半空间上任意弹性层具有频率相关路径跟踪的最小条件刚度矩阵

Andrew Peplow, Bilong Liu
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摘要

本文介绍了一种分析谐波在层状弹性介质中传播的高效计算程序。这种方法有几个优点,包括能够处理弹性半空间上方的任意频率、深度和层数,并研究了跟踪频散曲线和标记可能的奇异点的工作。虽然在计算精度和容量方面存在固有限制,但这种方法可以直接用于研究自由或受迫振动,并获得相关响应数据。我们展示了频域和时域的波数频散图、相位速度图和响应数据的计算结果。这些计算结果针对两个示例情况:平面应变和轴对称。我们的方法基于专门为深层地层分析定制的、条件良好的动态刚度方法。我们引入了一种创新方法,用于有效计算波数频散曲线。通过跟踪这些曲线的斜率,用户可以有效地管理延续参数。我们通过一个实际案例研究中的层共振数值证据来说明这一技术,该共振的特点是频散曲线出现折叠。此外,该框架对于工程师解决地面振动相关问题尤其有利。它能在频域和时域分析零群速度(ZGV)等出现奇点的现象,揭示此类情况的独特特征。由于问题的维度缩小了,这种表述方式可以在 MASW 或 SASW 技术等领域为地球物理学家和工程师提供很大帮助。
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Minimal Conditioned Stiffness Matrices with Frequency-Dependent Path Following for Arbitrary Elastic Layers over Half-Spaces
This paper introduces an efficient computational procedure for analyzing the propagation of harmonic waves in layered elastic media. This offers several advantages, including the ability to handle arbitrary frequencies, depths, and the number of layers above an elastic half-space, and efforts to follow dispersion curves and flag up possible singularities are investigated. While there are inherent limitations in terms of computational accuracy and capacity, this methodology is straightforward to implement for studying free or forced vibrations and obtaining relevant response data. We present computations of wavenumber dispersion diagrams, phase velocity plots, and response data in both the frequency and time domains. These computational results are provided for two example cases: plane strain and axisymmetry. Our methodology is grounded in a well-conditioned dynamic stiffness approach specifically tailored for deep-layered strata analysis. We introduce an innovative method for efficiently computing wavenumber dispersion curves. By tracking the slope of these curves, users can effectively manage continuation parameters. We illustrate this technique through numerical evidence of a layer resonance in a real-life case study characterized by a fold in the dispersion curves. Furthermore, this framework is particularly advantageous for engineers addressing problems related to ground-borne vibrations. It enables the analysis of phenomena such as zero group velocity (ZGV), where a singularity occurs, both in the frequency and time domains, shedding light on the unique characteristics of such cases. Given the reduced dimension of the problem, this formulation can considerably aid geophysicists and engineers in areas such as MASW or SASW techniques.
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