4.7 Article

Susceptibility mapping of groundwater salinity using machine learning models

Journal

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
Volume 28, Issue 9, Pages 10804-10817

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11356-020-11319-5

Keywords

Salinity mapping; Machine learning; Feature selection; Simulated annealing; Dichotomous prediction

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Rising groundwater salinity globally poses significant environmental and health risks. Developing innovative methods for spatial salinity modeling and prediction is crucial for resource management and policy planning. This study demonstrates the use of machine learning models to map groundwater salinity, with the support vector machine model showing superior performance and identifying key contributing factors in different regions.
Increasing groundwater salinity has recently raised severe environmental and health concerns around the world. Advancement of the novel methods for spatial salinity modeling and prediction would be essential for effective management of the resources and planning mitigation policies. The current research presents the application of machine learning (ML) models in groundwater salinity mapping based on the dichotomous predictions. The groundwater salinity is predicted using the essential factors (i.e., identified by the simulated annealing feature selection methodology) through k-fold cross-validation methodology. Six ML models, namely, flexible discriminant analysis (FDA), mixture discriminant analysis (MAD), boosted regression tree (BRT), multivariate adaptive regression spline (MARS), random forest (RF), support vector machine (SVM), were employed to groundwater salinity mapping. The results of the modeling indicated that the SVM model had superior performance than other models. Variables of soil order, groundwater withdrawal, precipitation, land use, and elevation had the most contribute to groundwater salinity mapping. Results highlighted that the southern parts of the region and some parts in the north, northeast, and west have a high groundwater salinity, in which these areas are mostly matched with soil order of Entisols, bareland areas, and low elevations.

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