Surface Wave Dispersion in a Layered Medium for Varying Subsurface Scenarios

IF 0.5 Q4 ENGINEERING, GEOLOGICAL
N. Roy, Aniket Desai, R. Jakka
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引用次数: 1

Abstract

Surface wave techniques are widely used to characterize a site based on shear wave velocity (Vs) or stiffness variation with depth. It utilizes the dispersion property of Rayleigh wave in a heterogeneous media. Dispersion curve is obtained from analyzing collected field test data and the final Vs profile is extracted from the inversion of the generated dispersion curve. The varying subsoil structures influence whether one or more Rayleigh modes will participate in the resulting wave propagation phenomenon. So, neglecting the higher mode participation may sometimes results in a completely different velocity profile than the actual existing one. In this paper, a detailed and comprehensive numerical study has been performed using finite element method for different types of soil profiles with different half-space impedances to assess how it affects the surface wave dispersion phenomenon. In addition to that, the effect of different data acquisition parameters on surface wave dispersion has also been studied.
不同地下情况下层状介质中的表面波色散
面波技术被广泛用于根据横波速度(Vs)或刚度随深度的变化来表征一个地点。它利用了非均质介质中瑞利波的色散特性。对采集的现场试验数据进行分析得到色散曲线,并对生成的色散曲线进行反演,提取最终的Vs剖面。不同的底土结构会影响一个或多个瑞利模态是否参与所产生的波传播现象。因此,忽略高模态参与有时可能会导致与实际存在的速度曲线完全不同的速度曲线。本文采用有限元方法对不同半空间阻抗类型的土壤剖面进行了详细而全面的数值研究,以评估其对表面波色散现象的影响。此外,还研究了不同数据采集参数对表面波色散的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
1.90
自引率
25.00%
发文量
11
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