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Application of passive source surface-wave method in site engineering seismic survey

机译:被动源面波法在场地工程地震勘察中的应用

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Abstract Site engineering seismic survey provides basic data for seismic effect analysis. As an important parameter of soil, shear-wave velocity is usually obtained through wave velocity testing in borehole. In this paper, the passive source surface-wave method is introduced into the site engineering seismic survey and practically applied in an engineering site of Shijingshan District. By recording the ubiquitous weak vibration on the earth surface, extract the dispersion curve from the surface-wave components using the SPAC method and obtain the shear-wave velocity structure from inversion. Over the depth of 42?m underground, it totally consists of five layers with interface depth of 3.31, 4.50, 7.23, 17.41, and 42.00?m; and shear-wave velocity of 144.0, 198.3, 339.4, 744.2, and 903.7?m/s, respectively. The inversion result is used to evaluate site classification, determine the maximum shear modulus of soil, provide basis for further seismic hazard analysis and site assessment or site zoning, etc. The result shows that the passive source surface-wave method is feasible in the site engineering seismic survey and can replace boreholes, shorten survey period, and reduce engineering cost to some extent.
机译:摘要现场工程地震勘测为地震作用分析提供了基础数据。作为土壤的重要参数,剪切波速通常是通过钻孔中的波速测试获得的。本文将被动源面波法引入现场工程地震勘测中,并在石景山区某工程现场实际应用。通过记录地球表面普遍存在的弱振动,使用SPAC方法从表面波分量中提取色散曲线,并通过反演获得剪切波速度结构。在地下42?m的深度上,它总共由五层组成,界面深度分别为3.31、4.50、7.23、17.41和42.00?m。横波速度分别为144.0、198.3、339.4、744.2和903.7?m / s。反演结果用于评估场地分类,确定土壤的最大剪切模量,为进一步的地震危险性分析和场地评估或场地分区等提供依据。结果表明,被动源面波法在场地中是可行的工程地震勘测,可代替井眼,缩短勘测周期,在一定程度上降低工程成本。

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