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首页> 外文期刊>Soil Dynamics and Earthquake Engineering >Surface topography and site stratigraphy effects on the seismic response of a slope in the Achaia-Ilia (Greece) 2008 M(w)6.4 earthquake
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Surface topography and site stratigraphy effects on the seismic response of a slope in the Achaia-Ilia (Greece) 2008 M(w)6.4 earthquake

机译:表面形貌和场地地层学对Achaia-Ilia(希腊)2008 M(w)6.4地震的边坡地震响应的影响

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摘要

Following an overview of the state of knowledge on the effects of slope topography on the seismic ground response, the results of numerical analyses of the response of a 28 degrees slope, with a height of 24 m, located in the meizoseismal area of the Achaia-Ilia (Greece) 2008 M-w 6.4 earthquake, are presented. The 2-D and 1-D FEM equivalent-linear analyses were based on the results of an extensive geotechnical investigation and on input motions estimated on the basis of recorded acceleration time histories in the broader area of the slope. The results of analyses were (a) found to be in a good agreement with the observed distribution of structural damages in the area of the town, (b) used to separate the effects of pure topography from the effects of soil stratigraphy, and (c) used to check the validity of a simplified prediction of topography effects, by superimposing the de coupled 1-D and 2-D amplification of motions.
机译:概述了关于坡度地形对地震地面响应的影响的知识状态之后,对位于Achaia-Meizoseismal地区的高度为24 m的28度坡度的响应进行了数值分析的结果介绍了伊利亚(希腊)2008年兆瓦6.4级地震。 2-D和1-D FEM等效线性分析是基于广泛的岩土工程研究的结果,并且基于输入的运动,该输入的运动是基于在更宽的斜坡区域记录的加速时间历史记录进行估算的。分析的结果是(a)与城镇区域内观察到的结构破坏分布非常吻合;(b)用于将纯地形的影响与土壤地层的影响分开;以及(c )通过叠加解耦的运动的一维和二维放大率来检查地形效果简化预测的有效性。

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