Abstract:Base on the stratigraphic distribution, the geologic structure and hydrogeologic conditions of Sanmenxia bauxite, the hydrogeologic conceptual model of karst-fracture aquifer system of water enrichment Cambrian-Ordovirian Period limestone was generalized, and the numerical model of groundwater flow was established using finite difference method of Visual Modflow to simulate variation of groundwater level and to predict water discharging, which the groundwater flow mathematical model was corrected and the hydrogeolocical parameters were inversed combining with observation value of groundwater level of group drilling pumping tests in mining area boreholes, and then utilizing the corrected mathematical model and parameters to predict the groundwater level distribution and mine discharge changes at different designed mining drainage level in well. The reliable basis is provided for controlling groundwater effectively and safe rational mining bauxite.