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Site effects and site amplification due to the 2009 Abruzzo earthquake

机译:由于2009年Abruzzo地震导致的现场效果和站点放大

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This paper presents the results of numerical analyses carried out to assess the different seismic response of two sites in the urban area of L'Aquila, selected as representative of typical subsoil conditions in the old city centre and in the recently developed suburban Pettino district. Both areas were severely damaged by the April 6, 2009 earthquake. The geotechnical model of the subsoil at each of the two sites and the related parameters, defined based on accurate site investigations, are described. The comparison of results of seismic response analyses at the two sites, in agreement with strong motion recordings of the April 6, 2009 main shock, confirms that site effects due to different subsoil conditions played an important role in the observed non-uniform damage distribution. Particularly in the city centre, characterized by an inversion of the shear wave velocity V_S with depth, the simplified approach based on elastic response spectra defined according to ground type (V_(S,30)) of the Italian building code tends to underestimate the seismic action and should be used with caution.
机译:本文介绍了数值分析的结果,以评估L'Aquila市区两个地点的不同地震反应,被选为旧城中心典型的底土条件,最近发达的郊区Pettino区。这两个领域因2009年4月6日地震严重损坏。描述了两个站点中的每一个和相关参数的岩土模型,基于准确的位点调查定义。两个地点的地震反应分析结果的比较,与2009年4月6日的强烈运动录音同意,确认由于不同的底土条件导致的现场效应在观察到的非均匀损伤分布中起重要作用。特别是在市中心,其特征在于剪切波速度V_S的反转深度,基于意大利建筑代码的地面类型(V_(S,30))定义的弹性响应光谱的简化方法倾向于低估地震行动,应该谨慎使用。

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