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对于隐伏式岩溶矿床地下水运动与补给方式的认识,通常认为是以水平侧向补给为主要形式,对矿床水文地质条件的评价以边界条件为主要依据,根据地质构造类型与边界进水条件(断层两侧含水层对接关系)判断强弱补给边界,据此作为预计水量等的主要依据。但现在认为上述分析认识并不全面,即使具备良好的边界进水条件,但并不真实存在补给关系,更重要的是地下岩溶水运动与补给方式极为复杂,其补给源不只是来源于边界,也可能来自矿床内的垂向补给。具有垂向补给的岩溶充水矿床,水文地质条件更为复杂。垂向补给问题是焦作矿区水文地质条件复杂性的根源所在。
For the understanding of the underground karst deposit groundwater movement and replenishment mode, it is generally considered to be horizontal lateral replenishment as the main form. The evaluation of the hydrogeological conditions of the deposit is mainly based on the boundary conditions. According to the geological structure type and boundary inflow conditions (faults The two sides of the aquifer docking relationship) to determine the strength of the supply boundary, thus as the main basis for the estimated amount of water. However, we do not think the above analysis is comprehensive enough. There is no real supply relationship even though there is a good boundary water supply condition. More importantly, the underground karst water movement and supply mode are extremely complicated. The sources of supply are not only from the border, It may also come from the vertical recharge within the deposit. Hydrogeological conditions are more complicated with karst waterflooding deposits with vertical recharge. Vertical supply is the root cause of the complexity of hydrogeological conditions in Jiaozuo Mining Area.