1. Spatial variability of the groundwater exploitation potential in an arid alluvial-diluvial plain using GIS-based Dempster-Shafer theory
- Author
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Xiaoning Zhao, Xu Zhou, Chengyi Zhao, Fengzhi Shi, Xinhu Li, and Jianting Zhu
- Subjects
Hydrology ,010506 paleontology ,geography ,geography.geographical_feature_category ,Land use ,Drainage basin ,010502 geochemistry & geophysics ,Spatial distribution ,Soil type ,01 natural sciences ,Arid ,Environmental science ,Alluvium ,Spatial variability ,Groundwater ,0105 earth and related environmental sciences ,Earth-Surface Processes - Abstract
The spatial distribution of groundwater exploitation potential is crucial to the sustainable management of groundwater resources in arid regions. In this study, an effective approach is developed using a geographical information system (GIS) associated with the Dempster-Shafer (D-S) theory to explore the groundwater exploitation potential based on eight factors (i.e., slope, topography, distance to a river, canal density, lithology, land use, soil type, and groundwater depth)based on pumping test data. Different groundwater exploitation potential zones from the output map are classified as follows: very high (0.67–0.96, 8% of the total area), high (0.45–0.67, 8%), moderate (0.27–0.45, 14%), low (0.13–0.27, 24%), and very low (0.02–0.13, 46%), in the Hotan River basin of the Kunlun Mountains, China. The groundwater exploitation potential is highest in a gravel plain in the piedmont and gradually decreases from the piedmont to the desert. The predicted spatial variability of groundwater exploitation potential can explain 71% of the measured pumping test data. The uncertainty of the groundwater exploitation potential map ranges from
- Published
- 2021
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