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Ambient Noise and Site Response: From Estimation of Site Effects to Determination of the Subsoil Structure

机译:环境噪声和站点响应:从估计地点效应到确定底土结构

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Damage distribution during large earthquakes is frequently conditionedby site effects. Site effect are best determined using earthquake data. However, thatdata is not always available and ambient noise measurements have been used asan inexpensive alternative. Microtremor measurements have been used along twopaths to study site effects: estimation of a local transfer function, and estimation ofthe subsoil structure (once this structure is known, it is possible to compute expectedground motion amplification). Currently, the estimation of a transfer function usesH/V spectral ratios almost exclusively. Estimation of the subsoil structure exploitsdata from array measurements of microtremors applying techniques such as SPAC,ReMi and time domain analysis of cross-correlation. This paper discusses those twopaths and shows the results that were obtained in two dissimilar examples: Parkwaybasin and Colima city. It is shown that results need to be validated; it is unsafe touse a single technique. In addition, it is clear that no single technique is adapted toall possible cases.
机译:大地震期间的损伤分布经常有条件的现场效应。使用地震数据最佳确定现场效果。然而,该数据并不总是可用的,并且使用ASAN廉价的替代方案使用环境噪声测量。沿Thopaths使用微调测量来研究现场效果:估计局部传递函数,以及估计子土结构(一旦知道该结构,就可以计算预期的地面运动扩增)。目前,几乎完全估计了传递函数USESH / V光谱比率。估计Subsoil结构ExploitSDATA从阵列测量的微调施用技术,例如SPAC,REMI和时域分析的互相关性。本文讨论了那些双胞胎,并展示了两种不同的例子中获得的结果:百日田纳辛和科里马市。结果表明,需要验证结果;它是不安全的替代单一技术。此外,很明显,没有单一技术适于可能的情况。

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