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Reliability of rayleigh wave dispersion curve obtained from f-k spectral analysis of microtremor array measurement

机译:通过微震阵列测量的f-k谱分析获得的瑞利波频散曲线的可靠性

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摘要

The paper utilizes previously developed microtremor simulation technique to evaluate the reliability of Rayleigh wave dispersion curve estimated by f-k spectral analysis of microtremor array measurement. The simulated microtremors are obtained for a fictitious (TEST) site. Attempt is also made to obtain the dispersion curve for two real sites (OHDATE and SKC) by inverse analysis of the microtremor array measurement using f-k spectra method. The estimated dispersion curve from simulated microtremors (TEST site) compares well with the theoretical dispersion curve, demonstrating the reliability of f-k spectra method and indicating that the estimated dispersion curve from microtremor measurements could be adequately used as the target for inverse analysis purposes. It is also demonstrated that the dispersion curve from microtremor measurements can be utilized to estimate the soil profile at OHDATE and SKC sites by inverse analysis. Results show that the theoretical dispersion curve of the fundamental mode of Rayleigh wave after the end of inverse analysis are in good agreement with the dispersion curve obtained by f-k spectral analysis of microtremor array measurement.
机译:本文利用先前开发的微震模拟技术评估通过微震阵列测量的f-k谱分析估计的瑞利波频散曲线的可靠性。在虚拟(TEST)站点获得了模拟的微震。还尝试通过使用f-k光谱法对微震阵列测量值进行反分析来获得两个真实位点(OHDATE和SKC)的色散曲线。模拟微震(TEST站点)的估计频散曲线与理论频散曲线有很好的比较,证明了f-k谱方法的可靠性,并表明微震测量的频散曲线估计值可以充分用作反分析的目标。还证明了通过微震测量得到的弥散曲线可用于通过反分析估算OHDATE和SKC站点的土壤剖面。结果表明,逆分析结束后瑞利波基本模的理论色散曲线与通过微震阵列测量的f-k谱分析获得的色散曲线非常吻合。

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