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Application of Surface-Wave Methods for Seismic Site Characterization

机译:面波方法在地震现场表征中的应用

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Surface-wave dispersion analysis is widely used in geophysics to infer a shear wave velocity model of the subsoil for a wide variety of applications. A shear-wave velocity model is obtained from the solution of an inverse problem based on the surface wave dispersive propagation in vertically heterogeneous media. The analysis can be based either on active source measurements or on seismic noise recordings. This paper discusses the most typical choices for collection and interpretation of experimental data, providing a state of the art on the different steps involved in surface wave surveys. In particular, the different strategies for processing experimental data and to solve the inverse problem are presented, along with their advantages and disadvantages. Also, some issues related to the characteristics of passive surface wave data and their use in H/V spectral ratio technique are discussed as additional information to be used independently or in conjunction with dispersion analysis. Finally, some recommendations for the use of surface wave methods are presented, while also outlining future trends in the research of this topic.
机译:地表波频散分析在地球物理学中被广泛使用,以推断地下土的剪切波速度模型,从而具有广泛的应用。基于在垂直非均质介质中表面波的色散传播,从反问题的解中获得了剪切波速度模型。该分析可以基于活动源测量或地震噪声记录。本文讨论了收集和解释实验数据的最典型选择,提供了有关表面波调查涉及的不同步骤的最新技术。特别是,提出了处理实验数据和解决反问题的不同策略,以及它们的优缺点。此外,还讨论了一些与无源表面波数据的特性及其在H / V谱比技术中的使用有关的问题,作为可独立使用或与色散分析结合使用的附加信息。最后,提出了一些有关使用表面波方法的建议,同时概述了该主题研究的未来趋势。

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