Geospatial heterogeneity-informed machine learning for mapping soil hydraulic properties across China’s drylands

• Development of novel PTFs for SHP prediction using 17 machine learning (ML) algorithms. • Geospatial heterogeneity-informed ML and ensemble models substantially improve PTF performance. • High-resolution (500 m) mapping of SHPs across China’s drylands to a 2 m depth. • New PTFs achieve 31–79% performance gains over existing models, enhancing regional applicability. Soil hydraulic properties (SHPs) are essential for hydrological modeling, yet their large-scale measurement remains challenging. Pedotransfer functions (PTFs) provide an alternative for estimating SHPs at broader scales. Integrating geospatial data into machine learning (ML) frameworks can significantly enhance the predictive performance and generalizability of PTFs, highlighting their potential for large-scale SHP estimation. In this study, we developed spatially explicit PTFs for China’s drylands using data from 4,382 sites (12,306 soil samples) combined with more than ten ML algorithms. Results demonstrate that ML models accounting for geospatial heterogeneity outperformed simpler ML algorithms substantially. By integrating soil, vegetation, climate, and topographic factors, the models improved the prediction accuracy of various SHPs, including saturated soil hydraulic conductivity ( K s ) and van Genuchten parameters ( θ s , θ r , α , n ), by 31 %–79 % compared to existing PTFs, exhibiting strong robustness for applications in China’s drylands. The optimal PTFs were applied to a 500 m × 500 m regional map of soil and environmental variables, generating maps of five SHPs ( K s , θ s , θ r , α , n ) across six soil depths (0–5, 5–10, 25–30, 55–60, 95–100, and 195–200 cm) in the study region. From these maps, four additional SHPs, i.e., field capacity ( θ fc ), wilting point ( θ wp ), plant available water ( θ pa ), and soil macroporosity (ϕ m ), were derived at the same depths and resolution. The SHP dataset reveals distinct spatial distribution patterns and vertical heterogeneity of SHPs across China’s drylands. This high-resolution, deep-profile dataset provides a robust foundation for large-scale hydrological and land surface modeling in China’s drylands.

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Publication Details

Journal
Geoderma
Published
2025-11-25
DOI
https://doi.org/10.1016/j.geoderma.2025.117622
Primary Topic
Soil and Unsaturated Flow
Type
article
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article

Geospatial heterogeneity-informed machine learning for mapping soil hydraulic properties across China’s drylands

Geoderma
Soil and Unsaturated Flow
article

Geospatial heterogeneity-informed machine learning for mapping soil hydraulic properties across China’s drylands

article en

Abstract

• Development of novel PTFs for SHP prediction using 17 machine learning (ML) algorithms. • Geospatial heterogeneity-informed ML and ensemble models substantially improve PTF performance. • High-resolution (500 m) mapping of SHPs across China’s drylands to a 2 m depth. • New PTFs achieve 31–79% performance gains over existing models, enhancing regional applicability. Soil hydraulic properties (SHPs) are essential for hydrological modeling, yet their large-scale measurement remains challenging. Pedotransfer functions (PTFs) provide an alternative for estimating SHPs at broader scales. Integrating geospatial data into machine learning (ML) frameworks can significantly enhance the predictive performance and generalizability of PTFs, highlighting their potential for large-scale SHP estimation. In this study, we developed spatially explicit PTFs for China’s drylands using data from 4,382 sites (12,306 soil samples) combined with more than ten ML algorithms. Results demonstrate that ML models accounting for geospatial heterogeneity outperformed simpler ML algorithms substantially. By integrating soil, vegetation, climate, and topographic factors, the models improved the prediction accuracy of various SHPs, including saturated soil hydraulic conductivity ( K s ) and van Genuchten parameters ( θ s , θ r , α , n ), by 31 %–79 % compared to existing PTFs, exhibiting strong robustness for applications in China’s drylands. The optimal PTFs were applied to a 500 m × 500 m regional map of soil and environmental variables, generating maps of five SHPs ( K s , θ s , θ r , α , n ) across six soil depths (0–5, 5–10, 25–30, 55–60, 95–100, and 195–200 cm) in the study region. From these maps, four additional SHPs, i.e., field capacity ( θ fc ), wilting point ( θ wp ), plant available water ( θ pa ), and soil macroporosity (ϕ m ), were derived at the same depths and resolution. The SHP dataset reveals distinct spatial distribution patterns and vertical heterogeneity of SHPs across China’s drylands. This high-resolution, deep-profile dataset provides a robust foundation for large-scale hydrological and land surface modeling in China’s drylands.

GeodermaVol. 464
Chinese Academy of Sciences (CN), Beijing Normal University (CN), Institute of Soil and Water Conservation (CN), Institute of Geographic Sciences and Natural Resources Research (CN), University of Chinese Academy of Sciences (CN), Institute of Soil Science (CN)
Climate action
Openalex Percentile: Top 47%
Soil and Unsaturated Flow
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