Abstract
Overexploitation of groundwater in the eastern part of San Jacinto Watershed Basin in conjunction with reservoir leakage in the western part has reversed the groundwater flow direction and has caused migration of groundwater with high total dissolved solids (TDS) into an area of better-quality groundwater. The regional groundwater flow and transport model presented here shows how decreased pumping and artificial recharge in the east and extraction of high-TDS groundwater in the west can impact the area.
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