Current empirical ground-motion prediction equations for Europe and their application to Eurocode 8

被引:29
作者
Bommer, Julian J. [1 ]
Stafford, Peter J. [1 ]
Akkar, Sinan [2 ]
机构
[1] Univ London Imperial Coll Sci Technol & Med, Dept Civil & Environm Engn, London SW7 2AZ, England
[2] Middle E Tech Univ, Dept Civil Engn, TR-06531 Ankara, Turkey
关键词
Europe; Middle East; Ground-motion prediction; Attenuation; Peak ground acceleration; Peak ground velocity; Response spectra; Eurocode; 8; DISPLACEMENT RESPONSE SPECTRA; AVERAGE HORIZONTAL COMPONENT; SEISMIC-HAZARD; ATTENUATION RELATIONSHIP; MAGNITUDE RANGE; EARTHQUAKE; ACCELERATION; SIMULATION; RECORDS; MODELS;
D O I
10.1007/s10518-009-9122-9
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The first ground-motion prediction equation derived from European and Middle Eastern strong-motion data was published more than 30 years ago; since then strong-motion networks and the resulting databank of accelerograms in the region have expanded significantly. Many equations for the prediction of peak ground-motion parameters and response spectral ordinates have been published in recent years both for the entire Euro-Mediterranean and Middle Eastern region as well as for individual countries within this region. Comparisons among empirical ground-motion models for these parameters, developed using large regional datasets, do not support the hypothesis of there being significant differences in earthquake ground-motions from one area of crustal seismicity to another. However, there are certain regions within Europe-affected by different tectonic regimes-for which the existing pan-European equations may not be applicable. The most recent European equations make it possible to now implement overdue modifications to the presentation of seismic design actions in Eurocode 8 that allow an improved approximation to the target uniform hazard spectrum (UHS). Using these recent equations, this study outlines a new approach via which an approximation to the UHS may be constructed using hazard maps calculated for peak ground velocity and the corner period T (D) in addition to the maps for peak ground acceleration that underpin the current stipulations of Eurocode 8.
引用
收藏
页码:5 / 26
页数:22
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