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Active-passive Array Surface Wave Inversion and Comparison to Borehole Logs in Southeast Missouri

机译:密苏里州东南部有源-被动阵列面波反演与钻孔测井的比较

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摘要

In May 2002, both active- and passive-source surface wave data were acquired using 4-channel arrays at six selected bridge sites in southeast Missouri. Processing of acquired data (increase of signal-to-noise ratio, estimation of phase velocities) was carried out and dispersion curves of Rayleigh wave phase velocities were constructed. Each fundamental mode dispersion curve was then inverted by linearised optimization to a layered shear-wave velocity profile to depths of up to 60 m.
机译:2002年5月,在密苏里州东南部的六个选定桥梁 站点使用4通道阵列获取了有源和无源表面波数据 。进行获取数据的处理(增加信噪比,估计相速度),并进行瑞利波相速度的色散曲线 已建造。 将每个基本模式色散曲线进行线性化优化,然后将其反转为分层的剪切波 速度剖面,深度最大为60 m。

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  • 来源
    《Journal of Environmental & Engineering Geophysics》 |2005年第3期|00000243-00000250|共8页
  • 作者单位

    Geophysical Survey of Russian Academy of Sciences, 189, Lenin Av., Obninsk, Kaluga district, 249035, Russia Email: amal@gsras.ru;

    Department of Geology and Geophysics, University of Missouri-Rolla, Rolla, Mo., 65401 Email: nanders@umr.edu;

    Mining Institute, Ural Branch, Russian Academy of Sciences78a, Sibirskaya St., Perm, 614007, Russia Email: mal@mi-perm.ru;

    Mining Institute, Ural Branch, Russian Academy of Sciences78a, Sibirskaya St., Perm, 614007, Russia Email: mal@mi-perm.ru;

    Mining Institute, Ural Branch, Russian Academy of Sciences78a, Sibirskaya St., Perm, 614007, Russia Email: mal@mi-perm.ru;

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