电阻率测深法在地下水探测中的应用  

The Application of Resistivity Sounding Method In Groundwater Detection

作　　者：林峻 陈伟波 LIN Jun;CHEN WeiBo(Henan Water Conservancy Survey Co,Ltd.,Zhengzhou Henan 450003;Zhengzhou Zhongyong Geological Survey Engineering Co,Ltd.,Zhengzhou Henan 450003)

机构地区：[1]河南省水利勘测有限公司,河南郑州450003 [2]郑州众永地质勘察工程有限公司,河南郑州450001

出　　处：《河南科技》2018年第22期85-87,共3页Henan Science and Technology

摘　　要：常规电阻率测深法是一种传统的寻找地下水源的物探方法.通过在安徽省西南部一处水资源枯乏区, 运用电阻率测深法对含水层埋深、 厚度及其富水性等作出综合评价, 确定裂隙破碎带位置是可行的.Conventional resistivity sounding is a traditional geophysical prospecting method for underground water sources. The depth, thickness and water-rich of aquifer were comprehensively evaluated by resistivity sounding method in a water shortage area in southwestern Anhui Province. It was feasible to determine the location of fractured zone.

关 键 词：电阻率测深 含水层分析 裂隙破碎带 

分 类 号：P641.7[天文地球—地质矿产勘探] P631.322[天文地球—地质学]