摘要
采用高密度电法和瞬态面波方法对工程区域进行勘察,获取地层的电阻率和面波速度,并参考钻探资料对其进一步对比、分析和修正,最终获取覆盖层、基岩面等地下地质结构情况,综合评价工程区域的地层分布情况,为工程施工建设提供可靠的科学依据。
High-density resistivity method and instant surface wave method were adopted to investigate the site and achieve the resistivity and surface wave speed,which were then further analyzed and modified to obtain finally the geologic condition of underground structures such as the covering layer and bedrock layer,so as to provide a scientific basis for the comprehensive assessment of the distribution of layers in the engineering area.
引文
[1]李公正,张玉池,周明芳,等.瞬态瑞利面波技术探测原理及其应用[J].矿产与地质,2003(5):661-663.
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