SoilGrids1km-Global Soil Information Based on Automated Mapping

被引:815
作者
Hengl, Tomislav [1 ]
de Jesus, Jorge Mendes [1 ]
MacMillan, Robert A. [2 ]
Batjes, Niels H. [1 ]
Heuvelink, Gerard B. M. [1 ,3 ]
Ribeiro, Eloi [1 ]
Samuel-Rosa, Alessandro [4 ]
Kempen, Bas [1 ]
Leenaars, Johan G. B. [1 ]
Walsh, Markus G. [5 ,6 ]
Gonzalez, Maria Ruiperez [1 ]
机构
[1] ISRIC World Soil Informat, Wageningen, Netherlands
[2] LandMapper Environm Solut Inc, Edmonton, AB, Canada
[3] Wageningen Univ, NL-6700 AP Wageningen, Netherlands
[4] Univ Fed Rural Rio de Janeiro, Rio De Janeiro, Brazil
[5] Columbia Univ, Earth Inst, New York, NY USA
[6] Selian Agr Res Inst, Arusha, Tanzania
来源
PLOS ONE | 2014年 / 9卷 / 08期
关键词
ORGANIC-CARBON; CLIMATE; INTERPOLATION; MODELS; MAP;
D O I
10.1371/journal.pone.0105992
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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.
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页数:17
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