摘要
在蒲州新闸消力池综合电法勘查中 ,使用高密度电阻率法圈定了消力池区域内砂体的分布位置 ;用自然电场法查明了地下水的渗流方向 ,解释了该区内桩体离析、缩颈的原因 。
In the synthetically electrical prospect of Puzhou new river tax station's subduction force pool, we outlined the position of sands in that region by high\|density resistivity method. At the same time we ascertained the seepage direction of ground water by self\|potential method. The results explained the segregation and gapping of those cast\|in\|place piles. We also gave our advisement to deal with those piles.
出处
《华东地质学院学报》
2001年第2期119-122,共4页
Journal of East China Geological Institute