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 16.4, + "sl5": 16.57, + "sl6": 14.0, + "sl7": 14.0 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 + "sl1": 50.0, + "sl2": 50.0, + "sl3": 50.0, + "sl4": 50.0, + "sl5": 49.86, + "sl6": 50.2, + "sl7": 51.5 }, "site": { "siteData": { @@ -545,9 +673,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -561,94 +693,162 @@ "sl7": 120 }, "cec": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 30.2, - "sl5": 29.71, - "sl6": 29.2, - "sl7": 28.83 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 8.8, + "sl5": 8.43, + "sl6": 8.0, + "sl7": 7.83 }, "clay": { - "sl1": 47.0, - "sl2": 47.0, - "sl3": 47.0, - "sl4": 48.6, - "sl5": 48.57, - "sl6": 48.0, - "sl7": 46.83 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 18.2, + "sl5": 18.29, + "sl6": 18.0, + "sl7": 17.67 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.4, - "sl5": 0.29, - "sl6": 0.2, - "sl7": 0.17 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.71, + "sl6": 2.8, + "sl7": 3.0 }, "id": { - "component": "Chromic luvisols", - "name": "Chromic luvisols", - "rank_loc": "7", - "score_loc": 0.047 + "component": "Calcaric regosols", + "name": "Calcaric regosols", + "rank_loc": "8", + "score_loc": 0.029 }, "ph": { - "sl1": 7.3, - "sl2": 7.3, - "sl3": 7.3, - "sl4": 7.38, - "sl5": 7.43, - "sl6": 7.54, - "sl7": 7.57 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.06, + "sl5": 8.07, + "sl6": 8.08, + "sl7": 8.07 }, "rock_fragments": { "sl1": 4.0, "sl2": 4.0, "sl3": 4.0, - "sl4": 4.0, + "sl4": 3.4, "sl5": 3.86, - "sl6": 3.8, - "sl7": 4.17 + "sl6": 7.2, + "sl7": 9.5 }, "sand": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 15.8, - "sl5": 15.43, - "sl6": 15.4, - "sl7": 15.83 + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 45.8, + "sl5": 45.86, + "sl6": 46.0, + "sl7": 46.33 }, "site": { "siteData": { - "componentID": 150227, - "distance": 72409.687, - "mapunitID": 67, - "minCompDistance": 72409.6869, - "share": 33, + "componentID": 101346, + "distance": 0.0, + "mapunitID": 103, + "minCompDistance": 0.0, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", - "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" - } + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20 + }, + "cec": { + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0 + }, + "id": { + "component": "Haplic solonchaks", + "name": "Haplic solonchaks", + "rank_loc": "9", + "score_loc": 0.014 + }, + "ph": { + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7 + }, + "rock_fragments": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0 + }, + "sand": { + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0 + }, + "site": { + "siteData": { + "componentID": 135083, + "distance": 35571.412, + "mapunitID": 374, + "minCompDistance": 35571.4122, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_es": "Los Solonchaks Háplicos son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", + "Description_fr": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Description_ks": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", + "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", + "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", + "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam" + } }, { "bottom_depth": { @@ -688,10 +888,10 @@ "sl7": 1.0 }, "id": { - "component": "Calcaric regosols", - "name": "Calcaric regosols", - "rank_loc": "8", - "score_loc": 0.029 + "component": "Gypsisols", + "name": "Gypsisols", + "rank_loc": "10", + "score_loc": 0.014 }, "ph": { "sl1": 6.5, @@ -720,106 +920,6 @@ "sl6": 32.6, "sl7": 33.0 }, - "site": { - "siteData": { - "componentID": 101346, - "distance": 0.0, - "mapunitID": 103, - "minCompDistance": 0.0, - "share": 5, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", - "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.4, - "sl5": 13.29, - "sl6": 13.0, - "sl7": 12.67 - }, - "clay": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.4, - "sl5": 15.43, - "sl6": 15.8, - "sl7": 16.17 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.6, - "sl5": 1.71, - "sl6": 1.6, - "sl7": 1.83 - }, - "id": { - "component": "Gypsisols", - "name": "Gypsisols", - "rank_loc": "9", - "score_loc": 0.014 - }, - "ph": { - "sl1": 8.2, - "sl2": 8.2, - "sl3": 8.2, - "sl4": 8.26, - "sl5": 8.27, - "sl6": 8.28, - "sl7": 8.28 - }, - "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 9.4, - "sl5": 8.0, - "sl6": 7.4, - "sl7": 7.83 - }, - "sand": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 54.0, - "sl5": 53.71, - "sl6": 52.8, - "sl7": 52.5 - }, "site": { "siteData": { "componentID": 135084, @@ -841,13 +941,13 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -861,131 +961,31 @@ "sl7": 120 }, "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 8.8, - "sl5": 8.43, - "sl6": 8.0, - "sl7": 7.83 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 30.2, + "sl5": 29.71, + "sl6": 29.2, + "sl7": 28.83 }, "clay": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 18.2, - "sl5": 18.29, - "sl6": 18.0, - "sl7": 17.67 - }, - "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.6, - "sl5": 2.71, - "sl6": 2.8, - "sl7": 3.0 - }, - "id": { - "component": "Haplic solonchaks", - "name": "Haplic solonchaks", - "rank_loc": "10", - "score_loc": 0.014 - }, - "ph": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 8.06, - "sl5": 8.07, - "sl6": 8.08, - "sl7": 8.07 - }, - "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 3.4, - "sl5": 3.86, - "sl6": 7.2, - "sl7": 9.5 - }, - "sand": { "sl1": 47.0, "sl2": 47.0, "sl3": 47.0, - "sl4": 45.8, - "sl5": 45.86, - "sl6": 46.0, - "sl7": 46.33 - }, - "site": { - "siteData": { - "componentID": 135083, - "distance": 35571.412, - "mapunitID": 374, - "minCompDistance": 35571.4122, - "share": 10, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Description_es": "Los Solonchaks Háplicos son suelos que contienen sales en la superficie del suelo o cerca de ella. Estos suelos se forman en los desiertos o cerca de las costas.", - "Description_fr": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Description_ks": "Haplic Solonchaks are soils that contain salts at or near the soil surface. These soils form in either deserts or close to coastlines.", - "Management_en": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", - "Management_es": "Estos suelos suelen tener un alto contenido de sales totales.
Tienen una productividad muy pobre, y no pueden utilizarse a menos que se disponga de un riego de alta calidad para eliminar las sales acumuladas. *Estos suelos no son adecuados para la agricultura y es mejor utilizarlos para el pastoreo o dejarlos en barbecho.", - "Management_fr": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. ", - "Management_ks": "These soils are typically high in total salts.
They have very poor productivity, and cannot be used unless high quality irrigation is available to remove accumulated salts.
These soils are not well suited for agriculture and are best used for grazing, or left fallow. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 17.0, - "sl5": 16.86, - "sl6": 16.8, - "sl7": 16.17 - }, - "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 24.4, - "sl5": 24.29, - "sl6": 24.0, - "sl7": 23.17 + "sl4": 48.6, + "sl5": 48.57, + "sl6": 48.0, + "sl7": 46.83 }, "ec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 15.2, - "sl5": 16.14, - "sl6": 16.8, - "sl7": 16.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 }, "id": { "component": "Lithic leptosols", @@ -994,31 +994,31 @@ "score_loc": 0.049 }, "ph": { - "sl1": 8.1, - "sl2": 8.1, - "sl3": 8.1, - "sl4": 8.16, - "sl5": 8.17, - "sl6": 8.2, - "sl7": 8.23 + "sl1": 7.3, + "sl2": 7.3, + "sl3": 7.3, + "sl4": 7.38, + "sl5": 7.43, + "sl6": 7.54, + "sl7": 7.57 }, "rock_fragments": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 16.4, - "sl5": 16.57, - "sl6": 14.0, - "sl7": 14.0 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 3.86, + "sl6": 3.8, + "sl7": 4.17 }, "sand": { - "sl1": 50.0, - "sl2": 50.0, - "sl3": 50.0, - "sl4": 50.0, - "sl5": 49.86, - "sl6": 50.2, - "sl7": 51.5 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 15.8, + "sl5": 15.43, + "sl6": 15.4, + "sl7": 15.83 }, "site": { "siteData": { @@ -1041,13 +1041,13 @@ } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Unknown", + "sl2": "Unknown", + "sl3": "Unknown", + "sl4": "Unknown", + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" } } ] @@ -1059,135 +1059,135 @@ }, "soilRank": [ { - "component": "Gypsisols", + "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 135084, - "name": "Gypsisols", + "componentID": 101346, + "name": "Calcaric regosols", "rank_data": "1", "rank_data_loc": "1", - "rank_loc": "9", - "score_data": 0.59, + "rank_loc": "8", + "score_data": 0.515, "score_data_loc": 1.0, - "score_loc": 0.014 + "score_loc": 0.029 }, { - "component": "Solonchaks", + "component": "Chromic cambisols", "componentData": "Data Complete", - "componentID": 101343, - "name": "Solonchaks", - "rank_data": "2", + "componentID": 101344, + "name": "Chromic cambisols", + "rank_data": "3", "rank_data_loc": "2", - "rank_loc": "4", - "score_data": 0.484, - "score_data_loc": 0.991, + "rank_loc": "2", + "score_data": 0.409, + "score_data_loc": 0.962, "score_loc": 0.114 }, { - "component": "Chromic cambisols", + "component": "Gypsisols", "componentData": "Data Complete", - "componentID": 101344, - "name": "Chromic cambisols", - "rank_data": "6", + "componentID": 135084, + "name": "Gypsisols", + "rank_data": "2", "rank_data_loc": "3", - "rank_loc": "2", - "score_data": 0.334, - "score_data_loc": 0.742, - "score_loc": 0.114 + "rank_loc": "10", + "score_data": 0.484, + "score_data_loc": 0.916, + "score_loc": 0.014 }, { - "component": "Calcaric fluvisols", + "component": "Solonchaks", "componentData": "Data Complete", - "componentID": 101342, - "name": "Calcaric fluvisols", - "rank_data": "9", + "componentID": 101343, + "name": "Solonchaks", + "rank_data": "5", "rank_data_loc": "4", - "rank_loc": "1", - "score_data": 0.263, - "score_data_loc": 0.72, - "score_loc": 0.172 + "rank_loc": "4", + "score_data": 0.38, + "score_data_loc": 0.909, + "score_loc": 0.114 }, { "component": "Haplic calcisols", "componentData": "Data Complete", "componentID": 101345, "name": "Haplic calcisols", - "rank_data": "8", + "rank_data": "7", "rank_data_loc": "5", "rank_loc": "3", - "score_data": 0.302, - "score_data_loc": 0.69, + "score_data": 0.333, + "score_data_loc": 0.822, "score_loc": 0.114 }, { - "component": "Vertic cambisols", - "componentData": "Missing Data", - "componentID": 150228, - "name": "Vertic cambisols", - "rank_data": "4", - "rank_data_loc": "6", - "rank_loc": "6", - "score_data": 0.356, - "score_data_loc": 0.668, - "score_loc": 0.047 - }, - { - "component": "Calcaric regosols", + "component": "Calcaric fluvisols", "componentData": "Data Complete", - "componentID": 101346, - "name": "Calcaric regosols", - "rank_data": "5", - "rank_data_loc": "7", - "rank_loc": "8", - "score_data": 0.348, - "score_data_loc": 0.624, - "score_loc": 0.029 + "componentID": 101342, + "name": "Calcaric fluvisols", + "rank_data": "10", + "rank_data_loc": "6", + "rank_loc": "1", + "score_data": 0.263, + "score_data_loc": 0.799, + "score_loc": 0.172 }, { "component": "Haplic solonchaks", "componentData": "Data Complete", "componentID": 135083, "name": "Haplic solonchaks", - "rank_data": "7", - "rank_data_loc": "8", - "rank_loc": "10", - "score_data": 0.333, - "score_data_loc": 0.574, + "rank_data": "4", + "rank_data_loc": "7", + "rank_loc": "9", + "score_data": 0.386, + "score_data_loc": 0.736, "score_loc": 0.014 }, + { + "component": "Vertic cambisols", + "componentData": "Missing Data", + "componentID": 150228, + "name": "Vertic cambisols", + "rank_data": "6", + "rank_data_loc": "8", + "rank_loc": "7", + "score_data": 0.344, + "score_data_loc": 0.718, + "score_loc": 0.047 + }, { "component": "Chromic luvisols", "componentData": "Missing Data", "componentID": 150227, "name": "Chromic luvisols", - "rank_data": "10", + "rank_data": "9", "rank_data_loc": "9", - "rank_loc": "7", - "score_data": 0.242, - "score_data_loc": 0.479, + "rank_loc": "6", + "score_data": 0.264, + "score_data_loc": 0.571, "score_loc": 0.047 }, { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 101347, - "name": "Lithic leptosols1", - "rank_data": "3", + "componentID": 150226, + "name": "Lithic leptosols2", + "rank_data": "Not Displayed", "rank_data_loc": "10", - "rank_loc": "5", - "score_data": 0.377, - "score_data_loc": 0.003, + "rank_loc": "Not Displayed", + "score_data": 0.292, + "score_data_loc": 0.004, "score_loc": 0.049 }, { "component": "Lithic leptosols", "componentData": "Missing Data", - "componentID": 150226, - "name": "Lithic leptosols2", - "rank_data": "Not Displayed", + "componentID": 101347, + "name": "Lithic leptosols1", + "rank_data": "8", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.354, - "score_data_loc": 0.003, + "rank_loc": "5", + "score_data": 0.314, + "score_data_loc": 0.004, "score_loc": 0.049 } ] diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json index b41d304..b635404 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[34.5,69.16667].json @@ -18,38 +18,22 @@ "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl3": 20 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.4, - "sl5": 16.29, - "sl6": 16.0, - "sl7": 15.67 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 21.2, - "sl5": 21.29, - "sl6": 21.0, - "sl7": 20.83 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0 }, "ec": { "sl1": 1.0, "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.67 + "sl3": 1.0 }, "id": { "component": "Calcaric cambisols", @@ -58,39 +42,27 @@ "score_loc": 0.007 }, "ph": { - "sl1": 8.2, - "sl2": 8.2, - "sl3": 8.2, - "sl4": 8.22, - "sl5": 8.24, - "sl6": 8.26, - "sl7": 8.27 + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 5.0, - "sl5": 6.14, - "sl6": 7.4, - "sl7": 7.17 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0 }, "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 41.2, - "sl5": 41.14, - "sl6": 41.6, - "sl7": 41.83 + "sl1": 66.0, + "sl2": 66.0, + "sl3": 66.0 }, "site": { "siteData": { - "componentID": 128966, - "distance": 3776.17, - "mapunitID": 33042, - "minCompDistance": 3776.1698, - "share": 90, + "componentID": 128926, + "distance": 8501.441, + "mapunitID": 33019, + "minCompDistance": 8501.4411, + "share": 21, "soilDepth": 200 }, "siteDescription": { @@ -105,13 +77,9 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam" } }, { @@ -125,31 +93,31 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.4, - "sl5": 16.29, - "sl6": 16.0, - "sl7": 15.67 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 21.2, - "sl5": 21.29, - "sl6": 21.0, - "sl7": 20.83 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.67 + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 }, "id": { "component": "Calcaric regosols", @@ -161,28 +129,28 @@ "sl1": 8.2, "sl2": 8.2, "sl3": 8.2, - "sl4": 8.22, - "sl5": 8.24, - "sl6": 8.26, - "sl7": 8.27 + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 5.0, - "sl5": 6.14, + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, "sl6": 7.4, - "sl7": 7.17 + "sl7": 7.83 }, "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 41.2, - "sl5": 41.14, - "sl6": 41.6, - "sl7": 41.83 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 }, "site": { "siteData": { @@ -205,13 +173,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -452,8 +420,8 @@ "sl7": 0.67 }, "id": { - "component": "Rendzic leptosols", - "name": "Rendzic leptosols", + "component": "Calcaric arenosols", + "name": "Calcaric arenosols1", "rank_loc": "5", "score_loc": 0.003 }, @@ -486,22 +454,22 @@ }, "site": { "siteData": { - "componentID": 129097, - "distance": 47480.618, - "mapunitID": 33127, - "minCompDistance": 47480.6175, - "share": 82, - "soilDepth": 40 + "componentID": 130338, + "distance": 94026.373, + "mapunitID": 33860, + "minCompDistance": 94026.3732, + "share": 65, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", - "Description_es": "Los Leptosoles Rendzicos tienen un volumen de enraizamiento muy limitado debido a la roca continua, material altamente calcáreo, horizontes cementados, o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles Rendzic son altamente calcáreos en la superficie del suelo. ", - "Description_fr": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", - "Description_ks": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo será alto (> 7,0) en estos suelos, y no será necesario el encalado.
Cualquier uso agrícola debe ser para el pastoreo o la agrosilvicultura, con el mantenimiento continuo de la cubierta.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", + "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " } }, "texture": { @@ -525,93 +493,93 @@ "sl7": 120 }, "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 16.4, - "sl5": 16.29, - "sl6": 16.2, - "sl7": 16.33 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 }, "clay": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 30.2, - "sl5": 30.14, - "sl6": 29.8, - "sl7": 30.0 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, + "sl7": 16.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 0.6, - "sl5": 0.57, - "sl6": 0.4, - "sl7": 0.5 + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 }, "id": { - "component": "Calcaric arenosols", - "name": "Calcaric arenosols1", + "component": "Rendzic leptosols", + "name": "Rendzic leptosols", "rank_loc": "6", "score_loc": 0.003 }, "ph": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 8.06, - "sl5": 8.09, - "sl6": 8.1, - "sl7": 8.1 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 }, "rock_fragments": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.6, - "sl5": 6.57, - "sl6": 8.8, - "sl7": 10.17 - }, - "sand": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 29.6, - "sl5": 29.29, - "sl6": 29.2, - "sl7": 28.67 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 }, "site": { "siteData": { - "componentID": 130338, - "distance": 94026.373, - "mapunitID": 33860, - "minCompDistance": 94026.3732, - "share": 65, - "soilDepth": 200 + "componentID": 129097, + "distance": 47480.618, + "mapunitID": 33127, + "minCompDistance": 47480.6175, + "share": 82, + "soilDepth": 40 }, "siteDescription": { - "Description_en": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Description_es": "Los Arenosoles Calcáricos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen carbonatos por encima de los 50 cm.", - "Description_fr": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Description_ks": "Calcaric Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils have carbonates above 50 cm.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
La presencia de carbonatos no afectará mucho a la productividad.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
The presence of carbonates will not greatly affect productivity. " + "Description_en": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Description_es": "Los Leptosoles Rendzicos tienen un volumen de enraizamiento muy limitado debido a la roca continua, material altamente calcáreo, horizontes cementados, o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles Rendzic son altamente calcáreos en la superficie del suelo. ", + "Description_fr": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Description_ks": "Rendzic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Rendzic Leptosols are highly calcareous at the soil surface. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
El pH del suelo será alto (> 7,0) en estos suelos, y no será necesario el encalado.
Cualquier uso agrícola debe ser para el pastoreo o la agrosilvicultura, con el mantenimiento continuo de la cubierta.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Soil pH will be high (> 7.0) in these soils, and no liming will be needed.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -725,31 +693,31 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.4, - "sl5": 13.29, - "sl6": 13.0, - "sl7": 12.67 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 }, "clay": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.4, - "sl5": 15.43, - "sl6": 15.8, - "sl7": 16.17 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 21.2, + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.6, - "sl5": 1.71, - "sl6": 1.6, - "sl7": 1.83 + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 }, "id": { "component": "Calcaric fluvisols", @@ -761,28 +729,28 @@ "sl1": 8.2, "sl2": 8.2, "sl3": 8.2, - "sl4": 8.26, - "sl5": 8.27, - "sl6": 8.28, - "sl7": 8.28 + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 }, "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 9.4, - "sl5": 8.0, + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, "sl6": 7.4, - "sl7": 7.83 + "sl7": 7.17 }, "sand": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 54.0, - "sl5": 53.71, - "sl6": 52.8, - "sl7": 52.5 + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 }, "site": { "siteData": { @@ -805,13 +773,13 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -914,6 +882,82 @@ "sl7": "Sandy loam" } }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 40 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 14.5 + }, + "clay": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 23.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 2.0 + }, + "id": { + "component": "Cambisols", + "name": "Cambisols", + "rank_loc": "10", + "score_loc": 0.001 + }, + "ph": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.05 + }, + "rock_fragments": { + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 38.0 + }, + "sand": { + "sl1": 47.0, + "sl2": 47.0, + "sl3": 47.0, + "sl4": 46.5 + }, + "site": { + "siteData": { + "componentID": 132402, + "distance": 84530.897, + "mapunitID": 3503, + "minCompDistance": 84530.8969, + "share": 25, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los cambisoles tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam" + } + }, { "bottom_depth": { "sl1": 1, @@ -954,7 +998,7 @@ "id": { "component": "Umbric leptosols", "name": "Umbric leptosols", - "rank_loc": "10", + "rank_loc": "11", "score_loc": 0.001 }, "ph": { @@ -1025,144 +1069,172 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.4, - "sl5": 16.43, - "sl6": 16.6, - "sl7": 16.17 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 14.0 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 24.6, - "sl5": 25.0, - "sl6": 25.4, - "sl7": 25.17 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.2, + "sl5": 20.86, + "sl6": 21.2, + "sl7": 21.33 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 1.14, - "sl6": 1.2, - "sl7": 1.5 + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Cambisols", - "name": "Cambisols", - "rank_loc": "11", - "score_loc": 0.001 + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", + "rank_loc": "Not Displayed", + "score_loc": 0.007 }, "ph": { - "sl1": 7.9, - "sl2": 7.9, - "sl3": 7.9, - "sl4": 7.98, - "sl5": 8.01, - "sl6": 8.06, - "sl7": 8.03 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.72, + "sl5": 7.81, + "sl6": 7.92, + "sl7": 8.0 }, "rock_fragments": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 13.4, - "sl5": 12.86, - "sl6": 12.4, - "sl7": 12.5 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.8, + "sl5": 27.86, + "sl6": 29.8, + "sl7": 30.17 }, "sand": { - "sl1": 44.0, - "sl2": 44.0, - "sl3": 44.0, - "sl4": 42.8, - "sl5": 42.14, - "sl6": 41.2, - "sl7": 41.0 + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 62.4, + "sl5": 62.0, + "sl6": 62.0, + "sl7": 61.83 }, "site": { "siteData": { - "componentID": 132402, - "distance": 84530.897, - "mapunitID": 3503, - "minCompDistance": 84530.8969, - "share": 25, + "componentID": 129002, + "distance": 17680.575, + "mapunitID": 33067, + "minCompDistance": 8501.4411, + "share": 90, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_es": "Los Cambisoles son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", - "Description_fr": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Description_ks": "Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los cambisoles tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20 + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.14, + "sl6": 16.0, + "sl7": 15.83 }, "clay": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.0, + "sl5": 20.0, + "sl6": 20.2, + "sl7": 20.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { "component": "Calcaric cambisols", - "name": "Calcaric cambisols2", + "name": "Calcaric cambisols3", "rank_loc": "Not Displayed", "score_loc": 0.007 }, "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.2, + "sl5": 8.2, + "sl6": 8.2, + "sl7": 8.2 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 4.2, + "sl5": 5.0, + "sl6": 5.2, + "sl7": 5.33 }, "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.6, + "sl5": 39.86, + "sl6": 39.8, + "sl7": 39.67 }, "site": { "siteData": { - "componentID": 128926, - "distance": 8501.441, - "mapunitID": 33019, - "minCompDistance": 3776.1698, - "share": 21, + "componentID": 128904, + "distance": 73527.269, + "mapunitID": 33007, + "minCompDistance": 8501.4411, + "share": 100, "soilDepth": 200 }, "siteDescription": { @@ -1177,9 +1249,13 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -1205,7 +1281,7 @@ }, "id": { "component": "Calcaric cambisols", - "name": "Calcaric cambisols3", + "name": "Calcaric cambisols4", "rank_loc": "Not Displayed", "score_loc": 0.007 }, @@ -1226,11 +1302,11 @@ }, "site": { "siteData": { - "componentID": 129002, - "distance": 17680.575, - "mapunitID": 33067, - "minCompDistance": 3776.1698, - "share": 90, + "componentID": 128910, + "distance": 73924.187, + "mapunitID": 33010, + "minCompDistance": 8501.4411, + "share": 100, "soilDepth": 200 }, "siteDescription": { @@ -1261,71 +1337,71 @@ "sl7": 120 }, "cec": { - "sl1": 89.0, - "sl2": 89.0, - "sl3": 89.0, - "sl4": 87.6, - "sl5": 85.14, - "sl6": 80.0, - "sl7": 75.67 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.43, + "sl6": 16.6, + "sl7": 16.17 }, "clay": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 27.2, - "sl5": 25.86, - "sl6": 23.8, - "sl7": 22.5 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.6, + "sl5": 25.0, + "sl6": 25.4, + "sl7": 25.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.5 }, "id": { "component": "Calcaric cambisols", - "name": "Calcaric cambisols4", + "name": "Calcaric cambisols5", "rank_loc": "Not Displayed", "score_loc": 0.007 }, "ph": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.06, - "sl5": 5.09, - "sl6": 5.14, - "sl7": 5.18 + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 7.98, + "sl5": 8.01, + "sl6": 8.06, + "sl7": 8.03 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 12.2, - "sl5": 13.86, - "sl6": 15.0, - "sl7": 15.5 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 13.4, + "sl5": 12.86, + "sl6": 12.4, + "sl7": 12.5 }, "sand": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 32.2, - "sl5": 33.86, - "sl6": 37.6, - "sl7": 40.83 + "sl1": 44.0, + "sl2": 44.0, + "sl3": 44.0, + "sl4": 42.8, + "sl5": 42.14, + "sl6": 41.2, + "sl7": 41.0 }, "site": { "siteData": { - "componentID": 128904, - "distance": 73527.269, - "mapunitID": 33007, - "minCompDistance": 3776.1698, + "componentID": 129504, + "distance": 89326.37, + "mapunitID": 33378, + "minCompDistance": 8501.4411, "share": 100, "soilDepth": 200 }, @@ -1341,10 +1417,10 @@ } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", "sl5": "Loam", "sl6": "Loam", "sl7": "Loam" @@ -1355,29 +1431,41 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 40 + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { "sl1": 17.0, "sl2": 17.0, "sl3": 17.0, - "sl4": 14.5 + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.2, + "sl7": 16.33 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 23.5 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 30.2, + "sl5": 30.14, + "sl6": 29.8, + "sl7": 30.0 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 2.0 + "sl4": 0.6, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.5 }, "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols5", + "component": "Calcaric regosols", + "name": "Calcaric regosols5", "rank_loc": "Not Displayed", "score_loc": 0.007 }, @@ -1385,45 +1473,57 @@ "sl1": 8.0, "sl2": 8.0, "sl3": 8.0, - "sl4": 8.05 + "sl4": 8.06, + "sl5": 8.09, + "sl6": 8.1, + "sl7": 8.1 }, "rock_fragments": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 38.0 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 6.57, + "sl6": 8.8, + "sl7": 10.17 }, "sand": { - "sl1": 47.0, - "sl2": 47.0, - "sl3": 47.0, - "sl4": 46.5 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 29.6, + "sl5": 29.29, + "sl6": 29.2, + "sl7": 28.67 }, "site": { "siteData": { - "componentID": 128910, - "distance": 73924.187, - "mapunitID": 33010, - "minCompDistance": 3776.1698, - "share": 100, + "componentID": 129080, + "distance": 68431.355, + "mapunitID": 33111, + "minCompDistance": 924.4281, + "share": 90, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1464,8 +1564,8 @@ "sl7": 0.0 }, "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols6", + "component": "Calcaric regosols", + "name": "Calcaric regosols4", "rank_loc": "Not Displayed", "score_loc": 0.007 }, @@ -1498,22 +1598,22 @@ }, "site": { "siteData": { - "componentID": 129504, - "distance": 89326.37, - "mapunitID": 33378, - "minCompDistance": 3776.1698, - "share": 100, + "componentID": 128899, + "distance": 43357.696, + "mapunitID": 33002, + "minCompDistance": 924.4281, + "share": 21, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { @@ -1631,37 +1731,25 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl4": 40 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 14.0, - "sl5": 14.0, - "sl6": 14.0, - "sl7": 14.0 - }, - "clay": { "sl1": 17.0, "sl2": 17.0, "sl3": 17.0, - "sl4": 20.2, - "sl5": 20.86, - "sl6": 21.2, - "sl7": 21.33 + "sl4": 15.5 + }, + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 20.0 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl4": 0.5 }, "id": { "component": "Calcaric regosols", @@ -1670,39 +1758,30 @@ "score_loc": 0.007 }, "ph": { - "sl1": 7.5, - "sl2": 7.5, - "sl3": 7.5, - "sl4": 7.72, - "sl5": 7.81, - "sl6": 7.92, - "sl7": 8.0 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.05 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 24.8, - "sl5": 27.86, - "sl6": 29.8, - "sl7": 30.17 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.5 }, "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 62.4, - "sl5": 62.0, - "sl6": 62.0, - "sl7": 61.83 + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 53.0 }, "site": { "siteData": { - "componentID": 128899, - "distance": 43357.696, - "mapunitID": 33002, + "componentID": 129155, + "distance": 32199.391, + "mapunitID": 33166, "minCompDistance": 924.4281, - "share": 21, + "share": 100, "soilDepth": 200 }, "siteDescription": { @@ -1717,13 +1796,10 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Sandy loam" } }, { @@ -1737,72 +1813,72 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.4, - "sl5": 16.14, - "sl6": 16.0, - "sl7": 15.83 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.6, + "sl5": 15.71, + "sl6": 15.6, + "sl7": 15.5 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 20.0, - "sl5": 20.0, - "sl6": 20.2, - "sl7": 20.17 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 22.4, + "sl5": 22.71, + "sl6": 22.6, + "sl7": 22.33 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { "component": "Calcaric regosols", - "name": "Calcaric regosols4", + "name": "Calcaric regosols6", "rank_loc": "Not Displayed", "score_loc": 0.007 }, "ph": { - "sl1": 8.2, - "sl2": 8.2, - "sl3": 8.2, - "sl4": 8.2, - "sl5": 8.2, - "sl6": 8.2, - "sl7": 8.2 + "sl1": 7.6, + "sl2": 7.6, + "sl3": 7.6, + "sl4": 7.86, + "sl5": 7.94, + "sl6": 8.02, + "sl7": 8.03 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 4.2, - "sl5": 5.0, - "sl6": 5.2, - "sl7": 5.33 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 9.4, + "sl5": 10.86, + "sl6": 12.6, + "sl7": 13.0 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 39.6, - "sl5": 39.86, - "sl6": 39.8, - "sl7": 39.67 + "sl1": 48.0, + "sl2": 48.0, + "sl3": 48.0, + "sl4": 46.4, + "sl5": 45.86, + "sl6": 46.0, + "sl7": 46.17 }, "site": { "siteData": { - "componentID": 129080, - "distance": 68431.355, - "mapunitID": 33111, + "componentID": 129500, + "distance": 77496.323, + "mapunitID": 33373, "minCompDistance": 924.4281, - "share": 90, + "share": 28, "soilDepth": 200 }, "siteDescription": { @@ -1848,108 +1924,20 @@ "clay": { "sl1": 16.0, "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.6, - "sl5": 16.71, - "sl6": 17.0, - "sl7": 17.5 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.6, - "sl5": 1.71, - "sl6": 1.6, - "sl7": 1.83 - }, - "id": { - "component": "Calcaric regosols", - "name": "Calcaric regosols5", - "rank_loc": "Not Displayed", - "score_loc": 0.007 - }, - "ph": { - "sl1": 7.8, - "sl2": 7.8, - "sl3": 7.8, - "sl4": 7.86, - "sl5": 7.93, - "sl6": 7.98, - "sl7": 8.02 - }, - "rock_fragments": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 15.6, - "sl5": 16.57, - "sl6": 17.0, - "sl7": 17.17 - }, - "sand": { - "sl1": 57.0, - "sl2": 57.0, - "sl3": 57.0, - "sl4": 56.2, - "sl5": 55.57, - "sl6": 54.4, - "sl7": 53.5 - }, - "site": { - "siteData": { - "componentID": 129500, - "distance": 77496.323, - "mapunitID": 33373, - "minCompDistance": 924.4281, - "share": 28, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", - "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 40 - }, - "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 15.5 - }, - "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 20.0 + "sl3": 16.0, + "sl4": 16.6, + "sl5": 16.71, + "sl6": 17.0, + "sl7": 17.5 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 0.5 + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.83 }, "id": { "component": "Lithic leptosols", @@ -1958,22 +1946,31 @@ "score_loc": 0.006 }, "ph": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.05 + "sl1": 7.8, + "sl2": 7.8, + "sl3": 7.8, + "sl4": 7.86, + "sl5": 7.93, + "sl6": 7.98, + "sl7": 8.02 }, "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 14.5 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 15.6, + "sl5": 16.57, + "sl6": 17.0, + "sl7": 17.17 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0, - "sl4": 53.0 + "sl1": 57.0, + "sl2": 57.0, + "sl3": 57.0, + "sl4": 56.2, + "sl5": 55.57, + "sl6": 54.4, + "sl7": 53.5 }, "site": { "siteData": { @@ -1996,10 +1993,13 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Sandy loam" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" } }, { @@ -2013,22 +2013,22 @@ "sl7": 120 }, "cec": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.6, - "sl5": 15.71, - "sl6": 15.6, - "sl7": 15.5 + "sl1": 89.0, + "sl2": 89.0, + "sl3": 89.0, + "sl4": 87.6, + "sl5": 85.14, + "sl6": 80.0, + "sl7": 75.67 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 22.4, - "sl5": 22.71, - "sl6": 22.6, - "sl7": 22.33 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 27.2, + "sl5": 25.86, + "sl6": 23.8, + "sl7": 22.5 }, "ec": { "sl1": 1.0, @@ -2046,31 +2046,31 @@ "score_loc": 0.003 }, "ph": { - "sl1": 7.6, - "sl2": 7.6, - "sl3": 7.6, - "sl4": 7.86, - "sl5": 7.94, - "sl6": 8.02, - "sl7": 8.03 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.06, + "sl5": 5.09, + "sl6": 5.14, + "sl7": 5.18 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 9.4, - "sl5": 10.86, - "sl6": 12.6, - "sl7": 13.0 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 12.2, + "sl5": 13.86, + "sl6": 15.0, + "sl7": 15.5 }, "sand": { - "sl1": 48.0, - "sl2": 48.0, - "sl3": 48.0, - "sl4": 46.4, - "sl5": 45.86, - "sl6": 46.0, - "sl7": 46.17 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 32.2, + "sl5": 33.86, + "sl6": 37.6, + "sl7": 40.83 }, "site": { "siteData": { @@ -2093,10 +2093,10 @@ } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", "sl5": "Loam", "sl6": "Loam", "sl7": "Loam" @@ -2113,11 +2113,11 @@ { "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 128966, - "name": "Calcaric cambisols1", + "componentID": 128910, + "name": "Calcaric cambisols4", "rank_data": "2", "rank_data_loc": "1", - "rank_loc": "1", + "rank_loc": "Not Displayed", "score_data": 1.0, "score_data_loc": 1.0, "score_loc": 0.007 @@ -2125,11 +2125,11 @@ { "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 128969, - "name": "Calcaric regosols1", - "rank_data": "3", + "componentID": 129155, + "name": "Calcaric regosols3", + "rank_data": "Not Displayed", "rank_data_loc": "2", - "rank_loc": "2", + "rank_loc": "Not Displayed", "score_data": 1.0, "score_data_loc": 1.0, "score_loc": 0.007 @@ -2151,7 +2151,7 @@ "componentData": "Data Complete", "componentID": 130333, "name": "Calcaric arenosols2", - "rank_data": "1", + "rank_data": "Not Displayed", "rank_data_loc": "4", "rank_loc": "Not Displayed", "score_data": 1.0, @@ -2159,49 +2159,49 @@ "score_loc": 0.003 }, { - "component": "Cambisols", + "component": "Calcaric fluvisols", "componentData": "Data Complete", - "componentID": 132402, - "name": "Cambisols", - "rank_data": "4", + "componentID": 129425, + "name": "Calcaric fluvisols", + "rank_data": "3", "rank_data_loc": "5", - "rank_loc": "11", + "rank_loc": "8", "score_data": 1.0, - "score_data_loc": 0.994, - "score_loc": 0.001 + "score_data_loc": 0.995, + "score_loc": 0.002 }, { "component": "Calcic luvisols", "componentData": "Data Complete", "componentID": 129392, "name": "Calcic luvisols", - "rank_data": "9", + "rank_data": "8", "rank_data_loc": "6", "rank_loc": "7", - "score_data": 0.613, - "score_data_loc": 0.611, + "score_data": 0.63, + "score_data_loc": 0.628, "score_loc": 0.003 }, { - "component": "Calcaric fluvisols", + "component": "Regosols", "componentData": "Data Complete", - "componentID": 129425, - "name": "Calcaric fluvisols", - "rank_data": "8", + "componentID": 132579, + "name": "Regosols", + "rank_data": "10", "rank_data_loc": "7", - "rank_loc": "8", + "rank_loc": "9", "score_data": 0.613, - "score_data_loc": 0.611, - "score_loc": 0.002 + "score_data_loc": 0.609, + "score_loc": 0.001 }, { - "component": "Regosols", + "component": "Cambisols", "componentData": "Data Complete", - "componentID": 132579, - "name": "Regosols", - "rank_data": "10", + "componentID": 132402, + "name": "Cambisols", + "rank_data": "9", "rank_data_loc": "8", - "rank_loc": "9", + "rank_loc": "10", "score_data": 0.613, "score_data_loc": 0.609, "score_loc": 0.001 @@ -2225,7 +2225,7 @@ "name": "Rendzic leptosols", "rank_data": "7", "rank_data_loc": "10", - "rank_loc": "5", + "rank_loc": "6", "score_data": 1.0, "score_data_loc": 0.002, "score_loc": 0.003 @@ -2237,17 +2237,17 @@ "name": "Umbric leptosols", "rank_data": "11", "rank_data_loc": "11", - "rank_loc": "10", + "rank_loc": "11", "score_data": 0.613, "score_data_loc": 0.002, "score_loc": 0.001 }, { - "component": "Calcaric cambisols", + "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 129002, - "name": "Calcaric cambisols3", - "rank_data": "Not Displayed", + "componentID": 129080, + "name": "Calcaric regosols5", + "rank_data": "4", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", "score_data": 1.0, @@ -2255,58 +2255,58 @@ "score_loc": 0.007 }, { - "component": "Calcaric cambisols", + "component": "Calcaric arenosols", "componentData": "Data Complete", - "componentID": 128910, - "name": "Calcaric cambisols5", - "rank_data": "Not Displayed", + "componentID": 130338, + "name": "Calcaric arenosols1", + "rank_data": "1", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", + "rank_loc": "5", "score_data": 1.0, - "score_data_loc": 1.0, - "score_loc": 0.007 + "score_data_loc": 0.996, + "score_loc": 0.003 }, { "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 129080, + "componentID": 128899, "name": "Calcaric regosols4", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 1.0, - "score_data_loc": 1.0, + "score_data": 0.63, + "score_data_loc": 0.632, "score_loc": 0.007 }, { "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 128904, - "name": "Calcaric cambisols4", + "componentID": 129002, + "name": "Calcaric cambisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.63, - "score_data_loc": 0.633, + "score_data": 0.613, + "score_data_loc": 0.616, "score_loc": 0.007 }, { - "component": "Calcaric arenosols", + "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 130338, - "name": "Calcaric arenosols1", + "componentID": 128904, + "name": "Calcaric cambisols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "6", - "score_data": 0.63, - "score_data_loc": 0.629, - "score_loc": 0.003 + "rank_loc": "Not Displayed", + "score_data": 0.613, + "score_data_loc": 0.616, + "score_loc": 0.007 }, { "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 128926, - "name": "Calcaric cambisols2", + "componentID": 129504, + "name": "Calcaric cambisols5", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2317,8 +2317,8 @@ { "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 128899, - "name": "Calcaric regosols3", + "componentID": 128933, + "name": "Calcaric regosols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2330,7 +2330,7 @@ "component": "Calcaric regosols", "componentData": "Data Complete", "componentID": 129500, - "name": "Calcaric regosols5", + "name": "Calcaric regosols6", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", @@ -2341,11 +2341,11 @@ { "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 129504, - "name": "Calcaric cambisols6", + "componentID": 128926, + "name": "Calcaric cambisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", + "rank_loc": "1", "score_data": 0.37, "score_data_loc": 0.374, "score_loc": 0.007 @@ -2353,11 +2353,11 @@ { "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 128933, - "name": "Calcaric regosols2", + "componentID": 128969, + "name": "Calcaric regosols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", + "rank_loc": "2", "score_data": 0.37, "score_data_loc": 0.374, "score_loc": 0.007 diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json index eaeff9c..9161999 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[37.33333,-5.4].json @@ -25,93 +25,93 @@ "sl7": 120 }, "cec": { - "sl1": 41.0, - "sl2": 41.0, - "sl3": 41.0, - "sl4": 41.0, - "sl5": 41.0, - "sl6": 41.0, - "sl7": 40.5 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.6, + "sl5": 13.57, + "sl6": 13.6, + "sl7": 14.0 }, "clay": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 56.8, - "sl5": 57.14, - "sl6": 57.0, - "sl7": 56.5 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 21.2, + "sl5": 21.43, + "sl6": 21.8, + "sl7": 22.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.6, - "sl7": 0.67 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.29, + "sl6": 2.4, + "sl7": 2.33 }, "id": { - "component": "Eutric vertisols", - "name": "Eutric vertisols", + "component": "Calcaric cambisols", + "name": "Calcaric cambisols1", "rank_loc": "1", - "score_loc": 0.115 + "score_loc": 0.086 }, "ph": { - "sl1": 6.8, - "sl2": 6.8, - "sl3": 6.8, - "sl4": 7.02, - "sl5": 7.13, - "sl6": 7.26, - "sl7": 7.33 + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 8.02, + "sl5": 8.04, + "sl6": 8.06, + "sl7": 8.05 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.0, - "sl5": 4.14, - "sl6": 4.2, - "sl7": 4.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.4, + "sl5": 3.86, + "sl6": 5.0, + "sl7": 5.83 }, "sand": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 12.4, - "sl5": 12.29, - "sl6": 12.4, - "sl7": 12.5 + "sl1": 39.0, + "sl2": 39.0, + "sl3": 39.0, + "sl4": 39.6, + "sl5": 39.71, + "sl6": 39.4, + "sl7": 38.67 }, "site": { "siteData": { - "componentID": 157428, - "distance": 0.0, - "mapunitID": 9683, - "minCompDistance": 0.0, - "share": 80, + "componentID": 157401, + "distance": 21368.302, + "mapunitID": 9673, + "minCompDistance": 21368.3019, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_es": "Los Vertisoles Éutricos son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua.
Los Vertisoles Eutricos son suelos relativamente productivos con una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Description_ks": "Eutric Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.
Eutric Vertisols are relatively productive soils with high base saturation in the subsoil.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_es": "Los Vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite la labranza excesiva cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero será necesaria una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que promuevan el drenaje y la infiltración del agua.
Con un drenaje y una gestión del agua adecuados, estos suelos pueden ser muy productivos, ya que la fertilidad del suelo nativo es alta.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed.
With proper drainage and water management, these soils can be highly productive, as the native soil fertility is high. " + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -152,10 +152,10 @@ "sl7": 0.5 }, "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols1", + "component": "Calcaric fluvisols", + "name": "Calcaric fluvisols", "rank_loc": "2", - "score_loc": 0.086 + "score_loc": 0.029 }, "ph": { "sl1": 8.0, @@ -186,22 +186,22 @@ }, "site": { "siteData": { - "componentID": 157401, + "componentID": 157400, "distance": 21368.302, "mapunitID": 9673, "minCompDistance": 21368.3019, - "share": 20, + "share": 80, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { @@ -225,122 +225,22 @@ "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 16.4, - "sl5": 16.29, - "sl6": 16.0, - "sl7": 15.67 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 21.2, - "sl5": 21.29, - "sl6": 21.0, - "sl7": 20.83 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 0.86, - "sl6": 0.6, - "sl7": 0.67 - }, - "id": { - "component": "Gleyic acrisols", - "name": "Gleyic acrisols", - "rank_loc": "3", - "score_loc": 0.033 - }, - "ph": { - "sl1": 8.2, - "sl2": 8.2, - "sl3": 8.2, - "sl4": 8.22, - "sl5": 8.24, - "sl6": 8.26, - "sl7": 8.27 - }, - "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 5.0, - "sl5": 6.14, - "sl6": 7.4, - "sl7": 7.17 - }, - "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 41.2, - "sl5": 41.14, - "sl6": 41.6, - "sl7": 41.83 - }, - "site": { - "siteData": { - "componentID": 157547, - "distance": 1849.359, - "mapunitID": 9723, - "minCompDistance": 1849.3591, - "share": 45, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", - "Description_es": "Los Acrisoles Gleyicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles gleyicos tienen un nivel freático alto estacional que provoca la saturación durante algunas épocas del año. ", - "Description_fr": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", - "Description_ks": "Gleyic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Gleyic Acrisols have a seasonal high-water table resulting in saturation during some time of the year.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.
Los períodos de saturación limitan el crecimiento de las raíces y aumentan la pérdida de nitrógeno.
Para evitar la pérdida de N por lixiviación y/o desnitrificación, considere el uso de fertilizantes de liberación lenta de N (urea recubierta de azufre (SCU), por ejemplo), si esos productos de liberación lenta están disponibles, o utilice estiércol u otros residuos orgánicos por sus propiedades de liberación lenta.
Puede ser necesario el drenaje de estos suelos, pero esto puede ser problemático, ya que la humedad se debe al alto nivel freático. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry.
Periods of saturation limit root growth and increase nitrogen loss.
To prevent N loss from leaching anddenitrification consider use of slow-release N fertilizers (sulfur-coated urea (SCU), for example), if those slow-release products are available, or use manures or other organic wastes for their slow-release properties.
Drainage of these soils may be needed, but this can be problematic, as the wetness is due to the high water table. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 7.0, - "sl5": 7.0, - "sl6": 7.4, - "sl7": 7.83 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 3.8, + "sl5": 3.43, + "sl6": 3.0, + "sl7": 2.83 }, "clay": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 21.4, - "sl5": 24.86, - "sl6": 28.2, - "sl7": 29.17 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.8, + "sl5": 2.57, + "sl6": 2.6, + "sl7": 2.67 }, "ec": { "sl1": 0.0, @@ -354,35 +254,35 @@ "id": { "component": "Calcic luvisols", "name": "Calcic luvisols", - "rank_loc": "4", + "rank_loc": "3", "score_loc": 0.029 }, "ph": { - "sl1": 5.2, - "sl2": 5.2, - "sl3": 5.2, - "sl4": 5.1, - "sl5": 5.03, - "sl6": 4.96, - "sl7": 4.93 + "sl1": 5.8, + "sl2": 5.8, + "sl3": 5.8, + "sl4": 5.86, + "sl5": 5.87, + "sl6": 5.88, + "sl7": 5.88 }, "rock_fragments": { "sl1": 2.0, "sl2": 2.0, "sl3": 2.0, - "sl4": 2.0, - "sl5": 3.0, - "sl6": 4.0, - "sl7": 4.5 + "sl4": 2.4, + "sl5": 2.86, + "sl6": 2.8, + "sl7": 5.33 }, "sand": { - "sl1": 57.0, - "sl2": 57.0, - "sl3": 57.0, - "sl4": 51.8, - "sl5": 49.57, - "sl6": 48.0, - "sl7": 47.83 + "sl1": 92.0, + "sl2": 92.0, + "sl3": 92.0, + "sl4": 92.2, + "sl5": 92.71, + "sl6": 93.2, + "sl7": 93.33 }, "site": { "siteData": { @@ -405,13 +305,13 @@ } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Sand", + "sl2": "Sand", + "sl3": "Sand", + "sl4": "Sand", + "sl5": "Sand", + "sl6": "Sand", + "sl7": "Sand" } }, { @@ -425,93 +325,93 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 14.0, - "sl5": 14.0, - "sl6": 14.0, - "sl7": 14.0 - }, - "clay": { "sl1": 17.0, "sl2": 17.0, "sl3": 17.0, - "sl4": 20.2, - "sl5": 20.86, - "sl6": 21.2, - "sl7": 21.33 + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.4, + "sl7": 16.83 }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "clay": { + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 21.6, + "sl5": 21.57, + "sl6": 21.6, + "sl7": 22.0 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.29, + "sl6": 2.4, + "sl7": 2.33 }, "id": { - "component": "Eutric regosols", - "name": "Eutric regosols1", - "rank_loc": "5", + "component": "Chromic luvisols", + "name": "Chromic luvisols1", + "rank_loc": "4", "score_loc": 0.029 }, "ph": { - "sl1": 7.5, - "sl2": 7.5, - "sl3": 7.5, - "sl4": 7.72, - "sl5": 7.81, - "sl6": 7.92, - "sl7": 8.0 + "sl1": 6.8, + "sl2": 6.8, + "sl3": 6.8, + "sl4": 7.0, + "sl5": 7.07, + "sl6": 7.16, + "sl7": 7.2 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 24.8, - "sl5": 27.86, - "sl6": 29.8, - "sl7": 30.17 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 4.2, + "sl5": 4.0, + "sl6": 3.4, + "sl7": 4.83 }, "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 62.4, - "sl5": 62.0, - "sl6": 62.0, - "sl7": 61.83 + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.4, + "sl5": 36.43, + "sl6": 36.4, + "sl7": 35.5 }, "site": { "siteData": { - "componentID": 157429, - "distance": 0.0, - "mapunitID": 9683, - "minCompDistance": 0.0, - "share": 20, + "componentID": 157483, + "distance": 43336.529, + "mapunitID": 9700, + "minCompDistance": 43336.5293, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Description_es": "Regosoles Éutricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Eutricos tienen una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Description_ks": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -528,19 +428,19 @@ "sl1": 12.0, "sl2": 12.0, "sl3": 12.0, - "sl4": 12.0, - "sl5": 12.0, - "sl6": 12.0, - "sl7": 12.0 + "sl4": 10.6, + "sl5": 10.86, + "sl6": 11.2, + "sl7": 11.5 }, "clay": { "sl1": 16.0, "sl2": 16.0, "sl3": 16.0, - "sl4": 17.2, - "sl5": 17.29, - "sl6": 17.2, - "sl7": 17.5 + "sl4": 17.0, + "sl5": 17.14, + "sl6": 18.0, + "sl7": 18.67 }, "ec": { "sl1": 1.0, @@ -549,59 +449,59 @@ "sl4": 1.0, "sl5": 1.14, "sl6": 1.2, - "sl7": 1.17 + "sl7": 1.0 }, "id": { - "component": "Calcaric fluvisols", - "name": "Calcaric fluvisols", - "rank_loc": "6", - "score_loc": 0.029 + "component": "Eutric cambisols", + "name": "Eutric cambisols", + "rank_loc": "5", + "score_loc": 0.016 }, "ph": { - "sl1": 6.6, - "sl2": 6.6, - "sl3": 6.6, - "sl4": 6.7, - "sl5": 6.76, - "sl6": 6.8, - "sl7": 6.83 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.52, + "sl5": 5.6, + "sl6": 5.66, + "sl7": 5.68 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 18.8, - "sl5": 21.0, - "sl6": 22.8, - "sl7": 22.17 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 16.0, + "sl5": 15.71, + "sl6": 15.6, + "sl7": 16.17 }, "sand": { - "sl1": 56.0, - "sl2": 56.0, - "sl3": 56.0, - "sl4": 55.6, - "sl5": 55.86, - "sl6": 56.2, + "sl1": 54.0, + "sl2": 54.0, + "sl3": 54.0, + "sl4": 54.8, + "sl5": 56.14, + "sl6": 55.8, "sl7": 54.83 }, "site": { "siteData": { - "componentID": 157400, - "distance": 21368.302, - "mapunitID": 9673, - "minCompDistance": 21368.3019, - "share": 80, + "componentID": 157525, + "distance": 54147.509, + "mapunitID": 9714, + "minCompDistance": 54147.5094, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", - "Description_es": "Los Fluvisoles Calcáricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles calcáricos tienen carbonatos y un pH elevado en la parte superior del suelo.", - "Description_fr": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", - "Description_ks": "Calcaric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Calcaric Fluvisols have carbonates and high pH in the upper portion of soil.", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o el manejo de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Una vez en cultivo continuo se debe tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una vía para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { @@ -625,93 +525,93 @@ "sl7": 120 }, "cec": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 12.0, - "sl5": 12.0, - "sl6": 12.0, - "sl7": 12.0 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 14.2, + "sl5": 13.14, + "sl6": 12.2, + "sl7": 11.83 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 17.2, - "sl5": 17.29, - "sl6": 17.2, - "sl7": 17.5 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.4, + "sl5": 20.29, + "sl6": 20.2, + "sl7": 19.83 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.14, - "sl6": 1.2, - "sl7": 1.17 + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 }, "id": { - "component": "Chromic luvisols", - "name": "Chromic luvisols1", - "rank_loc": "7", - "score_loc": 0.029 + "component": "Dystric planosols", + "name": "Dystric planosols", + "rank_loc": "6", + "score_loc": 0.014 }, "ph": { - "sl1": 6.6, - "sl2": 6.6, - "sl3": 6.6, - "sl4": 6.7, - "sl5": 6.76, - "sl6": 6.8, - "sl7": 6.83 + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.26, + "sl5": 5.27, + "sl6": 5.3, + "sl7": 5.32 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 18.8, - "sl5": 21.0, - "sl6": 22.8, - "sl7": 22.17 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.0, + "sl5": 21.57, + "sl6": 23.4, + "sl7": 23.83 }, "sand": { - "sl1": 56.0, - "sl2": 56.0, - "sl3": 56.0, - "sl4": 55.6, - "sl5": 55.86, - "sl6": 56.2, - "sl7": 54.83 + "sl1": 44.0, + "sl2": 44.0, + "sl3": 44.0, + "sl4": 44.0, + "sl5": 44.57, + "sl6": 45.0, + "sl7": 45.83 }, "site": { "siteData": { - "componentID": 157483, - "distance": 43336.529, - "mapunitID": 9700, - "minCompDistance": 43336.5293, - "share": 5, + "componentID": 157549, + "distance": 1849.359, + "mapunitID": 9723, + "minCompDistance": 1849.3591, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", - "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.", + "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed." } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -725,83 +625,83 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.6, - "sl5": 13.57, - "sl6": 13.6, - "sl7": 14.0 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.29, + "sl6": 16.0, + "sl7": 15.67 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, "sl4": 21.2, - "sl5": 21.43, - "sl6": 21.8, - "sl7": 22.0 + "sl5": 21.29, + "sl6": 21.0, + "sl7": 20.83 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.0, - "sl5": 2.29, - "sl6": 2.4, - "sl7": 2.33 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.67 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols1", - "rank_loc": "8", - "score_loc": 0.029 + "component": "Cambic arenosols", + "name": "Cambic arenosols", + "rank_loc": "7", + "score_loc": 0.014 }, "ph": { - "sl1": 7.9, - "sl2": 7.9, - "sl3": 7.9, - "sl4": 8.02, - "sl5": 8.04, - "sl6": 8.06, - "sl7": 8.05 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.22, + "sl5": 8.24, + "sl6": 8.26, + "sl7": 8.27 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.4, - "sl5": 3.86, - "sl6": 5.0, - "sl7": 5.83 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.0, + "sl5": 6.14, + "sl6": 7.4, + "sl7": 7.17 }, "sand": { - "sl1": 39.0, - "sl2": 39.0, - "sl3": 39.0, - "sl4": 39.6, - "sl5": 39.71, - "sl6": 39.4, - "sl7": 38.67 + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 41.14, + "sl6": 41.6, + "sl7": 41.83 }, "site": { "siteData": { - "componentID": 157466, - "distance": 45664.921, - "mapunitID": 9696, - "minCompDistance": 45664.9211, - "share": 15, - "soilDepth": 20 + "componentID": 157415, + "distance": 81555.369, + "mapunitID": 9679, + "minCompDistance": 81555.3694, + "share": 40, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_es": "Los Arenosoles Cámbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles cámbicos tienen un horizonte del subsuelo mínimamente desarrollado que puede retener cantidades ligeramente superiores de nutrientes y agua.", + "Description_fr": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Description_ks": "Cambic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Cambic Arenosols have a minimally developed subsoil horizon that can retain slightly higher amounts of nutrients and water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " } }, "texture": { @@ -814,6 +714,106 @@ "sl7": "Loam" } }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 11.8, + "sl5": 12.14, + "sl6": 12.2, + "sl7": 12.17 + }, + "clay": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 24.2, + "sl5": 25.43, + "sl6": 26.2, + "sl7": 26.0 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Calcaric regosols", + "name": "Calcaric regosols1", + "rank_loc": "8", + "score_loc": 0.014 + }, + "ph": { + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.62, + "sl5": 6.66, + "sl6": 6.76, + "sl7": 6.83 + }, + "rock_fragments": { + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 12.0, + "sl5": 12.71, + "sl6": 16.0, + "sl7": 18.0 + }, + "sand": { + "sl1": 67.0, + "sl2": 67.0, + "sl3": 67.0, + "sl4": 62.6, + "sl5": 61.71, + "sl6": 61.0, + "sl7": 61.17 + }, + "site": { + "siteData": { + "componentID": 157495, + "distance": 13892.147, + "mapunitID": 9703, + "minCompDistance": 13892.147, + "share": 20, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, { "bottom_depth": { "sl1": 1, @@ -852,10 +852,10 @@ "sl7": 1.0 }, "id": { - "component": "Gleyic luvisols", - "name": "Gleyic luvisols", + "component": "Dystric regosols", + "name": "Dystric regosols1", "rank_loc": "9", - "score_loc": 0.025 + "score_loc": 0.014 }, "ph": { "sl1": 6.5, @@ -886,22 +886,22 @@ }, "site": { "siteData": { - "componentID": 157548, - "distance": 1849.359, - "mapunitID": 9723, - "minCompDistance": 1849.3591, - "share": 35, + "componentID": 157601, + "distance": 39019.995, + "mapunitID": 9742, + "minCompDistance": 39019.9951, + "share": 15, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", - "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.", - "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", - "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", + "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " } }, "texture": { @@ -918,136 +918,100 @@ "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20 + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 24.6, + "sl5": 23.29, + "sl6": 21.2, + "sl7": 20.5 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 + "sl1": 25.0, + "sl2": 25.0, + "sl3": 25.0, + "sl4": 24.4, + "sl5": 22.71, + "sl6": 20.4, + "sl7": 19.83 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Luvic arenosols", - "name": "Luvic arenosols", + "component": "Dystric cambisols", + "name": "Dystric cambisols", "rank_loc": "10", - "score_loc": 0.021 + "score_loc": 0.009 }, "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 8.12, + "sl5": 8.2, + "sl6": 8.26, + "sl7": 8.27 }, "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0 + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 15.8, + "sl5": 19.14, + "sl6": 20.6, + "sl7": 18.67 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 + "sl1": 38.0, + "sl2": 38.0, + "sl3": 38.0, + "sl4": 36.8, + "sl5": 38.71, + "sl6": 41.0, + "sl7": 41.17 }, "site": { "siteData": { - "componentID": 157414, - "distance": 81555.369, - "mapunitID": 9679, - "minCompDistance": 81555.3694, - "share": 60, + "componentID": 157464, + "distance": 45664.921, + "mapunitID": 9696, + "minCompDistance": 45664.9211, + "share": 25, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Luvic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Luvic Arenosols have slightly increased clay content with depth and thus increased moisture and nutrient retention.", - "Description_es": "Los Arenosoles Lúvicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Los arenosoles lúvicos tienen un contenido de arcilla ligeramente mayor con la profundidad y, por tanto, una mayor retención de humedad y nutrientes. ", - "Description_fr": "Luvic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Luvic Arenosols have slightly increased clay content with depth and thus increased moisture and nutrient retention.", - "Description_ks": "Luvic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
Luvic Arenosols have slightly increased clay content with depth and thus increased moisture and nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization. " + "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", + "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " } }, "texture": { "sl1": "Loam", "sl2": "Loam", - "sl3": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0 - }, - "clay": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Humic cambisols", - "name": "Humic cambisols", - "rank_loc": "11", - "score_loc": 0.018 - }, - "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4 - }, - "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0 - }, - "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0 - }, - "site": { - "siteData": { - "componentID": 157468, - "distance": 37691.376, - "mapunitID": 9697, - "minCompDistance": 37691.3759, - "share": 50, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Description_es": "Los Cambisoles Húmicos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Estos suelos tienen más materia orgánica en los horizontes superficiales.
Cuando el clima y el paisaje son favorables, estos suelos pueden ser productivos. ", - "Description_fr": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Description_ks": "Humic Cambisols are widely occurring soils with limited soil development.
These soils have higher organic matter in surface horizons.
When climate and landscape are favorable, these soils can be productive. ", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " - } - }, - "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam" + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -1061,93 +1025,93 @@ "sl7": 120 }, "cec": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 11.8, - "sl5": 12.14, - "sl6": 12.2, - "sl7": 12.17 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 16.4, + "sl5": 16.43, + "sl6": 16.6, + "sl7": 16.17 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 24.2, - "sl5": 25.43, - "sl6": 26.2, - "sl7": 26.0 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 24.6, + "sl5": 25.0, + "sl6": 25.4, + "sl7": 25.17 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.5 }, "id": { - "component": "Stagnic luvisols", - "name": "Stagnic luvisols", - "rank_loc": "12", - "score_loc": 0.018 + "component": "Calcaric phaeozems", + "name": "Calcaric phaeozems", + "rank_loc": "11", + "score_loc": 0.007 }, "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.62, - "sl5": 6.66, - "sl6": 6.76, - "sl7": 6.83 + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 7.98, + "sl5": 8.01, + "sl6": 8.06, + "sl7": 8.03 }, "rock_fragments": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 12.0, - "sl5": 12.71, - "sl6": 16.0, - "sl7": 18.0 + "sl1": 16.0, + "sl2": 16.0, + "sl3": 16.0, + "sl4": 13.4, + "sl5": 12.86, + "sl6": 12.4, + "sl7": 12.5 }, "sand": { - "sl1": 67.0, - "sl2": 67.0, - "sl3": 67.0, - "sl4": 62.6, - "sl5": 61.71, - "sl6": 61.0, - "sl7": 61.17 + "sl1": 44.0, + "sl2": 44.0, + "sl3": 44.0, + "sl4": 42.8, + "sl5": 42.14, + "sl6": 41.2, + "sl7": 41.0 }, "site": { "siteData": { - "componentID": 157546, - "distance": 65551.867, - "mapunitID": 9722, - "minCompDistance": 65551.8665, - "share": 50, + "componentID": 157489, + "distance": 65814.76, + "mapunitID": 9702, + "minCompDistance": 65814.7603, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Stagnic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Stagnic Luvisols are ponded and saturated in and above surface horizons during wet times of the year.", - "Description_es": "Los Luvisoles Stágnicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Estálicos están encharcados y saturados en los horizontes superficiales y por encima de ellos durante las épocas húmedas del año.", - "Description_fr": "Stagnic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Stagnic Luvisols are ponded and saturated in and above surface horizons during wet times of the year.", - "Description_ks": "Stagnic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Stagnic Luvisols are ponded and saturated in and above surface horizons during wet times of the year.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Dado que la saturación es causada por el agua superficial, podría ser útil el drenaje superficial y/o el mantenimiento de la cubierta para mejorar la infiltración y la retención de agua.
Considerar el uso de cultivos con raíces poco profundas.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
Se puede conseguir un uso más eficiente del N por parte de los cultivos en estos suelos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + "Description_en": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Description_es": "Los Phaeozems Calcáricos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems calcáreos son calcáreos en la parte superior del subsuelo.", + "Description_fr": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Description_ks": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Estos suelos tienen grandes cantidades de carbonato cálcico libre en el horizonte superior del suelo, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -1161,21 +1125,21 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.2, - "sl5": 13.43, - "sl6": 13.6, - "sl7": 13.83 - }, - "clay": { "sl1": 14.0, "sl2": 14.0, "sl3": 14.0, - "sl4": 14.8, - "sl5": 15.14, - "sl6": 15.6, + "sl4": 13.4, + "sl5": 13.29, + "sl6": 13.0, + "sl7": 12.67 + }, + "clay": { + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.4, + "sl5": 15.43, + "sl6": 15.8, "sl7": 16.17 }, "ec": { @@ -1188,56 +1152,56 @@ "sl7": 1.83 }, "id": { - "component": "Calcaric cambisols", - "name": "Calcaric cambisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.086 + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "12", + "score_loc": 0.004 }, "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4, - "sl4": 7.44, - "sl5": 7.51, - "sl6": 7.66, - "sl7": 7.75 + "sl1": 8.2, + "sl2": 8.2, + "sl3": 8.2, + "sl4": 8.26, + "sl5": 8.27, + "sl6": 8.28, + "sl7": 8.28 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 23.0, - "sl5": 25.0, - "sl6": 26.0, - "sl7": 26.17 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 9.4, + "sl5": 8.0, + "sl6": 7.4, + "sl7": 7.83 }, "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0, - "sl4": 65.6, - "sl5": 64.86, - "sl6": 63.8, - "sl7": 62.83 + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 54.0, + "sl5": 53.71, + "sl6": 52.8, + "sl7": 52.5 }, "site": { "siteData": { - "componentID": 157476, - "distance": 73872.608, - "mapunitID": 9699, - "minCompDistance": 21368.3019, - "share": 65, + "componentID": 157432, + "distance": 53340.839, + "mapunitID": 9684, + "minCompDistance": 53340.8394, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", - "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", - "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", - "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", - "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { @@ -1261,93 +1225,93 @@ "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 15.6, - "sl5": 16.43, - "sl6": 17.0, - "sl7": 17.0 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.8, + "sl5": 16.0, + "sl6": 15.8, + "sl7": 15.67 }, "clay": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 24.0, - "sl5": 26.43, - "sl6": 27.8, - "sl7": 27.67 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.8, + "sl5": 21.14, + "sl6": 21.2, + "sl7": 21.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.57, - "sl6": 1.0, - "sl7": 1.33 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.29, + "sl6": 1.2, + "sl7": 1.17 }, "id": { - "component": "Eutric regosols", - "name": "Eutric regosols2", + "component": "Calcaric cambisols", + "name": "Calcaric cambisols2", "rank_loc": "Not Displayed", - "score_loc": 0.029 + "score_loc": 0.086 }, "ph": { - "sl1": 5.7, - "sl2": 5.7, - "sl3": 5.7, - "sl4": 5.76, - "sl5": 5.8, - "sl6": 5.9, - "sl7": 5.98 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.64, + "sl5": 7.69, + "sl6": 7.72, + "sl7": 7.77 }, "rock_fragments": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.43, - "sl6": 2.6, - "sl7": 2.5 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 12.4, + "sl5": 14.0, + "sl6": 16.0, + "sl7": 16.0 }, "sand": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 28.2, - "sl5": 27.14, - "sl6": 26.8, - "sl7": 27.17 + "sl1": 52.0, + "sl2": 52.0, + "sl3": 52.0, + "sl4": 51.2, + "sl5": 50.86, + "sl6": 51.0, + "sl7": 51.0 }, "site": { "siteData": { - "componentID": 157437, - "distance": 5598.48, - "mapunitID": 9686, - "minCompDistance": 0.0, - "share": 30, + "componentID": 157476, + "distance": 73872.608, + "mapunitID": 9699, + "minCompDistance": 21368.3019, + "share": 65, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Description_es": "Regosoles Éutricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Eutricos tienen una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Description_ks": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + "Description_en": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_es": "Los Cambisoles Calcáreos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos son calcáreos en una capa del suelo por debajo de la superficie.", + "Description_fr": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Description_ks": "Calcaric Cambisols are widely occurring soils with limited soil development.
These soils are calcareous in a soil layer below the surface.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En las regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en las regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Estos suelos son muy adecuados para la producción de cultivos, y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Silt loam", - "sl2": "Silt loam", - "sl3": "Silt loam", + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", "sl4": "Loam", "sl5": "Loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl6": "Sandy clay loam", + "sl7": "Loam" } }, { @@ -1361,93 +1325,93 @@ "sl7": 120 }, "cec": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 3.2, - "sl5": 2.86, - "sl6": 2.6, - "sl7": 2.67 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 14.0, + "sl5": 14.0, + "sl6": 14.0, + "sl7": 14.0 }, "clay": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.6, - "sl5": 5.71, - "sl6": 6.0, - "sl7": 6.33 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.2, + "sl5": 20.86, + "sl6": 21.2, + "sl7": 21.33 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Eutric regosols", - "name": "Eutric regosols3", + "component": "Chromic luvisols", + "name": "Chromic luvisols2", "rank_loc": "Not Displayed", "score_loc": 0.029 }, "ph": { - "sl1": 5.8, - "sl2": 5.8, - "sl3": 5.8, - "sl4": 5.82, - "sl5": 5.84, - "sl6": 5.86, - "sl7": 5.92 + "sl1": 7.5, + "sl2": 7.5, + "sl3": 7.5, + "sl4": 7.72, + "sl5": 7.81, + "sl6": 7.92, + "sl7": 8.0 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.6, - "sl5": 3.29, - "sl6": 4.4, - "sl7": 5.17 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 24.8, + "sl5": 27.86, + "sl6": 29.8, + "sl7": 30.17 }, "sand": { - "sl1": 88.0, - "sl2": 88.0, - "sl3": 88.0, - "sl4": 87.2, - "sl5": 87.43, - "sl6": 87.6, - "sl7": 87.5 + "sl1": 65.0, + "sl2": 65.0, + "sl3": 65.0, + "sl4": 62.4, + "sl5": 62.0, + "sl6": 62.0, + "sl7": 61.83 }, "site": { "siteData": { - "componentID": 157568, - "distance": 74171.143, - "mapunitID": 9731, - "minCompDistance": 0.0, - "share": 45, + "componentID": 157477, + "distance": 73872.608, + "mapunitID": 9699, + "minCompDistance": 43336.5293, + "share": 35, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Description_es": "Regosoles Éutricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Eutricos tienen una alta saturación de base en el subsuelo. ", - "Description_fr": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Description_ks": "Eutric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Eutric Regosols have high base saturation in the subsoil. ", - "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Estos suelos pueden ser productivos, si se les proporciona riego y fertilización.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", - "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", - "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
This soil can be productive, if irrigation and fertilization are provided.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { - "sl1": "Sand", - "sl2": "Sand", - "sl3": "Sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -1461,83 +1425,83 @@ "sl7": 120 }, "cec": { - "sl1": 27.0, - "sl2": 27.0, - "sl3": 27.0, - "sl4": 21.6, - "sl5": 19.86, - "sl6": 18.2, - "sl7": 17.17 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 13.2, + "sl5": 14.71, + "sl6": 15.8, + "sl7": 15.67 }, "clay": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 22.0, - "sl5": 21.86, - "sl6": 21.4, - "sl7": 21.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 25.6, + "sl5": 31.86, + "sl6": 36.2, + "sl7": 36.33 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.4, - "sl5": 0.29, - "sl6": 0.2, - "sl7": 0.17 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Chromic luvisols", - "name": "Chromic luvisols2", + "component": "Dystric regosols", + "name": "Dystric regosols2", "rank_loc": "Not Displayed", - "score_loc": 0.029 + "score_loc": 0.014 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.18, - "sl5": 5.21, - "sl6": 5.26, - "sl7": 5.28 + "sl1": 4.7, + "sl2": 4.7, + "sl3": 4.7, + "sl4": 4.78, + "sl5": 4.76, + "sl6": 4.74, + "sl7": 4.87 }, "rock_fragments": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 18.4, - "sl5": 19.71, - "sl6": 22.0, - "sl7": 23.67 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 13.2, + "sl5": 11.14, + "sl6": 10.2, + "sl7": 12.67 }, "sand": { - "sl1": 44.0, - "sl2": 44.0, - "sl3": 44.0, - "sl4": 44.2, - "sl5": 44.71, - "sl6": 45.8, - "sl7": 46.67 + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 43.0, + "sl5": 38.14, + "sl6": 35.2, + "sl7": 36.33 }, "site": { "siteData": { - "componentID": 157477, - "distance": 73872.608, - "mapunitID": 9699, - "minCompDistance": 43336.5293, - "share": 35, + "componentID": 157463, + "distance": 45664.921, + "mapunitID": 9696, + "minCompDistance": 39019.9951, + "share": 40, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", - "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_es": "Los Regosoles Dístricos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.
Los Regosoles Dístricos tienen una baja saturación de base en el subsuelo. ", + "Description_fr": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Description_ks": "Dystric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Dystric Regosols have low base saturation in the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo. *Incluso cuando se utilizan para el pastoreo, el riego será necesario debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos. *Con una baja saturación de bases, estos suelos pueden responder a la adición de bases como el potasio, el calcio o el magnesio. ", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils.
With a low base saturation these soils may respond to addition of bases such as potassium, calcium or magnesium. " } }, "texture": { @@ -1545,9 +1509,9 @@ "sl2": "Loam", "sl3": "Loam", "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1561,93 +1525,93 @@ "sl7": 120 }, "cec": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.6, - "sl5": 16.29, - "sl6": 16.8, - "sl7": 17.0 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.8, + "sl5": 14.43, + "sl6": 13.2, + "sl7": 12.17 }, "clay": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 25.6, - "sl5": 27.57, - "sl6": 29.2, - "sl7": 29.83 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 25.4, + "sl5": 25.86, + "sl6": 24.0, + "sl7": 22.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.2, - "sl5": 0.43, - "sl6": 0.8, - "sl7": 1.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.6, + "sl5": 1.71, + "sl6": 1.6, + "sl7": 1.33 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", + "component": "Calcaric regosols", + "name": "Calcaric regosols2", "rank_loc": "Not Displayed", - "score_loc": 0.029 + "score_loc": 0.014 }, "ph": { "sl1": 5.8, "sl2": 5.8, "sl3": 5.8, - "sl4": 5.88, - "sl5": 5.94, - "sl6": 6.04, - "sl7": 6.1 + "sl4": 5.54, + "sl5": 5.44, + "sl6": 5.42, + "sl7": 5.45 }, "rock_fragments": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 8.4, - "sl5": 7.29, - "sl6": 6.0, - "sl7": 5.5 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 20.6, + "sl5": 21.14, + "sl6": 22.4, + "sl7": 23.67 }, "sand": { - "sl1": 25.0, - "sl2": 25.0, - "sl3": 25.0, - "sl4": 23.2, - "sl5": 22.29, - "sl6": 22.2, - "sl7": 22.33 + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 40.2, + "sl5": 39.0, + "sl6": 42.4, + "sl7": 44.5 }, "site": { "siteData": { - "componentID": 157488, - "distance": 65814.76, - "mapunitID": 9702, - "minCompDistance": 45664.9211, - "share": 35, - "soilDepth": 20 + "componentID": 157504, + "distance": 48258.508, + "mapunitID": 9706, + "minCompDistance": 13892.147, + "share": 20, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { - "sl1": "Silt loam", - "sl2": "Silt loam", - "sl3": "Silt loam", - "sl4": "Silt loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } } ] @@ -1659,208 +1623,196 @@ }, "soilRank": [ { - "component": "Eutric vertisols", - "componentData": "No Data", - "componentID": 157428, - "name": "Eutric vertisols", - "rank_data": "2", + "component": "Calcaric fluvisols", + "componentData": "Data Complete", + "componentID": 157400, + "name": "Calcaric fluvisols", + "rank_data": "1", "rank_data_loc": "1", - "rank_loc": "1", - "score_data": 0.879, + "rank_loc": "2", + "score_data": 0.802, "score_data_loc": 1.0, - "score_loc": 0.115 + "score_loc": 0.029 }, { - "component": "Luvic arenosols", + "component": "Calcic luvisols", "componentData": "Data Complete", - "componentID": 157414, - "name": "Luvic arenosols", - "rank_data": "1", + "componentID": 157534, + "name": "Calcic luvisols", + "rank_data": "3", "rank_data_loc": "2", - "rank_loc": "10", - "score_data": 0.885, - "score_data_loc": 0.912, - "score_loc": 0.021 + "rank_loc": "3", + "score_data": 0.802, + "score_data_loc": 1.0, + "score_loc": 0.029 }, { - "component": "Humic cambisols", - "componentData": "Data Complete", - "componentID": 157468, - "name": "Humic cambisols", - "rank_data": "3", + "component": "Chromic luvisols", + "componentData": "Missing Data", + "componentID": 157483, + "name": "Chromic luvisols1", + "rank_data": "4", "rank_data_loc": "3", - "rank_loc": "11", - "score_data": 0.865, - "score_data_loc": 0.888, - "score_loc": 0.018 + "rank_loc": "4", + "score_data": 0.802, + "score_data_loc": 1.0, + "score_loc": 0.029 }, { - "component": "Eutric regosols", + "component": "Eutric cambisols", "componentData": "Data Complete", - "componentID": 157437, - "name": "Eutric regosols2", - "rank_data": "4", + "componentID": 157525, + "name": "Eutric cambisols", + "rank_data": "6", "rank_data_loc": "4", - "rank_loc": "Not Displayed", - "score_data": 0.753, - "score_data_loc": 0.787, - "score_loc": 0.029 + "rank_loc": "5", + "score_data": 0.802, + "score_data_loc": 0.985, + "score_loc": 0.016 }, { - "component": "Gleyic acrisols", + "component": "Dystric regosols", "componentData": "Data Complete", - "componentID": 157547, - "name": "Gleyic acrisols", + "componentID": 157463, + "name": "Dystric regosols2", "rank_data": "5", "rank_data_loc": "5", - "rank_loc": "3", - "score_data": 0.748, - "score_data_loc": 0.785, - "score_loc": 0.033 + "rank_loc": "Not Displayed", + "score_data": 0.802, + "score_data_loc": 0.983, + "score_loc": 0.014 }, { - "component": "Chromic luvisols", + "component": "Calcaric phaeozems", "componentData": "Data Complete", - "componentID": 157477, - "name": "Chromic luvisols2", - "rank_data": "7", + "componentID": 157489, + "name": "Calcaric phaeozems", + "rank_data": "2", "rank_data_loc": "6", - "rank_loc": "Not Displayed", - "score_data": 0.711, - "score_data_loc": 0.744, - "score_loc": 0.029 + "rank_loc": "11", + "score_data": 0.802, + "score_data_loc": 0.974, + "score_loc": 0.007 }, { - "component": "Calcaric fluvisols", + "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 157400, - "name": "Calcaric fluvisols", - "rank_data": "8", + "componentID": 157476, + "name": "Calcaric cambisols2", + "rank_data": "9", "rank_data_loc": "7", - "rank_loc": "6", - "score_data": 0.697, - "score_data_loc": 0.73, - "score_loc": 0.029 + "rank_loc": "Not Displayed", + "score_data": 0.686, + "score_data_loc": 0.929, + "score_loc": 0.086 }, { - "component": "Calcaric cambisols", - "componentData": "Data Complete", - "componentID": 157401, - "name": "Calcaric cambisols1", - "rank_data": "11", + "component": "Dystric planosols", + "componentData": "Missing Data", + "componentID": 157549, + "name": "Dystric planosols", + "rank_data": "7", "rank_data_loc": "8", - "rank_loc": "2", - "score_data": 0.614, - "score_data_loc": 0.704, - "score_loc": 0.086 + "rank_loc": "6", + "score_data": 0.756, + "score_data_loc": 0.927, + "score_loc": 0.014 }, { - "component": "Calcic luvisols", + "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 157534, - "name": "Calcic luvisols", - "rank_data": "9", + "componentID": 157504, + "name": "Calcaric regosols2", + "rank_data": "8", "rank_data_loc": "9", - "rank_loc": "4", - "score_data": 0.627, - "score_data_loc": 0.66, - "score_loc": 0.029 + "rank_loc": "Not Displayed", + "score_data": 0.753, + "score_data_loc": 0.923, + "score_loc": 0.014 }, { - "component": "Stagnic luvisols", - "componentData": "Missing Data", - "componentID": 157546, - "name": "Stagnic luvisols", + "component": "Dystric cambisols", + "componentData": "Data Complete", + "componentID": 157464, + "name": "Dystric cambisols", "rank_data": "10", "rank_data_loc": "10", - "rank_loc": "12", - "score_data": 0.627, - "score_data_loc": 0.649, - "score_loc": 0.018 + "rank_loc": "10", + "score_data": 0.641, + "score_data_loc": 0.783, + "score_loc": 0.009 }, { - "component": "Gleyic luvisols", + "component": "Cambic arenosols", "componentData": "Data Complete", - "componentID": 157548, - "name": "Gleyic luvisols", + "componentID": 157415, + "name": "Cambic arenosols", "rank_data": "12", "rank_data_loc": "11", - "rank_loc": "9", - "score_data": 0.614, - "score_data_loc": 0.643, - "score_loc": 0.025 + "rank_loc": "7", + "score_data": 0.632, + "score_data_loc": 0.777, + "score_loc": 0.014 }, { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 157466, - "name": "Lithic leptosols1", - "rank_data": "6", + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 157432, + "name": "Eutric fluvisols", + "rank_data": "11", "rank_data_loc": "12", - "rank_loc": "8", - "score_data": 0.748, - "score_data_loc": 0.002, - "score_loc": 0.029 + "rank_loc": "12", + "score_data": 0.641, + "score_data_loc": 0.776, + "score_loc": 0.004 }, { "component": "Chromic luvisols", - "componentData": "Missing Data", - "componentID": 157483, - "name": "Chromic luvisols1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "7", - "score_data": 0.697, - "score_data_loc": 0.73, - "score_loc": 0.029 - }, - { - "component": "Eutric regosols", "componentData": "Data Complete", - "componentID": 157429, - "name": "Eutric regosols1", + "componentID": 157477, + "name": "Chromic luvisols2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "5", - "score_data": 0.62, - "score_data_loc": 0.652, + "rank_loc": "Not Displayed", + "score_data": 0.756, + "score_data_loc": 0.944, "score_loc": 0.029 }, { "component": "Calcaric cambisols", "componentData": "Data Complete", - "componentID": 157476, - "name": "Calcaric cambisols2", + "componentID": 157401, + "name": "Calcaric cambisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.548, - "score_data_loc": 0.638, + "rank_loc": "1", + "score_data": 0.662, + "score_data_loc": 0.9, "score_loc": 0.086 }, { - "component": "Eutric regosols", + "component": "Dystric regosols", "componentData": "Data Complete", - "componentID": 157568, - "name": "Eutric regosols3", + "componentID": 157601, + "name": "Dystric regosols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.311, - "score_data_loc": 0.342, - "score_loc": 0.029 + "rank_loc": "9", + "score_data": 0.662, + "score_data_loc": 0.814, + "score_loc": 0.014 }, { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 157488, - "name": "Lithic leptosols2", + "component": "Calcaric regosols", + "componentData": "Data Complete", + "componentID": 157495, + "name": "Calcaric regosols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.594, - "score_data_loc": 0.002, - "score_loc": 0.029 + "rank_loc": "8", + "score_data": 0.266, + "score_data_loc": 0.338, + "score_loc": 0.014 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json index 90782ea..108ecdf 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[48.71667,126.13333].json @@ -14,106 +14,6 @@ } }, "soilList": [ - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 34.0, - "sl2": 34.0, - "sl3": 34.0, - "sl4": 30.2, - "sl5": 28.86, - "sl6": 26.8, - "sl7": 25.67 - }, - "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 19.8, - "sl5": 19.71, - "sl6": 18.8, - "sl7": 18.5 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.6, - "sl5": 0.71, - "sl6": 0.8, - "sl7": 0.83 - }, - "id": { - "component": "Haplic andosols", - "name": "Haplic andosols", - "rank_loc": "1", - "score_loc": 0.142 - }, - "ph": { - "sl1": 5.9, - "sl2": 5.9, - "sl3": 5.9, - "sl4": 6.08, - "sl5": 6.13, - "sl6": 6.18, - "sl7": 6.18 - }, - "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 13.6, - "sl5": 14.43, - "sl6": 16.8, - "sl7": 18.5 - }, - "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 39.4, - "sl5": 40.14, - "sl6": 42.4, - "sl7": 43.5 - }, - "site": { - "siteData": { - "componentID": 103927, - "distance": 1111.692, - "mapunitID": 11370, - "minCompDistance": 1111.6922, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", - "Description_es": "Los Andosoles Háplicos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas. ", - "Description_fr": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", - "Description_ks": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", - "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", - "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Debido a que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.", - "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", - "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" - } - }, { "bottom_depth": { "sl1": 1, @@ -152,10 +52,10 @@ "sl7": 0.0 }, "id": { - "component": "Haplic phaeozems", - "name": "Haplic phaeozems", - "rank_loc": "2", - "score_loc": 0.054 + "component": "Haplic andosols", + "name": "Haplic andosols", + "rank_loc": "1", + "score_loc": 0.142 }, "ph": { "sl1": 6.2, @@ -186,22 +86,22 @@ }, "site": { "siteData": { - "componentID": 103604, - "distance": 2611.703, - "mapunitID": 11112, - "minCompDistance": 2611.7029, + "componentID": 103927, + "distance": 1111.692, + "mapunitID": 11370, + "minCompDistance": 1111.6922, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", - "Description_es": "Los Phaeozems Háplicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que se necesite el riego para la producción.", - "Description_fr": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", - "Description_ks": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.", - "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed." + "Description_en": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Description_es": "Los Andosoles Háplicos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas. ", + "Description_fr": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Description_ks": "Haplic Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility. ", + "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", + "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Debido a que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.", + "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. ", + "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion. " } }, "texture": { @@ -214,106 +114,6 @@ "sl7": "Loam" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 - }, - "cec": { - "sl1": 28.0, - "sl2": 28.0, - "sl3": 28.0, - "sl4": 23.4, - "sl5": 21.0, - "sl6": 18.2, - "sl7": 16.83 - }, - "clay": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 10.0, - "sl5": 10.14, - "sl6": 10.2, - "sl7": 9.83 - }, - "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 - }, - "id": { - "component": "Umbric andosols", - "name": "Umbric andosols", - "rank_loc": "3", - "score_loc": 0.035 - }, - "ph": { - "sl1": 5.7, - "sl2": 5.7, - "sl3": 5.7, - "sl4": 5.82, - "sl5": 5.84, - "sl6": 5.84, - "sl7": 5.85 - }, - "rock_fragments": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0, - "sl4": 15.0, - "sl5": 17.43, - "sl6": 20.0, - "sl7": 21.0 - }, - "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 39.6, - "sl5": 41.29, - "sl6": 43.6, - "sl7": 46.17 - }, - "site": { - "siteData": { - "componentID": 103928, - "distance": 7836.2, - "mapunitID": 11371, - "minCompDistance": 7836.2001, - "share": 100, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ", - "Description_es": "Los Andosoles Úmbricos se forman en materiales volcánicos.
Estos suelos son muy erosionables y tienen una alta fijación de P, pero la mayoría tienen una capacidad de retención de agua y una fertilidad del suelo relativamente buenas.
Los Andosoles úmbricos tienen un horizonte superficial grueso, pero los suelos son más húmedos y tienen menos nutrientes que los Andosoles móllicos. ", - "Description_fr": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ", - "Description_ks": "Umbric Andosols form in volcanic materials.
These soils are highly erodible and have high P fixation, but most have relatively good water holding capacity and soil fertility.
Umbric Andosols have a thick surface horizon but soils are wetter and have fewer nutrients than Mollic Andosols. ", - "Management_en": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. ", - "Management_es": "La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Dado que estos suelos se forman a partir de materiales volcánicos, una parte de su carga es positiva, lo que significa que pueden \"fijar\" el fósforo, haciéndolo inaccesible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y rendimiento adecuados de los cultivos.
Los cultivos de cobertura y las rotaciones que incluyan leguminosas y la inclusión de cultivos con alta biomasa serán beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Los sistemas agroforestales pueden ayudar a minimizar la erosión.
El drenaje adicional puede hacer que estos suelos sean más productivos.
La fertilización será esencial para la producción efectiva de los cultivos.", - "Management_fr": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. ", - "Management_ks": "Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Because these soils are formed from volcanic materials a part of their soil charge is positive, which means they can ‘fix’ phosphorus, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Agroforestry systems can help minimize erosion.
Additional drainage may make these soils more productive.
Fertilization will be essential for effective crop production. " - } - }, - "texture": { - "sl1": "Silt loam", - "sl2": "Silt loam", - "sl3": "Silt loam", - "sl4": "Silt loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" - } - }, { "bottom_depth": { "sl1": 1, @@ -352,10 +152,10 @@ "sl7": 0.0 }, "id": { - "component": "Gleyic phaeozems", - "name": "Gleyic phaeozems", - "rank_loc": "4", - "score_loc": 0.035 + "component": "Haplic phaeozems", + "name": "Haplic phaeozems", + "rank_loc": "2", + "score_loc": 0.054 }, "ph": { "sl1": 7.1, @@ -386,22 +186,22 @@ }, "site": { "siteData": { - "componentID": 103605, - "distance": 12988.596, - "mapunitID": 11113, - "minCompDistance": 12988.596, + "componentID": 103604, + "distance": 2611.703, + "mapunitID": 11112, + "minCompDistance": 2611.7029, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", - "Description_es": "Los Phaeozems Gléyicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems gleyicos están saturados de agua subterránea poco profunda a menos de un metro de la superficie del suelo.", - "Description_fr": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", - "Description_ks": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que hay que considerar los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + "Description_en": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", + "Description_es": "Los Phaeozems Háplicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que se necesite el riego para la producción.", + "Description_fr": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", + "Description_ks": "Haplic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.", + "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed." } }, "texture": { @@ -425,83 +225,83 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 17.4, - "sl5": 17.43, - "sl6": 17.4, - "sl7": 17.0 + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 26.8, + "sl5": 26.43, + "sl6": 25.6, + "sl7": 25.0 }, "clay": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 31.8, - "sl5": 32.0, - "sl6": 31.8, - "sl7": 31.17 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.4, + "sl5": 33.43, + "sl6": 34.2, + "sl7": 34.5 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.6, - "sl7": 0.83 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Eutric gleysols", - "name": "Eutric gleysols", - "rank_loc": "5", + "component": "Calcaric phaeozems", + "name": "Calcaric phaeozems", + "rank_loc": "3", "score_loc": 0.035 }, "ph": { - "sl1": 6.3, - "sl2": 6.3, - "sl3": 6.3, - "sl4": 6.5, - "sl5": 6.57, - "sl6": 6.66, - "sl7": 6.75 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.56, + "sl5": 6.66, + "sl6": 6.74, + "sl7": 6.78 }, "rock_fragments": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 8.0, - "sl5": 8.86, - "sl6": 9.0, - "sl7": 9.33 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.6, + "sl5": 2.86, + "sl6": 3.4, + "sl7": 3.67 }, "sand": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 23.0, - "sl5": 23.14, - "sl6": 23.2, - "sl7": 23.0 + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 27.6, + "sl5": 27.14, + "sl6": 26.8, + "sl7": 26.67 }, "site": { "siteData": { - "componentID": 104276, - "distance": 14827.397, - "mapunitID": 11663, - "minCompDistance": 14827.3974, + "componentID": 103981, + "distance": 73247.232, + "mapunitID": 11413, + "minCompDistance": 73247.2321, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", - "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " + "Description_en": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Description_es": "Los Phaeozems Calcáricos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems calcáreos son calcáreos en la parte superior del subsuelo.", + "Description_fr": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Description_ks": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", + "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Estos suelos tienen grandes cantidades de carbonato cálcico libre en el horizonte superior del suelo, por lo que el pH del suelo será superior a 7,0.", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. " } }, "texture": { @@ -525,92 +325,92 @@ "sl7": 120 }, "cec": { - "sl1": 15.0, - "sl2": 15.0, - "sl3": 15.0, - "sl4": 15.0, - "sl5": 15.0, - "sl6": 14.8, - "sl7": 14.5 + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 24.2, + "sl5": 22.86, + "sl6": 21.0, + "sl7": 20.0 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 23.0, - "sl5": 24.14, - "sl6": 24.6, - "sl7": 24.5 + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 28.6, + "sl5": 28.43, + "sl6": 27.6, + "sl7": 27.0 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl5": 1.29, + "sl6": 1.8, + "sl7": 2.0 }, "id": { - "component": "Haplic luvisols", - "name": "Haplic luvisols", - "rank_loc": "6", + "component": "Calcic chernozems", + "name": "Calcic chernozems", + "rank_loc": "4", "score_loc": 0.035 }, "ph": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.02, - "sl5": 6.06, - "sl6": 6.12, - "sl7": 6.2 + "sl1": 7.4, + "sl2": 7.4, + "sl3": 7.4, + "sl4": 7.58, + "sl5": 7.7, + "sl6": 7.84, + "sl7": 7.9 }, "rock_fragments": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 11.0, - "sl5": 12.29, - "sl6": 13.6, - "sl7": 14.17 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 5.8, + "sl5": 7.57, + "sl6": 9.8, + "sl7": 10.83 }, "sand": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 31.2, - "sl5": 31.71, - "sl6": 33.0, - "sl7": 33.83 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 28.4, + "sl5": 28.71, + "sl6": 29.8, + "sl7": 30.33 }, "site": { "siteData": { - "componentID": 104597, - "distance": 22984.344, - "mapunitID": 11909, - "minCompDistance": 22984.3437, + "componentID": 103635, + "distance": 90543.48, + "mapunitID": 11138, + "minCompDistance": 90543.4796, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", - "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + "Description_en": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Description_es": "Los Chernozems Cálcicos son suelos altamente productivos con buenas propiedades físicas y químicas.
Tienen una alta calidad de suelo y capas superficiales oscuras y ricas.
Los Chernozems Cálcicos tienen carbonatos y un pH elevado en la parte superior del suelo.", + "Description_fr": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Description_ks": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", + "Management_en": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", + "Management_es": "Son, en general, suelos excelentes para la producción de cultivos.
Tienen una excelente porosidad y retención de agua, y son adecuados para una amplia gama de sistemas de producción de cultivos.
Algunos cultivos especiales pueden ser sensibles a los suelos con pH más alto, y puede ser necesario un suplemento de hierro.
Puede ser necesario el uso de fertilizantes.
Al tener un subsuelo calcáreo, pueden fijar el fósforo, por lo que puede ser necesaria una fertilización adecuada de P.", + "Management_fr": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", + "Management_ks": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. " } }, "texture": { - "sl1": "Silt loam", - "sl2": "Silt loam", - "sl3": "Silt loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", "sl7": "Loam" } }, @@ -625,81 +425,81 @@ "sl7": 120 }, "cec": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 28.4, - "sl5": 25.71, - "sl6": 22.6, - "sl7": 21.17 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 26.6, + "sl5": 25.29, + "sl6": 23.8, + "sl7": 22.67 }, "clay": { - "sl1": 28.0, - "sl2": 28.0, - "sl3": 28.0, - "sl4": 26.8, - "sl5": 26.57, - "sl6": 26.0, - "sl7": 25.67 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 31.4, + "sl5": 31.71, + "sl6": 31.4, + "sl7": 30.83 }, "ec": { "sl1": 1.0, "sl2": 1.0, "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 1.0, - "sl7": 1.33 + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.6, + "sl7": 1.83 }, "id": { - "component": "Mollic gleysols", - "name": "Mollic gleysols", - "rank_loc": "7", + "component": "Eutric gleysols", + "name": "Eutric gleysols", + "rank_loc": "5", "score_loc": 0.035 }, "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7, - "sl4": 6.98, - "sl5": 7.09, - "sl6": 7.2, - "sl7": 7.25 + "sl1": 6.9, + "sl2": 6.9, + "sl3": 6.9, + "sl4": 7.06, + "sl5": 7.16, + "sl6": 7.28, + "sl7": 7.35 }, "rock_fragments": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 2.2, - "sl5": 2.43, - "sl6": 2.8, - "sl7": 3.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 2.0, + "sl5": 2.29, + "sl6": 3.2, + "sl7": 3.5 }, "sand": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 34.0, - "sl5": 34.57, - "sl6": 35.8, - "sl7": 36.67 + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 26.0, + "sl5": 25.86, + "sl6": 26.0, + "sl7": 26.5 }, "site": { "siteData": { - "componentID": 104132, - "distance": 31367.734, - "mapunitID": 11539, - "minCompDistance": 31367.734, + "componentID": 104276, + "distance": 14827.397, + "mapunitID": 11663, + "minCompDistance": 14827.3974, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", - "Description_es": "Los Mollic Gleysols tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles móllicos tienen relativamente más materia orgánica y nutrientes en los horizontes superficiales.", - "Description_fr": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", - "Description_ks": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } @@ -708,10 +508,10 @@ "sl1": "Clay loam", "sl2": "Clay loam", "sl3": "Clay loam", - "sl4": "Loam", - "sl5": "Loam", - "sl6": "Loam", - "sl7": "Loam" + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -725,93 +525,93 @@ "sl7": 120 }, "cec": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 17.6, - "sl5": 18.29, - "sl6": 18.6, - "sl7": 18.33 + "sl1": 34.0, + "sl2": 34.0, + "sl3": 34.0, + "sl4": 30.2, + "sl5": 28.86, + "sl6": 26.8, + "sl7": 25.67 }, "clay": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 26.8, - "sl5": 28.71, - "sl6": 29.6, - "sl7": 29.5 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 19.8, + "sl5": 19.71, + "sl6": 18.8, + "sl7": 18.5 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.14, - "sl6": 1.4, - "sl7": 1.67 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.6, + "sl5": 0.71, + "sl6": 0.8, + "sl7": 0.83 }, "id": { - "component": "Gleyic luvisols", - "name": "Gleyic luvisols", - "rank_loc": "8", + "component": "Eutric cambisols", + "name": "Eutric cambisols", + "rank_loc": "6", "score_loc": 0.035 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.02, - "sl5": 6.03, - "sl6": 6.12, - "sl7": 6.22 + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 6.08, + "sl5": 6.13, + "sl6": 6.18, + "sl7": 6.18 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 2.8, - "sl5": 2.71, - "sl6": 3.0, - "sl7": 3.33 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 13.6, + "sl5": 14.43, + "sl6": 16.8, + "sl7": 18.5 }, "sand": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 21.4, - "sl5": 20.86, - "sl6": 20.8, - "sl7": 21.0 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 39.4, + "sl5": 40.14, + "sl6": 42.4, + "sl7": 43.5 }, "site": { "siteData": { - "componentID": 104608, - "distance": 59323.866, - "mapunitID": 11919, - "minCompDistance": 59323.8661, + "componentID": 104610, + "distance": 49566.694, + "mapunitID": 11920, + "minCompDistance": 49566.6944, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", - "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.", - "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", - "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + "Description_en": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_es": "Los Cambisoles Eútricos son suelos que se dan ampliamente con un desarrollo limitado del suelo.
Son suelos productivos con alta saturación de bases (Ca, Mg y K) en la parte superior del suelo. ", + "Description_fr": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Description_ks": "Eutric Cambisols are widely occurring soils with limited soil development.
These are productive soils with high base saturation (Ca, Mg and K) in the upper portion of soil. ", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
Los Cambisoles eútricos tendrán una alta saturación de bases, lo que significa que los nutrientes disponibles en el suelo serán predominantemente calcio, potasio y magnesio.
Estos suelos son muy adecuados para la producción de cultivos y pueden utilizarse de forma intensiva.
La fertilización debe utilizarse para mejorar la productividad, y puede incluirse el riego para aumentar aún más la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Eutric Cambisols will have high base saturation, which means that the available soil nutrients will be predominantly calcium, potassium, and magnesium.
These soils are well suited for crop production, and can be intensively used.
Fertilization should be used to improve productivity, and irrigation can be included to further boost productivity. " } }, "texture": { - "sl1": "Silt loam", - "sl2": "Silt loam", - "sl3": "Silt loam", - "sl4": "Silt loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" } }, { @@ -852,9 +652,9 @@ "sl7": 0.0 }, "id": { - "component": "Calcaric phaeozems", - "name": "Calcaric phaeozems", - "rank_loc": "9", + "component": "Gleyic luvisols", + "name": "Gleyic luvisols", + "rank_loc": "7", "score_loc": 0.035 }, "ph": { @@ -886,22 +686,22 @@ }, "site": { "siteData": { - "componentID": 103981, - "distance": 73247.232, - "mapunitID": 11413, - "minCompDistance": 73247.2321, + "componentID": 104608, + "distance": 59323.866, + "mapunitID": 11919, + "minCompDistance": 59323.8661, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", - "Description_es": "Los Phaeozems Calcáricos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems calcáreos son calcáreos en la parte superior del subsuelo.", - "Description_fr": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", - "Description_ks": "Calcaric Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Calcaric Phaeozems are calcareous in the upper portion of the subsoil.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", - "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Estos suelos tienen grandes cantidades de carbonato cálcico libre en el horizonte superior del suelo, por lo que el pH del suelo será superior a 7,0.", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. ", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
These soils will have large amounts of free calcium carbonate in the upper soil horizon, and thus the soil pH will be > 7.0. " + "Description_en": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_es": "Los Luvisoles Gleyicos son suelos productivos con alta saturación de la base y subsuelos relativamente arcillosos.
Los Luvisoles Gleyicos están saturados con agua subterránea poco profunda en el metro superior del perfil del suelo.", + "Description_fr": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Description_ks": "Gleyic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Gleyic Luvisols are saturated with shallow groundwater in the upper one meter of the soil profile.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " } }, "texture": { @@ -925,83 +725,183 @@ "sl7": 120 }, "cec": { - "sl1": 27.0, - "sl2": 27.0, - "sl3": 27.0, - "sl4": 26.8, - "sl5": 26.43, - "sl6": 25.6, - "sl7": 25.0 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 28.4, + "sl5": 25.71, + "sl6": 22.6, + "sl7": 21.17 }, "clay": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 32.4, - "sl5": 33.43, - "sl6": 34.2, - "sl7": 34.5 + "sl1": 28.0, + "sl2": 28.0, + "sl3": 28.0, + "sl4": 26.8, + "sl5": 26.57, + "sl6": 26.0, + "sl7": 25.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 1.0, + "sl7": 1.33 }, "id": { - "component": "Stagnic phaeozems", - "name": "Stagnic phaeozems", - "rank_loc": "10", + "component": "Gleyic chernozems", + "name": "Gleyic chernozems", + "rank_loc": "8", "score_loc": 0.035 }, "ph": { - "sl1": 6.4, - "sl2": 6.4, - "sl3": 6.4, - "sl4": 6.56, - "sl5": 6.66, - "sl6": 6.74, - "sl7": 6.78 - }, - "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.6, - "sl5": 2.86, - "sl6": 3.4, - "sl7": 3.67 + "sl1": 6.7, + "sl2": 6.7, + "sl3": 6.7, + "sl4": 6.98, + "sl5": 7.09, + "sl6": 7.2, + "sl7": 7.25 + }, + "rock_fragments": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 2.2, + "sl5": 2.43, + "sl6": 2.8, + "sl7": 3.0 }, "sand": { - "sl1": 28.0, - "sl2": 28.0, - "sl3": 28.0, - "sl4": 27.6, - "sl5": 27.14, - "sl6": 26.8, - "sl7": 26.67 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 34.0, + "sl5": 34.57, + "sl6": 35.8, + "sl7": 36.67 }, "site": { "siteData": { - "componentID": 103607, - "distance": 84701.498, - "mapunitID": 11115, - "minCompDistance": 84701.4983, + "componentID": 103642, + "distance": 89693.916, + "mapunitID": 11141, + "minCompDistance": 89693.9156, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", - "Description_es": "Los Phaeozems Stágnicos son suelos fértiles y productivos de praderas con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los Faeozems estancados están encharcados y saturados en y por encima de los horizontes superficiales durante las épocas húmedas del año.", - "Description_fr": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", - "Description_ks": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", - "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Puede ser necesario el drenaje de estos suelos.
Dado que la saturación es causada por el agua superficial, podría ser útil el drenaje superficial y/o el mantenimiento de la cubierta para mejorar la infiltración y la retención de agua.
Considerar el uso de cultivos con raíces poco profundas.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
Se puede conseguir un uso más eficiente del N por parte de los cultivos en estos suelos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", - "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + "Description_en": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", + "Description_es": "Los Chernozems Gleyicos son suelos altamente productivos con buenas propiedades físicas y químicas.
Tienen una alta calidad de suelo y capas superficiales oscuras y ricas.
Los chernozems gleyicos están saturados de agua subterránea poco profunda por encima de un metro de profundidad del suelo.", + "Description_fr": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", + "Description_ks": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", + "Management_en": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Son, en general, suelos excelentes para la producción de cultivos.
Tienen una excelente porosidad y retención de agua, y son adecuados para una amplia gama de sistemas de producción de cultivos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación procedente de aguas subterráneas, puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + } + }, + "texture": { + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.4, + "sl5": 17.43, + "sl6": 17.4, + "sl7": 17.0 + }, + "clay": { + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 31.8, + "sl5": 32.0, + "sl6": 31.8, + "sl7": 31.17 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.83 + }, + "id": { + "component": "Gleyic phaeozems", + "name": "Gleyic phaeozems", + "rank_loc": "9", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.3, + "sl2": 6.3, + "sl3": 6.3, + "sl4": 6.5, + "sl5": 6.57, + "sl6": 6.66, + "sl7": 6.75 + }, + "rock_fragments": { + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 8.0, + "sl5": 8.86, + "sl6": 9.0, + "sl7": 9.33 + }, + "sand": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 23.0, + "sl5": 23.14, + "sl6": 23.2, + "sl7": 23.0 + }, + "site": { + "siteData": { + "componentID": 103605, + "distance": 12988.596, + "mapunitID": 11113, + "minCompDistance": 12988.596, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", + "Description_es": "Los Phaeozems Gléyicos son suelos fértiles y productivos de pastizales con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los feozems gleyicos están saturados de agua subterránea poco profunda a menos de un metro de la superficie del suelo.", + "Description_fr": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", + "Description_ks": "Gleyic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Gleyic Phaeozems are saturated with shallow groundwater within one meter of the soil surface.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son muy productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación a través de las aguas subterráneas, esto puede no ser posible, por lo que hay que considerar los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
However, since this is saturation via groundwater this may not be possible, and thus shallow-rooted crops must be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " } }, "texture": { @@ -1025,22 +925,122 @@ "sl7": 120 }, "cec": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 26.6, - "sl5": 25.29, - "sl6": 23.8, - "sl7": 22.67 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 15.0, + "sl5": 15.0, + "sl6": 14.8, + "sl7": 14.5 }, "clay": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 31.4, + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 23.0, + "sl5": 24.14, + "sl6": 24.6, + "sl7": 24.5 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 + }, + "id": { + "component": "Haplic luvisols", + "name": "Haplic luvisols", + "rank_loc": "10", + "score_loc": 0.035 + }, + "ph": { + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.02, + "sl5": 6.06, + "sl6": 6.12, + "sl7": 6.2 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 11.0, + "sl5": 12.29, + "sl6": 13.6, + "sl7": 14.17 + }, + "sand": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 31.2, "sl5": 31.71, - "sl6": 31.4, - "sl7": 30.83 + "sl6": 33.0, + "sl7": 33.83 + }, + "site": { + "siteData": { + "componentID": 104597, + "distance": 22984.344, + "mapunitID": 11909, + "minCompDistance": 22984.3437, + "share": 100, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_es": "Los Luvisoles Háplicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.", + "Description_fr": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Description_ks": "Haplic Luvisols are productive soils with high base saturation and relatively clayey subsoils.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." + } + }, + "texture": { + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", + "sl7": "Loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 17.6, + "sl5": 18.29, + "sl6": 18.6, + "sl7": 18.33 + }, + "clay": { + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 26.8, + "sl5": 28.71, + "sl6": 29.6, + "sl7": 29.5 }, "ec": { "sl1": 1.0, @@ -1048,67 +1048,67 @@ "sl3": 1.0, "sl4": 1.0, "sl5": 1.14, - "sl6": 1.6, - "sl7": 1.83 + "sl6": 1.4, + "sl7": 1.67 }, "id": { - "component": "Gleyic chernozems", - "name": "Gleyic chernozems", + "component": "Mollic gleysols", + "name": "Mollic gleysols", "rank_loc": "11", "score_loc": 0.035 }, "ph": { - "sl1": 6.9, - "sl2": 6.9, - "sl3": 6.9, - "sl4": 7.06, - "sl5": 7.16, - "sl6": 7.28, - "sl7": 7.35 + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.02, + "sl5": 6.03, + "sl6": 6.12, + "sl7": 6.22 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.0, - "sl5": 2.29, - "sl6": 3.2, - "sl7": 3.5 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 2.8, + "sl5": 2.71, + "sl6": 3.0, + "sl7": 3.33 }, "sand": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 26.0, - "sl5": 25.86, - "sl6": 26.0, - "sl7": 26.5 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 21.4, + "sl5": 20.86, + "sl6": 20.8, + "sl7": 21.0 }, "site": { "siteData": { - "componentID": 103642, - "distance": 89693.916, - "mapunitID": 11141, - "minCompDistance": 89693.9156, + "componentID": 104132, + "distance": 31367.734, + "mapunitID": 11539, + "minCompDistance": 31367.734, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", - "Description_es": "Los Chernozems Gleyicos son suelos altamente productivos con buenas propiedades físicas y químicas.
Tienen una alta calidad de suelo y capas superficiales oscuras y ricas.
Los chernozems gleyicos están saturados de agua subterránea poco profunda por encima de un metro de profundidad del suelo.", - "Description_fr": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", - "Description_ks": "Gleyic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality, and dark and rich topsoil layers.
Gleyic Chernozems are saturated with shallow groundwater above one meter of soil depth. ", - "Management_en": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_es": "Son, en general, suelos excelentes para la producción de cultivos.
Tienen una excelente porosidad y retención de agua, y son adecuados para una amplia gama de sistemas de producción de cultivos.
Puede ser necesario el drenaje de estos suelos.
Sin embargo, al tratarse de una saturación procedente de aguas subterráneas, puede no ser posible la instalación de líneas de drenaje, por lo que deben considerarse los cultivos de raíz superficial.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
El uso más eficiente del N por parte de los cultivos en estos suelos puede lograrse mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", - "Management_fr": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", - "Management_ks": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Drainage of these soils may be needed.
However, since this is saturation from groundwater, installation of drainage lines may not be possible, and thus shallow-rooted crops should be considered.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " + "Description_en": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", + "Description_es": "Los Mollic Gleysols tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles móllicos tienen relativamente más materia orgánica y nutrientes en los horizontes superficiales.", + "Description_fr": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", + "Description_ks": "Mollic Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Mollic Gleysols have relatively higher organic matter and nutrients in surface horizons.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados y, si se cultivan, se requiere un drenaje importante.
Una vez drenados, estos suelos pueden ser muy productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", + "sl1": "Silt loam", + "sl2": "Silt loam", + "sl3": "Silt loam", + "sl4": "Silt loam", "sl5": "Clay loam", "sl6": "Clay loam", "sl7": "Clay loam" @@ -1125,92 +1125,92 @@ "sl7": 120 }, "cec": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 24.2, - "sl5": 22.86, - "sl6": 21.0, - "sl7": 20.0 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 14.6, + "sl5": 13.57, + "sl6": 12.8, + "sl7": 12.33 }, "clay": { - "sl1": 28.0, - "sl2": 28.0, - "sl3": 28.0, - "sl4": 28.6, - "sl5": 28.43, - "sl6": 27.6, - "sl7": 27.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.2, + "sl5": 14.43, + "sl6": 14.6, + "sl7": 14.5 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, "sl5": 1.29, - "sl6": 1.8, - "sl7": 2.0 + "sl6": 1.2, + "sl7": 1.17 }, "id": { - "component": "Calcic chernozems", - "name": "Calcic chernozems", + "component": "Stagnic phaeozems", + "name": "Stagnic phaeozems", "rank_loc": "12", "score_loc": 0.035 }, "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4, - "sl4": 7.58, - "sl5": 7.7, - "sl6": 7.84, - "sl7": 7.9 + "sl1": 6.2, + "sl2": 6.2, + "sl3": 6.2, + "sl4": 6.36, + "sl5": 6.44, + "sl6": 6.54, + "sl7": 6.6 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 5.8, - "sl5": 7.57, - "sl6": 9.8, - "sl7": 10.83 + "sl1": 15.0, + "sl2": 15.0, + "sl3": 15.0, + "sl4": 18.8, + "sl5": 20.71, + "sl6": 23.0, + "sl7": 24.0 }, "sand": { - "sl1": 29.0, - "sl2": 29.0, - "sl3": 29.0, - "sl4": 28.4, - "sl5": 28.71, - "sl6": 29.8, - "sl7": 30.33 + "sl1": 40.0, + "sl2": 40.0, + "sl3": 40.0, + "sl4": 42.2, + "sl5": 43.43, + "sl6": 45.0, + "sl7": 46.0 }, "site": { "siteData": { - "componentID": 103635, - "distance": 90543.48, - "mapunitID": 11138, - "minCompDistance": 90543.4796, + "componentID": 103607, + "distance": 84701.498, + "mapunitID": 11115, + "minCompDistance": 84701.4983, "share": 100, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", - "Description_es": "Los Chernozems Cálcicos son suelos altamente productivos con buenas propiedades físicas y químicas.
Tienen una alta calidad de suelo y capas superficiales oscuras y ricas.
Los Chernozems Cálcicos tienen carbonatos y un pH elevado en la parte superior del suelo.", - "Description_fr": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", - "Description_ks": "Calcic Chernozems are highly productive soils with good physical and chemical properties.
They have high soil quality and dark and rich topsoil layers.
Calcic Chernozems have carbonates and high pH in the upper portion of soil.", - "Management_en": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", - "Management_es": "Son, en general, suelos excelentes para la producción de cultivos.
Tienen una excelente porosidad y retención de agua, y son adecuados para una amplia gama de sistemas de producción de cultivos.
Algunos cultivos especiales pueden ser sensibles a los suelos con pH más alto, y puede ser necesario un suplemento de hierro.
Puede ser necesario el uso de fertilizantes.
Al tener un subsuelo calcáreo, pueden fijar el fósforo, por lo que puede ser necesaria una fertilización adecuada de P.", - "Management_fr": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. ", - "Management_ks": "These are, in general, excellent soils for crop production.
They have excellent porosity and water holding, and are suitable for a wide range of crop production systems.
Some specialty crops may be sensitive to being grown in higher pH soils, and supplemental iron may be needed.
Use of fertilizers may be needed.
Because they have a calcareous subsoil they can fix phosphorus, and thus proper P fertilization may be needed. " + "Description_en": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", + "Description_es": "Los Phaeozems Stágnicos son suelos fértiles y productivos de praderas con una materia orgánica y una saturación de bases relativamente altas.
Su presencia en climas secos significa que es probable que el riego sea necesario para la producción.
Los Faeozems estancados están encharcados y saturados en y por encima de los horizontes superficiales durante las épocas húmedas del año.", + "Description_fr": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", + "Description_ks": "Stagnic Phaeozems are fertile and productive soils of grasslands with relatively high organic matter and base saturation.
Their occurrence in dry climates means that irrigation is likely needed for production.
Stagnic Phaeozems are ponded and saturated in and above surface horizons during wet times of the year.", + "Management_en": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_es": "Estos suelos son altamente productivos y fértiles, y constituyen excelentes tierras de cultivo.
Son ricos en materia orgánica.
Sin embargo, corren el riesgo de perder el suelo por la erosión del viento y del agua.
Por lo tanto, se necesitan prácticas para mantener la cobertura del suelo (mantillos, labranza de conservación, cortavientos).
Puede ser necesario el drenaje de estos suelos.
Dado que la saturación es causada por el agua superficial, podría ser útil el drenaje superficial y/o el mantenimiento de la cubierta para mejorar la infiltración y la retención de agua.
Considerar el uso de cultivos con raíces poco profundas.
Si se fertiliza y no se drena, es posible la pérdida de nitrógeno (N) aplicado por desnitrificación o lixiviación.
Se puede conseguir un uso más eficiente del N por parte de los cultivos en estos suelos mediante: 1) el drenaje, y, 2) el uso de fertilizantes de N de liberación lenta (si están disponibles).", + "Management_fr": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). ", + "Management_ks": "These soils are highly productive and fertile, and make excellent cropland.
They are rich in organic matter.
However, they are at risk for soil loss through both wind and water erosion.
Thus, practices to maintain soil cover (mulches, conservation tillage, windbreaks) are needed.
Drainage of these soils may be needed.
Since saturation is caused by surface water, surface drainage andmaintenance of cover to improve infiltration and water holding could be useful.
Consider use of shallow rooted crops.
If fertilized and not drained, loss of applied nitrogen (N) by denitrification or leaching is possible.
More efficient crop N use in these soils can be achieved by: 1) drainage, and, 2) use of slow-release N fertilizers (if available). " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam", + "sl5": "Loam", + "sl6": "Loam", "sl7": "Loam" } } @@ -1227,47 +1227,35 @@ "componentData": "Data Complete", "componentID": 103927, "name": "Haplic andosols", - "rank_data": "2", + "rank_data": "3", "rank_data_loc": "1", "rank_loc": 1, "score_data": 0.431, "score_data_loc": 1.0, "score_loc": 0.142 }, - { - "component": "Haplic phaeozems", - "componentData": "Data Complete", - "componentID": 103604, - "name": "Haplic phaeozems", - "rank_data": "3", - "rank_data_loc": "2", - "rank_loc": 2, - "score_data": 0.431, - "score_data_loc": 0.847, - "score_loc": 0.054 - }, { "component": "Calcaric phaeozems", "componentData": "Data Complete", "componentID": 103981, "name": "Calcaric phaeozems", "rank_data": "1", - "rank_data_loc": "3", - "rank_loc": 9, + "rank_data_loc": "2", + "rank_loc": 3, "score_data": 0.431, "score_data_loc": 0.814, "score_loc": 0.035 }, { - "component": "Gleyic luvisols", - "componentData": "Missing Data", - "componentID": 104608, - "name": "Gleyic luvisols", - "rank_data": "4", - "rank_data_loc": "4", + "component": "Gleyic chernozems", + "componentData": "Data Complete", + "componentID": 103642, + "name": "Gleyic chernozems", + "rank_data": "2", + "rank_data_loc": "3", "rank_loc": 8, - "score_data": 0.385, - "score_data_loc": 0.733, + "score_data": 0.431, + "score_data_loc": 0.814, "score_loc": 0.035 }, { @@ -1275,6 +1263,18 @@ "componentData": "Data Complete", "componentID": 104597, "name": "Haplic luvisols", + "rank_data": "4", + "rank_data_loc": "4", + "rank_loc": 10, + "score_data": 0.431, + "score_data_loc": 0.814, + "score_loc": 0.035 + }, + { + "component": "Eutric cambisols", + "componentData": "Data Complete", + "componentID": 104610, + "name": "Eutric cambisols", "rank_data": "5", "rank_data_loc": "5", "rank_loc": 6, @@ -1283,25 +1283,37 @@ "score_loc": 0.035 }, { - "component": "Umbric andosols", - "componentData": "Data Complete", - "componentID": 103928, - "name": "Umbric andosols", + "component": "Gleyic phaeozems", + "componentData": "Missing Data", + "componentID": 103605, + "name": "Gleyic phaeozems", "rank_data": "6", "rank_data_loc": "6", - "rank_loc": 3, + "rank_loc": 9, "score_data": 0.385, "score_data_loc": 0.733, "score_loc": 0.035 }, + { + "component": "Haplic phaeozems", + "componentData": "Data Complete", + "componentID": 103604, + "name": "Haplic phaeozems", + "rank_data": "10", + "rank_data_loc": "7", + "rank_loc": 2, + "score_data": 0.068, + "score_data_loc": 0.214, + "score_loc": 0.054 + }, { "component": "Calcic chernozems", "componentData": "Data Complete", "componentID": 103635, "name": "Calcic chernozems", "rank_data": "7", - "rank_data_loc": "7", - "rank_loc": 12, + "rank_data_loc": "8", + "rank_loc": 4, "score_data": 0.068, "score_data_loc": 0.181, "score_loc": 0.035 @@ -1312,32 +1324,20 @@ "componentID": 104276, "name": "Eutric gleysols", "rank_data": "8", - "rank_data_loc": "8", - "rank_loc": 5, - "score_data": 0.068, - "score_data_loc": 0.181, - "score_loc": 0.035 - }, - { - "component": "Gleyic chernozems", - "componentData": "Data Complete", - "componentID": 103642, - "name": "Gleyic chernozems", - "rank_data": "9", "rank_data_loc": "9", - "rank_loc": 11, + "rank_loc": 5, "score_data": 0.068, "score_data_loc": 0.181, "score_loc": 0.035 }, { - "component": "Gleyic phaeozems", + "component": "Gleyic luvisols", "componentData": "Missing Data", - "componentID": 103605, - "name": "Gleyic phaeozems", - "rank_data": "10", + "componentID": 104608, + "name": "Gleyic luvisols", + "rank_data": "9", "rank_data_loc": "10", - "rank_loc": 4, + "rank_loc": 7, "score_data": 0.068, "score_data_loc": 0.181, "score_loc": 0.035 @@ -1349,7 +1349,7 @@ "name": "Mollic gleysols", "rank_data": "11", "rank_data_loc": "11", - "rank_loc": 7, + "rank_loc": 11, "score_data": 0.068, "score_data_loc": 0.181, "score_loc": 0.035 @@ -1361,7 +1361,7 @@ "name": "Stagnic phaeozems", "rank_data": "12", "rank_data_loc": "12", - "rank_loc": 10, + "rank_loc": 12, "score_data": 0.068, "score_data_loc": 0.181, "score_loc": 0.035 diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json index fb213d6..0341681 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[7.3318,-1.4631].json @@ -25,35 +25,35 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 17.6, - "sl5": 17.86, - "sl6": 18.4, - "sl7": 18.83 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 7.29, + "sl6": 7.8, + "sl7": 7.83 }, "clay": { - "sl1": 33.0, - "sl2": 33.0, - "sl3": 33.0, - "sl4": 35.8, - "sl5": 36.71, - "sl6": 37.8, - "sl7": 38.5 + "sl1": 17.0, + "sl2": 17.0, + "sl3": 17.0, + "sl4": 23.4, + "sl5": 26.57, + "sl6": 29.6, + "sl7": 30.83 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.6, - "sl7": 0.67 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Eutric gleysols", - "name": "Eutric gleysols", + "name": "Eutric gleysols1", "rank_loc": "1", "score_loc": 0.025 }, @@ -61,28 +61,28 @@ "sl1": 5.9, "sl2": 5.9, "sl3": 5.9, - "sl4": 5.96, - "sl5": 5.97, - "sl6": 6.02, - "sl7": 6.05 + "sl4": 5.82, + "sl5": 5.8, + "sl6": 5.8, + "sl7": 5.8 }, "rock_fragments": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 17.6, - "sl5": 17.14, - "sl6": 14.8, - "sl7": 15.83 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 16.4, + "sl5": 19.71, + "sl6": 23.4, + "sl7": 25.33 }, "sand": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 33.6, - "sl5": 33.29, - "sl6": 32.8, - "sl7": 31.83 + "sl1": 63.0, + "sl2": 63.0, + "sl3": 63.0, + "sl4": 57.8, + "sl5": 54.86, + "sl6": 51.8, + "sl7": 50.33 }, "site": { "siteData": { @@ -105,9 +105,109 @@ } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 11.2, + "sl5": 10.57, + "sl6": 10.2, + "sl7": 10.5 + }, + "clay": { + "sl1": 27.0, + "sl2": 27.0, + "sl3": 27.0, + "sl4": 30.0, + "sl5": 31.57, + "sl6": 33.0, + "sl7": 33.67 + }, + "ec": { + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.4, + "sl7": 0.33 + }, + "id": { + "component": "Eutric plinthosols", + "name": "Eutric plinthosols", + "rank_loc": "2", + "score_loc": 0.022 + }, + "ph": { + "sl1": 4.8, + "sl2": 4.8, + "sl3": 4.8, + "sl4": 4.94, + "sl5": 5.0, + "sl6": 5.06, + "sl7": 5.08 + }, + "rock_fragments": { + "sl1": 7.0, + "sl2": 7.0, + "sl3": 7.0, + "sl4": 4.8, + "sl5": 4.86, + "sl6": 5.4, + "sl7": 5.33 + }, + "sand": { + "sl1": 43.0, + "sl2": 43.0, + "sl3": 43.0, + "sl4": 41.2, + "sl5": 40.71, + "sl6": 40.6, + "sl7": 40.5 + }, + "site": { + "siteData": { + "componentID": 133231, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 35, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", + "Description_es": "Los Plinthosoles Éutricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles eútricos tienen una alta saturación de bases en los subsuelos.", + "Description_fr": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", + "Description_ks": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", + "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.", + "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una escasa fertilidad del suelo, que combinada con un suelo poco profundo y rocoso hace que no sea posible la agricultura.
Estos suelos deberían utilizarse para cosas como materiales de superficie para carreteras.", + "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.", + "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads." + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", "sl4": "Clay loam", "sl5": "Clay loam", "sl6": "Clay loam", @@ -125,22 +225,122 @@ "sl7": 120 }, "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.8, - "sl5": 7.29, + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.4, + "sl5": 8.57, "sl6": 7.8, - "sl7": 7.83 + "sl7": 8.17 }, "clay": { - "sl1": 17.0, - "sl2": 17.0, - "sl3": 17.0, - "sl4": 23.4, - "sl5": 26.57, - "sl6": 29.6, - "sl7": 30.83 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 24.2, + "sl5": 24.29, + "sl6": 24.2, + "sl7": 24.5 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 + }, + "id": { + "component": "Eutric leptosols", + "name": "Eutric leptosols", + "rank_loc": "3", + "score_loc": 0.016 + }, + "ph": { + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.96, + "sl5": 4.99, + "sl6": 5.04, + "sl7": 5.08 + }, + "rock_fragments": { + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.8, + "sl5": 7.0, + "sl6": 9.4, + "sl7": 9.67 + }, + "sand": { + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 49.2, + "sl5": 49.71, + "sl6": 50.8, + "sl7": 50.67 + }, + "site": { + "siteData": { + "componentID": 133765, + "distance": 30108.037, + "mapunitID": 36118, + "minCompDistance": 30108.037, + "share": 100, + "soilDepth": 40 + }, + "siteDescription": { + "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + } + }, + "texture": { + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 6.0, + "sl6": 6.4, + "sl7": 6.67 + }, + "clay": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 26.4, + "sl5": 29.0, + "sl6": 31.6, + "sl7": 33.17 }, "ec": { "sl1": 0.0, @@ -152,56 +352,56 @@ "sl7": 0.0 }, "id": { - "component": "Eutric plinthosols", - "name": "Eutric plinthosols", - "rank_loc": "2", - "score_loc": 0.022 + "component": "Dystric planosols", + "name": "Dystric planosols", + "rank_loc": "4", + "score_loc": 0.016 }, "ph": { - "sl1": 5.9, - "sl2": 5.9, - "sl3": 5.9, - "sl4": 5.82, - "sl5": 5.8, - "sl6": 5.8, - "sl7": 5.8 - }, - "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 16.4, - "sl5": 19.71, - "sl6": 23.4, - "sl7": 25.33 + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.16, + "sl5": 5.17, + "sl6": 5.18, + "sl7": 5.18 }, - "sand": { - "sl1": 63.0, - "sl2": 63.0, - "sl3": 63.0, - "sl4": 57.8, - "sl5": 54.86, - "sl6": 51.8, - "sl7": 50.33 + "rock_fragments": { + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.2, + "sl5": 20.71, + "sl6": 21.4, + "sl7": 20.33 + }, + "sand": { + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.2, + "sl5": 44.86, + "sl6": 42.4, + "sl7": 40.83 }, "site": { "siteData": { - "componentID": 133231, + "componentID": 133240, "distance": 0.0, "mapunitID": 36001, "minCompDistance": 0.0, - "share": 35, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", - "Description_es": "Los Plinthosoles Éutricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles eútricos tienen una alta saturación de bases en los subsuelos.", - "Description_fr": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", - "Description_ks": "Eutric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Eutric Plinthosols are have high base saturation in subsoils.", - "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.", - "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una escasa fertilidad del suelo, que combinada con un suelo poco profundo y rocoso hace que no sea posible la agricultura.
Estos suelos deberían utilizarse para cosas como materiales de superficie para carreteras.", - "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.", - "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads." + "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.", + "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", + "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.", + "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", + "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed." } }, "texture": { @@ -209,9 +409,9 @@ "sl2": "Sandy loam", "sl3": "Sandy loam", "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -252,10 +452,10 @@ "sl7": 0.0 }, "id": { - "component": "Dystric planosols", - "name": "Dystric planosols", - "rank_loc": "3", - "score_loc": 0.016 + "component": "Ferralic arenosols", + "name": "Ferralic arenosols", + "rank_loc": "5", + "score_loc": 0.011 }, "ph": { "sl1": 5.0, @@ -286,22 +486,22 @@ }, "site": { "siteData": { - "componentID": 133240, - "distance": 0.0, - "mapunitID": 36001, - "minCompDistance": 0.0, + "componentID": 133291, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 49166.7104, "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", - "Description_es": "Los Planosoles Dístricos están estacionalmente encharcados o saturados de agua en la parte superior debido a un subsuelo rico en arcilla y lentamente permeable.
Estos suelos son propensos a la compactación y requieren de drenaje para la producción de cultivos.
Los Planosoles Dístricos son suelos menos productivos con baja saturación de base en el subsuelo.", - "Description_fr": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", - "Description_ks": "Dystric Planosols are seasonally ponded or saturated with water in the upper portion due to a slowly permeable, clay-rich subsoil.
These soils are prone to compaction and require drainage for crop production.
Dystric Planosols are less productive soils with low base saturation in the subsoil.", - "Management_en": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", - "Management_es": "Situados en terrenos planos, estos suelos son los más adecuados para la producción de arroz con cáscara.
Se requerirá el drenaje para la producción.
Los rendimientos más elevados requerirán una fertilización adicional.
Los niveles de calcio son muy bajos en el perfil inferior de este suelo.
Se necesitará una fertilización suplementaria.", - "Management_fr": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed.", - "Management_ks": "Located on flat land, these soils are best suited for paddy rice production.
Drainage will be required for production.
Highest yields will require additional fertilization.
Very low levels of calcium are available in the lower profile of this soil.
Supplemental fertilization will be needed." + "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", + "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " } }, "texture": { @@ -325,93 +525,93 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.71, - "sl6": 6.8, - "sl7": 6.83 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.6, + "sl5": 17.86, + "sl6": 18.4, + "sl7": 18.83 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.2, - "sl5": 30.29, - "sl6": 33.2, - "sl7": 34.33 + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 35.8, + "sl5": 36.71, + "sl6": 37.8, + "sl7": 38.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.67 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols1", - "rank_loc": "4", - "score_loc": 0.016 + "component": "Dystric gleysols", + "name": "Dystric gleysols", + "rank_loc": "6", + "score_loc": 0.011 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.12, - "sl5": 6.07, + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.96, + "sl5": 5.97, "sl6": 6.02, - "sl7": 6.02 + "sl7": 6.05 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 9.8, - "sl5": 10.43, - "sl6": 10.6, - "sl7": 10.5 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 17.6, + "sl5": 17.14, + "sl6": 14.8, + "sl7": 15.83 }, "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 60.2, - "sl5": 57.57, - "sl6": 54.8, - "sl7": 53.0 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.6, + "sl5": 33.29, + "sl6": 32.8, + "sl7": 31.83 }, "site": { "siteData": { - "componentID": 133488, - "distance": 15267.702, - "mapunitID": 36051, - "minCompDistance": 15267.7017, - "share": 45, + "componentID": 133232, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. " } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -419,75 +619,99 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 40 + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.0 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.14, + "sl6": 17.6, + "sl7": 17.5 }, "clay": { - "sl1": 26.0, - "sl2": 26.0, - "sl3": 26.0, - "sl4": 27.0 + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.2, + "sl5": 32.14, + "sl6": 31.6, + "sl7": 31.33 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Eutric leptosols", - "name": "Eutric leptosols", - "rank_loc": "5", - "score_loc": 0.016 + "component": "Dystric fluvisols", + "name": "Dystric fluvisols1", + "rank_loc": "7", + "score_loc": 0.011 }, "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.55 + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.24, + "sl5": 6.3, + "sl6": 6.38, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 30.5 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.6, + "sl5": 9.86, + "sl6": 10.2, + "sl7": 10.33 }, "sand": { - "sl1": 45.0, - "sl2": 45.0, - "sl3": 45.0, - "sl4": 44.0 + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.2, + "sl5": 36.86, + "sl6": 38.4, + "sl7": 38.83 }, "site": { "siteData": { - "componentID": 133765, - "distance": 30108.037, - "mapunitID": 36118, - "minCompDistance": 30108.037, - "share": 100, - "soilDepth": 40 + "componentID": 133237, + "distance": 0.0, + "mapunitID": 36001, + "minCompDistance": 0.0, + "share": 5, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_es": "Los Leptosoles Eútricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los Leptosoles eútricos tienen una alta saturación de la base sobre la capa limitante de las raíces poco profundas. ", - "Description_fr": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Description_ks": "Eutric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Eutric Leptosols have high base saturation over the shallow root limiting layer. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables deben ser utilizados para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Se debe considerar el uso exclusivo para el pastoreo o la agroforestería.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Estos suelos pueden ser productivos para la agricultura, pero el enfoque debe ser el uso para el pastoreo.
Cualquier uso para el cultivo debe limitarse y combinarse con prácticas de conservación del suelo.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Onlyuses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
These soils can be productive for agriculture, but the focus should be on use for grazing.
Any use for cropping must be limited and combined with soil conservation practices. " + "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -501,22 +725,22 @@ "sl7": 120 }, "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 6.4, - "sl5": 6.29, - "sl6": 6.2, - "sl7": 6.17 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 2.4, + "sl5": 2.29, + "sl6": 2.2, + "sl7": 2.0 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 28.8, - "sl5": 31.14, - "sl6": 33.4, - "sl7": 34.33 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.2, + "sl5": 6.43, + "sl6": 6.8, + "sl7": 7.0 }, "ec": { "sl1": 0.0, @@ -528,202 +752,242 @@ "sl7": 0.0 }, "id": { - "component": "Haplic acrisols", - "name": "Haplic acrisols1", - "rank_loc": "6", - "score_loc": 0.016 + "component": "Dystric leptosols", + "name": "Dystric leptosols", + "rank_loc": "8", + "score_loc": 0.011 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.04, - "sl5": 5.03, - "sl6": 5.02, - "sl7": 5.02 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.34, + "sl6": 5.36, + "sl7": 5.37 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 12.4, - "sl5": 13.29, - "sl6": 13.0, - "sl7": 14.0 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.2, + "sl5": 4.43, + "sl6": 4.6, + "sl7": 4.5 }, "sand": { - "sl1": 59.0, - "sl2": 59.0, - "sl3": 59.0, - "sl4": 54.4, - "sl5": 52.29, - "sl6": 50.2, - "sl7": 49.17 + "sl1": 87.0, + "sl2": 87.0, + "sl3": 87.0, + "sl4": 86.8, + "sl5": 86.57, + "sl6": 86.2, + "sl7": 86.0 }, "site": { "siteData": { - "componentID": 134061, - "distance": 33211.766, - "mapunitID": 36185, - "minCompDistance": 33211.7658, - "share": 10, - "soilDepth": 200 + "componentID": 133329, + "distance": 48484.096, + "mapunitID": 36018, + "minCompDistance": 48484.0959, + "share": 5, + "soilDepth": 40 }, "siteDescription": { - "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Description_es": "Los Leptosoles Dístricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles dísticos tienen una baja saturación de la base sobre la capa limitante de las raíces poco profundas. ", + "Description_fr": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Description_ks": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", + "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Este suelo prácticamente no tiene calcio disponible para el uso de las plantas.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cobertura.", + "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", + "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } }, { "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20 + "sl3": 20, + "sl4": 40 }, "cec": { "sl1": 6.0, "sl2": 6.0, - "sl3": 6.0 + "sl3": 6.0, + "sl4": 7.0 }, "clay": { - "sl1": 12.0, - "sl2": 12.0, - "sl3": 12.0 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 22.0 }, "ec": { "sl1": 1.0, "sl2": 1.0, - "sl3": 1.0 + "sl3": 1.0, + "sl4": 0.5 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols1", - "rank_loc": "7", - "score_loc": 0.016 + "component": "Chromic luvisols", + "name": "Chromic luvisols", + "rank_loc": "9", + "score_loc": 0.008 }, "ph": { - "sl1": 7.4, - "sl2": 7.4, - "sl3": 7.4 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.0 }, "rock_fragments": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0 + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 25.5 }, "sand": { - "sl1": 66.0, - "sl2": 66.0, - "sl3": 66.0 + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 51.5 }, "site": { "siteData": { - "componentID": 148823, - "distance": 33726.73, - "mapunitID": 60, - "minCompDistance": 33726.7301, - "share": 100, - "soilDepth": 20 + "componentID": 133611, + "distance": 56496.236, + "mapunitID": 36082, + "minCompDistance": 56496.236, + "share": 30, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam" } }, { "bottom_depth": { "sl1": 1, "sl2": 10, - "sl3": 20 + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 }, "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 17.0, + "sl5": 16.29, + "sl6": 15.6, + "sl7": 15.33 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.8, + "sl5": 30.14, + "sl6": 30.0, + "sl7": 29.67 }, "ec": { "sl1": 1.0, "sl2": 1.0, - "sl3": 1.0 + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 }, "id": { - "component": "Ferric lixisols", - "name": "Ferric lixisols", - "rank_loc": "8", - "score_loc": 0.014 + "component": "Dystric cambisols", + "name": "Dystric cambisols1", + "rank_loc": "10", + "score_loc": 0.005 }, "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.02, + "sl5": 5.06, + "sl6": 5.12, + "sl7": 5.13 }, "rock_fragments": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.4, + "sl5": 14.43, + "sl6": 15.2, + "sl7": 16.67 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 42.6, + "sl5": 42.57, + "sl6": 42.6, + "sl7": 43.0 }, "site": { "siteData": { - "componentID": 107928, - "distance": 34218.133, - "mapunitID": 1444, - "minCompDistance": 34218.1332, - "share": 50, + "componentID": 133494, + "distance": 15267.702, + "mapunitID": 36051, + "minCompDistance": 15267.7017, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_es": "Los Lixisoles Férricos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta.
Los Lixisoles férricos tienen concentraciones de hierro blandas y cementadas en los subsuelos, y una estructura poco desarrollada entre las concentraciones de hierro que puede ser susceptible de compactación. ", - "Description_fr": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Description_ks": "Ferric Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation.
Ferric Lixisols have soft and cemented iron concentrations in subsoils, and poorly developed structure between iron concentrations which can be susceptible to compaction. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.
Estos suelos son especialmente sensibles a la erosión, por lo que se necesitan prácticas que trabajen para mantener una estructura fuerte del suelo (como los cultivos perennes).", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
These soils are particularly sensitive to erosion, and so practices that work to maintain surface cover and strong soil structure (such as perennial crops) are needed. " + "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", + "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -737,68 +1001,68 @@ "sl7": 120 }, "cec": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 6.4, - "sl5": 6.29, - "sl6": 6.2, - "sl7": 6.17 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.6, + "sl5": 14.71, + "sl6": 15.0, + "sl7": 15.17 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 28.8, - "sl5": 31.14, - "sl6": 33.4, - "sl7": 34.33 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 28.6, + "sl5": 29.86, + "sl6": 30.6, + "sl7": 30.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Dystric gleysols", - "name": "Dystric gleysols", - "rank_loc": "9", - "score_loc": 0.011 + "component": "Dystric plinthosols", + "name": "Dystric plinthosols1", + "rank_loc": "11", + "score_loc": 0.003 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.04, - "sl5": 5.03, - "sl6": 5.02, - "sl7": 5.02 + "sl1": 6.4, + "sl2": 6.4, + "sl3": 6.4, + "sl4": 6.42, + "sl5": 6.44, + "sl6": 6.44, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 12.4, - "sl5": 13.29, - "sl6": 13.0, - "sl7": 14.0 + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.8, + "sl5": 9.29, + "sl6": 13.4, + "sl7": 12.5 }, "sand": { - "sl1": 59.0, - "sl2": 59.0, - "sl3": 59.0, - "sl4": 54.4, - "sl5": 52.29, - "sl6": 50.2, - "sl7": 49.17 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 49.0, + "sl5": 47.71, + "sl6": 46.6, + "sl7": 46.67 }, "site": { "siteData": { - "componentID": 133232, + "componentID": 133239, "distance": 0.0, "mapunitID": 36001, "minCompDistance": 0.0, @@ -806,14 +1070,14 @@ "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", - "Description_es": "Los Gleysoles Dístricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
Es necesario un drenaje profundo para su cultivo.
Los Gleysoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", - "Description_fr": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", - "Description_ks": "Dystric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Dystric Gleysols are less productive soils with low base saturation in the upper portion of soil.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", - "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.
Estos suelos tienen poco calcio, magnesio u otras bases disponibles en el suelo, y pueden requerir fertilización suplementaria.
Si es necesario, el encalado aportará el calcio, y posiblemente el magnesio (cal dolomítica)..", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose.
These soils have little available calcium, magnesium or other bases in the soil, and may require supplemental fertilization.
If needed, liming will supply the calcium, and possibly the magnesium (dolomitic lime).. " + "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.", + "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.", + "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil." } }, "texture": { @@ -831,99 +1095,75 @@ "sl1": 1, "sl2": 10, "sl3": 20, - "sl4": 50, - "sl5": 70, - "sl6": 100, - "sl7": 120 + "sl4": 40 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.71, - "sl6": 6.8, - "sl7": 6.83 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 13.0 }, "clay": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.2, - "sl5": 30.29, - "sl6": 33.2, - "sl7": 34.33 + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 27.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0 }, "id": { - "component": "Dystric fluvisols", - "name": "Dystric fluvisols1", - "rank_loc": "10", - "score_loc": 0.011 + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "12", + "score_loc": 0.002 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.12, - "sl5": 6.07, - "sl6": 6.02, - "sl7": 6.02 + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.55 }, "rock_fragments": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 9.8, - "sl5": 10.43, - "sl6": 10.6, - "sl7": 10.5 + "sl1": 22.0, + "sl2": 22.0, + "sl3": 22.0, + "sl4": 30.5 }, "sand": { - "sl1": 65.0, - "sl2": 65.0, - "sl3": 65.0, - "sl4": 60.2, - "sl5": 57.57, - "sl6": 54.8, - "sl7": 53.0 + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 44.0 }, "site": { "siteData": { - "componentID": 133237, - "distance": 0.0, - "mapunitID": 36001, - "minCompDistance": 0.0, + "componentID": 133290, + "distance": 49166.71, + "mapunitID": 36011, + "minCompDistance": 49166.7104, "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", - "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", - "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", - "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", + "sl4": "Loam" } }, { @@ -937,22 +1177,22 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 7.0, - "sl5": 7.0, - "sl6": 7.0, - "sl7": 7.0 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 6.0, + "sl6": 6.4, + "sl7": 6.67 }, "clay": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0, - "sl4": 21.6, - "sl5": 24.71, - "sl6": 28.0, - "sl7": 29.33 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 26.4, + "sl5": 29.0, + "sl6": 31.6, + "sl7": 33.17 }, "ec": { "sl1": 0.0, @@ -963,57 +1203,57 @@ "sl6": 0.0, "sl7": 0.0 }, - "id": { - "component": "Dystric leptosols", - "name": "Dystric leptosols", - "rank_loc": "11", - "score_loc": 0.011 + "id": { + "component": "Eutric gleysols", + "name": "Eutric gleysols2", + "rank_loc": "Not Displayed", + "score_loc": 0.025 }, "ph": { - "sl1": 6.2, - "sl2": 6.2, - "sl3": 6.2, - "sl4": 6.1, - "sl5": 6.03, - "sl6": 5.96, - "sl7": 5.93 + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.16, + "sl5": 5.17, + "sl6": 5.18, + "sl7": 5.18 }, "rock_fragments": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 18.6, - "sl5": 19.43, - "sl6": 20.2, - "sl7": 19.83 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.2, + "sl5": 20.71, + "sl6": 21.4, + "sl7": 20.33 }, "sand": { - "sl1": 68.0, - "sl2": 68.0, - "sl3": 68.0, - "sl4": 63.2, - "sl5": 60.43, - "sl6": 57.0, - "sl7": 55.33 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.2, + "sl5": 44.86, + "sl6": 42.4, + "sl7": 40.83 }, "site": { "siteData": { - "componentID": 133329, - "distance": 48484.096, - "mapunitID": 36018, - "minCompDistance": 48484.0959, + "componentID": 134213, + "distance": 49713.155, + "mapunitID": 36225, + "minCompDistance": 49166.7104, "share": 5, - "soilDepth": 40 + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", - "Description_es": "Los Leptosoles Dístricos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles dísticos tienen una baja saturación de la base sobre la capa limitante de las raíces poco profundas. ", - "Description_fr": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", - "Description_ks": "Dystric Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Dystic Leptosols have low base saturation over the shallow root limiting layer. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Este suelo prácticamente no tiene calcio disponible para el uso de las plantas.
Cualquier uso agrícola debe ser para el pastoreo o la agroforestería, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
This soil has virtually no calcium available for plant use.
Any agricultural use should be for grazing or agroforestry, with cover continuously maintained. " + "Description_en": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los gleysoles Eútricos tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los Gleysoles Eutricos son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Eutric Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Eutric Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { @@ -1021,9 +1261,9 @@ "sl2": "Sandy loam", "sl3": "Sandy loam", "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1037,90 +1277,90 @@ "sl7": 120 }, "cec": { - "sl1": 13.0, - "sl2": 13.0, - "sl3": 13.0, - "sl4": 11.2, - "sl5": 10.57, - "sl6": 10.2, - "sl7": 10.5 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.6, + "sl5": 6.0, + "sl6": 6.4, + "sl7": 6.67 }, "clay": { - "sl1": 27.0, - "sl2": 27.0, - "sl3": 27.0, - "sl4": 30.0, - "sl5": 31.57, - "sl6": 33.0, - "sl7": 33.67 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 26.4, + "sl5": 29.0, + "sl6": 31.6, + "sl7": 33.17 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.8, - "sl5": 0.57, - "sl6": 0.4, - "sl7": 0.33 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Ferralic arenosols", - "name": "Ferralic arenosols", - "rank_loc": "12", + "component": "Dystric fluvisols", + "name": "Dystric fluvisols2", + "rank_loc": "Not Displayed", "score_loc": 0.011 }, "ph": { - "sl1": 4.8, - "sl2": 4.8, - "sl3": 4.8, - "sl4": 4.94, - "sl5": 5.0, - "sl6": 5.06, - "sl7": 5.08 + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.16, + "sl5": 5.17, + "sl6": 5.18, + "sl7": 5.18 }, "rock_fragments": { - "sl1": 7.0, - "sl2": 7.0, - "sl3": 7.0, - "sl4": 4.8, - "sl5": 4.86, - "sl6": 5.4, - "sl7": 5.33 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 20.2, + "sl5": 20.71, + "sl6": 21.4, + "sl7": 20.33 }, "sand": { - "sl1": 43.0, - "sl2": 43.0, - "sl3": 43.0, - "sl4": 41.2, - "sl5": 40.71, - "sl6": 40.6, - "sl7": 40.5 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.2, + "sl5": 44.86, + "sl6": 42.4, + "sl7": 40.83 }, "site": { "siteData": { - "componentID": 133291, - "distance": 49166.71, - "mapunitID": 36011, - "minCompDistance": 49166.7104, + "componentID": 134011, + "distance": 57794.629, + "mapunitID": 36174, + "minCompDistance": 0.0, "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_es": "Los Arenosoles Ferrálicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos tienen un alto contenido en hierro y una baja retención de nutrientes.", - "Description_fr": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Description_ks": "Ferralic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are high in iron and have low nutrient retention.", - "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_es": "Dado que estos suelos tienen poca capacidad de retención de agua y nutrientes, deben ser fertilizados y regados para obtener una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
Puede ser necesario prestar más atención al suministro de fósforo, ya que el exceso de hierro puede aumentar la fijación de P en estos suelos.", - "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. ", - "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
Increased attention to the supply of phosphorus may be needed, as excessive iron may increase P fixation in these soils. " + "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Clay loam", + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy clay loam", "sl5": "Clay loam", "sl6": "Clay loam", "sl7": "Clay loam" @@ -1164,10 +1404,10 @@ "sl7": 1.67 }, "id": { - "component": "Haplic lixisols", - "name": "Haplic lixisols2", + "component": "Dystric cambisols", + "name": "Dystric cambisols2", "rank_loc": "Not Displayed", - "score_loc": 0.016 + "score_loc": 0.005 }, "ph": { "sl1": 4.9, @@ -1198,22 +1438,22 @@ }, "site": { "siteData": { - "componentID": 134019, - "distance": 52599.161, - "mapunitID": 36178, + "componentID": 134337, + "distance": 16514.333, + "mapunitID": 36265, "minCompDistance": 15267.7017, - "share": 20, + "share": 5, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_es": "Los Lixisoles Háplicos se forman en climas cálidos con subsuelos relativamente arcillosos dominados por caolinita y óxidos de hierro, pero con una saturación de bases relativamente alta. ", - "Description_fr": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Description_ks": "Haplic Lixisols form in warm climates with relatively clayey subsoils dominated by kaolinite and iron oxides, but relatively high base saturation. ", - "Management_en": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_es": "Estos suelos están fuertemente meteorizados, lo que significa que la fertilización (y posiblemente la cal) será necesaria para la producción.
Aunque tienen arcilla caolinita y óxidos de hierro, tienen una toxicidad de aluminio bastante baja.
Las mejores prácticas de producción para este suelo incluirán la fertilización regular, y el cultivo consistente en cultivos perennes o la silvicultura.
Los suelos son sensibles a la erosión, por lo que son importantes las prácticas que mantienen la cobertura de la superficie.", - "Management_fr": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. ", - "Management_ks": "These soils are heavily weathered soils, which means that fertilization (and possibly lime) will be needed for production.
Although they do have kaolinite clay and iron oxides, they have fairly low aluminum toxicity.
Best production practices for this soil will include regular fertilization, and consistent cropping in perennial crops or forestry.
The soils are sensitive to erosion, and so practices that maintain surface cover are important. " + "Description_en": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Cambisoles Dístricos son suelos de amplia ocurrencia con un desarrollo limitado del suelo.
Son suelos menos productivos con baja saturación de bases en la parte superior del suelo.", + "Description_fr": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Cambisols are widely occurring soils with limited soil development.
These are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes del suelo.
Debido a que este suelo tiene una baja saturación de bases, puede ser necesaria la aplicación de bases (a través de la fertlización) para un rendimiento más productivo del cultivo.
Si el pH del suelo es bajo, el calcio (y posiblemente el magnesio, si se utiliza cal dolomítica) puede ser suministrado a través de la adición de cal.
Si el pH del suelo es adecuado para la producción de cultivos, entonces el yeso (CaSO4) puede ser utilizado como fuente de Ca, si es necesario, u otras fuentes como MgSO4 podrían ser aplicadas (si la prueba del suelo indica una necesidad).
Una fertilización adecuada también aportará potasio, si el análisis del suelo indica que es necesario.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
Because this soil has a low base saturation, the application of bases (through fertlization) may be needed for most productive crop yield.
If the soil pH is low calcium (and possibly magnesium, if dolomitic lime is used) can be supplied through the addition of lime.
If the soil pH is suitable for crop production then gypsum (CaSO4) can be used as the Ca source, if needed, or other sources such as MgSO4 could be applied (if soil test indicates a need).
Proper fertilization will also supply potassium, if soil test indicates a need. " } }, "texture": { @@ -1226,82 +1466,6 @@ "sl7": "Sandy clay loam" } }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20, - "sl4": 40 - }, - "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 7.0 - }, - "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 22.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 0.5 - }, - "id": { - "component": "Haplic acrisols", - "name": "Haplic acrisols2", - "rank_loc": "Not Displayed", - "score_loc": 0.016 - }, - "ph": { - "sl1": 5.0, - "sl2": 5.0, - "sl3": 5.0, - "sl4": 5.0 - }, - "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0, - "sl4": 25.5 - }, - "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0, - "sl4": 51.5 - }, - "site": { - "siteData": { - "componentID": 133287, - "distance": 49166.71, - "mapunitID": 36011, - "minCompDistance": 33211.7658, - "share": 20, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " - } - }, - "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", - "sl4": "Sandy clay loam" - } - }, { "bottom_depth": { "sl1": 1, @@ -1313,93 +1477,93 @@ "sl7": 120 }, "cec": { - "sl1": 3.0, - "sl2": 3.0, - "sl3": 3.0, - "sl4": 2.4, - "sl5": 2.29, - "sl6": 2.2, - "sl7": 2.0 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 17.6, + "sl5": 17.86, + "sl6": 18.4, + "sl7": 18.83 }, "clay": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.2, - "sl5": 6.43, - "sl6": 6.8, - "sl7": 7.0 + "sl1": 33.0, + "sl2": 33.0, + "sl3": 33.0, + "sl4": 35.8, + "sl5": 36.71, + "sl6": 37.8, + "sl7": 38.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.8, + "sl5": 0.57, + "sl6": 0.6, + "sl7": 0.67 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", + "component": "Dystric plinthosols", + "name": "Dystric plinthosols2", "rank_loc": "Not Displayed", - "score_loc": 0.016 + "score_loc": 0.003 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.32, - "sl5": 5.34, - "sl6": 5.36, - "sl7": 5.37 + "sl1": 5.9, + "sl2": 5.9, + "sl3": 5.9, + "sl4": 5.96, + "sl5": 5.97, + "sl6": 6.02, + "sl7": 6.05 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.2, - "sl5": 4.43, - "sl6": 4.6, - "sl7": 4.5 + "sl1": 13.0, + "sl2": 13.0, + "sl3": 13.0, + "sl4": 17.6, + "sl5": 17.14, + "sl6": 14.8, + "sl7": 15.83 }, "sand": { - "sl1": 87.0, - "sl2": 87.0, - "sl3": 87.0, - "sl4": 86.8, - "sl5": 86.57, - "sl6": 86.2, - "sl7": 86.0 + "sl1": 35.0, + "sl2": 35.0, + "sl3": 35.0, + "sl4": 33.6, + "sl5": 33.29, + "sl6": 32.8, + "sl7": 31.83 }, "site": { "siteData": { - "componentID": 107931, - "distance": 34218.133, - "mapunitID": 1444, - "minCompDistance": 33726.7301, - "share": 10, - "soilDepth": 20 + "componentID": 133885, + "distance": 24336.539, + "mapunitID": 36145, + "minCompDistance": 0.0, + "share": 20, + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.", + "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.", + "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil." } }, "texture": { - "sl1": "Loamy sand", - "sl2": "Loamy sand", - "sl3": "Loamy sand", - "sl4": "Loamy sand", - "sl5": "Loamy sand", - "sl6": "Loamy sand", - "sl7": "Loamy sand" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1413,93 +1577,93 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 9.4, - "sl5": 8.57, - "sl6": 7.8, - "sl7": 8.17 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 17.0, + "sl5": 16.29, + "sl6": 15.6, + "sl7": 15.33 }, "clay": { - "sl1": 23.0, - "sl2": 23.0, - "sl3": 23.0, - "sl4": 24.2, - "sl5": 24.29, - "sl6": 24.2, - "sl7": 24.5 + "sl1": 29.0, + "sl2": 29.0, + "sl3": 29.0, + "sl4": 29.8, + "sl5": 30.14, + "sl6": 30.0, + "sl7": 29.67 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 0.86, + "sl6": 0.6, + "sl7": 0.5 }, "id": { - "component": "Dystric fluvisols", - "name": "Dystric fluvisols2", + "component": "Dystric plinthosols", + "name": "Dystric plinthosols3", "rank_loc": "Not Displayed", - "score_loc": 0.011 + "score_loc": 0.003 }, "ph": { - "sl1": 4.9, - "sl2": 4.9, - "sl3": 4.9, - "sl4": 4.96, - "sl5": 4.99, - "sl6": 5.04, - "sl7": 5.08 + "sl1": 5.0, + "sl2": 5.0, + "sl3": 5.0, + "sl4": 5.02, + "sl5": 5.06, + "sl6": 5.12, + "sl7": 5.13 }, "rock_fragments": { - "sl1": 4.0, - "sl2": 4.0, - "sl3": 4.0, - "sl4": 4.8, - "sl5": 7.0, - "sl6": 9.4, - "sl7": 9.67 + "sl1": 14.0, + "sl2": 14.0, + "sl3": 14.0, + "sl4": 14.4, + "sl5": 14.43, + "sl6": 15.2, + "sl7": 16.67 }, "sand": { - "sl1": 49.0, - "sl2": 49.0, - "sl3": 49.0, - "sl4": 49.2, - "sl5": 49.71, - "sl6": 50.8, - "sl7": 50.67 + "sl1": 42.0, + "sl2": 42.0, + "sl3": 42.0, + "sl4": 42.6, + "sl5": 42.57, + "sl6": 42.6, + "sl7": 43.0 }, "site": { "siteData": { - "componentID": 134011, - "distance": 57794.629, - "mapunitID": 36174, + "componentID": 133858, + "distance": 43472.724, + "mapunitID": 36139, "minCompDistance": 0.0, - "share": 5, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", - "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", - "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", - "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " + "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.", + "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.", + "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil." } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Sandy clay loam", - "sl7": "Sandy clay loam" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } } ] @@ -1511,61 +1675,61 @@ }, "soilRank": [ { - "component": "Haplic lixisols", + "component": "Dystric planosols", "componentData": "Missing Data", - "componentID": 134019, - "name": "Haplic lixisols2", - "rank_data": "5", + "componentID": 133240, + "name": "Dystric planosols", + "rank_data": "3", "rank_data_loc": "1", - "rank_loc": "Not Displayed", + "rank_loc": "4", "score_data": 1.0, "score_data_loc": 1.0, "score_loc": 0.016 }, { - "component": "Ferric lixisols", - "componentData": "Data Complete", - "componentID": 107928, - "name": "Ferric lixisols", - "rank_data": "4", + "component": "Dystric gleysols", + "componentData": "Missing Data", + "componentID": 133232, + "name": "Dystric gleysols", + "rank_data": "2", "rank_data_loc": "2", - "rank_loc": "8", + "rank_loc": "6", "score_data": 1.0, - "score_data_loc": 0.998, - "score_loc": 0.014 + "score_data_loc": 0.995, + "score_loc": 0.011 }, { - "component": "Dystric fluvisols", + "component": "Ferralic arenosols", "componentData": "Data Complete", - "componentID": 134011, - "name": "Dystric fluvisols2", - "rank_data": "1", + "componentID": 133291, + "name": "Ferralic arenosols", + "rank_data": "4", "rank_data_loc": "3", - "rank_loc": "Not Displayed", + "rank_loc": "5", "score_data": 1.0, "score_data_loc": 0.995, "score_loc": 0.011 }, { - "component": "Ferralic arenosols", + "component": "Dystric cambisols", "componentData": "Data Complete", - "componentID": 133291, - "name": "Ferralic arenosols", - "rank_data": "3", + "componentID": 134337, + "name": "Dystric cambisols2", + "rank_data": "1", "rank_data_loc": "4", - "rank_loc": "12", + "rank_loc": "Not Displayed", "score_data": 1.0, - "score_data_loc": 0.995, - "score_loc": 0.011 + "score_data_loc": 0.989, + "score_loc": 0.005 }, { "component": "Eutric gleysols", "componentData": "Missing Data", - "componentID": 133289, - "name": "Eutric gleysols", - "rank_data": "6", + "componentID": 134213, + "name": "Eutric gleysols2", + "rank_data": "7", "rank_data_loc": "5", - "rank_loc": "1", + "rank_loc": "Not Displayed", "score_data": 0.63, "score_data_loc": 0.645, "score_loc": 0.025 @@ -1578,54 +1742,66 @@ "rank_data": "9", "rank_data_loc": "6", "rank_loc": "2", - "score_data": 0.613, - "score_data_loc": 0.625, + "score_data": 0.63, + "score_data_loc": 0.642, "score_loc": 0.022 }, { - "component": "Dystric planosols", - "componentData": "Missing Data", - "componentID": 133240, - "name": "Dystric planosols", - "rank_data": "8", + "component": "Dystric fluvisols", + "componentData": "Data Complete", + "componentID": 134011, + "name": "Dystric fluvisols2", + "rank_data": "5", "rank_data_loc": "7", - "rank_loc": "3", - "score_data": 0.613, - "score_data_loc": 0.619, - "score_loc": 0.016 + "rank_loc": "Not Displayed", + "score_data": 0.63, + "score_data_loc": 0.631, + "score_loc": 0.011 }, { - "component": "Haplic acrisols", + "component": "Eutric fluvisols", "componentData": "Data Complete", - "componentID": 133287, - "name": "Haplic acrisols2", - "rank_data": "Not Displayed", + "componentID": 133290, + "name": "Eutric fluvisols", + "rank_data": "6", "rank_data_loc": "8", - "rank_loc": "Not Displayed", - "score_data": 0.535, - "score_data_loc": 0.542, - "score_loc": 0.016 + "rank_loc": "12", + "score_data": 0.63, + "score_data_loc": 0.622, + "score_loc": 0.002 }, { - "component": "Dystric gleysols", - "componentData": "Missing Data", - "componentID": 133232, - "name": "Dystric gleysols", - "rank_data": "11", + "component": "Chromic luvisols", + "componentData": "Data Complete", + "componentID": 133611, + "name": "Chromic luvisols", + "rank_data": "10", "rank_data_loc": "9", "rank_loc": "9", - "score_data": 0.535, - "score_data_loc": 0.537, - "score_loc": 0.011 + "score_data": 0.613, + "score_data_loc": 0.611, + "score_loc": 0.008 + }, + { + "component": "Dystric plinthosols", + "componentData": "Missing Data", + "componentID": 133239, + "name": "Dystric plinthosols1", + "rank_data": "12", + "rank_data_loc": "10", + "rank_loc": "11", + "score_data": 0.613, + "score_data_loc": 0.606, + "score_loc": 0.003 }, { "component": "Dystric leptosols", "componentData": "Missing Data", "componentID": 133329, "name": "Dystric leptosols", - "rank_data": "7", - "rank_data_loc": "10", - "rank_loc": "11", + "rank_data": "11", + "rank_data_loc": "11", + "rank_loc": "8", "score_data": 0.613, "score_data_loc": 0.002, "score_loc": 0.011 @@ -1635,48 +1811,48 @@ "componentData": "Missing Data", "componentID": 133765, "name": "Eutric leptosols", - "rank_data": "2", - "rank_data_loc": "11", - "rank_loc": "5", - "score_data": 1.0, + "rank_data": "8", + "rank_data_loc": "12", + "rank_loc": "3", + "score_data": 0.63, "score_data_loc": 0.002, "score_loc": 0.016 }, { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 148823, - "name": "Lithic leptosols1", - "rank_data": "10", - "rank_data_loc": "12", - "rank_loc": "7", + "component": "Dystric cambisols", + "componentData": "Data Complete", + "componentID": 133494, + "name": "Dystric cambisols1", + "rank_data": "Not Displayed", + "rank_data_loc": "Not Displayed", + "rank_loc": "10", "score_data": 0.613, - "score_data_loc": 0.002, - "score_loc": 0.016 + "score_data_loc": 0.608, + "score_loc": 0.005 }, { - "component": "Haplic acrisols", - "componentData": "Data Complete", - "componentID": 134061, - "name": "Haplic acrisols1", - "rank_data": "12", + "component": "Dystric plinthosols", + "componentData": "Missing Data", + "componentID": 133885, + "name": "Dystric plinthosols2", + "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "6", - "score_data": 0.535, - "score_data_loc": 0.542, - "score_loc": 0.016 + "rank_loc": "Not Displayed", + "score_data": 0.613, + "score_data_loc": 0.606, + "score_loc": 0.003 }, { - "component": "Haplic lixisols", + "component": "Eutric gleysols", "componentData": "Missing Data", - "componentID": 133488, - "name": "Haplic lixisols1", + "componentID": 133289, + "name": "Eutric gleysols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "4", + "rank_loc": "1", "score_data": 0.535, - "score_data_loc": 0.542, - "score_loc": 0.016 + "score_data_loc": 0.552, + "score_loc": 0.025 }, { "component": "Dystric fluvisols", @@ -1685,22 +1861,22 @@ "name": "Dystric fluvisols1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "10", + "rank_loc": "7", "score_data": 0.535, "score_data_loc": 0.537, "score_loc": 0.011 }, { - "component": "Lithic leptosols", + "component": "Dystric plinthosols", "componentData": "Missing Data", - "componentID": 107931, - "name": "Lithic leptosols2", + "componentID": 133858, + "name": "Dystric plinthosols3", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", "score_data": 0.37, - "score_data_loc": 0.002, - "score_loc": 0.016 + "score_data_loc": 0.367, + "score_loc": 0.003 } ] } diff --git a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json index 77da511..7658209 100644 --- a/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json +++ b/soil_id/tests/global/__snapshots__/test_global/test_soil_location[8.48333,76.95].json @@ -25,31 +25,31 @@ "sl7": 120 }, "cec": { - "sl1": 9.0, - "sl2": 9.0, - "sl3": 9.0, - "sl4": 7.6, - "sl5": 7.0, - "sl6": 6.4, + "sl1": 6.0, + "sl2": 6.0, + "sl3": 6.0, + "sl4": 6.0, + "sl5": 6.0, + "sl6": 6.0, "sl7": 6.0 }, "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0, - "sl4": 18.0, - "sl5": 17.14, - "sl6": 16.0, - "sl7": 15.67 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 25.6, + "sl5": 28.14, + "sl6": 30.0, + "sl7": 30.5 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.14, - "sl6": 1.2, - "sl7": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { "component": "Dystric regosols", @@ -58,31 +58,31 @@ "score_loc": 0.078 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.08, - "sl5": 5.13, + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.2, + "sl5": 5.19, "sl6": 5.16, - "sl7": 5.18 + "sl7": 5.13 }, "rock_fragments": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 30.6, - "sl5": 31.14, - "sl6": 35.2, - "sl7": 36.67 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.71, + "sl6": 6.2, + "sl7": 5.83 }, "sand": { - "sl1": 55.0, - "sl2": 55.0, - "sl3": 55.0, - "sl4": 57.6, - "sl5": 58.71, - "sl6": 60.2, - "sl7": 60.17 + "sl1": 53.0, + "sl2": 53.0, + "sl3": 53.0, + "sl4": 47.8, + "sl5": 45.86, + "sl6": 44.8, + "sl7": 44.83 }, "site": { "siteData": { @@ -108,10 +108,10 @@ "sl1": "Sandy loam", "sl2": "Sandy loam", "sl3": "Sandy loam", - "sl4": "Sandy loam", - "sl5": "Sandy loam", - "sl6": "Sandy loam", - "sl7": "Sandy loam" + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -125,31 +125,31 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 11.0, - "sl5": 11.0, - "sl6": 11.0, - "sl7": 10.83 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.6, + "sl5": 6.14, + "sl6": 5.8, + "sl7": 5.67 }, "clay": { "sl1": 30.0, "sl2": 30.0, "sl3": 30.0, - "sl4": 37.6, - "sl5": 41.0, - "sl6": 44.2, - "sl7": 45.17 + "sl4": 31.4, + "sl5": 32.0, + "sl6": 32.6, + "sl7": 33.0 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 0.4, + "sl5": 0.29, + "sl6": 0.2, + "sl7": 0.17 }, "id": { "component": "Haplic nitisols", @@ -158,31 +158,31 @@ "score_loc": 0.074 }, "ph": { - "sl1": 5.5, - "sl2": 5.5, - "sl3": 5.5, - "sl4": 5.36, - "sl5": 5.31, - "sl6": 5.28, - "sl7": 5.27 + "sl1": 5.2, + "sl2": 5.2, + "sl3": 5.2, + "sl4": 5.2, + "sl5": 5.2, + "sl6": 5.2, + "sl7": 5.18 }, "rock_fragments": { - "sl1": 10.0, - "sl2": 10.0, - "sl3": 10.0, - "sl4": 13.2, - "sl5": 14.14, - "sl6": 13.0, - "sl7": 11.5 + "sl1": 12.0, + "sl2": 12.0, + "sl3": 12.0, + "sl4": 9.4, + "sl5": 9.86, + "sl6": 10.6, + "sl7": 10.5 }, "sand": { - "sl1": 46.0, - "sl2": 46.0, - "sl3": 46.0, - "sl4": 40.6, - "sl5": 38.0, - "sl6": 35.4, - "sl7": 34.67 + "sl1": 45.0, + "sl2": 45.0, + "sl3": 45.0, + "sl4": 43.0, + "sl5": 42.29, + "sl6": 41.4, + "sl7": 41.0 }, "site": { "siteData": { @@ -205,13 +205,13 @@ } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", "sl4": "Clay loam", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -252,8 +252,8 @@ "sl7": 0.0 }, "id": { - "component": "Dystric plinthosols", - "name": "Dystric plinthosols", + "component": "Chromic luvisols", + "name": "Chromic luvisols", "rank_loc": "3", "score_loc": 0.063 }, @@ -286,22 +286,22 @@ }, "site": { "siteData": { - "componentID": 134462, - "distance": 22688.376, - "mapunitID": 3656, - "minCompDistance": 22688.3756, + "componentID": 135560, + "distance": 56569.283, + "mapunitID": 3780, + "minCompDistance": 56569.2834, "share": 60, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", - "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.", - "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", - "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", - "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", - "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.", - "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", - "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil." + "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", + "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", + "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", + "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", + "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." } }, "texture": { @@ -325,229 +325,93 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 18.2, - "sl5": 18.43, - "sl6": 18.4, - "sl7": 17.83 + "sl1": 8.0, + "sl2": 8.0, + "sl3": 8.0, + "sl4": 6.8, + "sl5": 6.57, + "sl6": 6.4, + "sl7": 6.33 }, "clay": { - "sl1": 30.0, - "sl2": 30.0, - "sl3": 30.0, - "sl4": 34.2, - "sl5": 35.86, - "sl6": 37.2, - "sl7": 37.5 + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 31.2, + "sl5": 34.0, + "sl6": 36.6, + "sl7": 37.67 }, "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0, - "sl4": 1.0, - "sl5": 1.0, - "sl6": 1.0, - "sl7": 1.0 + "sl1": 0.0, + "sl2": 0.0, + "sl3": 0.0, + "sl4": 0.0, + "sl5": 0.0, + "sl6": 0.0, + "sl7": 0.0 }, "id": { - "component": "Chromic luvisols", - "name": "Chromic luvisols", + "component": "Dystric plinthosols", + "name": "Dystric plinthosols", "rank_loc": "4", "score_loc": 0.063 }, "ph": { - "sl1": 6.5, - "sl2": 6.5, - "sl3": 6.5, - "sl4": 6.56, - "sl5": 6.57, - "sl6": 6.58, - "sl7": 6.55 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.18, + "sl5": 5.16, + "sl6": 5.14, + "sl7": 5.13 }, "rock_fragments": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 10.6, - "sl5": 10.14, - "sl6": 9.8, - "sl7": 11.33 - }, - "sand": { - "sl1": 37.0, - "sl2": 37.0, - "sl3": 37.0, - "sl4": 34.4, - "sl5": 33.43, - "sl6": 32.6, - "sl7": 33.0 - }, - "site": { - "siteData": { - "componentID": 135560, - "distance": 56569.283, - "mapunitID": 3780, - "minCompDistance": 56569.2834, - "share": 60, - "soilDepth": 200 - }, - "siteDescription": { - "Description_en": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_es": "Los Luvisoles Crómicos son suelos productivos con alta saturación de bases y subsuelos relativamente arcillosos.
Los Luvisoles crómicos tienen un subsuelo rico en hierro.", - "Description_fr": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Description_ks": "Chromic Luvisols are productive soils with high base saturation and relatively clayey subsoils.
Chromic Luvisols have an iron rich subsoil.", - "Management_en": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_es": "Estos suelos son fértiles y pueden utilizarse para una amplia gama de prácticas de cultivo.
Sin embargo, son sensibles a la pérdida de suelo por erosión, y hay que tener cuidado para proteger el suelo de la pérdida.
Si el suelo ya está erosionado, pueden ser más adecuados para el pastoreo y/o los cultivos arbóreos.", - "Management_fr": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops.", - "Management_ks": "These soils are fertile, and can be used for a wide range of cropping practices.
However, they are sensitive to soil loss through erosion, and care must be taken to protect the soil from loss.
If the soil is already eroded they may best be suited for grazing andtree crops." - } - }, - "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", - "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols1", - "rank_loc": "5", - "score_loc": 0.053 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 - }, - "rock_fragments": { - "sl1": 36.0, - "sl2": 36.0, - "sl3": 36.0 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 27.8, + "sl5": 28.29, + "sl6": 27.2, + "sl7": 26.33 }, "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 + "sl1": 56.0, + "sl2": 56.0, + "sl3": 56.0, + "sl4": 50.2, + "sl5": 47.71, + "sl6": 45.2, + "sl7": 43.83 }, "site": { "siteData": { - "componentID": 134464, + "componentID": 134462, "distance": 22688.376, "mapunitID": 3656, "minCompDistance": 22688.3756, - "share": 10, - "soilDepth": 20 - }, - "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " - } - }, - "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" - } - }, - { - "bottom_depth": { - "sl1": 1, - "sl2": 10, - "sl3": 20 - }, - "cec": { - "sl1": 16.0, - "sl2": 16.0, - "sl3": 16.0 - }, - "clay": { - "sl1": 20.0, - "sl2": 20.0, - "sl3": 20.0 - }, - "ec": { - "sl1": 1.0, - "sl2": 1.0, - "sl3": 1.0 - }, - "id": { - "component": "Humic acrisols", - "name": "Humic acrisols", - "rank_loc": "6", - "score_loc": 0.053 - }, - "ph": { - "sl1": 6.7, - "sl2": 6.7, - "sl3": 6.7 - }, - "rock_fragments": { - "sl1": 22.0, - "sl2": 22.0, - "sl3": 22.0 - }, - "sand": { - "sl1": 51.0, - "sl2": 51.0, - "sl3": 51.0 - }, - "site": { - "siteData": { - "componentID": 134394, - "distance": 98529.034, - "mapunitID": 3638, - "minCompDistance": 98529.0339, - "share": 50, + "share": 60, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ", - "Description_es": "Los Acrisoles Húmicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Los acrisoles húmicos contienen grandes cantidades de materia orgánica en la capa superior del suelo.
Suelen tener una estructura pobre, pero se vuelven más productivos en sistemas que incluyen rotaciones de cultivos, cultivos de cobertura o abonos verdes. ", - "Description_fr": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ", - "Description_ks": "Humic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
Humic Acrisols contain large amounts of organic matter in the upper soil layer.
They often have poor structure, but will become more productive in systems that include crop rotations, cover crops or green manures. ", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate) which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_es": "Los Plinthosoles Dístricos son suelos relativamente improductivos que se encuentran en regiones subtropicales o tropicales con altas cantidades de concentraciones ricas en hierro y pobres en humus de dureza y cementación variables.
Las concentraciones de hierro más blandas se endurecen irreversiblemente cuando se exponen en la superficie.
Estos suelos tienen un bajo volumen de enraizamiento y son relativamente ácidos, infértiles, muy erosionables y a menudo húmedos.
Los Plinthosoles Dístricos son suelos improductivos con baja saturación de bases en los subsuelos.", + "Description_fr": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Description_ks": "Dystric Plinthosols are relatively unproductive soils found in subtropical or tropical regions with high amounts of iron-rich, humus poor concentrations of variable hardness and cementation.
Softer iron concentrations irreversibly harden when exposed at the surface.
These soils have low rooting volume and are relatively acid, infertile, highly erodible, and often wet.
Dystric Plinthosols are unproductive soils with low base saturation in subsoils.", + "Management_en": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_es": "Este suelo no es muy adecuado para la agricultura.
La combinación de hierro duro y cementación hacen que este suelo sea el más adecuado para la construcción.
Tiene una pobre fertilidad del suelo, que cuando se combina con un suelo poco profundo y rocoso hace que la agricultura no sea posible.
Estos suelos deben utilizarse para cosas como materiales de superficie para carreteras.
Este suelo prácticamente no tiene calcio disponible en el subsuelo.", + "Management_fr": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil.", + "Management_ks": "This soil is not well suited for farming.
The combination of hard iron and cementation make this soil most suitable for construction.
It has poor soil fertility, which when combined with shallow and rocky soil makes arable farming not possible.
These soils should be used for things such as surface materials for roads.
This soil has virtually no available calcium in the subsoil." } }, "texture": { - "sl1": "Loam", - "sl2": "Loam", - "sl3": "Loam" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy clay loam", + "sl6": "Sandy clay", + "sl7": "Clay loam" } }, { @@ -561,22 +425,22 @@ "sl7": 120 }, "cec": { - "sl1": 18.0, - "sl2": 18.0, - "sl3": 18.0, - "sl4": 16.4, - "sl5": 15.57, - "sl6": 14.8, - "sl7": 14.5 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 11.0, + "sl5": 11.0, + "sl6": 11.0, + "sl7": 10.83 }, "clay": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 33.6, - "sl5": 35.0, - "sl6": 36.4, - "sl7": 37.67 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 37.6, + "sl5": 41.0, + "sl6": 44.2, + "sl7": 45.17 }, "ec": { "sl1": 0.0, @@ -588,66 +452,66 @@ "sl7": 0.0 }, "id": { - "component": "Eutric fluvisols", - "name": "Eutric fluvisols", - "rank_loc": "7", + "component": "Gleysols", + "name": "Gleysols", + "rank_loc": "5", "score_loc": 0.052 }, "ph": { - "sl1": 5.1, - "sl2": 5.1, - "sl3": 5.1, - "sl4": 5.16, - "sl5": 5.19, - "sl6": 5.22, - "sl7": 5.25 + "sl1": 5.5, + "sl2": 5.5, + "sl3": 5.5, + "sl4": 5.36, + "sl5": 5.31, + "sl6": 5.28, + "sl7": 5.27 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 3.0, - "sl5": 3.14, - "sl6": 3.6, - "sl7": 4.5 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 13.2, + "sl5": 14.14, + "sl6": 13.0, + "sl7": 11.5 }, "sand": { - "sl1": 35.0, - "sl2": 35.0, - "sl3": 35.0, - "sl4": 33.4, - "sl5": 32.71, - "sl6": 32.2, - "sl7": 31.0 + "sl1": 46.0, + "sl2": 46.0, + "sl3": 46.0, + "sl4": 40.6, + "sl5": 38.0, + "sl6": 35.4, + "sl7": 34.67 }, "site": { "siteData": { - "componentID": 136283, - "distance": 1300.283, - "mapunitID": 3844, - "minCompDistance": 1300.2831, + "componentID": 136008, + "distance": 5885.649, + "mapunitID": 3817, + "minCompDistance": 5885.6486, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", - "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", - "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", - "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", - "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." + "Description_en": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_es": "Los Gleysoles tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los gleysoles son suelos productivos con una alta saturación de la base en la parte superior del suelo.", + "Description_fr": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Description_ks": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", + "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", + "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", + "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " } }, "texture": { - "sl1": "Clay loam", - "sl2": "Clay loam", - "sl3": "Clay loam", + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", "sl4": "Clay loam", - "sl5": "Clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl5": "Unknown", + "sl6": "Unknown", + "sl7": "Unknown" } }, { @@ -661,83 +525,83 @@ "sl7": 120 }, "cec": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 18.4, - "sl5": 18.14, - "sl6": 17.6, - "sl7": 17.5 + "sl1": 18.0, + "sl2": 18.0, + "sl3": 18.0, + "sl4": 18.2, + "sl5": 18.43, + "sl6": 18.4, + "sl7": 17.83 }, "clay": { - "sl1": 31.0, - "sl2": 31.0, - "sl3": 31.0, - "sl4": 32.2, - "sl5": 32.14, - "sl6": 31.6, - "sl7": 31.33 + "sl1": 30.0, + "sl2": 30.0, + "sl3": 30.0, + "sl4": 34.2, + "sl5": 35.86, + "sl6": 37.2, + "sl7": 37.5 }, "ec": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 1.4, - "sl5": 1.43, - "sl6": 1.6, - "sl7": 1.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.0, + "sl6": 1.0, + "sl7": 1.0 }, "id": { - "component": "Gleysols", - "name": "Gleysols", - "rank_loc": "8", + "component": "Eutric fluvisols", + "name": "Eutric fluvisols", + "rank_loc": "6", "score_loc": 0.052 }, "ph": { - "sl1": 6.1, - "sl2": 6.1, - "sl3": 6.1, - "sl4": 6.24, - "sl5": 6.3, - "sl6": 6.38, - "sl7": 6.43 + "sl1": 6.5, + "sl2": 6.5, + "sl3": 6.5, + "sl4": 6.56, + "sl5": 6.57, + "sl6": 6.58, + "sl7": 6.55 }, "rock_fragments": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 11.6, - "sl5": 9.86, - "sl6": 10.2, - "sl7": 10.33 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 10.6, + "sl5": 10.14, + "sl6": 9.8, + "sl7": 11.33 }, "sand": { "sl1": 37.0, "sl2": 37.0, "sl3": 37.0, - "sl4": 36.2, - "sl5": 36.86, - "sl6": 38.4, - "sl7": 38.83 + "sl4": 34.4, + "sl5": 33.43, + "sl6": 32.6, + "sl7": 33.0 }, "site": { "siteData": { - "componentID": 136008, - "distance": 5885.649, - "mapunitID": 3817, - "minCompDistance": 5885.6486, + "componentID": 136283, + "distance": 1300.283, + "mapunitID": 3844, + "minCompDistance": 1300.2831, "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_es": "Los Gleysoles tienen aguas subterráneas poco profundas y están saturados durante gran parte del año.
El drenaje profundo es necesario para el cultivo.
Los gleysoles son suelos productivos con una alta saturación de la base en la parte superior del suelo.", - "Description_fr": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Description_ks": "Gleysols have shallow groundwater and are saturated for significant portions of the year.
Deep drainage is necessary for cultivation.
Gleysols are productive soils with high base saturation in the upper portion of soil.", - "Management_en": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_es": "Estos suelos están saturados, y si se cultivan se requiere un drenaje significativo.
Una vez drenados, estos suelos pueden ser altamente productivos.
El nivel freático debe bajarse mediante un drenaje profundo.
Una vez drenados, puede ser necesario el encalado, ya que la materia orgánica comienza a descomponerse.", - "Management_fr": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. ", - "Management_ks": "These soils are saturated, and if they are cultivated significant drainage is required.
Once drained, these soils can be highly productive.
The water table must be lowered using deep drainage.
Once drained, liming may be required as organic matter begins to decompose. " + "Description_en": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_es": "Los Fluvisoles Eútricos se encuentran principalmente en llanuras de inundación y zonas costeras, y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los fluvisoles eútricos son suelos productivos con una alta saturación de bases en la parte superior del suelo. ", + "Description_fr": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Description_ks": "Eutric Fluvisols are mostly found in floodplains and coastal areas, and have limited profile development with a range of properties.
Hydrological management is essential for production.
Eutric Fluvisols are productive soils with high base saturation in the upper portion of soil. ", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (mantillos, cultivos de cobertura), mejoren la infiltración del agua o proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered." } }, "texture": { @@ -788,9 +652,9 @@ "sl7": 0.33 }, "id": { - "component": "Ferric acrisols", - "name": "Ferric acrisols", - "rank_loc": "9", + "component": "Haplic acrisols", + "name": "Haplic acrisols", + "rank_loc": "7", "score_loc": 0.032 }, "ph": { @@ -822,22 +686,22 @@ }, "site": { "siteData": { - "componentID": 134463, - "distance": 22688.376, - "mapunitID": 3656, - "minCompDistance": 22688.3756, + "componentID": 134395, + "distance": 98529.034, + "mapunitID": 3638, + "minCompDistance": 98529.0339, "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", - "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", + "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { @@ -861,93 +725,93 @@ "sl7": 120 }, "cec": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.57, - "sl6": 6.4, - "sl7": 6.33 + "sl1": 11.0, + "sl2": 11.0, + "sl3": 11.0, + "sl4": 9.4, + "sl5": 8.57, + "sl6": 7.8, + "sl7": 8.17 }, "clay": { - "sl1": 24.0, - "sl2": 24.0, - "sl3": 24.0, - "sl4": 31.2, - "sl5": 34.0, - "sl6": 36.6, - "sl7": 37.67 + "sl1": 23.0, + "sl2": 23.0, + "sl3": 23.0, + "sl4": 24.2, + "sl5": 24.29, + "sl6": 24.2, + "sl7": 24.5 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Humic ferralsols", - "name": "Humic ferralsols", - "rank_loc": "10", + "component": "Ferric acrisols", + "name": "Ferric acrisols", + "rank_loc": "8", "score_loc": 0.032 }, "ph": { - "sl1": 5.3, - "sl2": 5.3, - "sl3": 5.3, - "sl4": 5.18, - "sl5": 5.16, - "sl6": 5.14, - "sl7": 5.13 + "sl1": 4.9, + "sl2": 4.9, + "sl3": 4.9, + "sl4": 4.96, + "sl5": 4.99, + "sl6": 5.04, + "sl7": 5.08 }, "rock_fragments": { - "sl1": 21.0, - "sl2": 21.0, - "sl3": 21.0, - "sl4": 27.8, - "sl5": 28.29, - "sl6": 27.2, - "sl7": 26.33 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.8, + "sl5": 7.0, + "sl6": 9.4, + "sl7": 9.67 }, "sand": { - "sl1": 56.0, - "sl2": 56.0, - "sl3": 56.0, - "sl4": 50.2, - "sl5": 47.71, - "sl6": 45.2, - "sl7": 43.83 + "sl1": 49.0, + "sl2": 49.0, + "sl3": 49.0, + "sl4": 49.2, + "sl5": 49.71, + "sl6": 50.8, + "sl7": 50.67 }, "site": { "siteData": { - "componentID": 135998, - "distance": 34926.783, - "mapunitID": 3816, - "minCompDistance": 34926.7828, + "componentID": 134463, + "distance": 22688.376, + "mapunitID": 3656, + "minCompDistance": 22688.3756, "share": 30, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Humic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Humic Ferralsols have slightly higher organic matter in the upper portions of the soil. ", - "Description_es": "Los Ferralsoles Húmicos son suelos bien desarrollados en climas húmedos y cálidos que están dominados por minerales de baja actividad como la caolinita y los óxidos de hierro y aluminio.
Suelen tener buenas propiedades físicas pero son ácidos, relativamente infértiles, tienen una alta fijación de P y tienen una capacidad limitada para retener nutrientes.
Los ferralisoles húmicos tienen una materia orgánica ligeramente superior en las partes superiores del suelo. ", - "Description_fr": "Humic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Humic Ferralsols have slightly higher organic matter in the upper portions of the soil. ", - "Description_ks": "Humic Ferralsols are well developed soils in humid, warm climates that are dominated by low activity minerals such as kaolinite and iron and aluminum oxides.
They often have good physical properties but are acid, relatively infertile, have high P fixation, and have limited ability to retain nutrients.
Humic Ferralsols have slightly higher organic matter in the upper portions of the soil. ", - "Management_en": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_es": "suelos son propensos a la fijación de fósforo, y el P aplicado por los fertilizantes o la mayor parte del P del suelo no estará inmediatamente disponible para su absorción y uso por los cultivos.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La fertilización adicional y la aplicación de cal, además del P, también serán necesarias para garantizar un crecimiento y un rendimiento adecuados de los cultivos.
En estos suelos también puede haber altos niveles de aluminio soluble, que es tóxico para las plantas.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) puede ayudar a reducir la toxicidad del aluminio.
Dado que estos suelos son infértiles, necesitarán aplicaciones de nutrientes para las plantas con el fin de obtener un mejor rendimiento de los cultivos, ya sea mediante la fertilización o la inclusión de residuos de cultivos, estiércol u otro material orgánico rico en nutrientes.
Estos suelos tienen una capacidad limitada para retener los fertilizantes nitrogenados. Deberían considerarse fuentes de nitrógeno de liberación lenta, si se dispone de ellas, o podría utilizarse la aplicación más frecuente de fuentes solubles a una tasa menor en cada aplicación.", - "Management_fr": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used.", - "Management_ks": "soils are prone to phosphorus fixation, and applied fertilizer P or most soil P will not be immediately available for crop uptake and use.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Additional fertilization and lime application, in addition to P, will also be needed to ensure adequate crop growth and yield.
High levels of soluble aluminum can also be present in these soils, and it is toxic to plants.
Application of lime (which both increases soil pH and ties up soluble aluminum) can help to reduce aluminum toxicity.
Since these soils are infertile they will require applications of plant nutrients for best crop performance, applied either by fertilization or inclusion of crop residues, manures or other nutrient-rich organic material.
These soils have a limited ability to retain nitrogen fertilizer. Slow-release nitrogen sources should be considered, if available, or more frequent application of soluble sources at a lower rate with each application could be used." + "Description_en": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_es": "Los Acrisoles Férricos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas.
Estos suelos tienen un alto contenido de hierro y es común la presencia de nódulos de hierro.", + "Description_fr": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Description_ks": "Ferric Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.
These soils are high in iron and iron nodules are commonly present.", + "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio), que extrae el aluminio de la solución, puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura.", + "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", + "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate), which will take Al out of solution, can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " } }, "texture": { - "sl1": "Sandy clay loam", - "sl2": "Sandy clay loam", - "sl3": "Sandy clay loam", + "sl1": "Loam", + "sl2": "Loam", + "sl3": "Loam", "sl4": "Sandy clay loam", "sl5": "Sandy clay loam", - "sl6": "Sandy clay", - "sl7": "Clay loam" + "sl6": "Sandy clay loam", + "sl7": "Sandy clay loam" } }, { @@ -961,93 +825,193 @@ "sl7": 120 }, "cec": { - "sl1": 11.0, - "sl2": 11.0, - "sl3": 11.0, - "sl4": 9.0, - "sl5": 8.29, - "sl6": 7.4, - "sl7": 7.0 + "sl1": 9.0, + "sl2": 9.0, + "sl3": 9.0, + "sl4": 7.6, + "sl5": 7.0, + "sl6": 6.4, + "sl7": 6.0 }, "clay": { - "sl1": 45.0, - "sl2": 45.0, - "sl3": 45.0, - "sl4": 47.2, - "sl5": 48.0, - "sl6": 48.6, - "sl7": 49.0 + "sl1": 20.0, + "sl2": 20.0, + "sl3": 20.0, + "sl4": 18.0, + "sl5": 17.14, + "sl6": 16.0, + "sl7": 15.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.0, - "sl6": 0.0, - "sl7": 0.0 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.0 + }, + "id": { + "component": "Albic arenosols", + "name": "Albic arenosols", + "rank_loc": "9", + "score_loc": 0.026 + }, + "ph": { + "sl1": 5.1, + "sl2": 5.1, + "sl3": 5.1, + "sl4": 5.08, + "sl5": 5.13, + "sl6": 5.16, + "sl7": 5.18 + }, + "rock_fragments": { + "sl1": 24.0, + "sl2": 24.0, + "sl3": 24.0, + "sl4": 30.6, + "sl5": 31.14, + "sl6": 35.2, + "sl7": 36.67 + }, + "sand": { + "sl1": 55.0, + "sl2": 55.0, + "sl3": 55.0, + "sl4": 57.6, + "sl5": 58.71, + "sl6": 60.2, + "sl7": 60.17 + }, + "site": { + "siteData": { + "componentID": 136286, + "distance": 1300.283, + "mapunitID": 3844, + "minCompDistance": 1300.2831, + "share": 10, + "soilDepth": 200 + }, + "siteDescription": { + "Description_en": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_es": "Los Arenosoles Álbicos son suelos arenosos con un desarrollo mínimo del suelo.
Son inherentemente bajos en nutrientes y capacidad de retención de agua.
Estos suelos están muy lixiviados con pocos nutrientes y agua disponible.", + "Description_fr": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Description_ks": "Albic Arenosols are sandy soils with minimal soil development.
They are inherently low in nutrients and water holding capacity.
These soils are highly leached with low nutrients and available water.", + "Management_en": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_es": "Dado que estos suelos tienen poca retención de agua y nutrientes, deben ser fertilizados y regados para lograr una productividad óptima.
Las prácticas de gestión para mejorar el suministro de nutrientes y la capacidad de retención de agua incluyen la adición de materia orgánica, el uso de cultivos de cobertura y la rotación de cultivos.
La mejor productividad se logrará mediante el uso de riego suplementario, el uso de herramientas como mantillos o cubiertas para preservar la humedad del suelo, y la fertilización.
En estos suelos se debe prestar especial atención a minimizar la pérdida de nutrientes durante la fertilización.
Si se dispone de ellas, deben considerarse fuentes de N de liberación lenta, o una aplicación más frecuente de N a tasas más bajas.", + "Management_fr": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. ", + "Management_ks": "Since these soils have poor water and nutrient retention they must be fertilized and irrigated for optimal productivity.
Management practices to improve nutrient supply and water holding capacity include the addition of organic matter, and use of cover crops and crop rotation.
Best productivity will be achieved through the use of supplemental irrigation, use of tools such as mulches or covers to preserve soil moisture, and fertilization.
These soils should have particular attention paid to minimizing nutrient loss during fertilization.
If available, slow release N sources should be considered, or more frequent application of N at lower rates. " + } + }, + "texture": { + "sl1": "Sandy loam", + "sl2": "Sandy loam", + "sl3": "Sandy loam", + "sl4": "Sandy loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Sandy loam" + } + }, + { + "bottom_depth": { + "sl1": 1, + "sl2": 10, + "sl3": 20, + "sl4": 50, + "sl5": 70, + "sl6": 100, + "sl7": 120 + }, + "cec": { + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 18.4, + "sl5": 18.14, + "sl6": 17.6, + "sl7": 17.5 + }, + "clay": { + "sl1": 31.0, + "sl2": 31.0, + "sl3": 31.0, + "sl4": 32.2, + "sl5": 32.14, + "sl6": 31.6, + "sl7": 31.33 + }, + "ec": { + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 1.4, + "sl5": 1.43, + "sl6": 1.6, + "sl7": 1.67 }, "id": { - "component": "Vertisols", - "name": "Vertisols", - "rank_loc": "11", - "score_loc": 0.032 + "component": "Calcaric regosols", + "name": "Calcaric regosols", + "rank_loc": "10", + "score_loc": 0.026 }, "ph": { - "sl1": 4.9, - "sl2": 4.9, - "sl3": 4.9, - "sl4": 4.92, - "sl5": 4.94, - "sl6": 4.98, - "sl7": 5.0 + "sl1": 6.1, + "sl2": 6.1, + "sl3": 6.1, + "sl4": 6.24, + "sl5": 6.3, + "sl6": 6.38, + "sl7": 6.43 }, "rock_fragments": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 15.4, - "sl5": 15.14, - "sl6": 16.6, - "sl7": 17.17 + "sl1": 19.0, + "sl2": 19.0, + "sl3": 19.0, + "sl4": 11.6, + "sl5": 9.86, + "sl6": 10.2, + "sl7": 10.33 }, "sand": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 37.8, - "sl5": 37.14, - "sl6": 36.8, - "sl7": 36.5 + "sl1": 37.0, + "sl2": 37.0, + "sl3": 37.0, + "sl4": 36.2, + "sl5": 36.86, + "sl6": 38.4, + "sl7": 38.83 }, "site": { "siteData": { - "componentID": 135561, - "distance": 56569.283, - "mapunitID": 3780, - "minCompDistance": 56569.2834, - "share": 30, + "componentID": 136285, + "distance": 1300.283, + "mapunitID": 3844, + "minCompDistance": 1300.2831, + "share": 10, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_es": "Los Vertisoles son suelos arcillosos que son pegajosos y plásticos cuando están húmedos y duros y masivos cuando están secos.
En general, estos suelos tienen propiedades químicas favorables, pero la gran cantidad de arcilla expansiva presenta propiedades físicas desafiantes, especialmente en lo que respecta a la gestión del agua. ", - "Description_fr": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Description_ks": "Vertisols are clayey soils that are sticky and plastic when wet and hard and massive when dry.
These soils generally have favorable chemical properties but the high amount of expansive clay presents challenging physical properties particularly with regard to water management.", - "Management_en": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_es": "Los vertisoles pueden ser suelos altamente productivos, pero las características de la arcilla en este suelo pueden hacer que su manejo sea un problema.
Debido al tipo de arcilla, estos suelos se hinchan cuando se humedecen y se encogen cuando se secan, lo que crea problemas para el cultivo (evite el laboreo excesivo cuando está húmedo), u otros problemas como la construcción.
Su fertilidad los hace aptos para la agricultura, pero se necesitará una fertilización adicional para obtener la mejor productividad.
Además, la gestión del agua es clave, y se necesitan prácticas que favorezcan el drenaje y la infiltración del agua.", - "Management_fr": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. ", - "Management_ks": "Vertisols can be highly productive soils, yet the characteristics of the clay in this soil can make management an issue.
Due to the clay type these soils swell when wet and shrink when dry, creating issues for cultivation (avoid excessive tillage when wet), or other issues such as construction.
Their fertility makes them suitable for agriculture, but additional fertilization will be needed for best productivity.
Additionally, water management is a key, and practices that promote drainage and water infiltration are needed. " + "Description_en": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_es": "Regosoles Calcáreos son suelos débilmente desarrollados que comúnmente son demasiado secos, o están en pendientes más pronunciadas que limitan la productividad.*Los Regosoles Cálcicos son calcáreos en la parte superior del subsuelo. ", + "Description_fr": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Description_ks": "Calcaric Regosols are weakly developed soils that commonly are too dry, or are on steeper slopes which limit productivity.
Calcaric Regosols are calcareous in the upper portion of the subsoil. ", + "Management_en": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_es": "Estos suelos tienen una baja capacidad de retención de agua, y son muy sensibles a la sequía.
Son propensos a la erosión, especialmente en zonas con pendiente.
La combinación de la sensibilidad a la sequía y el alto potencial de erosión hace que estos suelos sean los más adecuados para el pastoreo u otros usos con una cobertura constante del suelo.
Incluso cuando se utilicen para el pastoreo, será necesario el riego debido a la baja capacidad de retención de agua y la alta permeabilidad de estos suelos.", + "Management_fr": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. ", + "Management_ks": "These soils have low water holding capacity, and are very sensitive to drought.
They are prone to erosion, especially in areas with slope.
The combination of drought sensitivity and high erosion potential makes these soils best suited for grazing or other uses with constant soil cover.
Even when used for grazing, irrigation will be needed due to the low water holding capacity and high permeability of these soils. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Clay loam", + "sl2": "Clay loam", + "sl3": "Clay loam", + "sl4": "Clay loam", + "sl5": "Clay loam", + "sl6": "Clay loam", + "sl7": "Clay loam" } }, { @@ -1061,93 +1025,93 @@ "sl7": 120 }, "cec": { - "sl1": 40.0, - "sl2": 40.0, - "sl3": 40.0, - "sl4": 40.4, - "sl5": 40.29, - "sl6": 40.2, - "sl7": 39.67 + "sl1": 21.0, + "sl2": 21.0, + "sl3": 21.0, + "sl4": 17.8, + "sl5": 16.57, + "sl6": 15.8, + "sl7": 15.5 }, "clay": { - "sl1": 53.0, - "sl2": 53.0, - "sl3": 53.0, - "sl4": 54.8, - "sl5": 55.29, - "sl6": 55.6, - "sl7": 55.33 + "sl1": 26.0, + "sl2": 26.0, + "sl3": 26.0, + "sl4": 21.6, + "sl5": 20.0, + "sl6": 19.6, + "sl7": 19.67 }, "ec": { - "sl1": 0.0, - "sl2": 0.0, - "sl3": 0.0, - "sl4": 0.0, - "sl5": 0.14, - "sl6": 0.4, - "sl7": 0.67 + "sl1": 1.0, + "sl2": 1.0, + "sl3": 1.0, + "sl4": 1.0, + "sl5": 1.14, + "sl6": 1.2, + "sl7": 1.5 }, "id": { - "component": "Haplic acrisols", - "name": "Haplic acrisols", - "rank_loc": "12", - "score_loc": 0.032 + "component": "Dystric fluvisols", + "name": "Dystric fluvisols", + "rank_loc": "11", + "score_loc": 0.021 }, "ph": { - "sl1": 6.9, - "sl2": 6.9, - "sl3": 6.9, - "sl4": 7.06, - "sl5": 7.14, - "sl6": 7.3, - "sl7": 7.37 + "sl1": 7.9, + "sl2": 7.9, + "sl3": 7.9, + "sl4": 7.94, + "sl5": 8.0, + "sl6": 8.06, + "sl7": 8.08 }, "rock_fragments": { - "sl1": 2.0, - "sl2": 2.0, - "sl3": 2.0, - "sl4": 2.2, - "sl5": 2.43, - "sl6": 2.4, - "sl7": 2.33 + "sl1": 10.0, + "sl2": 10.0, + "sl3": 10.0, + "sl4": 13.0, + "sl5": 12.71, + "sl6": 11.6, + "sl7": 11.67 }, "sand": { - "sl1": 14.0, - "sl2": 14.0, - "sl3": 14.0, - "sl4": 13.4, - "sl5": 13.14, - "sl6": 13.0, - "sl7": 13.0 + "sl1": 51.0, + "sl2": 51.0, + "sl3": 51.0, + "sl4": 53.8, + "sl5": 54.14, + "sl6": 52.4, + "sl7": 51.17 }, "site": { "siteData": { - "componentID": 134395, - "distance": 98529.034, - "mapunitID": 3638, - "minCompDistance": 98529.0339, - "share": 30, + "componentID": 136009, + "distance": 5885.649, + "mapunitID": 3817, + "minCompDistance": 5885.6486, + "share": 20, "soilDepth": 200 }, "siteDescription": { - "Description_en": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_es": "Los Acrisoles Háplicos son suelos ácidos y relativamente infértiles.
Se necesita una fertilización y un encalado suplementarios para crear un suelo productivo para los cultivos.
Estos suelos también tienen un alto contenido de aluminio soluble (Al), que es tóxico para las plantas. ", - "Description_fr": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Description_ks": "Haplic Acrisols are acidic and relatively infertile soils.
Supplemental fertilization and liming will be needed to create a productive soil for crop use.
These soils are also high in soluble aluminum (Al) which is toxic to plants.", - "Management_en": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_es": "Debido a que el suelo tiende a ser ácido (tiene un pH bajo) y alto en Al, el fertilizante de fósforo es rápidamente \"fijado\" por el suelo, haciendo que no esté disponible para las plantas en la temporada de cultivo.
Las prácticas bien documentadas, como la aplicación en banda (directamente sobre la semilla o a un lado y abajo de la semilla) de fertilizantes fosfatados, ayudarán a reducir la fijación de P.
La aplicación de nitrógeno (N) es esencial, y esto puede lograrse mediante la aplicación de dosis correctas de fertilizantes (como la urea), o mediante el uso de cultivos de cobertura, abonos verdes y rotaciones.
Los cultivos de cobertura y las rotaciones que incluyen leguminosas y la inclusión de cultivos con alta biomasa serían beneficiosos, ya que añaden materia orgánica y nitrógeno para el cultivo posterior.
Incluso con cultivos de cobertura o prácticas similares, es probable que se necesite una fertilización suplementaria de N, ya que el N orgánico no se convertirá en el N inorgánico necesario para el cultivo en cantidades suficientes durante el año de cultivo.
La aplicación de cal (que aumenta el pH del suelo y retiene el aluminio soluble) o de yeso (sulfato de calcio, que extrae el aluminio de la solución) puede ayudar a reducir la toxicidad del aluminio.
La conservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo, la rotación de cultivos y la agrosilvicultura. ", - "Management_fr": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. ", - "Management_ks": "Because the soil tends to be acidic (has a low soil pH) and high in Al, phosphorus fertilizer is quickly “fixed” by the soil, making it unavailable to plants in the cropping season.
Well documented practices such as band application (either directly on the seed or to the side and down from the seed) of phosphate fertilizers will help to reduce P fixation.
Application of nitrogen (N) is essential, and this can be accomplished either through application of correct rates of fertilizer (such as urea), or through use of cover crops, green manures and rotations.
Cover crops and rotations that include legumes and inclusion of crops with high biomass would be beneficial, adding organic matter and nitrogen for the subsequent crop.
Even with cover crops or similar practices, supplemental N fertilization will likely be needed as organic N will not be converted to the crop-needed inorganic N in sufficient quantities in the cropping year.
Application of lime (which both increases soil pH and ties up soluble aluminum) or gypsum (calcium sulfate, which will take Al out of solution) can help to reduce aluminum toxicity.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover, crop rotation and agroforestry. " + "Description_en": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_es": "Los Fluvisoles Dístricos se encuentran sobre todo en llanuras de inundación y zonas costeras y tienen un desarrollo de perfil limitado con una serie de propiedades.
La gestión hidrológica es esencial para la producción.
Los Fluvisoles Dístricos son suelos menos productivos con una baja saturación de la base en la parte superior del suelo.", + "Description_fr": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Description_ks": "Dystric Fluvisols are mostly found in floodplains and coastal areas and have limited profile development with a range of properties.
Hydrological management is essential for production.
Dystric Fluvisols are less productive soils with low base saturation in the upper portion of soil.", + "Management_en": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_es": "Estos suelos son todos naturalmente fértiles y productivos.
El drenaje y/o la gestión de las aguas de inundación pueden hacerlos aptos para el cultivo continuo.
Sin embargo, el drenaje puede afectar al pH del suelo, por lo que debe realizarse un muestreo para evaluar la necesidad de cal.
Una vez en cultivo continuo hay que tener cuidado para evitar la erosión del suelo.
Deben considerarse métodos de producción que protejan la superficie del suelo (acolchados, cultivos de cobertura), que mejoren la infiltración del agua o que proporcionen una ruta para el movimiento del agua desde el campo a una velocidad no erosiva (terrazas, vías de drenaje).
Una baja saturación de bases (presencia de Ca, Mg, K) indica que el pH del suelo puede ser bajo, y puede estar justificado el encalado.", + "Management_fr": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. ", + "Management_ks": "These soils are all naturally fertile and productive.
Drainage andmanagement of floodwaters can make them suitable for continuous cultivation.
However, drainage may affect soil pH, and so sampling should be done to evaluate the need for lime.
Once under continuous cultivation care should be taken to avoid soil erosion.
Production methods that protect the soil surface (mulches, cover crops), improve water infiltration, or provide a route for water movement from the field in a non-erosive velocity (terraces, drainage ways) should be considered.
A low base saturation (presence of Ca, Mg, K) indicates that the soil pH may be low, and liming may be warranted. " } }, "texture": { - "sl1": "Unknown", - "sl2": "Unknown", - "sl3": "Unknown", - "sl4": "Unknown", - "sl5": "Unknown", - "sl6": "Unknown", - "sl7": "Unknown" + "sl1": "Sandy clay loam", + "sl2": "Sandy clay loam", + "sl3": "Sandy clay loam", + "sl4": "Sandy clay loam", + "sl5": "Sandy loam", + "sl6": "Sandy loam", + "sl7": "Loam" } }, { @@ -1161,22 +1125,22 @@ "sl7": 120 }, "cec": { - "sl1": 6.0, - "sl2": 6.0, - "sl3": 6.0, - "sl4": 6.0, - "sl5": 6.0, - "sl6": 6.0, - "sl7": 6.0 + "sl1": 3.0, + "sl2": 3.0, + "sl3": 3.0, + "sl4": 1.8, + "sl5": 1.57, + "sl6": 1.4, + "sl7": 1.33 }, "clay": { - "sl1": 19.0, - "sl2": 19.0, - "sl3": 19.0, - "sl4": 25.6, - "sl5": 28.14, - "sl6": 30.0, - "sl7": 30.5 + "sl1": 4.0, + "sl2": 4.0, + "sl3": 4.0, + "sl4": 4.0, + "sl5": 4.0, + "sl6": 4.0, + "sl7": 4.17 }, "ec": { "sl1": 0.0, @@ -1188,66 +1152,66 @@ "sl7": 0.0 }, "id": { - "component": "Lithic leptosols", - "name": "Lithic leptosols2", - "rank_loc": "Not Displayed", - "score_loc": 0.053 + "component": "Ferralic cambisols", + "name": "Ferralic cambisols", + "rank_loc": "12", + "score_loc": 0.011 }, "ph": { - "sl1": 5.2, - "sl2": 5.2, - "sl3": 5.2, - "sl4": 5.2, - "sl5": 5.19, - "sl6": 5.16, - "sl7": 5.13 + "sl1": 5.3, + "sl2": 5.3, + "sl3": 5.3, + "sl4": 5.32, + "sl5": 5.36, + "sl6": 5.42, + "sl7": 5.43 }, "rock_fragments": { - "sl1": 8.0, - "sl2": 8.0, - "sl3": 8.0, - "sl4": 6.8, - "sl5": 6.71, - "sl6": 6.2, - "sl7": 5.83 + "sl1": 2.0, + "sl2": 2.0, + "sl3": 2.0, + "sl4": 3.2, + "sl5": 3.43, + "sl6": 3.6, + "sl7": 4.5 }, "sand": { - "sl1": 53.0, - "sl2": 53.0, - "sl3": 53.0, - "sl4": 47.8, - "sl5": 45.86, - "sl6": 44.8, - "sl7": 44.83 + "sl1": 86.0, + "sl2": 86.0, + "sl3": 86.0, + "sl4": 86.8, + "sl5": 86.86, + "sl6": 86.6, + "sl7": 86.33 }, "site": { "siteData": { - "componentID": 134396, + "componentID": 134397, "distance": 98529.034, "mapunitID": 3638, - "minCompDistance": 22688.3756, + "minCompDistance": 98529.0339, "share": 10, - "soilDepth": 20 + "soilDepth": 200 }, "siteDescription": { - "Description_en": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_es": "Los leptosoles Líticos tienen un volumen de enraizamiento muy limitado debido a la presencia de roca continua, material altamente calcáreo, horizontes cementados o muchas rocas y fragmentos gruesos en la parte superior del suelo.
Los leptosoles en pendientes pronunciadas son muy erosionables.
Los leptosoles líticos tienen rocas duras a menos de 10 cm de la superficie del suelo. ", - "Description_fr": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Description_ks": "Lithic Leptosols have very limited rooting volume due to continuous rock, highly calcareous material, cemented horizons, or many rocks and coarse fragments in the upper portion of the soil.
Leptosols on steep slopes are highly erodible.
Lithic Leptosols have hard rock within 10 cm of the soil surface. ", - "Management_en": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_es": "Debido a que estos suelos son poco profundos, rocosos y erosionables, deben utilizarse para cultivos perennes, y no deben ser labrados.
Deben utilizarse prácticas para mantener la materia orgánica y la cobertura.
Sólo deben considerarse los usos para pastoreo o agroforestales.
La preservación del suelo superficial con su materia orgánica es importante, y la prevención de la erosión es fundamental.
Las prácticas de gestión de la tierra deben maximizar la cobertura del suelo.
Cualquier uso agrícola debe ser para el pastoreo, con el mantenimiento continuo de la cobertura.", - "Management_fr": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. ", - "Management_ks": "Because these soils are shallow, rocky and erodible they should be used for perennial crops, and not tilled.
Practices to maintain organic matter and cover should be used.
Only uses for grazing or agroforestry should be considered.
Preservation of the surface soil with its organic matter is important, and erosion prevention is critical.
Land management practices should maximize soil cover.
Any agricultural use should be for grazing, with cover continuously maintained. " + "Description_en": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_es": "Los Cambisoles Ferrálicos son suelos muy extendidos con un desarrollo limitado del suelo.
Estos suelos tienen una escasa capacidad para retener nutrientes debido a su baja capacidad de intercambio catiónico. Como retienen menos nutrientes, suelen ser menos productivos. ", + "Description_fr": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Description_ks": "Ferralic Cambisols are widely occurring soils with limited soil development.
These soils have a poor ability to retain nutrients due to low cation exchange capacity. Because they retain fewer nutrients they are typically less productive.", + "Management_en": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_es": "En regiones templadas los suelos tendrán un alto contenido de cationes básicos (potasio, calcio y magnesio), mientras que en regiones más húmedas pueden tener niveles más bajos de nutrientes en el suelo.
El tipo de arcilla de este suelo está extremadamente erosionado, y como tal tendrá una baja capacidad de suministro de nutrientes.
La fertilización será necesaria para mejorar la productividad.", + "Management_fr": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. ", + "Management_ks": "In temperate regions the soils will have a high content of basic cations (potassium, calcium and magnesium), while in more humid regions they may have lower levels of soil nutrients.
The clay type in this soil is extremely weathered, and as such will have low nutrient supplying capacity.
Fertilization will be required to improve productivity. " } }, "texture": { - "sl1": "Sandy loam", - "sl2": "Sandy loam", - "sl3": "Sandy loam", - "sl4": "Sandy clay loam", - "sl5": "Sandy clay loam", - "sl6": "Clay loam", - "sl7": "Clay loam" + "sl1": "Loamy sand", + "sl2": "Loamy sand", + "sl3": "Loamy sand", + "sl4": "Loamy sand", + "sl5": "Loamy sand", + "sl6": "Loamy sand", + "sl7": "Loamy sand" } } ] @@ -1265,118 +1229,130 @@ "name": "Gleysols", "rank_data": "1", "rank_data_loc": "1", - "rank_loc": "8", - "score_data": 0.669, + "rank_loc": 5, + "score_data": 0.678, "score_data_loc": 1.0, "score_loc": 0.052 }, - { - "component": "Vertisols", - "componentData": "No Data", - "componentID": 135561, - "name": "Vertisols", - "rank_data": "2", - "rank_data_loc": "2", - "rank_loc": "11", - "score_data": 0.6, - "score_data_loc": 0.876, - "score_loc": 0.032 - }, { "component": "Chromic luvisols", "componentData": "Missing Data", "componentID": 135560, "name": "Chromic luvisols", - "rank_data": "3", - "rank_data_loc": "3", - "rank_loc": "4", - "score_data": 0.537, - "score_data_loc": 0.832, + "rank_data": "2", + "rank_data_loc": "2", + "rank_loc": 3, + "score_data": 0.583, + "score_data_loc": 0.885, "score_loc": 0.063 }, { - "component": "Eutric fluvisols", + "component": "Calcaric regosols", "componentData": "Data Complete", - "componentID": 136283, - "name": "Eutric fluvisols", + "componentID": 136285, + "name": "Calcaric regosols", + "rank_data": "3", + "rank_data_loc": "3", + "rank_loc": 10, + "score_data": 0.568, + "score_data_loc": 0.814, + "score_loc": 0.026 + }, + { + "component": "Ferric acrisols", + "componentData": "Missing Data", + "componentID": 134463, + "name": "Ferric acrisols", "rank_data": "4", "rank_data_loc": "4", - "rank_loc": "7", - "score_data": 0.518, - "score_data_loc": 0.79, - "score_loc": 0.052 + "rank_loc": 8, + "score_data": 0.484, + "score_data_loc": 0.707, + "score_loc": 0.032 }, { - "component": "Dystric plinthosols", - "componentData": "Missing Data", - "componentID": 134462, - "name": "Dystric plinthosols", + "component": "Haplic acrisols", + "componentData": "Data Complete", + "componentID": 134395, + "name": "Haplic acrisols", "rank_data": "5", "rank_data_loc": "5", - "rank_loc": "3", - "score_data": 0.469, - "score_data_loc": 0.738, - "score_loc": 0.063 + "rank_loc": 7, + "score_data": 0.484, + "score_data_loc": 0.707, + "score_loc": 0.032 }, { - "component": "Haplic nitisols", - "componentData": "Missing Data", - "componentID": 134944, - "name": "Haplic nitisols", - "rank_data": "8", + "component": "Albic arenosols", + "componentData": "Data Complete", + "componentID": 136286, + "name": "Albic arenosols", + "rank_data": "6", "rank_data_loc": "6", - "rank_loc": "2", - "score_data": 0.428, - "score_data_loc": 0.696, - "score_loc": 0.074 + "rank_loc": 9, + "score_data": 0.456, + "score_data_loc": 0.66, + "score_loc": 0.026 }, { - "component": "Ferric acrisols", - "componentData": "Missing Data", - "componentID": 134463, - "name": "Ferric acrisols", + "component": "Ferralic cambisols", + "componentData": "Data Complete", + "componentID": 134397, + "name": "Ferralic cambisols", "rank_data": "7", "rank_data_loc": "7", - "rank_loc": "9", - "score_data": 0.438, - "score_data_loc": 0.651, - "score_loc": 0.032 + "rank_loc": 12, + "score_data": 0.451, + "score_data_loc": 0.633, + "score_loc": 0.011 + }, + { + "component": "Dystric fluvisols", + "componentData": "Data Complete", + "componentID": 136009, + "name": "Dystric fluvisols", + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": 11, + "score_data": 0.394, + "score_data_loc": 0.569, + "score_loc": 0.021 }, { - "component": "Humic acrisols", + "component": "Dystric plinthosols", "componentData": "Missing Data", - "componentID": 134394, - "name": "Humic acrisols", + "componentID": 134462, + "name": "Dystric plinthosols", "rank_data": "9", - "rank_data_loc": "8", - "rank_loc": "6", - "score_data": 0.37, - "score_data_loc": 0.587, - "score_loc": 0.053 + "rank_data_loc": "9", + "rank_loc": 4, + "score_data": 0.349, + "score_data_loc": 0.565, + "score_loc": 0.063 }, { - "component": "Haplic acrisols", - "componentData": "Data Complete", - "componentID": 134395, - "name": "Haplic acrisols", + "component": "Haplic nitisols", + "componentData": "Missing Data", + "componentID": 134944, + "name": "Haplic nitisols", "rank_data": "10", - "rank_data_loc": "9", - "rank_loc": "12", - "score_data": 0.37, - "score_data_loc": 0.556, - "score_loc": 0.032 + "rank_data_loc": "10", + "rank_loc": 2, + "score_data": 0.247, + "score_data_loc": 0.44, + "score_loc": 0.074 }, { - "component": "Humic ferralsols", - "componentData": "No Data", - "componentID": 135998, - "name": "Humic ferralsols", + "component": "Eutric fluvisols", + "componentData": "Data Complete", + "componentID": 136283, + "name": "Eutric fluvisols", "rank_data": "11", - "rank_data_loc": "10", - "rank_loc": "10", - "score_data": 0.279, - "score_data_loc": 0.431, - "score_loc": 0.032 + "rank_data_loc": "11", + "rank_loc": 6, + "score_data": 0.238, + "score_data_loc": 0.398, + "score_loc": 0.052 }, { "component": "Dystric regosols", @@ -1384,35 +1360,11 @@ "componentID": 136281, "name": "Dystric regosols", "rank_data": "12", - "rank_data_loc": "11", - "rank_loc": "1", - "score_data": 0.09, - "score_data_loc": 0.233, - "score_loc": 0.078 - }, - { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 134464, - "name": "Lithic leptosols1", - "rank_data": "6", "rank_data_loc": "12", - "rank_loc": "5", - "score_data": 0.457, - "score_data_loc": 0.003, - "score_loc": 0.053 - }, - { - "component": "Lithic leptosols", - "componentData": "Missing Data", - "componentID": 134396, - "name": "Lithic leptosols2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.296, - "score_data_loc": 0.003, - "score_loc": 0.053 + "rank_loc": 1, + "score_data": 0.083, + "score_data_loc": 0.222, + "score_loc": 0.078 } ] } diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json index 7ea87be..a589b99 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[33.81246789,-101.9733687].json @@ -78,8 +78,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=randall", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#randall", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff", "slope": 0.5, "taxsubgrp": "Ustic Epiaquerts", "textureInfill": "No" @@ -134,8 +134,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=amarillo", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#amarillo", "slope": 2.0, "taxsubgrp": "Aridic Paleustolls", "textureInfill": "No" @@ -190,8 +190,8 @@ "nirrcapscl": "c", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=olton", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#olton", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=friona", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#friona", "slope": 0.4, "taxsubgrp": "Aridic Paleustolls", "textureInfill": "No" @@ -246,8 +246,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=mclean", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#mclean", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado", "slope": 0.5, "taxsubgrp": "Udic Haplusterts", "textureInfill": "No" @@ -302,8 +302,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lockney", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lockney", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff", "slope": 0.5, "taxsubgrp": "Typic Haplusterts", "textureInfill": "No" @@ -358,8 +358,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=pullman", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#pullman", "slope": 2.0, "taxsubgrp": "Aridic Paleustolls", "textureInfill": "No" @@ -414,8 +414,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=friona", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#friona", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=randall", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#randall", "slope": 2.0, "taxsubgrp": "Petrocalcic Paleustolls", "textureInfill": "No" @@ -470,8 +470,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=amarillo", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#amarillo", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=mclean", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#mclean", "slope": 2.0, "taxsubgrp": "Aridic Paleustalfs", "textureInfill": "No" @@ -526,8 +526,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=pullman", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#pullman", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lockney", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lockney", "slope": 0.4, "taxsubgrp": "Torrertic Paleustolls", "textureInfill": "No" @@ -582,8 +582,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=acuff", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#acuff", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado", "slope": 0.5, "taxsubgrp": "Aridic Paleustolls", "textureInfill": "No" @@ -638,8 +638,8 @@ "nirrcapscl": "c", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=estacado", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#estacado", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=olton", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#olton", "slope": 0.5, "taxsubgrp": "Aridic Paleustolls", "textureInfill": "No" @@ -662,11 +662,11 @@ "componentData": "Missing Data", "componentID": 25623332, "name": "Randall", - "rank_data": "7", + "rank_data": "9", "rank_data_loc": "1", "rank_loc": "1", - "score_data": 0.465, - "score_data_loc": 0.633, + "score_data": 0.417, + "score_data_loc": 0.608, "score_loc": 0.8 }, { @@ -674,11 +674,11 @@ "componentData": "Data Complete", "componentID": 25623297, "name": "Acuff2", - "rank_data": "5", + "rank_data": "2", "rank_data_loc": "2", "rank_loc": "Not Displayed", - "score_data": 0.499, - "score_data_loc": 0.457, + "score_data": 0.616, + "score_data_loc": 0.515, "score_loc": 0.414 }, { @@ -686,47 +686,23 @@ "componentData": "Data Complete", "componentID": 25623299, "name": "Olton", - "rank_data": "8", + "rank_data": "7", "rank_data_loc": "3", "rank_loc": "3", - "score_data": 0.454, - "score_data_loc": 0.333, + "score_data": 0.485, + "score_data_loc": 0.348, "score_loc": 0.212 }, - { - "component": "Estacado", - "componentData": "Data Complete", - "componentID": 25623296, - "name": "Estacado2", - "rank_data": "1", - "rank_data_loc": "4", - "rank_loc": "Not Displayed", - "score_data": 0.598, - "score_data_loc": 0.314, - "score_loc": 0.029 - }, - { - "component": "Lockney", - "componentData": "Missing Data", - "componentID": 25623334, - "name": "Lockney", - "rank_data": "3", - "rank_data_loc": "5", - "rank_loc": "5", - "score_data": 0.571, - "score_data_loc": 0.31, - "score_loc": 0.05 - }, { "component": "Amarillo", "componentData": "Data Complete", "componentID": 25623212, "name": "Amarillo", - "rank_data": "2", - "rank_data_loc": "6", + "rank_data": "1", + "rank_data_loc": "4", "rank_loc": "8", - "score_data": 0.576, - "score_data_loc": 0.298, + "score_data": 0.646, + "score_data_loc": 0.332, "score_loc": 0.019 }, { @@ -734,11 +710,11 @@ "componentData": "Missing Data", "componentID": 25623333, "name": "Mclean", - "rank_data": "6", - "rank_data_loc": "7", + "rank_data": "5", + "rank_data_loc": "5", "rank_loc": "4", - "score_data": 0.482, - "score_data_loc": 0.291, + "score_data": 0.5, + "score_data_loc": 0.3, "score_loc": 0.1 }, { @@ -746,23 +722,47 @@ "componentData": "Data Complete", "componentID": 25623214, "name": "Friona", - "rank_data": "4", - "rank_data_loc": "8", + "rank_data": "3", + "rank_data_loc": "6", "rank_loc": "7", - "score_data": 0.506, - "score_data_loc": 0.265, + "score_data": 0.544, + "score_data_loc": 0.284, "score_loc": 0.024 }, + { + "component": "Lockney", + "componentData": "Missing Data", + "componentID": 25623334, + "name": "Lockney", + "rank_data": "4", + "rank_data_loc": "7", + "rank_loc": "5", + "score_data": 0.501, + "score_data_loc": 0.276, + "score_loc": 0.05 + }, + { + "component": "Estacado", + "componentData": "Data Complete", + "componentID": 25623296, + "name": "Estacado2", + "rank_data": "6", + "rank_data_loc": "8", + "rank_loc": "Not Displayed", + "score_data": 0.5, + "score_data_loc": 0.264, + "score_loc": 0.029 + }, { "component": "Pullman", "componentData": "Data Complete", "componentID": 25623298, "name": "Pullman", - "rank_data": "9", + "rank_data": "8", "rank_data_loc": "9", "rank_loc": "9", - "score_data": 0.357, - "score_data_loc": 0.188, + "score_data": 0.481, + "score_data_loc": 0.249, "score_loc": 0.018 }, { @@ -785,8 +785,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "6", - "score_data": 0.596, - "score_data_loc": 0.313, + "score_data": 0.416, + "score_data_loc": 0.223, "score_loc": 0.029 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json index 8080267..1f546c5 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[34.92816,-114.80764].json @@ -1,18 +1,18 @@ { "list": { - "AWS_PIW90": 14.84, + "AWS_PIW90": 12.86, "Soil Data Value": [ [ "rfv_class_30", - 0.5233758769036427 + 0.5364552662067039 ], [ - "rfv_class_0", - 0.48072314826451956 + "texture_30", + 0.38440865592401363 ], [ - "texture_30", - 0.25751396689198724 + "rfv_class_0", + 0.3604641496563463 ], [ "texture_0", @@ -146,10 +146,10 @@ } }, "id": { - "component": "Rillito", - "name": "Rillito", + "component": "Chuckawalla", + "name": "Chuckawalla", "rank_loc": "3", - "score_loc": 0.19 + "score_loc": 0.08 }, "lab": {}, "munsell": {}, @@ -158,24 +158,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185645", + "componentID": "14185601", "componentKind": "Series", - "componentPct": 19, + "componentPct": 2, "dataSource": "STATSGO", - "distance": 0.0, + "distance": 353.554689070506, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "660587", - "minCompDistance": 0.0, + "mapunitID": "660584", + "minCompDistance": 353.554689070506, "nirrcapcl": "7", - "nirrcapscl": "e", + "nirrcapscl": "s", "nirrcapunit": "None", - "rfvInfill": "No", + "rfvInfill": "Yes", "sdeURL": "", "seeURL": "", - "slope": 20.0, - "taxsubgrp": "Typic Haplocalcids", + "slope": 15.0, + "taxsubgrp": "Typic Calciargids", "textureInfill": "No" }, "siteDescription": "" @@ -196,10 +196,10 @@ } }, "id": { - "component": "Rositas", - "name": "Rositas1", + "component": "Beeline", + "name": "Beeline", "rank_loc": "4", - "score_loc": 0.091 + "score_loc": 0.05 }, "lab": {}, "munsell": {}, @@ -208,24 +208,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185600", + "componentID": "14185640", "componentKind": "Series", - "componentPct": 10, + "componentPct": 5, "dataSource": "STATSGO", - "distance": 353.554689070506, + "distance": 0.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "660584", - "minCompDistance": 353.554689070506, - "nirrcapcl": "8", - "nirrcapscl": "e", + "mapunitID": "660587", + "minCompDistance": 0.0, + "nirrcapcl": "7", + "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 5.0, - "taxsubgrp": "Typic Torripsamments", + "slope": 24.0, + "taxsubgrp": "Typic Torriorthents", "textureInfill": "No" }, "siteDescription": "" @@ -246,10 +246,10 @@ } }, "id": { - "component": "Chuckawalla", - "name": "Chuckawalla", + "component": "Cipriano", + "name": "Cipriano", "rank_loc": "5", - "score_loc": 0.08 + "score_loc": 0.05 }, "lab": {}, "munsell": {}, @@ -258,24 +258,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185601", + "componentID": "14185643", "componentKind": "Series", - "componentPct": 2, + "componentPct": 5, "dataSource": "STATSGO", - "distance": 353.554689070506, + "distance": 0.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "660584", - "minCompDistance": 353.554689070506, + "mapunitID": "660587", + "minCompDistance": 0.0, "nirrcapcl": "7", "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 15.0, - "taxsubgrp": "Typic Calciargids", + "slope": 18.0, + "taxsubgrp": "Typic Haplodurids", "textureInfill": "No" }, "siteDescription": "" @@ -296,8 +296,8 @@ } }, "id": { - "component": "Beeline", - "name": "Beeline", + "component": "Denure", + "name": "Denure", "rank_loc": "6", "score_loc": 0.05 }, @@ -308,7 +308,7 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185640", + "componentID": "14185639", "componentKind": "Series", "componentPct": 5, "dataSource": "STATSGO", @@ -324,8 +324,8 @@ "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 24.0, - "taxsubgrp": "Typic Torriorthents", + "slope": 4.0, + "taxsubgrp": "Typic Haplocambids", "textureInfill": "No" }, "siteDescription": "" @@ -346,8 +346,8 @@ } }, "id": { - "component": "Momoli", - "name": "Momoli", + "component": "Gilman", + "name": "Gilman", "rank_loc": "7", "score_loc": 0.05 }, @@ -358,24 +358,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185638", + "componentID": "14185646", "componentKind": "Series", "componentPct": 5, "dataSource": "STATSGO", "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", + "irrcapcl": "2", + "irrcapscl": "w", "irrcapunit": "None", "mapunitID": "660587", "minCompDistance": 0.0, "nirrcapcl": "7", - "nirrcapscl": "s", + "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 6.0, - "taxsubgrp": "Typic Haplocambids", + "slope": 3.0, + "taxsubgrp": "Typic Torrifluvents", "textureInfill": "No" }, "siteDescription": "" @@ -396,8 +396,8 @@ } }, "id": { - "component": "Gilman", - "name": "Gilman", + "component": "Mohall", + "name": "Mohall", "rank_loc": "8", "score_loc": 0.05 }, @@ -408,24 +408,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185646", + "componentID": "14185644", "componentKind": "Series", "componentPct": 5, "dataSource": "STATSGO", "distance": 0.0, - "irrcapcl": "2", - "irrcapscl": "w", + "irrcapcl": "None", + "irrcapscl": "None", "irrcapunit": "None", "mapunitID": "660587", "minCompDistance": 0.0, "nirrcapcl": "7", - "nirrcapscl": "w", + "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 3.0, - "taxsubgrp": "Typic Torrifluvents", + "slope": 4.0, + "taxsubgrp": "Typic Calciargids", "textureInfill": "No" }, "siteDescription": "" @@ -446,10 +446,10 @@ } }, "id": { - "component": "Mohall", - "name": "Mohall", + "component": "Antho", + "name": "Antho", "rank_loc": "9", - "score_loc": 0.05 + "score_loc": 0.018 }, "lab": {}, "munsell": {}, @@ -458,24 +458,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185644", + "componentID": "14185610", "componentKind": "Series", - "componentPct": 5, + "componentPct": 2, "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", + "distance": 353.554689070506, + "irrcapcl": "2", + "irrcapscl": "e", "irrcapunit": "None", - "mapunitID": "660587", - "minCompDistance": 0.0, + "mapunitID": "660584", + "minCompDistance": 353.554689070506, "nirrcapcl": "7", - "nirrcapscl": "s", + "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 4.0, - "taxsubgrp": "Typic Calciargids", + "slope": 3.0, + "taxsubgrp": "Typic Torrifluvents", "textureInfill": "No" }, "siteDescription": "" @@ -496,10 +496,10 @@ } }, "id": { - "component": "Cipriano", - "name": "Cipriano", + "component": "Aco", + "name": "Aco", "rank_loc": "10", - "score_loc": 0.05 + "score_loc": 0.009 }, "lab": {}, "munsell": {}, @@ -508,24 +508,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185643", + "componentID": "14185609", "componentKind": "Series", - "componentPct": 5, + "componentPct": 1, "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", + "distance": 353.554689070506, + "irrcapcl": "2", + "irrcapscl": "e", "irrcapunit": "None", - "mapunitID": "660587", - "minCompDistance": 0.0, + "mapunitID": "660584", + "minCompDistance": 353.554689070506, "nirrcapcl": "7", - "nirrcapscl": "s", + "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 18.0, - "taxsubgrp": "Typic Haplodurids", + "slope": 4.0, + "taxsubgrp": "Typic Haplocalcids", "textureInfill": "No" }, "siteDescription": "" @@ -546,10 +546,10 @@ } }, "id": { - "component": "Pinamt", - "name": "Pinamt", + "component": "Indio", + "name": "Indio", "rank_loc": "11", - "score_loc": 0.05 + "score_loc": 0.009 }, "lab": {}, "munsell": {}, @@ -558,24 +558,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185641", + "componentID": "14185607", "componentKind": "Series", - "componentPct": 5, + "componentPct": 1, "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", + "distance": 353.554689070506, + "irrcapcl": "2", + "irrcapscl": "e", "irrcapunit": "None", - "mapunitID": "660587", - "minCompDistance": 0.0, + "mapunitID": "660584", + "minCompDistance": 353.554689070506, "nirrcapcl": "7", - "nirrcapscl": "s", + "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 20.0, - "taxsubgrp": "Typic Calciargids", + "slope": 3.0, + "taxsubgrp": "Typic Torrifluvents", "textureInfill": "No" }, "siteDescription": "" @@ -596,10 +596,10 @@ } }, "id": { - "component": "Denure", - "name": "Denure", + "component": "Lethent", + "name": "Lethent", "rank_loc": "12", - "score_loc": 0.05 + "score_loc": 0.009 }, "lab": {}, "munsell": {}, @@ -608,24 +608,24 @@ "sand": {}, "site": { "siteData": { - "componentID": "14185639", + "componentID": "14185608", "componentKind": "Series", - "componentPct": 5, + "componentPct": 1, "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", + "distance": 353.554689070506, + "irrcapcl": "3", + "irrcapscl": "s", "irrcapunit": "None", - "mapunitID": "660587", - "minCompDistance": 0.0, + "mapunitID": "660584", + "minCompDistance": 353.554689070506, "nirrcapcl": "7", "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 4.0, - "taxsubgrp": "Typic Haplocambids", + "slope": 1.0, + "taxsubgrp": "Typic Natrargids", "textureInfill": "No" }, "siteDescription": "" @@ -782,106 +782,6 @@ }, "texture": {}, "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Rositas", - "name": "Rositas2", - "rank_loc": "Not Displayed", - "score_loc": 0.091 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14185596", - "componentKind": "Series", - "componentPct": 10, - "dataSource": "STATSGO", - "distance": 353.554689070506, - "irrcapcl": "3", - "irrcapscl": "s", - "irrcapunit": "None", - "mapunitID": "660584", - "minCompDistance": 353.554689070506, - "nirrcapcl": "7", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 1.0, - "taxsubgrp": "Typic Torripsamments", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Rositas", - "name": "Rositas3", - "rank_loc": "Not Displayed", - "score_loc": 0.091 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14185606", - "componentKind": "Series", - "componentPct": 5, - "dataSource": "STATSGO", - "distance": 353.554689070506, - "irrcapcl": "3", - "irrcapscl": "s", - "irrcapunit": "None", - "mapunitID": "660584", - "minCompDistance": 353.554689070506, - "nirrcapcl": "7", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 5.0, - "taxsubgrp": "Typic Torripsamments", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} } ] }, @@ -896,157 +796,145 @@ "componentData": "Missing Data", "componentID": 14185597, "name": "Carrizo3", - "rank_data": "6", + "rank_data": "7", "rank_data_loc": "1", "rank_loc": "Not Displayed", - "score_data": 0.785, - "score_data_loc": 0.574, + "score_data": 0.725, + "score_data_loc": 0.544, "score_loc": 0.363 }, { - "component": "Rositas", + "component": "Gunsight", "componentData": "Missing Data", - "componentID": 14185600, - "name": "Rositas1", - "rank_data": "1", + "componentID": 14185636, + "name": "Gunsight1", + "rank_data": "2", "rank_data_loc": "2", - "rank_loc": "4", - "score_data": 0.931, - "score_data_loc": 0.511, - "score_loc": 0.091 + "rank_loc": "2", + "score_data": 0.793, + "score_data_loc": 0.532, + "score_loc": 0.27 }, { "component": "Chuckawalla", "componentData": "Missing Data", "componentID": 14185601, "name": "Chuckawalla", - "rank_data": "2", + "rank_data": "1", "rank_data_loc": "3", - "rank_loc": "5", - "score_data": 0.931, - "score_data_loc": 0.505, + "rank_loc": "3", + "score_data": 0.804, + "score_data_loc": 0.442, "score_loc": 0.08 }, { - "component": "Gunsight", + "component": "Cipriano", "componentData": "Missing Data", - "componentID": 14185602, - "name": "Gunsight2", - "rank_data": "8", + "componentID": 14185643, + "name": "Cipriano", + "rank_data": "3", "rank_data_loc": "4", - "rank_loc": "Not Displayed", - "score_data": 0.717, - "score_data_loc": 0.494, - "score_loc": 0.27 + "rank_loc": "5", + "score_data": 0.784, + "score_data_loc": 0.417, + "score_loc": 0.05 }, { - "component": "Denure", + "component": "Gilman", "componentData": "Missing Data", - "componentID": 14185639, - "name": "Denure", - "rank_data": "3", + "componentID": 14185646, + "name": "Gilman", + "rank_data": "4", "rank_data_loc": "5", - "rank_loc": "12", - "score_data": 0.922, - "score_data_loc": 0.486, + "rank_loc": "7", + "score_data": 0.746, + "score_data_loc": 0.398, "score_loc": 0.05 }, { - "component": "Beeline", + "component": "Mohall", "componentData": "Missing Data", - "componentID": 14185640, - "name": "Beeline", - "rank_data": "4", + "componentID": 14185644, + "name": "Mohall", + "rank_data": "6", "rank_data_loc": "6", - "rank_loc": "6", - "score_data": 0.872, - "score_data_loc": 0.461, + "rank_loc": "8", + "score_data": 0.726, + "score_data_loc": 0.388, "score_loc": 0.05 }, { - "component": "Cipriano", + "component": "Antho", "componentData": "Missing Data", - "componentID": 14185643, - "name": "Cipriano", + "componentID": 14185610, + "name": "Antho", "rank_data": "5", "rank_data_loc": "7", - "rank_loc": "10", - "score_data": 0.835, - "score_data_loc": 0.443, - "score_loc": 0.05 + "rank_loc": "9", + "score_data": 0.746, + "score_data_loc": 0.382, + "score_loc": 0.018 }, { - "component": "Pinamt", + "component": "Beeline", "componentData": "Missing Data", - "componentID": 14185641, - "name": "Pinamt", - "rank_data": "7", + "componentID": 14185640, + "name": "Beeline", + "rank_data": "11", "rank_data_loc": "8", - "rank_loc": "11", - "score_data": 0.748, - "score_data_loc": 0.399, + "rank_loc": "4", + "score_data": 0.695, + "score_data_loc": 0.372, "score_loc": 0.05 }, { - "component": "Rillito", + "component": "Indio", "componentData": "Missing Data", - "componentID": 14185645, - "name": "Rillito", - "rank_data": "12", + "componentID": 14185607, + "name": "Indio", + "rank_data": "8", "rank_data_loc": "9", - "rank_loc": "3", - "score_data": 0.585, - "score_data_loc": 0.387, - "score_loc": 0.19 + "rank_loc": "11", + "score_data": 0.723, + "score_data_loc": 0.366, + "score_loc": 0.009 }, { - "component": "Gilman", + "component": "Lethent", "componentData": "Missing Data", - "componentID": 14185646, - "name": "Gilman", + "componentID": 14185608, + "name": "Lethent", "rank_data": "9", "rank_data_loc": "10", - "rank_loc": "8", - "score_data": 0.616, - "score_data_loc": 0.333, - "score_loc": 0.05 + "rank_loc": "12", + "score_data": 0.722, + "score_data_loc": 0.366, + "score_loc": 0.009 }, { - "component": "Mohall", + "component": "Aco", "componentData": "Missing Data", - "componentID": 14185644, - "name": "Mohall", + "componentID": 14185609, + "name": "Aco", "rank_data": "10", "rank_data_loc": "11", - "rank_loc": "9", - "score_data": 0.616, - "score_data_loc": 0.333, - "score_loc": 0.05 + "rank_loc": "10", + "score_data": 0.715, + "score_data_loc": 0.362, + "score_loc": 0.009 }, { - "component": "Momoli", + "component": "Denure", "componentData": "Missing Data", - "componentID": 14185638, - "name": "Momoli", - "rank_data": "11", + "componentID": 14185639, + "name": "Denure", + "rank_data": "12", "rank_data_loc": "12", - "rank_loc": "7", - "score_data": 0.616, - "score_data_loc": 0.333, + "rank_loc": "6", + "score_data": 0.636, + "score_data_loc": 0.343, "score_loc": 0.05 }, - { - "component": "Carrizo", - "componentData": "Missing Data", - "componentID": 14185605, - "name": "Carrizo2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.752, - "score_data_loc": 0.557, - "score_loc": 0.363 - }, { "component": "Carrizo", "componentData": "Missing Data", @@ -1055,45 +943,33 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "1", - "score_data": 0.653, - "score_data_loc": 0.508, + "score_data": 0.723, + "score_data_loc": 0.543, "score_loc": 0.363 }, { - "component": "Gunsight", - "componentData": "Missing Data", - "componentID": 14185636, - "name": "Gunsight1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "2", - "score_data": 0.702, - "score_data_loc": 0.486, - "score_loc": 0.27 - }, - { - "component": "Rositas", + "component": "Carrizo", "componentData": "Missing Data", - "componentID": 14185606, - "name": "Rositas3", + "componentID": 14185605, + "name": "Carrizo2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.783, - "score_data_loc": 0.437, - "score_loc": 0.091 + "score_data": 0.709, + "score_data_loc": 0.536, + "score_loc": 0.363 }, { - "component": "Rositas", + "component": "Gunsight", "componentData": "Missing Data", - "componentID": 14185596, - "name": "Rositas2", + "componentID": 14185602, + "name": "Gunsight2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.709, - "score_data_loc": 0.4, - "score_loc": 0.091 + "score_data": 0.768, + "score_data_loc": 0.519, + "score_loc": 0.27 } ] } diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json index 3e3c28a..0e5280f 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[35.59918,-120.491439].json @@ -1,21 +1,21 @@ { "list": { - "AWS_PIW90": 5.52, + "AWS_PIW90": 3.77, "Soil Data Value": [ [ - "rfv_class_0", - 0.0035457277021757605 + "texture_0", + 0.0 ], [ - "rfv_class_30", - 0.0035457277021757605 + "texture_30", + 0.0 ], [ - "texture_0", + "rfv_class_0", 0.0 ], [ - "texture_30", + "rfv_class_30", 0.0 ] ], @@ -78,73 +78,17 @@ "nirrcapscl": "e", "nirrcapunit": "nan", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=camatta", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#camatta", "slope": 40.0, "taxsubgrp": "Calcixerollic Xerochrepts", - "textureInfill": "No" + "textureInfill": "Yes" }, "siteDescription": "The Balcom series consists of moderately deep, well drained soils that formed in material that weathered from soft, calcareous shale and sandstone. Balcom soils are on hills and have slopes of 5 to 75 percent. The mean annual precipitation is about 18 inches and the mean annual air temperature is about 61 degrees F." }, "texture": {}, "top_depth": {} }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "R015XE082CA" - ], - "ecoclassname": [ - "Loamy South" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE082CA" - ] - } - }, - "id": { - "component": "Nacimiento", - "name": "Nacimiento1", - "rank_loc": "2", - "score_loc": 0.3 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "26027170", - "componentKind": "Series", - "componentPct": 20, - "dataSource": "SSURGO", - "distance": 44.0, - "irrcapcl": "6", - "irrcapscl": "e", - "irrcapunit": "nan", - "mapunitID": "457218", - "minCompDistance": 44.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "nan", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom", - "slope": 40.0, - "taxsubgrp": "Calcic Haploxerolls", - "textureInfill": "No" - }, - "siteDescription": "The Nacimiento series consists of moderately deep, well drained soils that formed in material weathered from calcareous shale and sandstone. Nacimiento soils are on rolling uplands and have mostly complex slopes of 9 to 75 percent. The mean annual precipitation is about 16 inches and the mean annual air temperature is about 60 degrees F." - }, - "texture": {}, - "top_depth": {} - }, { "bottom_depth": {}, "cec": {}, @@ -166,7 +110,7 @@ "id": { "component": "Los osos", "name": "Los osos1", - "rank_loc": "3", + "rank_loc": "2", "score_loc": 0.2 }, "lab": {}, @@ -190,11 +134,11 @@ "nirrcapscl": "e", "nirrcapunit": "nan", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nacimiento", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nacimiento", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom", "slope": 40.0, "taxsubgrp": "Typic Argixerolls", - "textureInfill": "No" + "textureInfill": "Yes" }, "siteDescription": "The Los Osos series consists of moderately deep, well drained soils that formed in material weathered from sandstone and shale. Los Osos soils are on uplands and have slopes of 5 to 75 percent. The mean annual precipitation is about 25 inches and the mean annual air temperature is about 60 degrees F." }, @@ -209,13 +153,13 @@ "esd": { "ESD": { "ecoclassid": [ - "R015XE020CA" + "R015XE082CA" ], "ecoclassname": [ - "Fine Loamy 9-13" + "Loamy South" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE020CA" + "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE082CA" ] } }, @@ -246,8 +190,8 @@ "nirrcapscl": "e", "nirrcapunit": "1.0", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=balcom", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#balcom", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=mocho", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#mocho", "slope": 20.0, "taxsubgrp": "Calcixerollic Xerochrepts", "textureInfill": "No" @@ -257,62 +201,6 @@ "texture": {}, "top_depth": {} }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "R015XE020CA" - ], - "ecoclassname": [ - "Fine Loamy 9-13" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/015X/R015XE020CA" - ] - } - }, - "id": { - "component": "Nacimiento", - "name": "Nacimiento2", - "rank_loc": "Not Displayed", - "score_loc": 0.3 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "26027161", - "componentKind": "Series", - "componentPct": 20, - "dataSource": "SSURGO", - "distance": 670.0, - "irrcapcl": "4", - "irrcapscl": "e", - "irrcapunit": "1.0", - "mapunitID": "457217", - "minCompDistance": 44.0, - "nirrcapcl": "4", - "nirrcapscl": "e", - "nirrcapunit": "1.0", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nacimiento", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nacimiento", - "slope": 20.0, - "taxsubgrp": "Calcic Haploxerolls", - "textureInfill": "No" - }, - "siteDescription": "The Nacimiento series consists of moderately deep, well drained soils that formed in material weathered from calcareous shale and sandstone. Nacimiento soils are on rolling uplands and have mostly complex slopes of 9 to 75 percent. The mean annual precipitation is about 16 inches and the mean annual air temperature is about 60 degrees F." - }, - "texture": {}, - "top_depth": {} - }, { "bottom_depth": {}, "cec": {}, @@ -358,11 +246,11 @@ "nirrcapscl": "e", "nirrcapunit": "3.0", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=los_osos", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#los_osos", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=linne", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#linne", "slope": 20.0, "taxsubgrp": "Typic Argixerolls", - "textureInfill": "No" + "textureInfill": "Yes" }, "siteDescription": "The Los Osos series consists of moderately deep, well drained soils that formed in material weathered from sandstone and shale. Los Osos soils are on uplands and have slopes of 5 to 75 percent. The mean annual precipitation is about 25 inches and the mean annual air temperature is about 60 degrees F." }, @@ -385,68 +273,44 @@ "rank_data": "1", "rank_data_loc": "1", "rank_loc": "Not Displayed", - "score_data": 0.573, - "score_data_loc": 0.445, + "score_data": 0.57, + "score_data_loc": 0.443, "score_loc": 0.316 }, - { - "component": "Nacimiento", - "componentData": "Data Complete", - "componentID": 26027161, - "name": "Nacimiento2", - "rank_data": "2", - "rank_data_loc": "2", - "rank_loc": "Not Displayed", - "score_data": 0.573, - "score_data_loc": 0.437, - "score_loc": 0.3 - }, { "component": "Los osos", "componentData": NaN, "componentID": 26027715, "name": "Los osos2", - "rank_data": "3", - "rank_data_loc": "3", + "rank_data": "2", + "rank_data_loc": "2", "rank_loc": "Not Displayed", - "score_data": 0.435, - "score_data_loc": 0.318, + "score_data": 0.544, + "score_data_loc": 0.372, "score_loc": 0.2 }, { "component": "Balcom", - "componentData": "Data Complete", + "componentData": NaN, "componentID": 26027166, "name": "Balcom2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "1", - "score_data": 0.355, - "score_data_loc": 0.336, + "score_data": 0.422, + "score_data_loc": 0.369, "score_loc": 0.316 }, - { - "component": "Nacimiento", - "componentData": "Data Complete", - "componentID": 26027170, - "name": "Nacimiento1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "2", - "score_data": 0.331, - "score_data_loc": 0.315, - "score_loc": 0.3 - }, { "component": "Los osos", - "componentData": "Data Complete", + "componentData": NaN, "componentID": 26027683, "name": "Los osos1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "3", - "score_data": 0.331, - "score_data_loc": 0.265, + "rank_loc": "2", + "score_data": 0.314, + "score_data_loc": 0.257, "score_loc": 0.2 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json index fc30087..3a4a911 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.422,-122.084].json @@ -78,8 +78,8 @@ "nirrcapscl": "s", "nirrcapunit": "5.0", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hangerone", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hangerone", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=xerorthents", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#xerorthents", "slope": 1.0, "taxsubgrp": "Cumulic Vertic Endoaquolls", "textureInfill": "No" @@ -190,8 +190,8 @@ "nirrcapscl": "w", "nirrcapunit": "2.0", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=aquic_xerorthents", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#aquic_xerorthents", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clear_lake", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clear_lake", "slope": 4.0, "taxsubgrp": "Aquic Xerorthents", "textureInfill": "No" @@ -246,8 +246,8 @@ "nirrcapscl": "s", "nirrcapunit": "5.0", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clear_lake", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clear_lake", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hangerone", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hangerone", "slope": 1.0, "taxsubgrp": "Xeric Endoaquerts", "textureInfill": "No" @@ -358,8 +358,8 @@ "nirrcapscl": "s", "nirrcapunit": "6.0", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=embarcadero", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#embarcadero", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=xerorthents", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#xerorthents", "slope": 1.0, "taxsubgrp": "Fluvaquentic Endoaquolls", "textureInfill": "No" @@ -433,40 +433,40 @@ "model": "v2" }, "soilRank": [ - { - "component": "Hangerone", - "componentData": "Data Complete", - "componentID": 26038467, - "name": "Hangerone", - "rank_data": "1", - "rank_data_loc": "1", - "rank_loc": "1", - "score_data": 0.78, - "score_data_loc": 0.545, - "score_loc": 0.311 - }, { "component": "Xerorthents", "componentData": "Missing Data", "componentID": 26038503, "name": "Xerorthents1", - "rank_data": "3", - "rank_data_loc": "2", + "rank_data": "1", + "rank_data_loc": "1", "rank_loc": "2", - "score_data": 0.764, - "score_data_loc": 0.534, + "score_data": 0.76, + "score_data_loc": 0.532, "score_loc": 0.304 }, + { + "component": "Hangerone", + "componentData": "Data Complete", + "componentID": 26038467, + "name": "Hangerone", + "rank_data": "5", + "rank_data_loc": "2", + "rank_loc": "1", + "score_data": 0.554, + "score_data_loc": 0.433, + "score_loc": 0.311 + }, { "component": "Aquic xerorthents", "componentData": "Missing Data", "componentID": 26038456, "name": "Aquic xerorthents", - "rank_data": "4", + "rank_data": "6", "rank_data_loc": "3", "rank_loc": "3", - "score_data": 0.764, - "score_data_loc": 0.501, + "score_data": 0.514, + "score_data_loc": 0.375, "score_loc": 0.237 }, { @@ -477,34 +477,34 @@ "rank_data": "2", "rank_data_loc": "4", "rank_loc": "6", - "score_data": 0.769, - "score_data_loc": 0.389, + "score_data": 0.732, + "score_data_loc": 0.371, "score_loc": 0.01 }, - { - "component": "Clear lake", - "componentData": "Data Complete", - "componentID": 26038466, - "name": "Clear lake", - "rank_data": "5", - "rank_data_loc": "5", - "rank_loc": "4", - "score_data": 0.548, - "score_data_loc": 0.285, - "score_loc": 0.021 - }, { "component": "Bayshore", "componentData": "Data Complete", "componentID": 26038468, "name": "Bayshore", - "rank_data": "6", - "rank_data_loc": "6", + "rank_data": "3", + "rank_data_loc": "5", "rank_loc": "5", - "score_data": 0.434, - "score_data_loc": 0.227, + "score_data": 0.709, + "score_data_loc": 0.364, "score_loc": 0.02 }, + { + "component": "Clear lake", + "componentData": "Data Complete", + "componentID": 26038466, + "name": "Clear lake", + "rank_data": "4", + "rank_data_loc": "6", + "rank_loc": "4", + "score_data": 0.597, + "score_data_loc": 0.309, + "score_loc": 0.021 + }, { "component": "Xerorthents", "componentData": "Missing Data", @@ -513,8 +513,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.612, - "score_data_loc": 0.458, + "score_data": 0.662, + "score_data_loc": 0.483, "score_loc": 0.304 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json index 757e700..9c588ee 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[37.48216451,-99.55016693].json @@ -78,8 +78,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=uly", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#uly", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=penden", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#penden", "slope": 5.0, "taxsubgrp": "Typic Haplustolls", "textureInfill": "No" @@ -190,8 +190,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bridgeport", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bridgeport", "slope": 6.0, "taxsubgrp": "Typic Ustorthents", "textureInfill": "No" @@ -246,8 +246,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=holdrege", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#holdrege", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=tobin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#tobin", "slope": 6.0, "taxsubgrp": "Typic Haplustalfs", "textureInfill": "No" @@ -302,8 +302,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=tobin", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#tobin", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=canlon", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#canlon", "slope": 1.0, "taxsubgrp": "Cumulic Haplustolls", "textureInfill": "No" @@ -358,8 +358,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=case", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#case", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney", "slope": 6.0, "taxsubgrp": "Typic Calciustepts", "textureInfill": "No" @@ -414,8 +414,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=penden", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#penden", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=uly", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#uly", "slope": 5.0, "taxsubgrp": "Typic Calciustolls", "textureInfill": "No" @@ -470,8 +470,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bridgeport", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bridgeport", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly", "slope": 3.0, "taxsubgrp": "Fluventic Haplustolls", "textureInfill": "No" @@ -526,8 +526,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=wakeen", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#wakeen", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney", "slope": 2.0, "taxsubgrp": "Entic Haplustolls", "textureInfill": "No" @@ -638,8 +638,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=canlon", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#canlon", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=aquolls", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#aquolls", "slope": 12.0, "taxsubgrp": "Lithic Ustorthents", "textureInfill": "No" @@ -750,8 +750,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly", "slope": 2.0, "taxsubgrp": "Typic Argiustolls", "textureInfill": "No" @@ -806,8 +806,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=harney", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#harney", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=holdrege", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#holdrege", "slope": 4.0, "taxsubgrp": "Typic Argiustolls", "textureInfill": "No" @@ -862,8 +862,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=coly", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#coly", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=case", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#case", "slope": 12.0, "taxsubgrp": "Typic Ustorthents", "textureInfill": "No" @@ -884,13 +884,13 @@ { "component": "Uly", "componentData": "Data Complete", - "componentID": 25865345, - "name": "Uly1", + "componentID": 25865522, + "name": "Uly2", "rank_data": "6", "rank_data_loc": "1", - "rank_loc": "1", - "score_data": 0.598, - "score_data_loc": 0.749, + "rank_loc": "Not Displayed", + "score_data": 0.612, + "score_data_loc": 0.756, "score_loc": 0.9 }, { @@ -898,11 +898,11 @@ "componentData": "Data Complete", "componentID": 25865346, "name": "Harney1", - "rank_data": "7", + "rank_data": "4", "rank_data_loc": "2", "rank_loc": "2", - "score_data": 0.598, - "score_data_loc": 0.675, + "score_data": 0.636, + "score_data_loc": 0.695, "score_loc": 0.753 }, { @@ -910,11 +910,11 @@ "componentData": "Data Complete", "componentID": 25865523, "name": "Coly2", - "rank_data": "2", + "rank_data": "3", "rank_data_loc": "3", "rank_loc": "Not Displayed", - "score_data": 0.697, - "score_data_loc": 0.538, + "score_data": 0.662, + "score_data_loc": 0.521, "score_loc": 0.38 }, { @@ -922,24 +922,24 @@ "componentData": "Data Complete", "componentID": 25865493, "name": "Holdrege", - "rank_data": "5", + "rank_data": "11", "rank_data_loc": "4", "rank_loc": "4", - "score_data": 0.611, - "score_data_loc": 0.467, + "score_data": 0.4, + "score_data_loc": 0.361, "score_loc": 0.322 }, { - "component": "Tobin", + "component": "Penden", "componentData": "Data Complete", - "componentID": 25865519, - "name": "Tobin", - "rank_data": "9", + "componentID": 25865344, + "name": "Penden", + "rank_data": "2", "rank_data_loc": "5", - "rank_loc": "5", - "score_data": 0.561, - "score_data_loc": 0.369, - "score_loc": 0.176 + "rank_loc": "7", + "score_data": 0.667, + "score_data_loc": 0.358, + "score_loc": 0.05 }, { "component": "Canlon", @@ -954,23 +954,23 @@ "score_loc": 0.006 }, { - "component": "Penden", + "component": "Tobin", "componentData": "Data Complete", - "componentID": 25865344, - "name": "Penden", - "rank_data": "3", + "componentID": 25865519, + "name": "Tobin", + "rank_data": "10", "rank_data_loc": "7", - "rank_loc": "7", - "score_data": 0.649, - "score_data_loc": 0.35, - "score_loc": 0.05 + "rank_loc": "5", + "score_data": 0.538, + "score_data_loc": 0.357, + "score_loc": 0.176 }, { "component": "Case", "componentData": "Data Complete", "componentID": 25865495, "name": "Case", - "rank_data": "8", + "rank_data": "7", "rank_data_loc": "8", "rank_loc": "6", "score_data": 0.593, @@ -982,11 +982,11 @@ "componentData": "Data Complete", "componentID": 25865551, "name": "Wakeen", - "rank_data": "4", + "rank_data": "5", "rank_data_loc": "9", "rank_loc": "9", - "score_data": 0.612, - "score_data_loc": 0.322, + "score_data": 0.625, + "score_data_loc": 0.329, "score_loc": 0.032 }, { @@ -994,11 +994,11 @@ "componentData": "Data Complete", "componentID": 25865494, "name": "Bridgeport", - "rank_data": "10", + "rank_data": "8", "rank_data_loc": "10", "rank_loc": "8", - "score_data": 0.523, - "score_data_loc": 0.279, + "score_data": 0.563, + "score_data_loc": 0.3, "score_loc": 0.036 }, { @@ -1006,23 +1006,23 @@ "componentData": "Missing Data", "componentID": 25865552, "name": "Aquolls", - "rank_data": "11", + "rank_data": "9", "rank_data_loc": "11", "rank_loc": "10", - "score_data": 0.393, - "score_data_loc": 0.201, + "score_data": 0.563, + "score_data_loc": 0.286, "score_loc": 0.008 }, { "component": "Uly", "componentData": "Data Complete", - "componentID": 25865522, - "name": "Uly2", + "componentID": 25865345, + "name": "Uly1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.588, - "score_data_loc": 0.744, + "rank_loc": "1", + "score_data": 0.547, + "score_data_loc": 0.724, "score_loc": 0.9 }, { @@ -1033,7 +1033,7 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.551, + "score_data": 0.55, "score_data_loc": 0.652, "score_loc": 0.753 }, @@ -1045,8 +1045,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.483, - "score_data_loc": 0.618, + "score_data": 0.534, + "score_data_loc": 0.644, "score_loc": 0.753 }, { @@ -1057,8 +1057,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "3", - "score_data": 0.611, - "score_data_loc": 0.495, + "score_data": 0.578, + "score_data_loc": 0.479, "score_loc": 0.38 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json index 8f6ae1c..2cd8e41 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[39.26009312,-85.50621214].json @@ -1,14 +1,14 @@ { "list": { - "AWS_PIW90": 3.71, + "AWS_PIW90": 5.34, "Soil Data Value": [ [ "rfv_class_0", - 0.6957144623170968 + 0.9241956327451439 ], [ "rfv_class_30", - 0.4977936090221524 + 0.9150919760274441 ], [ "texture_0", @@ -52,10 +52,10 @@ } }, "id": { - "component": "Miami", - "name": "Miami1", + "component": "Hennepin", + "name": "Hennepin1", "rank_loc": "1", - "score_loc": 0.85 + "score_loc": 0.225 }, "lab": {}, "munsell": {}, @@ -64,27 +64,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325339", + "componentID": "25325347", "componentKind": "Series", - "componentPct": 85, + "componentPct": 5, "dataSource": "SSURGO", - "distance": 0.0, + "distance": 59.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162394", - "minCompDistance": 0.0, - "nirrcapcl": "2", + "mapunitID": "162396", + "minCompDistance": 59.0, + "nirrcapcl": "7", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", - "slope": 4.0, - "taxsubgrp": "Oxyaquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=fincastle", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#fincastle", + "slope": 38.0, + "taxsubgrp": "Typic Eutrudepts", "textureInfill": "No" }, - "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." }, "texture": {}, "top_depth": {} @@ -97,21 +97,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XA009IN" + "" ], "ecoclassname": [ - "Till Ridge" + "" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + "" ] } }, "id": { - "component": "Williamstown", - "name": "Williamstown1", + "component": "Fincastle", + "name": "Fincastle", "rank_loc": "2", - "score_loc": 0.53 + "score_loc": 0.218 }, "lab": {}, "munsell": {}, @@ -120,27 +120,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325400", + "componentID": "25325308", "componentKind": "Series", "componentPct": 85, "dataSource": "SSURGO", - "distance": 59.0, + "distance": 170.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162415", - "minCompDistance": 59.0, + "mapunitID": "162380", + "minCompDistance": 170.0, "nirrcapcl": "2", - "nirrcapscl": "e", + "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=williamstown", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#williamstown", - "slope": 3.0, - "taxsubgrp": "Aquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=grayford", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#grayford", + "slope": 1.0, + "taxsubgrp": "Aeric Epiaqualfs", "textureInfill": "No" }, - "siteDescription": "The Williamstown series consists of very deep, moderately well drained soils that are moderately deep to dense till. The soils formed in as much as 56 cm (22 inches) of loess and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 11.1 degrees C (52 degrees F)." + "siteDescription": "The Fincastle series consists of very deep, somewhat poorly drained soils that are deep to dense till. Fincastle soils formed in loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." }, "texture": {}, "top_depth": {} @@ -153,21 +153,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XA007IN" + "" ], "ecoclassname": [ - "Till Depression Flatwood" + "" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" + "" ] } }, "id": { - "component": "Hennepin", - "name": "Hennepin1", + "component": "Hickory", + "name": "Hickory", "rank_loc": "3", - "score_loc": 0.225 + "score_loc": 0.217 }, "lab": {}, "munsell": {}, @@ -176,27 +176,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325347", + "componentID": "25325331", "componentKind": "Series", - "componentPct": 5, + "componentPct": 87, "dataSource": "SSURGO", - "distance": 59.0, + "distance": 936.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162396", - "minCompDistance": 59.0, + "mapunitID": "162389", + "minCompDistance": 936.0, "nirrcapcl": "7", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", - "slope": 38.0, - "taxsubgrp": "Typic Eutrudepts", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=bonnell", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#bonnell", + "slope": 40.0, + "taxsubgrp": "Typic Hapludalfs", "textureInfill": "No" }, - "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." + "siteDescription": "The Hickory series consists of very deep, well drained, soils on dissected till plains. They formed in till that can be capped with up to 20 inches of loess. Slope ranges from 5 to 70 percent. Mean annual air temperature is about 54 degrees F., and mean annual precipitation is about 40 inches." }, "texture": {}, "top_depth": {} @@ -209,21 +209,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XA009IN" + "F114XB503IN" ], "ecoclassname": [ - "Till Ridge" + "Till Upland Forest" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + "https://edit.jornada.nmsu.edu/catalogs/esd/114X/F114XB503IN" ] } }, "id": { - "component": "Fincastle", - "name": "Fincastle", + "component": "Crosby", + "name": "Crosby1", "rank_loc": "4", - "score_loc": 0.218 + "score_loc": 0.09 }, "lab": {}, "munsell": {}, @@ -232,27 +232,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325308", + "componentID": "25325341", "componentKind": "Series", - "componentPct": 85, + "componentPct": 9, "dataSource": "SSURGO", - "distance": 170.0, + "distance": 0.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162380", - "minCompDistance": 170.0, + "mapunitID": "162394", + "minCompDistance": 0.0, "nirrcapcl": "2", - "nirrcapscl": "w", + "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=fincastle", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#fincastle", - "slope": 1.0, + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hickory", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hickory", + "slope": 2.0, "taxsubgrp": "Aeric Epiaqualfs", "textureInfill": "No" }, - "siteDescription": "The Fincastle series consists of very deep, somewhat poorly drained soils that are deep to dense till. Fincastle soils formed in loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." }, "texture": {}, "top_depth": {} @@ -265,21 +265,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XA009IN" + "" ], "ecoclassname": [ - "Till Ridge" + "" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + "" ] } }, "id": { - "component": "Hickory", - "name": "Hickory", + "component": "Brookston", + "name": "Brookston", "rank_loc": "5", - "score_loc": 0.217 + "score_loc": 0.04 }, "lab": {}, "munsell": {}, @@ -288,27 +288,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325331", + "componentID": "25325342", "componentKind": "Series", - "componentPct": 87, + "componentPct": 4, "dataSource": "SSURGO", - "distance": 936.0, + "distance": 0.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162389", - "minCompDistance": 936.0, - "nirrcapcl": "7", - "nirrcapscl": "e", + "mapunitID": "162394", + "minCompDistance": 0.0, + "nirrcapcl": "2", + "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hickory", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hickory", - "slope": 40.0, - "taxsubgrp": "Typic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=jessietown", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#jessietown", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", "textureInfill": "No" }, - "siteDescription": "The Hickory series consists of very deep, well drained, soils on dissected till plains. They formed in till that can be capped with up to 20 inches of loess. Slope ranges from 5 to 70 percent. Mean annual air temperature is about 54 degrees F., and mean annual precipitation is about 40 inches." + "siteDescription": "The Brookston series consists of very deep, poorly drained soils formed in as much as 51 cm (20 inches) of silty material and the underlying loamy till in depressions on till plains and moraines. Slope ranges from 0 to 3 percent. Mean annual precipitation is about 889 mm (35 inches), and mean annual temperature is about 10.0 degrees C (50 degrees F)." }, "texture": {}, "top_depth": {} @@ -321,21 +321,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XA009IN" + "F111XA008IN" ], "ecoclassname": [ - "Till Ridge" + "Wet Till Ridge" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" ] } }, "id": { - "component": "Xenia", - "name": "Xenia", + "component": "Cyclone", + "name": "Cyclone1", "rank_loc": "6", - "score_loc": 0.212 + "score_loc": 0.026 }, "lab": {}, "munsell": {}, @@ -344,27 +344,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325405", + "componentID": "25325348", "componentKind": "Series", - "componentPct": 85, + "componentPct": 3, "dataSource": "SSURGO", - "distance": 193.0, + "distance": 59.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162416", - "minCompDistance": 193.0, - "nirrcapcl": "1", - "nirrcapscl": "None", + "mapunitID": "162396", + "minCompDistance": 59.0, + "nirrcapcl": "2", + "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=xenia", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#xenia", - "slope": 1.0, - "taxsubgrp": "Aquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", "textureInfill": "No" }, - "siteDescription": "The Xenia series consists of very deep, moderately well drained soils that are deep or very deep to dense till. Xenia soils formed in loess or other silty material and in the underlying loamy till on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1067 mm (42 inches), and mean annual temperature is about 11.1 degrees C (52 degrees F)." + "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." }, "texture": {}, "top_depth": {} @@ -377,21 +377,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XA007IN" + "F111XA008IN" ], "ecoclassname": [ - "Till Depression Flatwood" + "Wet Till Ridge" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" ] } }, "id": { - "component": "Crosby", - "name": "Crosby1", + "component": "Celina", + "name": "Celina", "rank_loc": "7", - "score_loc": 0.09 + "score_loc": 0.013 }, "lab": {}, "munsell": {}, @@ -400,27 +400,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325341", + "componentID": "25325406", "componentKind": "Series", - "componentPct": 9, + "componentPct": 5, "dataSource": "SSURGO", - "distance": 0.0, + "distance": 193.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162394", - "minCompDistance": 0.0, + "mapunitID": "162416", + "minCompDistance": 193.0, "nirrcapcl": "2", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", - "slope": 2.0, - "taxsubgrp": "Aeric Epiaqualfs", + "slope": 4.0, + "taxsubgrp": "Aquic Hapludalfs", "textureInfill": "No" }, - "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + "siteDescription": "The Celina series consists of very deep, moderately well drained soils that are moderately deep to dense till. They formed in as much as 46 cm (18 inches) of loess and the underlying loamy till of high-lime content. They are on till plains and moraines. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 12 degrees C (53 degree F)." }, "texture": {}, "top_depth": {} @@ -433,21 +433,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XA008IN" + "F111XA009IN" ], "ecoclassname": [ - "Wet Till Ridge" + "Till Ridge" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" ] } }, "id": { - "component": "Brookston", - "name": "Brookston", + "component": "Holton", + "name": "Holton", "rank_loc": "8", - "score_loc": 0.04 + "score_loc": 0.01 }, "lab": {}, "munsell": {}, @@ -456,27 +456,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325342", + "componentID": "25325333", "componentKind": "Series", "componentPct": 4, "dataSource": "SSURGO", - "distance": 0.0, + "distance": 936.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162394", - "minCompDistance": 0.0, + "mapunitID": "162389", + "minCompDistance": 936.0, "nirrcapcl": "2", "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brookston", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brookston", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", "slope": 0.5, - "taxsubgrp": "Typic Argiaquolls", + "taxsubgrp": "Aeric Endoaquepts", "textureInfill": "No" }, - "siteDescription": "The Brookston series consists of very deep, poorly drained soils formed in as much as 51 cm (20 inches) of silty material and the underlying loamy till in depressions on till plains and moraines. Slope ranges from 0 to 3 percent. Mean annual precipitation is about 889 mm (35 inches), and mean annual temperature is about 10.0 degrees C (50 degrees F)." + "siteDescription": "The Holton Series consists of very deep, somewhat poorly drained soils formed in loamy alluvium on flood plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 1067 mm (42 inches), and mean annual temperature is about 11 degrees C (52 degrees F)." }, "texture": {}, "top_depth": {} @@ -489,21 +489,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XD010IN" + "F111XA007IN" ], "ecoclassname": [ - "Till Ridge" + "Till Depression Flatwood" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" ] } }, "id": { - "component": "Treaty", - "name": "Treaty1", + "component": "Bonnell", + "name": "Bonnell", "rank_loc": "9", - "score_loc": 0.031 + "score_loc": 0.007 }, "lab": {}, "munsell": {}, @@ -512,27 +512,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325340", + "componentID": "25325330", "componentKind": "Series", - "componentPct": 2, + "componentPct": 3, "dataSource": "SSURGO", - "distance": 0.0, + "distance": 936.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162394", - "minCompDistance": 0.0, - "nirrcapcl": "2", - "nirrcapscl": "w", + "mapunitID": "162389", + "minCompDistance": 936.0, + "nirrcapcl": "6", + "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", - "slope": 0.5, - "taxsubgrp": "Typic Argiaquolls", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone", + "slope": 21.0, + "taxsubgrp": "Typic Hapludalfs", "textureInfill": "No" }, - "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." + "siteDescription": "The Bonnell series consists of very deep, well drained soils that formed in less than 46 cm (18 inches) of loess or loamy materials and the underlying till. These soils are on dissected till plains. Slope ranges from 6 to 60 percent. Mean annual precipitation is about 1067 mm (42 inches), and mean annual temperature is about 12 degrees C (54 degrees F)." }, "texture": {}, "top_depth": {} @@ -545,21 +545,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XD008IN" + "F111XA008IN" ], "ecoclassname": [ - "Till Depression Flatwood" + "Wet Till Ridge" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD008IN" + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" ] } }, "id": { - "component": "Cyclone", - "name": "Cyclone1", + "component": "Cincinnati", + "name": "Cincinnati", "rank_loc": "10", - "score_loc": 0.026 + "score_loc": 0.005 }, "lab": {}, "munsell": {}, @@ -568,27 +568,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325348", + "componentID": "25325332", "componentKind": "Series", - "componentPct": 3, + "componentPct": 2, "dataSource": "SSURGO", - "distance": 59.0, + "distance": 936.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162396", - "minCompDistance": 59.0, - "nirrcapcl": "2", - "nirrcapscl": "w", + "mapunitID": "162389", + "minCompDistance": 936.0, + "nirrcapcl": "3", + "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone", - "slope": 0.5, - "taxsubgrp": "Typic Argiaquolls", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", + "slope": 9.0, + "taxsubgrp": "Oxyaquic Fragiudalfs", "textureInfill": "No" }, - "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." + "siteDescription": "The Cincinnati series consists of very deep, well drained soils that are moderately deep to a fragipan. These soils formed in a mantle of loess, a thin layer of pedisediment, and a paleosol formed in the underlying till. They are on till plains. Slope ranges from 1 to 18 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 12 degrees C (54 degrees F)." }, "texture": {}, "top_depth": {} @@ -601,21 +601,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XD010IN" + "F111XA009IN" ], "ecoclassname": [ "Till Ridge" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" ] } }, "id": { - "component": "Celina", - "name": "Celina", + "component": "Grayford", + "name": "Grayford", "rank_loc": "11", - "score_loc": 0.013 + "score_loc": 0.005 }, "lab": {}, "munsell": {}, @@ -624,27 +624,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325406", + "componentID": "25325329", "componentKind": "Series", - "componentPct": 5, + "componentPct": 2, "dataSource": "SSURGO", - "distance": 193.0, + "distance": 936.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162416", - "minCompDistance": 193.0, - "nirrcapcl": "2", + "mapunitID": "162389", + "minCompDistance": 936.0, + "nirrcapcl": "4", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=celina", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#celina", - "slope": 4.0, - "taxsubgrp": "Aquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", + "slope": 17.0, + "taxsubgrp": "Ultic Hapludalfs", "textureInfill": "No" }, - "siteDescription": "The Celina series consists of very deep, moderately well drained soils that are moderately deep to dense till. They formed in as much as 46 cm (18 inches) of loess and the underlying loamy till of high-lime content. They are on till plains and moraines. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 12 degrees C (53 degree F)." + "siteDescription": "The Grayford series consists of deep, well drained soils formed in less than 56 cm (22 inches) of loess and in the underlying till of Illinoian age and residuum from limestone. They are on dissected till plains and sinkholes. Slope ranges from 2 to 35 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 13 degrees C (55 degrees F)." }, "texture": {}, "top_depth": {} @@ -668,10 +668,10 @@ } }, "id": { - "component": "Rainsville", - "name": "Rainsville", + "component": "Jessietown", + "name": "Jessietown", "rank_loc": "12", - "score_loc": 0.013 + "score_loc": 0.005 }, "lab": {}, "munsell": {}, @@ -680,83 +680,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325345", + "componentID": "25325334", "componentKind": "Series", - "componentPct": 5, - "dataSource": "SSURGO", - "distance": 980.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162395", - "minCompDistance": 980.0, - "nirrcapcl": "3", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rainsville", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rainsville", - "slope": 8.0, - "taxsubgrp": "Oxyaquic Hapludalfs", - "textureInfill": "No" - }, - "siteDescription": "The Rainsville series consists of very deep, moderately well drained soils that are deep or very deep to dense till. The Rainsville soils formed in as much as 51 cm (20 inches) of loess or other silty material and in the underlying loamy outwash and till. They are on ground moraines and end moraines. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 940 mm (37 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA009IN" - ], - "ecoclassname": [ - "Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" - ] - } - }, - "id": { - "component": "Miami", - "name": "Miami2", - "rank_loc": "Not Displayed", - "score_loc": 0.85 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325349", - "componentKind": "Taxadjunct", - "componentPct": 92, + "componentPct": 2, "dataSource": "SSURGO", - "distance": 59.0, + "distance": 936.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162396", - "minCompDistance": 0.0, - "nirrcapcl": "4", + "mapunitID": "162389", + "minCompDistance": 936.0, + "nirrcapcl": "7", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", - "slope": 15.0, - "taxsubgrp": "Typic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=celina", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#celina", + "slope": 38.0, + "taxsubgrp": "Typic Hapludults", "textureInfill": "No" }, - "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + "siteDescription": "The Jessietown series consists of moderately deep, well drained soils formed in a thin mantle of silty material and residuum weathered from black fissile shale. Permeability is moderate. These gently sloping to steep soils are on upland ridges, side slopes, and toe slopes. Slopes range from 2 to 30 percent. The mean annual temperature is about 57 degrees F, and the mean annual precipitation is about 46 inches." }, "texture": {}, "top_depth": {} @@ -780,10 +724,10 @@ } }, "id": { - "component": "Miami", - "name": "Miami3", + "component": "Hennepin", + "name": "Hennepin2", "rank_loc": "Not Displayed", - "score_loc": 0.85 + "score_loc": 0.225 }, "lab": {}, "munsell": {}, @@ -792,27 +736,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325350", + "componentID": "25325325", "componentKind": "Series", - "componentPct": 96, + "componentPct": 90, "dataSource": "SSURGO", - "distance": 85.0, + "distance": 175.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162397", - "minCompDistance": 0.0, - "nirrcapcl": "4", + "mapunitID": "162386", + "minCompDistance": 59.0, + "nirrcapcl": "7", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", - "slope": 9.0, - "taxsubgrp": "Oxyaquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone", + "slope": 35.0, + "taxsubgrp": "Typic Eutrudepts", "textureInfill": "No" }, - "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." }, "texture": {}, "top_depth": {} @@ -836,10 +780,10 @@ } }, "id": { - "component": "Miami", - "name": "Miami4", + "component": "Hennepin", + "name": "Hennepin3", "rank_loc": "Not Displayed", - "score_loc": 0.85 + "score_loc": 0.225 }, "lab": {}, "munsell": {}, @@ -848,27 +792,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325326", + "componentID": "25325355", "componentKind": "Series", - "componentPct": 10, + "componentPct": 2, "dataSource": "SSURGO", - "distance": 175.0, + "distance": 502.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162386", - "minCompDistance": 0.0, - "nirrcapcl": "2", + "mapunitID": "162398", + "minCompDistance": 59.0, + "nirrcapcl": "6", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", - "slope": 4.0, - "taxsubgrp": "Oxyaquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", + "slope": 22.0, + "taxsubgrp": "Typic Eutrudepts", "textureInfill": "No" }, - "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." }, "texture": {}, "top_depth": {} @@ -881,21 +825,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F111XD010IN" + "" ], "ecoclassname": [ - "Till Ridge" + "" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" + "" ] } }, "id": { - "component": "Miami", - "name": "Miami5", + "component": "Crosby", + "name": "Crosby2", "rank_loc": "Not Displayed", - "score_loc": 0.85 + "score_loc": 0.09 }, "lab": {}, "munsell": {}, @@ -904,27 +848,27 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325352", + "componentID": "25325351", "componentKind": "Series", - "componentPct": 90, + "componentPct": 4, "dataSource": "SSURGO", - "distance": 502.0, + "distance": 85.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "162398", + "mapunitID": "162397", "minCompDistance": 0.0, - "nirrcapcl": "6", - "nirrcapscl": "e", + "nirrcapcl": "2", + "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", - "slope": 15.0, - "taxsubgrp": "Oxyaquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cincinnati", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cincinnati", + "slope": 1.0, + "taxsubgrp": "Aeric Epiaqualfs", "textureInfill": "No" }, - "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." }, "texture": {}, "top_depth": {} @@ -937,21 +881,21 @@ "esd": { "ESD": { "ecoclassid": [ - "F114XB503IN" + "" ], "ecoclassname": [ - "Till Upland Forest" + "" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/114X/F114XB503IN" + "" ] } }, "id": { - "component": "Miami", - "name": "Miami6", + "component": "Crosby", + "name": "Crosby3", "rank_loc": "Not Displayed", - "score_loc": 0.85 + "score_loc": 0.09 }, "lab": {}, "munsell": {}, @@ -960,9 +904,9 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325346", + "componentID": "25325344", "componentKind": "Series", - "componentPct": 85, + "componentPct": 5, "dataSource": "SSURGO", "distance": 980.0, "irrcapcl": "None", @@ -970,17 +914,17 @@ "irrcapunit": "None", "mapunitID": "162395", "minCompDistance": 0.0, - "nirrcapcl": "3", + "nirrcapcl": "2", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=miami", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#miami", - "slope": 8.0, - "taxsubgrp": "Oxyaquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=holton", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#holton", + "slope": 1.0, + "taxsubgrp": "Aeric Epiaqualfs", "textureInfill": "No" }, - "siteDescription": "The Miami series consists of very deep, moderately well drained soils that are moderately deep to dense till. Miami soils formed in as much as 46 cm (18 inches) of loess or silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 60 percent. Mean annual precipitation is 1016 mm (40 inches), and mean annual temperature is 11.1 degrees C (52 degrees F)." + "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." }, "texture": {}, "top_depth": {} @@ -1004,10 +948,10 @@ } }, "id": { - "component": "Williamstown", - "name": "Williamstown2", + "component": "Cyclone", + "name": "Cyclone2", "rank_loc": "Not Displayed", - "score_loc": 0.53 + "score_loc": 0.026 }, "lab": {}, "munsell": {}, @@ -1016,9 +960,9 @@ "sand": {}, "site": { "siteData": { - "componentID": "25325309", + "componentID": "25325310", "componentKind": "Series", - "componentPct": 5, + "componentPct": 10, "dataSource": "SSURGO", "distance": 170.0, "irrcapcl": "None", @@ -1027,855 +971,231 @@ "mapunitID": "162380", "minCompDistance": 59.0, "nirrcapcl": "2", - "nirrcapscl": "e", + "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=williamstown", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#williamstown", - "slope": 4.0, - "taxsubgrp": "Aquic Hapludalfs", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brookston", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brookston", + "slope": 0.5, + "taxsubgrp": "Typic Argiaquolls", "textureInfill": "No" }, - "siteDescription": "The Williamstown series consists of very deep, moderately well drained soils that are moderately deep to dense till. The soils formed in as much as 56 cm (22 inches) of loess and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 11.1 degrees C (52 degrees F)." + "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." }, "texture": {}, "top_depth": {} + } + ] + }, + "rank": { + "metadata": { + "location": "us", + "model": "v2" + }, + "soilRank": [ + { + "component": "Fincastle", + "componentData": "Data Complete", + "componentID": 25325308, + "name": "Fincastle", + "rank_data": "2", + "rank_data_loc": "1", + "rank_loc": "2", + "score_data": 0.671, + "score_data_loc": 0.445, + "score_loc": 0.218 }, { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA008IN" - ], - "ecoclassname": [ - "Wet Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" - ] - } - }, - "id": { - "component": "Williamstown", - "name": "Williamstown3", - "rank_loc": "Not Displayed", - "score_loc": 0.53 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325354", - "componentKind": "Series", - "componentPct": 1, - "dataSource": "SSURGO", - "distance": 502.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162398", - "minCompDistance": 59.0, - "nirrcapcl": "2", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=williamstown", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#williamstown", - "slope": 1.0, - "taxsubgrp": "Aquic Hapludalfs", - "textureInfill": "No" - }, - "siteDescription": "The Williamstown series consists of very deep, moderately well drained soils that are moderately deep to dense till. The soils formed in as much as 56 cm (22 inches) of loess and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 12 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual air temperature is about 11.1 degrees C (52 degrees F)." - }, - "texture": {}, - "top_depth": {} + "component": "Hennepin", + "componentData": "Data Complete", + "componentID": 25325355, + "name": "Hennepin3", + "rank_data": "6", + "rank_data_loc": "2", + "rank_loc": "Not Displayed", + "score_data": 0.624, + "score_data_loc": 0.425, + "score_loc": 0.225 }, { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA007IN" - ], - "ecoclassname": [ - "Till Depression Flatwood" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA007IN" - ] - } - }, - "id": { - "component": "Hennepin", - "name": "Hennepin2", - "rank_loc": "Not Displayed", - "score_loc": 0.225 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325325", - "componentKind": "Series", - "componentPct": 90, - "dataSource": "SSURGO", - "distance": 175.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162386", - "minCompDistance": 59.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", - "slope": 35.0, - "taxsubgrp": "Typic Eutrudepts", - "textureInfill": "No" - }, - "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA008IN" - ], - "ecoclassname": [ - "Wet Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA008IN" - ] - } - }, - "id": { - "component": "Hennepin", - "name": "Hennepin3", - "rank_loc": "Not Displayed", - "score_loc": 0.225 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325355", - "componentKind": "Series", - "componentPct": 2, - "dataSource": "SSURGO", - "distance": 502.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162398", - "minCompDistance": 59.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hennepin", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hennepin", - "slope": 22.0, - "taxsubgrp": "Typic Eutrudepts", - "textureInfill": "No" - }, - "siteDescription": "The Hennepin series consists of very deep, well drained soils formed in calcareous glacial till. These soils are on upland side slopes that border stream valleys and on moraines. Permeability is moderate or moderately slow. Slopes range from 10 to 70 percent. Mean annual temperature is about 52 degrees F, and mean annual precipitation is about 35 inches." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA009IN" - ], - "ecoclassname": [ - "Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" - ] - } - }, - "id": { - "component": "Crosby", - "name": "Crosby2", - "rank_loc": "Not Displayed", - "score_loc": 0.09 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325351", - "componentKind": "Series", - "componentPct": 4, - "dataSource": "SSURGO", - "distance": 85.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162397", - "minCompDistance": 0.0, - "nirrcapcl": "2", - "nirrcapscl": "w", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", - "slope": 1.0, - "taxsubgrp": "Aeric Epiaqualfs", - "textureInfill": "No" - }, - "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA009IN" - ], - "ecoclassname": [ - "Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" - ] - } - }, - "id": { - "component": "Crosby", - "name": "Crosby3", - "rank_loc": "Not Displayed", - "score_loc": 0.09 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325344", - "componentKind": "Series", - "componentPct": 5, - "dataSource": "SSURGO", - "distance": 980.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162395", - "minCompDistance": 0.0, - "nirrcapcl": "2", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=crosby", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#crosby", - "slope": 1.0, - "taxsubgrp": "Aeric Epiaqualfs", - "textureInfill": "No" - }, - "siteDescription": "The Crosby series consists of very deep, somewhat poorly drained soils that are moderately deep to dense till. Crosby soils formed in as much as 56 cm (22 inches) of loess or other silty material and in the underlying loamy till. They are on till plains. Slope ranges from 0 to 6 percent. Mean annual precipitation is about 1016 mm (40 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA009IN" - ], - "ecoclassname": [ - "Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" - ] - } - }, - "id": { - "component": "Treaty", - "name": "Treaty2", - "rank_loc": "Not Displayed", - "score_loc": 0.031 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325401", - "componentKind": "Series", - "componentPct": 5, - "dataSource": "SSURGO", - "distance": 59.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162415", - "minCompDistance": 0.0, - "nirrcapcl": "2", - "nirrcapscl": "w", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", - "slope": 0.5, - "taxsubgrp": "Typic Argiaquolls", - "textureInfill": "No" - }, - "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XA009IN" - ], - "ecoclassname": [ - "Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XA009IN" - ] - } - }, - "id": { - "component": "Treaty", - "name": "Treaty3", - "rank_loc": "Not Displayed", - "score_loc": 0.031 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325403", - "componentKind": "Series", - "componentPct": 5, - "dataSource": "SSURGO", - "distance": 193.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162416", - "minCompDistance": 0.0, - "nirrcapcl": "2", - "nirrcapscl": "w", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", - "slope": 0.5, - "taxsubgrp": "Typic Argiaquolls", - "textureInfill": "No" - }, - "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XD010IN" - ], - "ecoclassname": [ - "Till Ridge" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD010IN" - ] - } - }, - "id": { - "component": "Treaty", - "name": "Treaty4", - "rank_loc": "Not Displayed", - "score_loc": 0.031 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325343", - "componentKind": "Series", - "componentPct": 5, - "dataSource": "SSURGO", - "distance": 980.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162395", - "minCompDistance": 0.0, - "nirrcapcl": "2", - "nirrcapscl": "w", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=treaty", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#treaty", - "slope": 0.5, - "taxsubgrp": "Typic Argiaquolls", - "textureInfill": "No" - }, - "siteDescription": "The Treaty series consists of very deep, poorly drained soils that formed in loess and in the underlying loamy till. The Treaty soils are in depressions on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 965 mm (38 inches), and mean annual air temperature is about 11 degrees C (51 degrees F)." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F111XD008IN" - ], - "ecoclassname": [ - "Till Depression Flatwood" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/111X/F111XD008IN" - ] - } - }, - "id": { - "component": "Cyclone", - "name": "Cyclone2", - "rank_loc": "Not Displayed", - "score_loc": 0.026 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25325310", - "componentKind": "Series", - "componentPct": 10, - "dataSource": "SSURGO", - "distance": 170.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "162380", - "minCompDistance": 59.0, - "nirrcapcl": "2", - "nirrcapscl": "w", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=cyclone", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#cyclone", - "slope": 0.5, - "taxsubgrp": "Typic Argiaquolls", - "textureInfill": "No" - }, - "siteDescription": "The Cyclone series consists of very deep, poorly drained soils that formed in loess or silty material and in the underlying drift. Cyclone soils are on till plains. Slope ranges from 0 to 2 percent. Mean annual precipitation is about 991 mm (39 inches), and mean annual temperature is about 10.6 degrees C (51 degrees F)." - }, - "texture": {}, - "top_depth": {} - } - ] - }, - "rank": { - "metadata": { - "location": "us", - "model": "v2" - }, - "soilRank": [ - { - "component": "Miami", - "componentData": "Data Complete", - "componentID": 25325349, - "name": "Miami2", - "rank_data": "5", - "rank_data_loc": "1", - "rank_loc": "Not Displayed", - "score_data": 0.542, - "score_data_loc": 0.696, - "score_loc": 0.85 - }, - { - "component": "Williamstown", - "componentData": "Data Complete", - "componentID": 25325354, - "name": "Williamstown3", - "rank_data": "2", - "rank_data_loc": "2", - "rank_loc": "Not Displayed", - "score_data": 0.588, - "score_data_loc": 0.559, - "score_loc": 0.53 - }, - { - "component": "Hennepin", + "component": "Crosby", "componentData": "Data Complete", - "componentID": 25325325, - "name": "Hennepin2", + "componentID": 25325344, + "name": "Crosby3", "rank_data": "3", "rank_data_loc": "3", "rank_loc": "Not Displayed", - "score_data": 0.569, - "score_data_loc": 0.397, - "score_loc": 0.225 + "score_data": 0.665, + "score_data_loc": 0.377, + "score_loc": 0.09 }, { - "component": "Treaty", + "component": "Hickory", "componentData": "Data Complete", - "componentID": 25325401, - "name": "Treaty2", - "rank_data": "1", + "componentID": 25325331, + "name": "Hickory", + "rank_data": "12", "rank_data_loc": "4", - "rank_loc": "Not Displayed", - "score_data": 0.652, - "score_data_loc": 0.341, - "score_loc": 0.031 + "rank_loc": "3", + "score_data": 0.499, + "score_data_loc": 0.358, + "score_loc": 0.217 }, { - "component": "Xenia", + "component": "Brookston", "componentData": "Data Complete", - "componentID": 25325405, - "name": "Xenia", - "rank_data": "6", + "componentID": 25325342, + "name": "Brookston", + "rank_data": "4", "rank_data_loc": "5", - "rank_loc": "6", - "score_data": 0.448, - "score_data_loc": 0.33, - "score_loc": 0.212 + "rank_loc": "5", + "score_data": 0.656, + "score_data_loc": 0.348, + "score_loc": 0.04 }, { - "component": "Crosby", + "component": "Bonnell", "componentData": "Data Complete", - "componentID": 25325351, - "name": "Crosby2", - "rank_data": "4", + "componentID": 25325330, + "name": "Bonnell", + "rank_data": "1", "rank_data_loc": "6", - "rank_loc": "Not Displayed", - "score_data": 0.569, - "score_data_loc": 0.329, - "score_loc": 0.09 + "rank_loc": "9", + "score_data": 0.689, + "score_data_loc": 0.348, + "score_loc": 0.007 }, { - "component": "Fincastle", + "component": "Holton", "componentData": "Data Complete", - "componentID": 25325308, - "name": "Fincastle", - "rank_data": "7", + "componentID": 25325333, + "name": "Holton", + "rank_data": "5", "rank_data_loc": "7", - "rank_loc": "4", - "score_data": 0.407, - "score_data_loc": 0.313, - "score_loc": 0.218 + "rank_loc": "8", + "score_data": 0.637, + "score_data_loc": 0.324, + "score_loc": 0.01 }, { - "component": "Hickory", + "component": "Cyclone", "componentData": "Data Complete", - "componentID": 25325331, - "name": "Hickory", + "componentID": 25325348, + "name": "Cyclone1", "rank_data": "8", "rank_data_loc": "8", - "rank_loc": "5", - "score_data": 0.407, - "score_data_loc": 0.312, - "score_loc": 0.217 + "rank_loc": "6", + "score_data": 0.613, + "score_data_loc": 0.32, + "score_loc": 0.026 }, { - "component": "Cyclone", + "component": "Cincinnati", "componentData": "Data Complete", - "componentID": 25325310, - "name": "Cyclone2", - "rank_data": "9", + "componentID": 25325332, + "name": "Cincinnati", + "rank_data": "7", "rank_data_loc": "9", - "rank_loc": "Not Displayed", - "score_data": 0.363, - "score_data_loc": 0.194, - "score_loc": 0.026 + "rank_loc": "10", + "score_data": 0.62, + "score_data_loc": 0.313, + "score_loc": 0.005 }, { "component": "Celina", "componentData": "Data Complete", "componentID": 25325406, "name": "Celina", - "rank_data": "10", + "rank_data": "9", "rank_data_loc": "10", - "rank_loc": "11", - "score_data": 0.333, - "score_data_loc": 0.173, + "rank_loc": "7", + "score_data": 0.611, + "score_data_loc": 0.312, "score_loc": 0.013 }, { - "component": "Rainsville", + "component": "Grayford", "componentData": "Data Complete", - "componentID": 25325345, - "name": "Rainsville", - "rank_data": "11", + "componentID": 25325329, + "name": "Grayford", + "rank_data": "10", "rank_data_loc": "11", - "rank_loc": "12", - "score_data": 0.333, - "score_data_loc": 0.173, - "score_loc": 0.013 + "rank_loc": "11", + "score_data": 0.524, + "score_data_loc": 0.265, + "score_loc": 0.005 }, { - "component": "Brookston", + "component": "Jessietown", "componentData": "Data Complete", - "componentID": 25325342, - "name": "Brookston", - "rank_data": "12", + "componentID": 25325334, + "name": "Jessietown", + "rank_data": "11", "rank_data_loc": "12", - "rank_loc": "8", - "score_data": 0.3, - "score_data_loc": 0.17, - "score_loc": 0.04 - }, - { - "component": "Miami", - "componentData": "Data Complete", - "componentID": 25325352, - "name": "Miami5", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.447, - "score_data_loc": 0.648, - "score_loc": 0.85 - }, - { - "component": "Miami", - "componentData": "Data Complete", - "componentID": 25325346, - "name": "Miami6", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.437, - "score_data_loc": 0.644, - "score_loc": 0.85 - }, - { - "component": "Miami", - "componentData": "Data Complete", - "componentID": 25325326, - "name": "Miami4", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.433, - "score_data_loc": 0.641, - "score_loc": 0.85 + "rank_loc": "12", + "score_data": 0.508, + "score_data_loc": 0.257, + "score_loc": 0.005 }, { - "component": "Miami", + "component": "Hennepin", "componentData": "Data Complete", - "componentID": 25325339, - "name": "Miami1", + "componentID": 25325347, + "name": "Hennepin1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "1", - "score_data": 0.42, - "score_data_loc": 0.635, - "score_loc": 0.85 - }, - { - "component": "Miami", - "componentData": "Data Complete", - "componentID": 25325350, - "name": "Miami3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.331, - "score_data_loc": 0.59, - "score_loc": 0.85 - }, - { - "component": "Williamstown", - "componentData": "Data Complete", - "componentID": 25325309, - "name": "Williamstown2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.447, - "score_data_loc": 0.488, - "score_loc": 0.53 - }, - { - "component": "Williamstown", - "componentData": "Data Complete", - "componentID": 25325400, - "name": "Williamstown1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "2", - "score_data": 0.407, - "score_data_loc": 0.469, - "score_loc": 0.53 + "score_data": 0.54, + "score_data_loc": 0.383, + "score_loc": 0.225 }, { "component": "Hennepin", "componentData": "Data Complete", - "componentID": 25325355, - "name": "Hennepin3", + "componentID": 25325325, + "name": "Hennepin2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.569, - "score_data_loc": 0.397, + "score_data": 0.536, + "score_data_loc": 0.381, "score_loc": 0.225 }, - { - "component": "Treaty", - "componentData": "Data Complete", - "componentID": 25325403, - "name": "Treaty3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.652, - "score_data_loc": 0.341, - "score_loc": 0.031 - }, { "component": "Crosby", "componentData": "Data Complete", - "componentID": 25325344, - "name": "Crosby3", + "componentID": 25325341, + "name": "Crosby1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.569, - "score_data_loc": 0.329, + "rank_loc": "4", + "score_data": 0.606, + "score_data_loc": 0.348, "score_loc": 0.09 }, - { - "component": "Hennepin", - "componentData": "Data Complete", - "componentID": 25325347, - "name": "Hennepin1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "3", - "score_data": 0.407, - "score_data_loc": 0.316, - "score_loc": 0.225 - }, - { - "component": "Treaty", - "componentData": "Data Complete", - "componentID": 25325343, - "name": "Treaty4", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.398, - "score_data_loc": 0.214, - "score_loc": 0.031 - }, { "component": "Crosby", "componentData": "Data Complete", - "componentID": 25325341, - "name": "Crosby1", + "componentID": 25325351, + "name": "Crosby2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "7", - "score_data": 0.3, - "score_data_loc": 0.195, + "rank_loc": "Not Displayed", + "score_data": 0.552, + "score_data_loc": 0.321, "score_loc": 0.09 }, { "component": "Cyclone", "componentData": "Data Complete", - "componentID": 25325348, - "name": "Cyclone1", + "componentID": 25325310, + "name": "Cyclone2", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "10", - "score_data": 0.333, - "score_data_loc": 0.18, + "rank_loc": "Not Displayed", + "score_data": 0.552, + "score_data_loc": 0.289, "score_loc": 0.026 - }, - { - "component": "Treaty", - "componentData": "Data Complete", - "componentID": 25325340, - "name": "Treaty1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "9", - "score_data": 0.3, - "score_data_loc": 0.165, - "score_loc": 0.031 } ] } diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json index 246b0db..034edc6 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.494912,-123.064531].json @@ -1,14 +1,14 @@ { "list": { - "AWS_PIW90": 9.5, + "AWS_PIW90": 9.79, "Soil Data Value": [ [ - "rfv_class_0", - 1.382609666499055 + "rfv_class_30", + 1.3604010133524282 ], [ - "rfv_class_30", - 1.3411411272079812 + "rfv_class_0", + 0.8793335839752081 ], [ "texture_0", @@ -78,8 +78,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ruch", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ruch", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=colestine", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#colestine", "slope": 14.0, "taxsubgrp": "Mollic Palexeralfs", "textureInfill": "No" @@ -107,66 +107,10 @@ ] } }, - "id": { - "component": "Vannoy", - "name": "Vannoy1", - "rank_loc": "2", - "score_loc": 0.528 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25443533", - "componentKind": "Series", - "componentPct": 80, - "dataSource": "SSURGO", - "distance": 52.0, - "irrcapcl": "nan", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "469685", - "minCompDistance": 52.0, - "nirrcapcl": "4", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=vannoy", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#vannoy", - "slope": 24.0, - "taxsubgrp": "Mollic Haploxeralfs", - "textureInfill": "No" - }, - "siteDescription": "The Vannoy series consists of moderately deep, well drained soils that formed in colluvium weathered from metamorphic and sedimentary rocks. Vannoy soils are on uplands and have slopes of 2 to 60 percent. The mean annual precipitation is about 30 inches. The mean annual temperature is about 50 degrees F." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F005XZ003CA" - ], - "ecoclassname": [ - "Terraces" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA" - ] - } - }, "id": { "component": "Abegg", "name": "Abegg", - "rank_loc": "3", + "rank_loc": "2", "score_loc": 0.207 }, "lab": {}, @@ -190,8 +134,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abegg", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abegg", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=beekman", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#beekman", "slope": 10.0, "taxsubgrp": "Ultic Haploxeralfs", "textureInfill": "No" @@ -209,20 +153,20 @@ "esd": { "ESD": { "ecoclassid": [ - "F005XZ007CA" + "R005XY016OR" ], "ecoclassname": [ - "Moderately Deep Mesic Hills 40-60Ppt" + "Poorly Drained Bottom" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ007CA" + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/R005XY016OR" ] } }, "id": { "component": "Caris", "name": "Caris", - "rank_loc": "4", + "rank_loc": "3", "score_loc": 0.15 }, "lab": {}, @@ -246,8 +190,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=caris", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#caris", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=aquolls", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#aquolls", "slope": 63.0, "taxsubgrp": "Typic Xerochrepts", "textureInfill": "No" @@ -265,20 +209,20 @@ "esd": { "ESD": { "ecoclassid": [ - "F005XZ024CA" + "F005XZ003CA" ], "ecoclassname": [ - "Ridges" + "Terraces" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ024CA" + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA" ] } }, "id": { "component": "Beekman", "name": "Beekman", - "rank_loc": "5", + "rank_loc": "4", "score_loc": 0.138 }, "lab": {}, @@ -302,8 +246,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=beekman", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#beekman", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gregory", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gregory", "slope": 65.0, "taxsubgrp": "Dystric Xerochrepts", "textureInfill": "No" @@ -321,20 +265,20 @@ "esd": { "ESD": { "ecoclassid": [ - "F005XZ014CA" + "F005XZ024CA" ], "ecoclassname": [ - "Mesic Mountains <40Ppt" + "Ridges" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ024CA" ] } }, "id": { "component": "Josephine", "name": "Josephine1", - "rank_loc": "6", + "rank_loc": "5", "score_loc": 0.138 }, "lab": {}, @@ -358,8 +302,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=josephine", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#josephine", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ruch", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ruch", "slope": 45.0, "taxsubgrp": "Typic Haploxerults", "textureInfill": "No" @@ -369,118 +313,6 @@ "texture": {}, "top_depth": {} }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F005XZ014CA" - ], - "ecoclassname": [ - "Mesic Mountains <40Ppt" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" - ] - } - }, - "id": { - "component": "Voorhies", - "name": "Voorhies", - "rank_loc": "7", - "score_loc": 0.135 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25443535", - "componentKind": "Series", - "componentPct": 30, - "dataSource": "SSURGO", - "distance": 100.0, - "irrcapcl": "nan", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "469686", - "minCompDistance": 100.0, - "nirrcapcl": "7", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=voorhies", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#voorhies", - "slope": 45.0, - "taxsubgrp": "Mollic Haploxeralfs", - "textureInfill": "No" - }, - "siteDescription": "The Voorhies series consists of moderately deep, well drained soils that formed in colluvium weathered from altered sedimentary and extrusive igneous rocks. Voorhies soils are on mountain slopes and have slopes of 35 to 55 percent. Mean annual precipitation is about 30 inches and mean annual temperature is about 50 degrees F." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F005XZ003CA" - ], - "ecoclassname": [ - "Terraces" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA" - ] - } - }, - "id": { - "component": "Speaker", - "name": "Speaker", - "rank_loc": "8", - "score_loc": 0.113 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25443479", - "componentKind": "Series", - "componentPct": 45, - "dataSource": "SSURGO", - "distance": 712.0, - "irrcapcl": "nan", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "469660", - "minCompDistance": 712.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=speaker", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#speaker", - "slope": 45.0, - "taxsubgrp": "Ultic Haploxeralfs", - "textureInfill": "No" - }, - "siteDescription": "The Speaker series consists of moderately deep, well drained soils that formed in colluvium weathered from sedimentary and metamorphic rocks. Speaker soils are on low rolling foot slopes and side slopes and have gradients of 2 to 75 percent. The mean annual precipitation is about 45 inches and the mean annual temperature is about 50 degrees F." - }, - "texture": {}, - "top_depth": {} - }, { "bottom_depth": {}, "cec": {}, @@ -502,7 +334,7 @@ "id": { "component": "Colestine", "name": "Colestine", - "rank_loc": "9", + "rank_loc": "6", "score_loc": 0.075 }, "lab": {}, @@ -526,8 +358,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=colestine", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#colestine", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=josephine", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#josephine", "slope": 65.0, "taxsubgrp": "Dystric Xerochrepts", "textureInfill": "No" @@ -558,7 +390,7 @@ "id": { "component": "Pollard", "name": "Pollard", - "rank_loc": "10", + "rank_loc": "7", "score_loc": 0.075 }, "lab": {}, @@ -582,8 +414,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=pollard", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#pollard", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abegg", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abegg", "slope": 24.0, "taxsubgrp": "Typic Haploxerults", "textureInfill": "No" @@ -614,7 +446,7 @@ "id": { "component": "Offenbacher", "name": "Offenbacher", - "rank_loc": "11", + "rank_loc": "8", "score_loc": 0.05 }, "lab": {}, @@ -638,8 +470,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=offenbacher", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#offenbacher", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=aqualfs", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#aqualfs", "slope": 63.0, "taxsubgrp": "Typic Xerochrepts", "textureInfill": "No" @@ -670,7 +502,7 @@ "id": { "component": "Gregory", "name": "Gregory", - "rank_loc": "12", + "rank_loc": "9", "score_loc": 0.02 }, "lab": {}, @@ -694,8 +526,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gregory", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gregory", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=offenbacher", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#offenbacher", "slope": 2.0, "taxsubgrp": "Pachic Argixerolls", "textureInfill": "No" @@ -713,69 +545,13 @@ "esd": { "ESD": { "ecoclassid": [ - "R005XY016OR" - ], - "ecoclassname": [ - "Poorly Drained Bottom" - ], - "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/R005XY016OR" - ] - } - }, - "id": { - "component": "Vannoy", - "name": "Vannoy2", - "rank_loc": "Not Displayed", - "score_loc": 0.528 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "25443534", - "componentKind": "Series", - "componentPct": 50, - "dataSource": "SSURGO", - "distance": 100.0, - "irrcapcl": "nan", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "469686", - "minCompDistance": 52.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=vannoy", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#vannoy", - "slope": 45.0, - "taxsubgrp": "Mollic Haploxeralfs", - "textureInfill": "No" - }, - "siteDescription": "The Vannoy series consists of moderately deep, well drained soils that formed in colluvium weathered from metamorphic and sedimentary rocks. Vannoy soils are on uplands and have slopes of 2 to 60 percent. The mean annual precipitation is about 30 inches. The mean annual temperature is about 50 degrees F." - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": [ - "F005XZ014CA" + "F005XZ003CA" ], "ecoclassname": [ - "Mesic Mountains <40Ppt" + "Terraces" ], "edit_url": [ - "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ014CA" + "https://edit.jornada.nmsu.edu/catalogs/esd/005X/F005XZ003CA" ] } }, @@ -806,8 +582,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=josephine", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#josephine", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=aqualfs", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#aqualfs", "slope": 24.0, "taxsubgrp": "Typic Haploxerults", "textureInfill": "No" @@ -830,156 +606,108 @@ "componentData": "Data Complete", "componentID": 25443415, "name": "Ruch", - "rank_data": "2", + "rank_data": "5", "rank_data_loc": "1", "rank_loc": "1", - "score_data": 0.704, - "score_data_loc": 0.752, + "score_data": 0.619, + "score_data_loc": 0.709, "score_loc": 0.8 }, { - "component": "Vannoy", + "component": "Abegg", "componentData": "Data Complete", - "componentID": 25443534, - "name": "Vannoy2", - "rank_data": "5", + "componentID": 25443548, + "name": "Abegg", + "rank_data": "2", "rank_data_loc": "2", - "rank_loc": "Not Displayed", - "score_data": 0.593, - "score_data_loc": 0.56, - "score_loc": 0.528 + "rank_loc": "2", + "score_data": 0.763, + "score_data_loc": 0.485, + "score_loc": 0.207 }, { - "component": "Abegg", + "component": "Gregory", "componentData": "Data Complete", - "componentID": 25443548, - "name": "Abegg", - "rank_data": "4", + "componentID": 25443414, + "name": "Gregory", + "rank_data": "1", "rank_data_loc": "3", - "rank_loc": "3", - "score_data": 0.648, - "score_data_loc": 0.427, - "score_loc": 0.207 + "rank_loc": "9", + "score_data": 0.767, + "score_data_loc": 0.394, + "score_loc": 0.02 }, { "component": "Josephine", - "componentData": "Data Complete", + "componentData": NaN, "componentID": 25443848, "name": "Josephine2", - "rank_data": "3", + "rank_data": "4", "rank_data_loc": "4", "rank_loc": "Not Displayed", - "score_data": 0.671, - "score_data_loc": 0.404, + "score_data": 0.648, + "score_data_loc": 0.393, "score_loc": 0.138 }, - { - "component": "Gregory", - "componentData": "Data Complete", - "componentID": 25443414, - "name": "Gregory", - "rank_data": "1", - "rank_data_loc": "5", - "rank_loc": "12", - "score_data": 0.731, - "score_data_loc": 0.376, - "score_loc": 0.02 - }, { "component": "Pollard", - "componentData": "Data Complete", + "componentData": NaN, "componentID": 25443850, "name": "Pollard", - "rank_data": "6", - "rank_data_loc": "6", - "rank_loc": "10", - "score_data": 0.538, - "score_data_loc": 0.306, + "rank_data": "3", + "rank_data_loc": "5", + "rank_loc": "7", + "score_data": 0.702, + "score_data_loc": 0.388, "score_loc": 0.075 }, { - "component": "Voorhies", - "componentData": "Data Complete", - "componentID": 25443535, - "name": "Voorhies", - "rank_data": "8", - "rank_data_loc": "7", - "rank_loc": "7", - "score_data": 0.442, - "score_data_loc": 0.288, - "score_loc": 0.135 + "component": "Caris", + "componentData": NaN, + "componentID": 25443598, + "name": "Caris", + "rank_data": "6", + "rank_data_loc": "6", + "rank_loc": "3", + "score_data": 0.549, + "score_data_loc": 0.349, + "score_loc": 0.15 }, { "component": "Beekman", "componentData": "Data Complete", "componentID": 25443287, "name": "Beekman", - "rank_data": "9", - "rank_data_loc": "8", - "rank_loc": "5", - "score_data": 0.432, - "score_data_loc": 0.285, - "score_loc": 0.138 - }, - { - "component": "Speaker", - "componentData": "Data Complete", - "componentID": 25443479, - "name": "Speaker", - "rank_data": "10", - "rank_data_loc": "9", - "rank_loc": "8", - "score_data": 0.432, - "score_data_loc": 0.272, - "score_loc": 0.113 - }, - { - "component": "Offenbacher", - "componentData": "Data Complete", - "componentID": 25443597, - "name": "Offenbacher", "rank_data": "7", - "rank_data_loc": "10", - "rank_loc": "11", - "score_data": 0.487, - "score_data_loc": 0.268, - "score_loc": 0.05 - }, - { - "component": "Caris", - "componentData": "Data Complete", - "componentID": 25443598, - "name": "Caris", - "rank_data": "12", - "rank_data_loc": "11", + "rank_data_loc": "7", "rank_loc": "4", - "score_data": 0.382, - "score_data_loc": 0.266, - "score_loc": 0.15 + "score_data": 0.532, + "score_data_loc": 0.335, + "score_loc": 0.138 }, { "component": "Colestine", "componentData": "Data Complete", "componentID": 25443286, "name": "Colestine", - "rank_data": "11", - "rank_data_loc": "12", - "rank_loc": "9", - "score_data": 0.405, - "score_data_loc": 0.24, + "rank_data": "8", + "rank_data_loc": "8", + "rank_loc": "6", + "score_data": 0.521, + "score_data_loc": 0.298, "score_loc": 0.075 }, { - "component": "Vannoy", + "component": "Offenbacher", "componentData": "Data Complete", - "componentID": 25443533, - "name": "Vannoy1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "2", - "score_data": 0.572, - "score_data_loc": 0.55, - "score_loc": 0.528 + "componentID": 25443597, + "name": "Offenbacher", + "rank_data": "9", + "rank_data_loc": "9", + "rank_loc": "8", + "score_data": 0.369, + "score_data_loc": 0.209, + "score_loc": 0.05 }, { "component": "Josephine", @@ -988,9 +716,9 @@ "name": "Josephine1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "6", - "score_data": 0.509, - "score_data_loc": 0.323, + "rank_loc": "5", + "score_data": 0.58, + "score_data_loc": 0.359, "score_loc": 0.138 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json index 8239ca5..6bc0145 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[42.63413723,-94.31005777].json @@ -78,8 +78,8 @@ "nirrcapscl": "None", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nicollet", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nicollet", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=storden", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#storden", "slope": 2.0, "taxsubgrp": "Aquic Hapludolls", "textureInfill": "No" @@ -134,8 +134,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=webster", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#webster", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clarion", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clarion", "slope": 1.0, "taxsubgrp": "Typic Endoaquolls", "textureInfill": "No" @@ -190,8 +190,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=clarion", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#clarion", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=webster", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#webster", "slope": 3.0, "taxsubgrp": "Oxyaquic Hapludolls", "textureInfill": "No" @@ -246,8 +246,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=okoboji", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#okoboji", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=nicollet", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#nicollet", "slope": 0.0, "taxsubgrp": "Cumulic Vertic Endoaquolls", "textureInfill": "No" @@ -302,8 +302,8 @@ "nirrcapscl": "w", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=glencoe", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#glencoe", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=okoboji", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#okoboji", "slope": 0.0, "taxsubgrp": "Cumulic Endoaquolls", "textureInfill": "No" @@ -358,8 +358,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=storden", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#storden", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=glencoe", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#glencoe", "slope": 8.0, "taxsubgrp": "Typic Eutrudepts", "textureInfill": "No" @@ -438,11 +438,11 @@ "componentData": "Data Complete", "componentID": 25584608, "name": "Nicollet", - "rank_data": "5", + "rank_data": "7", "rank_data_loc": "1", "rank_loc": 1, - "score_data": 0.344, - "score_data_loc": 0.597, + "score_data": 0.22, + "score_data_loc": 0.535, "score_loc": 0.85 }, { @@ -450,11 +450,11 @@ "componentData": "Data Complete", "componentID": 25584606, "name": "Webster", - "rank_data": "6", + "rank_data": "4", "rank_data_loc": "2", "rank_loc": 2, - "score_data": 0.268, - "score_data_loc": 0.473, + "score_data": 0.336, + "score_data_loc": 0.507, "score_loc": 0.679 }, { @@ -462,11 +462,11 @@ "componentData": "Data Complete", "componentID": 25584604, "name": "Clarion", - "rank_data": "4", + "rank_data": "1", "rank_data_loc": "3", "rank_loc": 3, - "score_data": 0.365, - "score_data_loc": 0.385, + "score_data": 0.48, + "score_data_loc": 0.442, "score_loc": 0.404 }, { @@ -474,7 +474,7 @@ "componentData": "Data Complete", "componentID": 25584602, "name": "Storden", - "rank_data": "1", + "rank_data": "2", "rank_data_loc": "4", "rank_loc": 6, "score_data": 0.458, @@ -486,11 +486,11 @@ "componentData": "Data Complete", "componentID": 25584960, "name": "Glencoe", - "rank_data": "2", + "rank_data": "3", "rank_data_loc": "5", "rank_loc": 5, - "score_data": 0.436, - "score_data_loc": 0.23, + "score_data": 0.402, + "score_data_loc": 0.213, "score_loc": 0.024 }, { @@ -498,11 +498,11 @@ "componentData": "Missing Data", "componentID": 25584952, "name": "Okoboji", - "rank_data": "3", + "rank_data": "5", "rank_data_loc": "6", "rank_loc": 4, - "score_data": 0.402, - "score_data_loc": 0.226, + "score_data": 0.315, + "score_data_loc": 0.182, "score_loc": 0.05 }, { @@ -510,11 +510,11 @@ "componentData": "Data Complete", "componentID": 25584962, "name": "Canisteo", - "rank_data": "7", + "rank_data": "6", "rank_data_loc": "7", "rank_loc": 7, - "score_data": 0.205, - "score_data_loc": 0.11, + "score_data": 0.268, + "score_data_loc": 0.142, "score_loc": 0.016 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json index 8b84e0b..6c88c5a 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[43.06450312,-119.4596489].json @@ -78,8 +78,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonely", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonely", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rinconflat", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rinconflat", "slope": 19.0, "taxsubgrp": "Xeric Haplocambids", "textureInfill": "No" @@ -134,11 +134,11 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=robson", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#robson", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ausmus", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ausmus", "slope": 10.0, "taxsubgrp": "Lithic Xeric Haplargids", - "textureInfill": "No" + "textureInfill": "Yes" }, "siteDescription": "The Robson series consists of shallow, well drained soils that formed in residuum derived from igneous rock. Robson soils are on hill and mountain crests and side slopes. Slopes are 2 to 75 percent. The mean annual precipitation is about 380 mm and the mean annual temperature is about 6 degrees C." }, @@ -246,8 +246,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rinconflat", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rinconflat", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=raz", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#raz", "slope": 7.0, "taxsubgrp": "Xeric Haplocambids", "textureInfill": "No" @@ -302,8 +302,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=actem", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#actem", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brace", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brace", "slope": 11.0, "taxsubgrp": "Xeric Argidurids", "textureInfill": "No" @@ -358,8 +358,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonegrave", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonegrave", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=robson", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#robson", "slope": 55.0, "taxsubgrp": "Xeric Haplocambids", "textureInfill": "No" @@ -414,8 +414,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=raz", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#raz", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonely", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonely", "slope": 11.0, "taxsubgrp": "Xeric Haplodurids", "textureInfill": "No" @@ -470,8 +470,8 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=brace", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#brace", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=lonegrave", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#lonegrave", "slope": 11.0, "taxsubgrp": "Xeric Argidurids", "textureInfill": "No" @@ -526,11 +526,11 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=ausmus", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#ausmus", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=actem", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#actem", "slope": 1.0, "taxsubgrp": "Aquic Natrargids", - "textureInfill": "Yes" + "textureInfill": "No" }, "siteDescription": "The Ausmus series consists of very deep, somewhat poorly drained or moderately well drained soils that formed in alluvium and lacustrine deposits derived from volcanic rocks and volcanic ash. Ausmus soils are on low lake terraces. Slopes are 0 to 2 percent. The mean annual precipitation is about 230 mm and the mean annual temperature is about 6.5 degrees C." }, @@ -553,8 +553,8 @@ "rank_data": "6", "rank_data_loc": "1", "rank_loc": 1, - "score_data": 0.63, - "score_data_loc": 0.565, + "score_data": 0.638, + "score_data_loc": 0.569, "score_loc": 0.5 }, { @@ -562,23 +562,47 @@ "componentData": "Data Complete", "componentID": 25442848, "name": "Robson", - "rank_data": "5", + "rank_data": "1", "rank_data_loc": "2", "rank_loc": 2, - "score_data": 0.646, - "score_data_loc": 0.498, + "score_data": 0.759, + "score_data_loc": 0.554, "score_loc": 0.35 }, + { + "component": "Reallis", + "componentData": "Data Complete", + "componentID": 25442630, + "name": "Reallis", + "rank_data": "2", + "rank_data_loc": "3", + "rank_loc": 3, + "score_data": 0.696, + "score_data_loc": 0.454, + "score_loc": 0.212 + }, { "component": "Actem", "componentData": "Data Complete", "componentID": 25443068, "name": "Actem", "rank_data": "4", - "rank_data_loc": "3", + "rank_data_loc": "4", "rank_loc": 5, - "score_data": 0.657, - "score_data_loc": 0.435, + "score_data": 0.649, + "score_data_loc": 0.43, + "score_loc": 0.212 + }, + { + "component": "Rinconflat", + "componentData": "Data Complete", + "componentID": 25442616, + "name": "Rinconflat", + "rank_data": "8", + "rank_data_loc": "5", + "rank_loc": 4, + "score_data": 0.593, + "score_data_loc": 0.403, "score_loc": 0.212 }, { @@ -586,11 +610,11 @@ "componentData": "Data Complete", "componentID": 25442636, "name": "Raz", - "rank_data": "3", - "rank_data_loc": "4", + "rank_data": "5", + "rank_data_loc": "6", "rank_loc": 7, - "score_data": 0.723, - "score_data_loc": 0.424, + "score_data": 0.648, + "score_data_loc": 0.387, "score_loc": 0.125 }, { @@ -598,47 +622,23 @@ "componentData": "Data Complete", "componentID": 25442637, "name": "Brace", - "rank_data": "1", - "rank_data_loc": "5", + "rank_data": "3", + "rank_data_loc": "7", "rank_loc": 8, - "score_data": 0.756, - "score_data_loc": 0.421, + "score_data": 0.652, + "score_data_loc": 0.369, "score_loc": 0.087 }, - { - "component": "Reallis", - "componentData": "Data Complete", - "componentID": 25442630, - "name": "Reallis", - "rank_data": "7", - "rank_data_loc": "6", - "rank_loc": 3, - "score_data": 0.588, - "score_data_loc": 0.4, - "score_loc": 0.212 - }, - { - "component": "Rinconflat", - "componentData": "Data Complete", - "componentID": 25442616, - "name": "Rinconflat", - "rank_data": "8", - "rank_data_loc": "7", - "rank_loc": 4, - "score_data": 0.587, - "score_data_loc": 0.4, - "score_loc": 0.212 - }, { "component": "Ausmus", "componentData": "Data Complete", "componentID": 25442629, "name": "Ausmus", - "rank_data": "2", + "rank_data": "7", "rank_data_loc": "8", "rank_loc": 9, - "score_data": 0.746, - "score_data_loc": 0.378, + "score_data": 0.633, + "score_data_loc": 0.322, "score_loc": 0.01 }, { @@ -649,8 +649,8 @@ "rank_data": "9", "rank_data_loc": "9", "rank_loc": 6, - "score_data": 0.406, - "score_data_loc": 0.284, + "score_data": 0.471, + "score_data_loc": 0.317, "score_loc": 0.163 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json index fdf0304..b4be3b9 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[45.88932423,-121.0347381].json @@ -117,11 +117,11 @@ "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=gunn", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#gunn", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=kiakus", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#kiakus", "slope": 19.0, "taxsubgrp": "Ultic Haploxeralfs", - "textureInfill": "No" + "textureInfill": "Yes" }, "siteDescription": "Landscape--plateaus, hills\nLandform--structural benches, hillslopes, ridgetops\nSlope--0 to 65 percent\nParent material--loess mixed with colluvium and residuum derived from basalt\nMean annual precipitation--about 530 mm\nMean annual air temperature--about 9 degrees C\nDepth class--deep, very deep\nDrainage class--well drained\nSoil moisture regime--xeric\nSoil temperature regime--mesic\nSoil moisture subclass--typic" }, @@ -138,14 +138,14 @@ "soilRank": [ { "component": "Gunn", - "componentData": "Data Complete", + "componentData": NaN, "componentID": 25483316, "name": "Gunn2", "rank_data": "1", "rank_data_loc": "1", "rank_loc": "Not Displayed", - "score_data": 0.443, - "score_data_loc": 0.697, + "score_data": 0.481, + "score_data_loc": 0.715, "score_loc": 0.95 }, { @@ -156,7 +156,7 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "1", - "score_data": 0.401, + "score_data": 0.399, "score_data_loc": 0.675, "score_loc": 0.95 } diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json index 1e94264..1e67dc3 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[47.213922,-69.28246582].json @@ -78,8 +78,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rawsonville", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rawsonville", "slope": 40.0, "taxsubgrp": "Lithic Udifolists", "textureInfill": "No" @@ -190,8 +190,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson", "slope": 25.0, "taxsubgrp": "Typic Haplorthods", "textureInfill": "No" @@ -246,8 +246,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock", "slope": 25.0, "taxsubgrp": "Lithic Haplorthods", "textureInfill": "No" @@ -302,8 +302,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hogback", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hogback", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram", "slope": 50.0, "taxsubgrp": "Lithic Haplohumods", "textureInfill": "No" @@ -358,8 +358,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=rawsonville", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#rawsonville", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock", "slope": 20.0, "taxsubgrp": "Typic Haplohumods", "textureInfill": "No" @@ -414,8 +414,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson", "slope": 30.0, "taxsubgrp": "Lithic Haplorthods", "textureInfill": "No" @@ -470,8 +470,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=knob_lock", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#knob_lock", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=hogback", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#hogback", "slope": 30.0, "taxsubgrp": "Lithic Udifolists", "textureInfill": "No" @@ -582,8 +582,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=chesuncook", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#chesuncook", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram", "slope": 12.0, "taxsubgrp": "Aquic Haplorthods", "textureInfill": "No" @@ -638,8 +638,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=chesuncook", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#chesuncook", "slope": 40.0, "taxsubgrp": "Typic Haplorthods", "textureInfill": "No" @@ -694,8 +694,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=monson", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#monson", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville", "slope": 40.0, "taxsubgrp": "Lithic Haplorthods", "textureInfill": "No" @@ -750,8 +750,8 @@ "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", - "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=abram", - "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#abram", + "sdeURL": "https://casoilresource.lawr.ucdavis.edu/sde/?series=elliottsville", + "seeURL": "https://casoilresource.lawr.ucdavis.edu/see/#elliottsville", "slope": 45.0, "taxsubgrp": "Lithic Haplorthods", "textureInfill": "No" @@ -772,13 +772,13 @@ { "component": "Chesuncook", "componentData": "Data Complete", - "componentID": 25209555, - "name": "Chesuncook1", + "componentID": 25209552, + "name": "Chesuncook2", "rank_data": "1", "rank_data_loc": "1", - "rank_loc": "2", - "score_data": 0.725, - "score_data_loc": 0.577, + "rank_loc": "Not Displayed", + "score_data": 0.726, + "score_data_loc": 0.578, "score_loc": 0.429 }, { @@ -786,11 +786,11 @@ "componentData": "Data Complete", "componentID": 25209556, "name": "Knob lock2", - "rank_data": "4", + "rank_data": "2", "rank_data_loc": "2", "rank_loc": "Not Displayed", - "score_data": 0.645, - "score_data_loc": 0.553, + "score_data": 0.667, + "score_data_loc": 0.563, "score_loc": 0.46 }, { @@ -798,11 +798,11 @@ "componentData": "Data Complete", "componentID": 25209557, "name": "Elliottsville1", - "rank_data": "2", + "rank_data": "3", "rank_data_loc": "3", "rank_loc": "3", - "score_data": 0.685, - "score_data_loc": 0.493, + "score_data": 0.648, + "score_data_loc": 0.475, "score_loc": 0.301 }, { @@ -810,7 +810,7 @@ "componentData": "Data Complete", "componentID": 25209554, "name": "Monson1", - "rank_data": "3", + "rank_data": "4", "rank_data_loc": "4", "rank_loc": "4", "score_data": 0.648, @@ -822,7 +822,7 @@ "componentData": "Data Complete", "componentID": 25208409, "name": "Rawsonville", - "rank_data": "6", + "rank_data": "5", "rank_data_loc": "5", "rank_loc": "6", "score_data": 0.624, @@ -834,11 +834,11 @@ "componentData": "Data Complete", "componentID": 25209553, "name": "Abram1", - "rank_data": "5", + "rank_data": "6", "rank_data_loc": "6", "rank_loc": "7", - "score_data": 0.631, - "score_data_loc": 0.332, + "score_data": 0.622, + "score_data_loc": 0.328, "score_loc": 0.034 }, { @@ -849,20 +849,20 @@ "rank_data": "7", "rank_data_loc": "7", "rank_loc": "5", - "score_data": 0.486, - "score_data_loc": 0.268, + "score_data": 0.497, + "score_data_loc": 0.274, "score_loc": 0.05 }, { "component": "Chesuncook", "componentData": "Data Complete", - "componentID": 25209552, - "name": "Chesuncook2", + "componentID": 25209555, + "name": "Chesuncook1", "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.692, - "score_data_loc": 0.561, + "rank_loc": "2", + "score_data": 0.717, + "score_data_loc": 0.573, "score_loc": 0.429 }, { @@ -873,8 +873,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "1", - "score_data": 0.584, - "score_data_loc": 0.522, + "score_data": 0.578, + "score_data_loc": 0.519, "score_loc": 0.46 }, { @@ -885,8 +885,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.529, - "score_data_loc": 0.494, + "score_data": 0.55, + "score_data_loc": 0.505, "score_loc": 0.46 }, { @@ -897,8 +897,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.434, - "score_data_loc": 0.367, + "score_data": 0.587, + "score_data_loc": 0.444, "score_loc": 0.301 }, { @@ -909,8 +909,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.603, - "score_data_loc": 0.351, + "score_data": 0.587, + "score_data_loc": 0.343, "score_loc": 0.1 }, { @@ -921,8 +921,8 @@ "rank_data": "Not Displayed", "rank_data_loc": "Not Displayed", "rank_loc": "Not Displayed", - "score_data": 0.571, - "score_data_loc": 0.302, + "score_data": 0.404, + "score_data_loc": 0.219, "score_loc": 0.034 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json deleted file mode 100644 index 28f661a..0000000 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[48.6956,-121.8166].json +++ /dev/null @@ -1,1162 +0,0 @@ -{ - "list": { - "AWS_PIW90": 5.71, - "Soil Data Value": [ - [ - "rfv_class_0", - 0.976020648236615 - ], - [ - "rfv_class_30", - 0.976020648236615 - ], - [ - "texture_0", - 0.0 - ], - [ - "texture_30", - 0.0 - ] - ], - "metadata": { - "location": "us", - "model": "v3", - "unit_measure": { - "cec": "cmol(c)/kg", - "clay": "%", - "depth": "cm", - "distance": "m", - "ec": "ds/m", - "rock_fragments": "cm3/100cm3", - "sand": "%" - } - }, - "soilList": [ - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Andic cryumbrepts", - "name": "Andic cryumbrepts", - "rank_loc": "1", - "score_loc": 0.152 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14269504", - "componentKind": "Taxon above family", - "componentPct": 20, - "dataSource": "STATSGO", - "distance": 994.2109898924772, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "676031", - "minCompDistance": 994.2109898924772, - "nirrcapcl": "7", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 53.0, - "taxsubgrp": "None", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Nimue", - "name": "Nimue1", - "rank_loc": "2", - "score_loc": 0.13 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268942", - "componentKind": "Series", - "componentPct": 13, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 48.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Cryorthods", - "name": "Cryorthods", - "rank_loc": "3", - "score_loc": 0.114 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14269505", - "componentKind": "Taxon above family", - "componentPct": 15, - "dataSource": "STATSGO", - "distance": 994.2109898924772, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "676031", - "minCompDistance": 994.2109898924772, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 60.0, - "taxsubgrp": "None", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Playco", - "name": "Playco1", - "rank_loc": "4", - "score_loc": 0.09 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268933", - "componentKind": "Series", - "componentPct": 9, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 48.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Cryumbrepts", - "name": "Cryumbrepts", - "rank_loc": "5", - "score_loc": 0.076 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14269506", - "componentKind": "Taxon above family", - "componentPct": 10, - "dataSource": "STATSGO", - "distance": 994.2109898924772, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "676031", - "minCompDistance": 994.2109898924772, - "nirrcapcl": "7", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 60.0, - "taxsubgrp": "None", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Getchell", - "name": "Getchell1", - "rank_loc": "6", - "score_loc": 0.06 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268946", - "componentKind": "Series", - "componentPct": 6, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 48.0, - "taxsubgrp": "Aquic Haplocryands", - "textureInfill": "Yes" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Oso", - "name": "Oso", - "rank_loc": "7", - "score_loc": 0.05 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268939", - "componentKind": "Series", - "componentPct": 5, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 78.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "Yes" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Wollard", - "name": "Wollard", - "rank_loc": "8", - "score_loc": 0.05 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268937", - "componentKind": "Series", - "componentPct": 4, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 48.0, - "taxsubgrp": "Alic Haplocryands", - "textureInfill": "Yes" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Diobsud", - "name": "Diobsud", - "rank_loc": "9", - "score_loc": 0.04 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268932", - "componentKind": "Series", - "componentPct": 4, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 48.0, - "taxsubgrp": "Andic Humicryods", - "textureInfill": "Yes" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Shuksan", - "name": "Shuksan", - "rank_loc": "10", - "score_loc": 0.04 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268938", - "componentKind": "Series", - "componentPct": 4, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 45.0, - "taxsubgrp": "Andic Humicryods", - "textureInfill": "Yes" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Cryaquepts", - "name": "Cryaquepts", - "rank_loc": "11", - "score_loc": 0.038 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14269507", - "componentKind": "Taxon above family", - "componentPct": 5, - "dataSource": "STATSGO", - "distance": 994.2109898924772, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "676031", - "minCompDistance": 994.2109898924772, - "nirrcapcl": "7", - "nirrcapscl": "w", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 2.0, - "taxsubgrp": "None", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Cryohumods", - "name": "Cryohumods", - "rank_loc": "12", - "score_loc": 0.038 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14269509", - "componentKind": "Taxon above family", - "componentPct": 5, - "dataSource": "STATSGO", - "distance": 994.2109898924772, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "676031", - "minCompDistance": 994.2109898924772, - "nirrcapcl": "7", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 60.0, - "taxsubgrp": "None", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Nimue", - "name": "Nimue2", - "rank_loc": "Not Displayed", - "score_loc": 0.13 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268930", - "componentKind": "Series", - "componentPct": 7, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 45.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Nimue", - "name": "Nimue3", - "rank_loc": "Not Displayed", - "score_loc": 0.13 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268934", - "componentKind": "Series", - "componentPct": 3, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 19.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Playco", - "name": "Playco2", - "rank_loc": "Not Displayed", - "score_loc": 0.09 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268941", - "componentKind": "Series", - "componentPct": 7, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 48.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Playco", - "name": "Playco3", - "rank_loc": "Not Displayed", - "score_loc": 0.09 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268940", - "componentKind": "Series", - "componentPct": 4, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 19.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Playco", - "name": "Playco4", - "rank_loc": "Not Displayed", - "score_loc": 0.09 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268936", - "componentKind": "Series", - "componentPct": 3, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 19.0, - "taxsubgrp": "Andic Haplocryods", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "Getchell", - "name": "Getchell2", - "rank_loc": "Not Displayed", - "score_loc": 0.06 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "14268944", - "componentKind": "Series", - "componentPct": 5, - "dataSource": "STATSGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "675975", - "minCompDistance": 0.0, - "nirrcapcl": "6", - "nirrcapscl": "e", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 17.0, - "taxsubgrp": "Aquic Haplocryands", - "textureInfill": "Yes" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - } - ] - }, - "rank": { - "metadata": { - "location": "us", - "model": "v2" - }, - "soilRank": [ - { - "component": "Playco", - "componentData": "Missing Data", - "componentID": 14268936, - "name": "Playco4", - "rank_data": "1", - "rank_data_loc": "1", - "rank_loc": "Not Displayed", - "score_data": 0.776, - "score_data_loc": 0.433, - "score_loc": 0.09 - }, - { - "component": "Nimue", - "componentData": "Missing Data", - "componentID": 14268942, - "name": "Nimue1", - "rank_data": "5", - "rank_data_loc": "2", - "rank_loc": "2", - "score_data": 0.578, - "score_data_loc": 0.354, - "score_loc": 0.13 - }, - { - "component": "Shuksan", - "componentData": "Missing Data", - "componentID": 14268938, - "name": "Shuksan", - "rank_data": "2", - "rank_data_loc": "3", - "rank_loc": "10", - "score_data": 0.663, - "score_data_loc": 0.351, - "score_loc": 0.04 - }, - { - "component": "Getchell", - "componentData": "Missing Data", - "componentID": 14268946, - "name": "Getchell1", - "rank_data": "3", - "rank_data_loc": "4", - "rank_loc": "6", - "score_data": 0.606, - "score_data_loc": 0.333, - "score_loc": 0.06 - }, - { - "component": "Cryorthods", - "componentData": "Missing Data", - "componentID": 14269505, - "name": "Cryorthods", - "rank_data": "7", - "rank_data_loc": "5", - "rank_loc": "3", - "score_data": 0.543, - "score_data_loc": 0.329, - "score_loc": 0.114 - }, - { - "component": "Diobsud", - "componentData": "Missing Data", - "componentID": 14268932, - "name": "Diobsud", - "rank_data": "4", - "rank_data_loc": "6", - "rank_loc": "9", - "score_data": 0.606, - "score_data_loc": 0.323, - "score_loc": 0.04 - }, - { - "component": "Wollard", - "componentData": "Missing Data", - "componentID": 14268937, - "name": "Wollard", - "rank_data": "6", - "rank_data_loc": "7", - "rank_loc": "8", - "score_data": 0.56, - "score_data_loc": 0.305, - "score_loc": 0.05 - }, - { - "component": "Oso", - "componentData": "Missing Data", - "componentID": 14268939, - "name": "Oso", - "rank_data": "9", - "rank_data_loc": "8", - "rank_loc": "7", - "score_data": 0.463, - "score_data_loc": 0.256, - "score_loc": 0.05 - }, - { - "component": "Cryaquepts", - "componentData": "Missing Data", - "componentID": 14269507, - "name": "Cryaquepts", - "rank_data": "8", - "rank_data_loc": "9", - "rank_loc": "11", - "score_data": 0.473, - "score_data_loc": 0.255, - "score_loc": 0.038 - }, - { - "component": "Andic cryumbrepts", - "componentData": "Missing Data", - "componentID": 14269504, - "name": "Andic cryumbrepts", - "rank_data": "12", - "rank_data_loc": "10", - "rank_loc": "1", - "score_data": 0.333, - "score_data_loc": 0.242, - "score_loc": 0.152 - }, - { - "component": "Cryumbrepts", - "componentData": "Missing Data", - "componentID": 14269506, - "name": "Cryumbrepts", - "rank_data": "10", - "rank_data_loc": "11", - "rank_loc": "5", - "score_data": 0.379, - "score_data_loc": 0.228, - "score_loc": 0.076 - }, - { - "component": "Cryohumods", - "componentData": "Missing Data", - "componentID": 14269509, - "name": "Cryohumods", - "rank_data": "11", - "rank_data_loc": "12", - "rank_loc": "12", - "score_data": 0.379, - "score_data_loc": 0.209, - "score_loc": 0.038 - }, - { - "component": "Playco", - "componentData": "Missing Data", - "componentID": 14268933, - "name": "Playco1", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "4", - "score_data": 0.614, - "score_data_loc": 0.352, - "score_loc": 0.09 - }, - { - "component": "Nimue", - "componentData": "Missing Data", - "componentID": 14268934, - "name": "Nimue3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.48, - "score_data_loc": 0.305, - "score_loc": 0.13 - }, - { - "component": "Playco", - "componentData": "Missing Data", - "componentID": 14268940, - "name": "Playco3", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.516, - "score_data_loc": 0.303, - "score_loc": 0.09 - }, - { - "component": "Getchell", - "componentData": "Missing Data", - "componentID": 14268944, - "name": "Getchell2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.505, - "score_data_loc": 0.283, - "score_loc": 0.06 - }, - { - "component": "Nimue", - "componentData": "Missing Data", - "componentID": 14268930, - "name": "Nimue2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.404, - "score_data_loc": 0.267, - "score_loc": 0.13 - }, - { - "component": "Playco", - "componentData": "Missing Data", - "componentID": 14268941, - "name": "Playco2", - "rank_data": "Not Displayed", - "rank_data_loc": "Not Displayed", - "rank_loc": "Not Displayed", - "score_data": 0.431, - "score_data_loc": 0.26, - "score_loc": 0.09 - } - ] - } -} diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json index 1e84820..2606fc9 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[60.42282639,-158.4018264].json @@ -382,71 +382,71 @@ "componentData": "Missing Data", "componentID": 26176414, "name": "D36-western maritime tussock scrub loamy eolian slopes", - "rank_data": "2", + "rank_data": "1", "rank_data_loc": "1", "rank_loc": 1, - "score_data": 0.48, - "score_data_loc": 0.36, + "score_data": 0.508, + "score_data_loc": 0.374, "score_loc": 0.24 }, { - "component": "D36-western maritime sedge organic depressions", + "component": "D36-western maritime dwarf scrub loamy glaciated slopes", "componentData": "Missing Data", - "componentID": 26176412, - "name": "D36-western maritime sedge organic depressions", - "rank_data": "3", + "componentID": 26176416, + "name": "D36-western maritime dwarf scrub loamy glaciated slopes", + "rank_data": "5", "rank_data_loc": "2", - "rank_loc": 3, - "score_data": 0.45, - "score_data_loc": 0.325, - "score_loc": 0.2 + "rank_loc": 2, + "score_data": 0.377, + "score_data_loc": 0.303, + "score_loc": 0.23 }, { "component": "D36-boreal forest loamy eolian slopes", "componentData": "Missing Data", "componentID": 26176415, "name": "D36-boreal forest loamy eolian slopes", - "rank_data": "1", + "rank_data": "2", "rank_data_loc": "3", "rank_loc": 5, - "score_data": 0.522, - "score_data_loc": 0.311, + "score_data": 0.495, + "score_data_loc": 0.297, "score_loc": 0.1 }, - { - "component": "D36-western maritime dwarf scrub loamy glaciated slopes", - "componentData": "Missing Data", - "componentID": 26176416, - "name": "D36-western maritime dwarf scrub loamy glaciated slopes", - "rank_data": "5", - "rank_data_loc": "4", - "rank_loc": 2, - "score_data": 0.377, - "score_data_loc": 0.303, - "score_loc": 0.23 - }, { "component": "D36-western maritime scrub organic peat mounds", "componentData": "Missing Data", "componentID": 26176417, "name": "D36-western maritime scrub organic peat mounds", "rank_data": "4", - "rank_data_loc": "5", + "rank_data_loc": "4", "rank_loc": 4, "score_data": 0.421, "score_data_loc": 0.295, "score_loc": 0.17 }, + { + "component": "D36-western maritime sedge organic depressions", + "componentData": "Missing Data", + "componentID": 26176412, + "name": "D36-western maritime sedge organic depressions", + "rank_data": "6", + "rank_data_loc": "5", + "rank_loc": 3, + "score_data": 0.332, + "score_data_loc": 0.266, + "score_loc": 0.2 + }, { "component": "D36-western maritime scrub drainageways", "componentData": "Missing Data", "componentID": 26176413, "name": "D36-western maritime scrub drainageways", - "rank_data": "6", + "rank_data": "3", "rank_data_loc": "6", "rank_loc": 6, - "score_data": 0.376, - "score_data_loc": 0.193, + "score_data": 0.495, + "score_data_loc": 0.252, "score_loc": 0.01 } ] diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json index 4bb5ec3..728cf8c 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[62.32776717,-157.2767099].json @@ -496,11 +496,11 @@ "componentData": "Missing Data", "componentID": 24913863, "name": "E30-boreal forest-silty slopes", - "rank_data": "2", + "rank_data": "1", "rank_data_loc": "1", "rank_loc": 1, - "score_data": 0.758, - "score_data_loc": 0.529, + "score_data": 0.822, + "score_data_loc": 0.561, "score_loc": 0.3 }, { @@ -515,29 +515,41 @@ "score_data_loc": 0.484, "score_loc": 0.29 }, + { + "component": "E30-boreal taiga-loamy frozen colluvial slopes", + "componentData": "Missing Data", + "componentID": 24913864, + "name": "E30-boreal taiga-loamy frozen colluvial slopes", + "rank_data": "2", + "rank_data_loc": "3", + "rank_loc": 3, + "score_data": 0.771, + "score_data_loc": 0.45, + "score_loc": 0.13 + }, { "component": "E30-boreal taiga-silty slopes", "componentData": "Missing Data", "componentID": 24913862, "name": "E30-boreal taiga-silty slopes", - "rank_data": "1", - "rank_data_loc": "3", + "rank_data": "3", + "rank_data_loc": "4", "rank_loc": 4, - "score_data": 0.794, - "score_data_loc": 0.432, + "score_data": 0.736, + "score_data_loc": 0.403, "score_loc": 0.07 }, { - "component": "E30-boreal taiga-loamy frozen colluvial slopes", + "component": "E30-boreal taiga/tussock-silty frozen slopes", "componentData": "Missing Data", - "componentID": 24913864, - "name": "E30-boreal taiga-loamy frozen colluvial slopes", - "rank_data": "3", - "rank_data_loc": "4", - "rank_loc": 3, - "score_data": 0.701, - "score_data_loc": 0.415, - "score_loc": 0.13 + "componentID": 24913861, + "name": "E30-boreal taiga/tussock-silty frozen slopes", + "rank_data": "6", + "rank_data_loc": "5", + "rank_loc": 5, + "score_data": 0.605, + "score_data_loc": 0.332, + "score_loc": 0.06 }, { "component": "E30-boreal scrub-silty frozen drainageways", @@ -545,34 +557,34 @@ "componentID": 24913859, "name": "E30-boreal scrub-silty frozen drainageways", "rank_data": "5", - "rank_data_loc": "5", + "rank_data_loc": "6", "rank_loc": 7, - "score_data": 0.644, - "score_data_loc": 0.342, + "score_data": 0.616, + "score_data_loc": 0.328, "score_loc": 0.04 }, { - "component": "E30-boreal taiga/tussock-silty frozen slopes", + "component": "E30-boreal subalpine woodland-gravelly colluvial slopes", "componentData": "Missing Data", - "componentID": 24913861, - "name": "E30-boreal taiga/tussock-silty frozen slopes", + "componentID": 24913858, + "name": "E30-boreal subalpine woodland-gravelly colluvial slopes", "rank_data": "7", - "rank_data_loc": "6", - "rank_loc": 5, - "score_data": 0.605, - "score_data_loc": 0.333, - "score_loc": 0.06 + "rank_data_loc": "7", + "rank_loc": 9, + "score_data": 0.567, + "score_data_loc": 0.298, + "score_loc": 0.03 }, { "component": "E30-boreal alpine dwarf scrub-gravelly colluvial slopes", "componentData": "Missing Data", "componentID": 24913857, "name": "E30-boreal alpine dwarf scrub-gravelly colluvial slopes", - "rank_data": "6", - "rank_data_loc": "7", + "rank_data": "8", + "rank_data_loc": "8", "rank_loc": 8, - "score_data": 0.613, - "score_data_loc": 0.321, + "score_data": 0.565, + "score_data_loc": 0.298, "score_loc": 0.03 }, { @@ -580,24 +592,12 @@ "componentData": "Missing Data", "componentID": 24913860, "name": "E30-boreal subalpine scrub-loamy colluvial slopes", - "rank_data": "8", - "rank_data_loc": "8", - "rank_loc": 6, - "score_data": 0.592, - "score_data_loc": 0.321, - "score_loc": 0.05 - }, - { - "component": "E30-boreal subalpine woodland-gravelly colluvial slopes", - "componentData": "Missing Data", - "componentID": 24913858, - "name": "E30-boreal subalpine woodland-gravelly colluvial slopes", "rank_data": "9", "rank_data_loc": "9", - "rank_loc": 9, - "score_data": 0.468, - "score_data_loc": 0.249, - "score_loc": 0.03 + "rank_loc": 6, + "score_data": 0.494, + "score_data_loc": 0.272, + "score_loc": 0.05 } ] } diff --git a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json index e9672a7..a56985b 100644 --- a/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json +++ b/soil_id/tests/us/__snapshots__/test_us/test_soil_location[63.52666854,-156.4422738].json @@ -1,18 +1,18 @@ { "list": { - "AWS_PIW90": 15.63, + "AWS_PIW90": 16.92, "Soil Data Value": [ [ "rfv_class_30", - 1.4455018975807923 + 1.6526274846637259 ], [ "rfv_class_0", - 0.9758207999450619 + 1.244640053758421 ], [ "texture_30", - 0.43867507444769327 + 0.47445381163959555 ], [ "texture_0", @@ -183,56 +183,6 @@ "texture": {}, "top_depth": {} }, - { - "bottom_depth": {}, - "cec": {}, - "clay": {}, - "ec": {}, - "esd": { - "ESD": { - "ecoclassid": "", - "ecoclassname": "", - "edit_url": "" - } - }, - "id": { - "component": "E30-boreal taiga/tussock-silty frozen terraces", - "name": "E30-boreal taiga/tussock-silty frozen terraces", - "rank_loc": "4", - "score_loc": 0.11 - }, - "lab": {}, - "munsell": {}, - "ph": {}, - "rock_fragments": {}, - "sand": {}, - "site": { - "siteData": { - "componentID": "24914407", - "componentKind": "Taxon above family", - "componentPct": 11, - "dataSource": "SSURGO", - "distance": 0.0, - "irrcapcl": "None", - "irrcapscl": "None", - "irrcapunit": "None", - "mapunitID": "3375385", - "minCompDistance": 0.0, - "nirrcapcl": "7", - "nirrcapscl": "s", - "nirrcapunit": "None", - "rfvInfill": "No", - "sdeURL": "", - "seeURL": "", - "slope": 1.0, - "taxsubgrp": "Typic Histoturbels", - "textureInfill": "No" - }, - "siteDescription": "" - }, - "texture": {}, - "top_depth": {} - }, { "bottom_depth": {}, "cec": {}, @@ -248,7 +198,7 @@ "id": { "component": "E30-boreal taiga-silty frozen loess slopes", "name": "E30-boreal taiga-silty frozen loess slopes", - "rank_loc": "5", + "rank_loc": "4", "score_loc": 0.107 }, "lab": {}, @@ -298,7 +248,7 @@ "id": { "component": "E30-boreal forest-loamy flood plains", "name": "E30-boreal forest-loamy flood plains", - "rank_loc": "6", + "rank_loc": "5", "score_loc": 0.09 }, "lab": {}, @@ -348,7 +298,7 @@ "id": { "component": "E30-boreal forest-silty slopes", "name": "E30-boreal forest-silty slopes", - "rank_loc": "7", + "rank_loc": "6", "score_loc": 0.07 }, "lab": {}, @@ -398,7 +348,7 @@ "id": { "component": "E30-boreal forest-silty loess slopes", "name": "E30-boreal forest-silty loess slopes", - "rank_loc": "8", + "rank_loc": "7", "score_loc": 0.058 }, "lab": {}, @@ -446,10 +396,10 @@ } }, "id": { - "component": "E30-boreal wet meadow-organic depressions", - "name": "E30-boreal wet meadow-organic depressions", - "rank_loc": "9", - "score_loc": 0.05 + "component": "E30-boreal scrub/sphagnum-organic depressions", + "name": "E30-boreal scrub/sphagnum-organic depressions", + "rank_loc": "8", + "score_loc": 0.03 }, "lab": {}, "munsell": {}, @@ -458,9 +408,9 @@ "sand": {}, "site": { "siteData": { - "componentID": "24914412", + "componentID": "24914410", "componentKind": "Taxon above family", - "componentPct": 5, + "componentPct": 3, "dataSource": "SSURGO", "distance": 0.0, "irrcapcl": "None", @@ -475,7 +425,7 @@ "sdeURL": "", "seeURL": "", "slope": 0.0, - "taxsubgrp": "Terric Cryofibrists", + "taxsubgrp": "Hydric Cryofibrists", "textureInfill": "No" }, "siteDescription": "" @@ -496,9 +446,9 @@ } }, "id": { - "component": "E30-boreal scrub/sphagnum-organic depressions", - "name": "E30-boreal scrub/sphagnum-organic depressions", - "rank_loc": "10", + "component": "E30-boreal taiga/tussock-silty frozen slopes", + "name": "E30-boreal taiga/tussock-silty frozen slopes", + "rank_loc": "9", "score_loc": 0.03 }, "lab": {}, @@ -508,24 +458,74 @@ "sand": {}, "site": { "siteData": { - "componentID": "24914410", + "componentID": "24914464", "componentKind": "Taxon above family", - "componentPct": 3, + "componentPct": 12, "dataSource": "SSURGO", - "distance": 0.0, + "distance": 350.0, "irrcapcl": "None", "irrcapscl": "None", "irrcapunit": "None", - "mapunitID": "3375385", - "minCompDistance": 0.0, - "nirrcapcl": "7", + "mapunitID": "3375378", + "minCompDistance": 350.0, + "nirrcapcl": "6", + "nirrcapscl": "e", + "nirrcapunit": "None", + "rfvInfill": "No", + "sdeURL": "", + "seeURL": "", + "slope": 2.0, + "taxsubgrp": "Typic Histoturbels", + "textureInfill": "No" + }, + "siteDescription": "" + }, + "texture": {}, + "top_depth": {} + }, + { + "bottom_depth": {}, + "cec": {}, + "clay": {}, + "ec": {}, + "esd": { + "ESD": { + "ecoclassid": "", + "ecoclassname": "", + "edit_url": "" + } + }, + "id": { + "component": "E30-boreal scrub-silty frozen drainageways", + "name": "E30-boreal scrub-silty frozen drainageways", + "rank_loc": "10", + "score_loc": 0.028 + }, + "lab": {}, + "munsell": {}, + "ph": {}, + "rock_fragments": {}, + "sand": {}, + "site": { + "siteData": { + "componentID": "24914387", + "componentKind": "Taxon above family", + "componentPct": 11, + "dataSource": "SSURGO", + "distance": 350.0, + "irrcapcl": "None", + "irrcapscl": "None", + "irrcapunit": "None", + "mapunitID": "3375378", + "minCompDistance": 350.0, + "nirrcapcl": "6", "nirrcapscl": "s", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 0.0, - "taxsubgrp": "Hydric Cryofibrists", + "slope": 1.0, + "taxsubgrp": "Fluvaquentic Historthels", "textureInfill": "No" }, "siteDescription": "" @@ -546,10 +546,10 @@ } }, "id": { - "component": "E30-boreal taiga/tussock-silty frozen slopes", - "name": "E30-boreal taiga/tussock-silty frozen slopes", + "component": "E30-boreal subalpine scrub-loamy colluvial slopes", + "name": "E30-boreal subalpine scrub-loamy colluvial slopes", "rank_loc": "11", - "score_loc": 0.03 + "score_loc": 0.003 }, "lab": {}, "munsell": {}, @@ -558,9 +558,9 @@ "sand": {}, "site": { "siteData": { - "componentID": "24914464", + "componentID": "24914388", "componentKind": "Taxon above family", - "componentPct": 12, + "componentPct": 1, "dataSource": "SSURGO", "distance": 350.0, "irrcapcl": "None", @@ -568,14 +568,14 @@ "irrcapunit": "None", "mapunitID": "3375378", "minCompDistance": 350.0, - "nirrcapcl": "6", + "nirrcapcl": "7", "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 2.0, - "taxsubgrp": "Typic Histoturbels", + "slope": 25.0, + "taxsubgrp": "Typic Dystrocryepts", "textureInfill": "No" }, "siteDescription": "" @@ -596,10 +596,10 @@ } }, "id": { - "component": "E30-boreal scrub-silty frozen drainageways", - "name": "E30-boreal scrub-silty frozen drainageways", + "component": "E30-boreal subalpine woodland-gravelly colluvial slopes", + "name": "E30-boreal subalpine woodland-gravelly colluvial slopes", "rank_loc": "12", - "score_loc": 0.028 + "score_loc": 0.003 }, "lab": {}, "munsell": {}, @@ -608,9 +608,9 @@ "sand": {}, "site": { "siteData": { - "componentID": "24914387", + "componentID": "24914463", "componentKind": "Taxon above family", - "componentPct": 11, + "componentPct": 1, "dataSource": "SSURGO", "distance": 350.0, "irrcapcl": "None", @@ -618,14 +618,14 @@ "irrcapunit": "None", "mapunitID": "3375378", "minCompDistance": 350.0, - "nirrcapcl": "6", - "nirrcapscl": "s", + "nirrcapcl": "7", + "nirrcapscl": "e", "nirrcapunit": "None", "rfvInfill": "No", "sdeURL": "", "seeURL": "", - "slope": 1.0, - "taxsubgrp": "Fluvaquentic Historthels", + "slope": 18.0, + "taxsubgrp": "Typic Dystrocryepts", "textureInfill": "No" }, "siteDescription": "" @@ -646,72 +646,72 @@ "componentData": "Missing Data", "componentID": 24914406, "name": "E30-boreal taiga-loamy frozen colluvial slopes", - "rank_data": "4", + "rank_data": "8", "rank_data_loc": "1", "rank_loc": 1, - "score_data": 0.613, - "score_data_loc": 0.477, + "score_data": 0.481, + "score_data_loc": 0.411, "score_loc": 0.34 }, { - "component": "E30-boreal forest-silty slopes", + "component": "E30-boreal taiga-organic frozen peat plateaus", "componentData": "Missing Data", - "componentID": 24914405, - "name": "E30-boreal forest-silty slopes", - "rank_data": "1", + "componentID": 24914411, + "name": "E30-boreal taiga-organic frozen peat plateaus", + "rank_data": "4", "rank_data_loc": "2", - "rank_loc": 7, - "score_data": 0.745, - "score_data_loc": 0.408, - "score_loc": 0.07 - }, - { - "component": "E30-boreal taiga-silty frozen loess slopes", - "componentData": "Missing Data", - "componentID": 24914462, - "name": "E30-boreal taiga-silty frozen loess slopes", - "rank_data": "3", - "rank_data_loc": "3", - "rank_loc": 5, - "score_data": 0.658, - "score_data_loc": 0.383, - "score_loc": 0.107 + "rank_loc": 3, + "score_data": 0.657, + "score_data_loc": 0.388, + "score_loc": 0.12 }, { "component": "E30-boreal forest-silty loess slopes", "componentData": "Missing Data", "componentID": 24914386, "name": "E30-boreal forest-silty loess slopes", - "rank_data": "2", - "rank_data_loc": "4", - "rank_loc": 8, - "score_data": 0.663, - "score_data_loc": 0.36, + "rank_data": "1", + "rank_data_loc": "3", + "rank_loc": 7, + "score_data": 0.706, + "score_data_loc": 0.382, "score_loc": 0.058 }, { - "component": "E30-boreal taiga/tussock-silty frozen terraces", + "component": "E30-boreal scrub-gravelly low flood plains", "componentData": "Missing Data", - "componentID": 24914407, - "name": "E30-boreal taiga/tussock-silty frozen terraces", + "componentID": 24914408, + "name": "E30-boreal scrub-gravelly low flood plains", "rank_data": "7", - "rank_data_loc": "5", - "rank_loc": 4, - "score_data": 0.497, - "score_data_loc": 0.304, - "score_loc": 0.11 + "rank_data_loc": "4", + "rank_loc": 2, + "score_data": 0.567, + "score_data_loc": 0.378, + "score_loc": 0.19 }, { - "component": "E30-boreal scrub-silty frozen drainageways", + "component": "E30-boreal forest-loamy flood plains", "componentData": "Missing Data", - "componentID": 24914387, - "name": "E30-boreal scrub-silty frozen drainageways", + "componentID": 24914409, + "name": "E30-boreal forest-loamy flood plains", "rank_data": "5", + "rank_data_loc": "5", + "rank_loc": 5, + "score_data": 0.649, + "score_data_loc": 0.369, + "score_loc": 0.09 + }, + { + "component": "E30-boreal subalpine woodland-gravelly colluvial slopes", + "componentData": "Missing Data", + "componentID": 24914463, + "name": "E30-boreal subalpine woodland-gravelly colluvial slopes", + "rank_data": "2", "rank_data_loc": "6", "rank_loc": 12, - "score_data": 0.552, - "score_data_loc": 0.29, - "score_loc": 0.028 + "score_data": 0.687, + "score_data_loc": 0.345, + "score_loc": 0.003 }, { "component": "E30-boreal taiga/tussock-silty frozen slopes", @@ -720,70 +720,70 @@ "name": "E30-boreal taiga/tussock-silty frozen slopes", "rank_data": "6", "rank_data_loc": "7", - "rank_loc": 11, - "score_data": 0.521, - "score_data_loc": 0.275, + "rank_loc": 9, + "score_data": 0.647, + "score_data_loc": 0.338, "score_loc": 0.03 }, { - "component": "E30-boreal wet meadow-organic depressions", + "component": "E30-boreal subalpine scrub-loamy colluvial slopes", "componentData": "Missing Data", - "componentID": 24914412, - "name": "E30-boreal wet meadow-organic depressions", - "rank_data": "8", + "componentID": 24914388, + "name": "E30-boreal subalpine scrub-loamy colluvial slopes", + "rank_data": "3", "rank_data_loc": "8", - "rank_loc": 9, - "score_data": 0.46, - "score_data_loc": 0.255, - "score_loc": 0.05 + "rank_loc": 11, + "score_data": 0.673, + "score_data_loc": 0.338, + "score_loc": 0.003 }, { - "component": "E30-boreal forest-loamy flood plains", + "component": "E30-boreal forest-silty slopes", "componentData": "Missing Data", - "componentID": 24914409, - "name": "E30-boreal forest-loamy flood plains", - "rank_data": "9", + "componentID": 24914405, + "name": "E30-boreal forest-silty slopes", + "rank_data": "10", "rank_data_loc": "9", "rank_loc": 6, - "score_data": 0.372, - "score_data_loc": 0.231, - "score_loc": 0.09 + "score_data": 0.473, + "score_data_loc": 0.271, + "score_loc": 0.07 }, { - "component": "E30-boreal taiga-organic frozen peat plateaus", + "component": "E30-boreal scrub/sphagnum-organic depressions", "componentData": "Missing Data", - "componentID": 24914411, - "name": "E30-boreal taiga-organic frozen peat plateaus", - "rank_data": "10", + "componentID": 24914410, + "name": "E30-boreal scrub/sphagnum-organic depressions", + "rank_data": "9", "rank_data_loc": "10", - "rank_loc": 3, - "score_data": 0.277, - "score_data_loc": 0.199, - "score_loc": 0.12 + "rank_loc": 8, + "score_data": 0.473, + "score_data_loc": 0.251, + "score_loc": 0.03 }, { - "component": "E30-boreal scrub/sphagnum-organic depressions", + "component": "E30-boreal scrub-silty frozen drainageways", "componentData": "Missing Data", - "componentID": 24914410, - "name": "E30-boreal scrub/sphagnum-organic depressions", + "componentID": 24914387, + "name": "E30-boreal scrub-silty frozen drainageways", "rank_data": "11", "rank_data_loc": "11", "rank_loc": 10, - "score_data": 0.277, - "score_data_loc": 0.154, - "score_loc": 0.03 + "score_data": 0.361, + "score_data_loc": 0.194, + "score_loc": 0.028 }, { - "component": "E30-boreal scrub-gravelly low flood plains", + "component": "E30-boreal taiga-silty frozen loess slopes", "componentData": "Missing Data", - "componentID": 24914408, - "name": "E30-boreal scrub-gravelly low flood plains", + "componentID": 24914462, + "name": "E30-boreal taiga-silty frozen loess slopes", "rank_data": "12", "rank_data_loc": "12", - "rank_loc": 2, - "score_data": 0.08, - "score_data_loc": 0.135, - "score_loc": 0.19 + "rank_loc": 4, + "score_data": 0.211, + "score_data_loc": 0.159, + "score_loc": 0.107 } ] } diff --git a/soil_id/us_soil.py b/soil_id/us_soil.py index fd69378..6d29890 100644 --- a/soil_id/us_soil.py +++ b/soil_id/us_soil.py @@ -270,7 +270,7 @@ def list_soils(lon, lat): muhorzdata_pd = muhorzdata_pd[~muhorzdata_pd["hzname"].str.contains("R", case=False, na=False)] # Group data by cokey (component key) - muhorzdata_group_cokey = [group for _, group in muhorzdata_pd.groupby("cokey", sort=False)] + muhorzdata_group_cokey = [group for _, group in muhorzdata_pd.groupby("cokey")] getProfile_cokey = [] comp_max_depths = [] @@ -651,9 +651,7 @@ def list_soils(lon, lat): if mucompdata_pd["compkind"].isin(OSD_compkind).any(): # Group data by cokey - OSDhorzdata_group_cokey = [ - group for _, group in OSDhorzdata_pd.groupby("cokey", sort=False) - ] + OSDhorzdata_group_cokey = [group for _, group in OSDhorzdata_pd.groupby("cokey")] # Initialize empty lists lab_lyrs = [] @@ -967,7 +965,7 @@ def list_soils(lon, lat): SEE_URL = [] # Group data by 'cokey' - OSDhorzdata_group_cokey = [g for _, g in OSDhorzdata_pd.groupby("cokey", sort=False)] + OSDhorzdata_group_cokey = [g for _, g in OSDhorzdata_pd.groupby("cokey")] for index, group in enumerate(OSDhorzdata_group_cokey): # Check if compkind is not in OSD_compkind or if series contains any null values @@ -1252,7 +1250,7 @@ def list_soils(lon, lat): r"[0-9]+", "", regex=True ) ESDcompdata_pd_comp_grps = [ - g for _, g in ESDcompdata_pd.groupby(["compname_grp"], sort=False) + g for _, g in ESDcompdata_pd.groupby(["compname_grp"]) ] ecoList_out = [] for i in range(len(ESDcompdata_pd_comp_grps)): @@ -1776,7 +1774,7 @@ def rank_soils( # Horizon Data Similarity if soilIDRank_output_pd is not None: - groups = [group for _, group in soilIDRank_output_pd.groupby(["compname"], sort=False)] + groups = [group for _, group in soilIDRank_output_pd.groupby(["compname"])] Comp_Rank_Status = [] Comp_Missing_Status = [] @@ -2035,7 +2033,7 @@ def rank_soils( # Sort and rank the components within each group soilIDList_data = [] - for _, group in D_final.groupby(["compname_grp"], sort=False): + for _, group in D_final.groupby(["compname_grp"]): # Sort by score, and then by compname group = group.sort_values(by=["Score_Data", "compname"], ascending=[False, True]) @@ -2144,7 +2142,7 @@ def rank_soils( # Sorting and reindexing of final dataframe based on component groups soilIDList_out = [] - for _, group in D_final_loc.groupby("compname_grp", sort=False): + for _, group in D_final_loc.groupby("compname_grp"): group = group.sort_values("Score_Data_Loc", ascending=False).reset_index(drop=True) group["soilID_rank_final"] = [True if idx == 0 else False for idx in range(len(group))] soilIDList_out.append(group) diff --git a/soil_id/utils.py b/soil_id/utils.py index 1909758..18c1432 100644 --- a/soil_id/utils.py +++ b/soil_id/utils.py @@ -705,7 +705,7 @@ def drop_cokey_horz(df): drop_instances = [] # Group by compname - for _, comp_group in df.groupby("compname", sort=False): + for _, comp_group in df.groupby("compname"): # Get unique cokeys and their data signature within this compname group cokey_map = comp_group.groupby("cokey")["_cokey_grouped"].first() @@ -1711,7 +1711,7 @@ def process_distance_scores(mucompdata_pd, ExpCoeff): mucompdata_pd = mucompdata_pd.reset_index(drop=True) # Create a list of component groups - mucompdata_comp_grps = [g for _, g in mucompdata_pd.groupby(["compname"], sort=False)] + mucompdata_comp_grps = [g for _, g in mucompdata_pd.groupby(["compname"])] mucompdata_comp_grps = mucompdata_comp_grps[: min(12, len(mucompdata_comp_grps))] # Assign max within-group location-based score to all members of the group @@ -2409,7 +2409,7 @@ def update_esd_data(df): # Replace group-specific data for missing ESD components df["compname_grp"] = df["compname"].str.replace(r"[0-9]+", "") - grouped = df.groupby("compname_grp", sort=False) + grouped = df.groupby("compname_grp") # Generate a list of updated groups updated_groups = []