采用高密度电法探测场地古河道沉积地层,沿多条测线布设电极阵列,采集地层电阻率剖面,识别砂层、黏性土的分布边界。结合钻孔取样资料校正剖面解译结果,分析地下水水位波动对电阻率数据造成的干扰,讨论测线布置方式对地层识别效果的影响,欢迎交流。 ;y"DEFs,u
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