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The role of aftershocks in the liquefaction phenomena caused by the Emilia 2012 seismic sequence

机译:余震在艾米利亚2012地震序列引起的液化现象中的作用

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Extensive and spectacular phenomena of soil liquefaction were observed during the Emilia seismic sequence that struck northern Italy on May-June 2012. A back-analysis with simplified procedures based on empirical correlations reveals a small liquefaction potential, which apparently underestimates the observed surface effects. Multiple and close-in-time events were a peculiar aspect of the sequence but cannot be accounted for within the simplified procedure. This study investigates their possible role in excess pore pressure build-up and hence liquefaction triggering. Results of a numerical analysis suggest that aftershocks played a determinant role, leading liquefaction phenomena to such a great extent as observed in the field. This evidence is to be considered when assessing the results obtained with empirical correlations. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在2012年5月至6月袭击意大利北部的艾米利亚地震序列中,观察到土壤液化的广泛而壮观的现象。基于经验相关性的简化分析方法的反向分析显示,液化潜力很小,显然低估了所观察到的表面效应。多个事件和实时事件是该序列的一个特殊方面,但是无法在简化过程中进行解释。这项研究调查了它们可能在过多的孔隙压力积累中并因此引发液化的作用。数值分析结果表明,余震起着决定性的作用,导致液化现象在现场引起了很大的影响。在评估通过经验相关获得的结果时,应考虑该证据。 (C)2015 Elsevier Ltd.保留所有权利。

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