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SoilGrids1km — Global Soil Information Based on Automated Mapping

BACKGROUND: Soils are widely recognized as a non-renewable natural resource and as biophysical carbon sinks. As such, there is a growing requirement for global soil information. Although several global soil information systems already exist, these tend to suffer from inconsistencies and limited spat...

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Autores principales: Hengl, Tomislav, de Jesus, Jorge Mendes, MacMillan, Robert A., Batjes, Niels H., Heuvelink, Gerard B. M., Ribeiro, Eloi, Samuel-Rosa, Alessandro, Kempen, Bas, Leenaars, Johan G. B., Walsh, Markus G., Gonzalez, Maria Ruiperez
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4149475/
https://www.ncbi.nlm.nih.gov/pubmed/25171179
http://dx.doi.org/10.1371/journal.pone.0105992
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author Hengl, Tomislav
de Jesus, Jorge Mendes
MacMillan, Robert A.
Batjes, Niels H.
Heuvelink, Gerard B. M.
Ribeiro, Eloi
Samuel-Rosa, Alessandro
Kempen, Bas
Leenaars, Johan G. B.
Walsh, Markus G.
Gonzalez, Maria Ruiperez
author_facet Hengl, Tomislav
de Jesus, Jorge Mendes
MacMillan, Robert A.
Batjes, Niels H.
Heuvelink, Gerard B. M.
Ribeiro, Eloi
Samuel-Rosa, Alessandro
Kempen, Bas
Leenaars, Johan G. B.
Walsh, Markus G.
Gonzalez, Maria Ruiperez
author_sort Hengl, Tomislav
collection PubMed
description BACKGROUND: Soils are widely recognized as a non-renewable natural resource and as biophysical carbon sinks. As such, there is a growing requirement for global soil information. Although several global soil information systems already exist, these tend to suffer from inconsistencies and limited spatial detail. METHODOLOGY/PRINCIPAL FINDINGS: We present SoilGrids1km — a global 3D soil information system at 1 km resolution — containing spatial predictions for a selection of soil properties (at six standard depths): soil organic carbon (g kg−1), soil pH, sand, silt and clay fractions (%), bulk density (kg m−3), cation-exchange capacity (cmol+/kg), coarse fragments (%), soil organic carbon stock (t ha−1), depth to bedrock (cm), World Reference Base soil groups, and USDA Soil Taxonomy suborders. Our predictions are based on global spatial prediction models which we fitted, per soil variable, using a compilation of major international soil profile databases (ca. 110,000 soil profiles), and a selection of ca. 75 global environmental covariates representing soil forming factors. Results of regression modeling indicate that the most useful covariates for modeling soils at the global scale are climatic and biomass indices (based on MODIS images), lithology, and taxonomic mapping units derived from conventional soil survey (Harmonized World Soil Database). Prediction accuracies assessed using 5–fold cross-validation were between 23–51%. CONCLUSIONS/SIGNIFICANCE: SoilGrids1km provide an initial set of examples of soil spatial data for input into global models at a resolution and consistency not previously available. Some of the main limitations of the current version of SoilGrids1km are: (1) weak relationships between soil properties/classes and explanatory variables due to scale mismatches, (2) difficulty to obtain covariates that capture soil forming factors, (3) low sampling density and spatial clustering of soil profile locations. However, as the SoilGrids system is highly automated and flexible, increasingly accurate predictions can be generated as new input data become available. SoilGrids1km are available for download via http://soilgrids.org under a Creative Commons Non Commercial license.
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spelling pubmed-41494752014-09-03 SoilGrids1km — Global Soil Information Based on Automated Mapping Hengl, Tomislav de Jesus, Jorge Mendes MacMillan, Robert A. Batjes, Niels H. Heuvelink, Gerard B. M. Ribeiro, Eloi Samuel-Rosa, Alessandro Kempen, Bas Leenaars, Johan G. B. Walsh, Markus G. Gonzalez, Maria Ruiperez PLoS One Research Article BACKGROUND: Soils are widely recognized as a non-renewable natural resource and as biophysical carbon sinks. As such, there is a growing requirement for global soil information. Although several global soil information systems already exist, these tend to suffer from inconsistencies and limited spatial detail. METHODOLOGY/PRINCIPAL FINDINGS: We present SoilGrids1km — a global 3D soil information system at 1 km resolution — containing spatial predictions for a selection of soil properties (at six standard depths): soil organic carbon (g kg−1), soil pH, sand, silt and clay fractions (%), bulk density (kg m−3), cation-exchange capacity (cmol+/kg), coarse fragments (%), soil organic carbon stock (t ha−1), depth to bedrock (cm), World Reference Base soil groups, and USDA Soil Taxonomy suborders. Our predictions are based on global spatial prediction models which we fitted, per soil variable, using a compilation of major international soil profile databases (ca. 110,000 soil profiles), and a selection of ca. 75 global environmental covariates representing soil forming factors. Results of regression modeling indicate that the most useful covariates for modeling soils at the global scale are climatic and biomass indices (based on MODIS images), lithology, and taxonomic mapping units derived from conventional soil survey (Harmonized World Soil Database). Prediction accuracies assessed using 5–fold cross-validation were between 23–51%. CONCLUSIONS/SIGNIFICANCE: SoilGrids1km provide an initial set of examples of soil spatial data for input into global models at a resolution and consistency not previously available. Some of the main limitations of the current version of SoilGrids1km are: (1) weak relationships between soil properties/classes and explanatory variables due to scale mismatches, (2) difficulty to obtain covariates that capture soil forming factors, (3) low sampling density and spatial clustering of soil profile locations. However, as the SoilGrids system is highly automated and flexible, increasingly accurate predictions can be generated as new input data become available. SoilGrids1km are available for download via http://soilgrids.org under a Creative Commons Non Commercial license. Public Library of Science 2014-08-29 /pmc/articles/PMC4149475/ /pubmed/25171179 http://dx.doi.org/10.1371/journal.pone.0105992 Text en © 2014 Hengl et al http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited.
spellingShingle Research Article
Hengl, Tomislav
de Jesus, Jorge Mendes
MacMillan, Robert A.
Batjes, Niels H.
Heuvelink, Gerard B. M.
Ribeiro, Eloi
Samuel-Rosa, Alessandro
Kempen, Bas
Leenaars, Johan G. B.
Walsh, Markus G.
Gonzalez, Maria Ruiperez
SoilGrids1km — Global Soil Information Based on Automated Mapping
title SoilGrids1km — Global Soil Information Based on Automated Mapping
title_full SoilGrids1km — Global Soil Information Based on Automated Mapping
title_fullStr SoilGrids1km — Global Soil Information Based on Automated Mapping
title_full_unstemmed SoilGrids1km — Global Soil Information Based on Automated Mapping
title_short SoilGrids1km — Global Soil Information Based on Automated Mapping
title_sort soilgrids1km — global soil information based on automated mapping
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4149475/
https://www.ncbi.nlm.nih.gov/pubmed/25171179
http://dx.doi.org/10.1371/journal.pone.0105992
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