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通过对禹王山断裂带水文地质作用的定性分析与定量评价，提出了对断裂水文地质作用的宏观主导性和局部变异性的定性、定量评价方法，并指出数值模拟是对断裂水文地质作用进行定性和定量评价不可缺少的手段。
Based on the qualitative and quantitative evaluation of the hydrological geology of the Yuwangshan fault zone, a qualitative and quantitative assessment method of the macroscopic dominant and local variability of the hydrogeological fault is put forward. It is pointed out that the numerical simulation is of the hydrogeological Qualitative and quantitative evaluation of the indispensable means.