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电测深法一般在水文地质、工程地质综合勘察中能取得较好的地质效果。为扩大其在成都平原水文地质工作中的效用,本文介绍试用电测深资料估算该平原上部含水层导水系数(T)及井位涌水量(O)0的初步成果。
Electric sounding method is generally in hydrogeology, engineering geological comprehensive survey can achieve better geological results. In order to expand its utility in hydrogeology work in Chengdu Plain, this paper introduces the preliminary results of estimating electrical conductivity coefficient (T) and well water inflow (O) 0 of upper aquifer in this plain by using electrical sounding data.