Isotope hydrogeological study has shown that the water supply exploration area in the Lu’ an coal mine may be divided into four zones of hydrodynamic conditions and the Xin’ancun Spring Basin where the mine is located may be divided into three Middle Ordovician karst water systems. This paper discusses the features of recharge, runoff and discharge of karst water in various zones, and hydrogeological parameters such as the age, flow rate and natural recharge of karst water have been estimated.
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