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Inelastic soil amplification in three sites during the Tokachi-oki M_(JMA) 8.0 earthquake

机译:十胜木M_(JMA)8.0地震中三个地点的非弹性土壤放大

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Earthquake case histories of soil response in the last half century have revealed the nonlinear behavior of soils under strong shaking. Over the years numerous efforts have been made to represent realistically soil behavior in the nonlinear range. In the aftermath of an international benchmark exercise (PRENOLIN) aimed at verifying 23 nonlinear codes and then validating them against the recorded seismic responses of two soil sites, this paper investigates the response of 3 soil sites in Hokkaido, Japan, shaken by the Tokachi-oki 2003 earthquake. Surface and deep ("in-borehole") accelerographs recorded the event at each site. The objective of our study is to see if available nonlinear codes, without any after-the-event calibration and with imperfect knowledge of the soil layer properties, can lead to practically acceptable results. Before embarking into the nonlinear analyses, the linear response to an aftershock is first simulated with reasonable success. Then, using three different nonlinear 1D soil-amplification codes, which incorporate different constitutive relations, numerical wave propagation analyses are performed for each site, excited with the motion recorded in each borehole (at the depth of the presumed bedrock). Computed results in the form of acceleration time histories and response spectra for the ground surface are systematically compared with the respective recorded motions. It is found that the numerical codes perform generally quite satisfactorily. Exceptions are discussed in the light of the other research findings.
机译:近半个世纪以来,土壤反应的地震案例历史揭示了强震动下土壤的非线性行为。多年来,已经做出了许多努力来真实地表示非线性范围内的土壤行为。在进行国际基准测试(PRENOLIN)之后,该方法旨在验证23种非线性代码,然后针对记录的两个土壤场地的地震响应对它们进行验证,本文研究了十胜晃动的日本北海道3个土壤场地的响应2003年冲绳地震。地面和深部(“井内”)加速度计记录了每个地点的事件。我们研究的目的是查看没有可用的事后校准且对土壤层特性的了解不完善的可用非线性编码是否可以导致实际上可接受的结果。在进行非线性分析之前,首先模拟了对余震的线性响应,并取得了一定的成功。然后,使用包含不同本构关系的三种不同的非线性一维土壤放大码,对每个部位进行数值波传播分析,并在每个钻孔中(假定基岩的深度)记录下的运动来激发。系统以加速时间历史和地面响应谱形式的计算结果与相应记录的运动进行了系统比较。已经发现,数字代码总体上令人满意地执行。根据其他研究结果讨论了例外情况。

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