4.6 Article

SoilGrids 2.0: producing soil information for the globe with quantified spatial uncertainty

Journal

SOIL
Volume 7, Issue 1, Pages 217-240

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/soil-7-217-2021

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Funding

  1. ISRIC core funding
  2. European Union's EU H2020 Research and Innovation Programme [774378]
  3. Netherlands Government
  4. H2020 Societal Challenges Programme [774378] Funding Source: H2020 Societal Challenges Programme

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SoilGrids generates global maps of soil properties using advanced technology and machine learning methods, incorporating soil observations and environmental factors to predict and analyze various soil properties worldwide. The research shows a good predictive performance for global soil properties, but also reveals the need for more soil observation data, especially in high-latitude regions.
SoilGrids produces maps of soil properties for the entire globe at medium spatial resolution (250 m cell size) using state-of-the-art machine learning methods to generate the necessary models. It takes as inputs soil observations from about 240 000 locations worldwide and over 400 global environmental covariates describing vegetation, terrain morphology, climate, geology and hydrology. The aim of this work was the production of global maps of soil properties, with cross-validation, hyper-parameter selection and quantification of spatially explicit uncertainty, as implemented in the SoilGrids version 2.0 product incorporating state-of-the-art practices and adapting them for global digital soil mapping with legacy data. The paper presents the evaluation of the global predictions produced for soil organic carbon content, total nitrogen, coarse fragments, pH (water), cation exchange capacity, bulk density and texture fractions at six standard depths (up to 200 cm). The quantitative evaluation showed metrics in line with previous global, continental and large-region studies. The qualitative evaluation showed that coarse-scale patterns are well reproduced. The spatial uncertainty at global scale highlighted the need for more soil observations, especially in high-latitude regions.

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