4.6 Article

Soil salinity estimation in Shule River Basin using support vector regression model

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LAND DEGRADATION & DEVELOPMENT
卷 -, 期 -, 页码 -

出版社

WILEY
DOI: 10.1002/ldr.4741

关键词

environmental covariates; soil mapping; soil salinity; spatial dependence; support vector regression spatial; total salt content

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Soil salinization globally deteriorates soil fertility. Evaluating the salinization scale is crucial for sustainable agriculture and land rehabilitation. In this study, a support vector regression spatial (SVR-S) model was proposed to predict soil salinity in the irrigation area of the Shule River Basin in northwestern China using spatial dependence information. The SVR-S model outperformed the SVR-O and GWR, with a correlation coefficient (R) of 0.87 and a root mean square error (RMSE) of 1.83%. Topographic indices integrating spatial information contributed significantly to salinity estimation in the study area. This study offers a new approach for accurate soil salinity mapping using spatial information.
Soil salinization is a progressive degradation process that spreads globally and leads to a decline in soil fertility. Assessing the scale of salinization is crucial for sustainable agricultural development and saline-land rehabilitation. In this study, we proposed a support vector regression spatial (SVR-S) model that utilizes spatial dependence information to predict soil salinity over the irrigation area of the Shule River Basin in northwestern China. To investigate the performance of the SVR-S model, 50 soil samples were collected in the field. Semivariograms of soil salinity (measured as total salt content and ion concentrations) were constructed to measure spatial dependence. The SVR-S model was compared with the original SVR model and the geographically weighted regression (GWR) model regarding the salinity prediction ability. The soil salinity in the experimental area demonstrated a strong spatial dependence pattern. The SVR-S model delivered a better performance than the SVR-O and GWR. SVR-S showed a correlation coefficient R of 0.87 and a root mean square error (RMSE) of 1.83%, while the performance of SVR-O (R = 0.75, RMSE = 3.32%) and GWR (R = 0.73, RMSE = 3.47%) was comparatively poor. Topographic indices integrating spatial information contributed the most to the estimation of salinity in the study area. This study provides a new approach to integrating spatial information for accurate soil salinity mapping.

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