Abstract
With the development of energy base in Ordos basin, the deficiency of groundwater becomes serious. Therefore, the hydrogeochemical evolution of groundwater is studied, which is in the Dusit-Yanchi watery system. Some results are obtained. The quality of groundwater in Dusit river system is better, and in the aquifer, the main water-rock action is the solution of gypsum, fluorite, and siderite, and the precipitation of calcite and dolomite.
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