A closer look at hazard-consistent ground motion record selection for building-specific risk assessment: Effect of soil characteristics and accelerograms’ scaling

危害 脆弱性 地震灾害 危害分析 一致性(知识库) 缩放比例 航程(航空) 选择(遗传算法) 地震动 集合(抽象数据类型) 非线性系统 强地震动 地质学 地震学 计算机科学 工程类 数学 可靠性工程 人工智能 物理 航空航天工程 几何学 有机化学 化学 程序设计语言 热力学 量子力学
作者
Pablo García de Quevedo Iñarritu,Nevena Šipčić,Luis Alvarez-Sanchez,Mohsen Kohrangi,Paolo Bazzurro
出处
期刊:Earthquake Spectra [SAGE]
卷期号:: 875529302311737-875529302311737
标识
DOI:10.1177/87552930231173713
摘要

Conditional spectrum (CS) record selection is a standard tool for the selection of ground motion recordings consistent with the hazard at a site of interest. For many important applications the seismic hazard is computed for reference rock conditions and the effects of local site conditions are investigated downstream via soil dynamics. Ideally, when selecting for rock conditions, the recordings should be real, recorded on rock sites, and strong enough to push the structure into its severe nonlinear range. However, rock-recorded ground motions are often scarce and the analyst is usually left with the suboptimal option of augmenting the set with scaled motions and motions recorded at soil stations. We investigated how this practice can affect the structural response estimates by means of nonlinear dynamic analyses of a comprehensive set of single-degree-of-freedom (SDOF) systems. We first performed site and structure-specific CS record selection using ground motion databases of only soil-recorded motions versus databases of only rock recorded ones. In addition, we performed the CS based on extreme cases of using ground motions scaled by either only small or only large factors. Our focus was on the statistical comparison of the common intensity measures (IMs) of the selected records and, more importantly, of the structural response estimates when these extreme opposite selection choices are made. We show no significant statistical differences in the distributions of the IMs and structural responses, while the fragility and response hazard remain almost identical, for all practical purposes. These results imply that, as long as hazard consistency is accurately enforced in the ground motion record selection, using CS, selecting soil-recorded motions or record scaled up to 10, will not bias the response estimates. Finally, repeating the above procedure for response prediction of one multiple degrees of freedom (MDOF) system suggests that our conclusions are applicable also to more complex structural systems.
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