Simulation of earthquake ground motion via stochastic finite-fault modeling considering the effect of rupture velocity

被引:0
作者
Pengfei Dang
Jie Cui
Qifang Liu
Yadong Li
机构
[1] Guangzhou University,School of Civil Engineering
[2] The Chinese University of Hong Kong,Earth System Science Programme, Faculty of Science
[3] Suzhou University of Science and Technology,School of Civil Engineering
来源
Stochastic Environmental Research and Risk Assessment | 2023年 / 37卷
关键词
Earthquake ground motions; Time series analysis; Earthquake source observations; Earthquake interaction, forecasting and prediction; Site effects;
D O I
暂无
中图分类号
学科分类号
摘要
The finite fault stochastic method is one of the most effective approaches widely used in seismic engineering to simulate near-field high-frequency ground motion (Motazedian and Atkinson in Bull Seismol Soc Am 95(3):995–1010, 2005; Boore in Bull Seismol Soc Am 99(6):3202–3216, 2009). However, the widely used static and dynamic corner frequencies are derived based on the ratio of rupture velocity to shear-wave velocity of 0.69 (Brune in J Geophys Res 75(26):4997–5009, 1970, J Geophys Res 76(20):5002–5002, 1971; Wang in Research on stochastic simulation method for high frequency of ground motions, Institute of Engineering Mechanics, China Earthquake Administration, Harbin, 2017), which obviously eliminates the influence of rupture velocity on corner frequency. In the currently distributed stochastic simulation program, the ratio of rupture velocity to shear-wave velocity is often set to 0.8 and is adopted as one of the important input parameters, which is obviously inconsistent with the assumption when deriving the corner frequency. In order to ensure that the input parameter values are consistent with the basic assumptions used in deriving the parameters, this study redefines the corner frequency associated with the rupture velocity, based on the displacement representation theory providing additional theoretical significance to the corner frequency. Also, the influence of rupture velocity on source rise time is investigated, and the improved corner frequency is verified by the Mw 6.6 Lushan earthquake occurred on April 20, 2013 (local time) in China. The comparison of the static and dynamic corner frequencies indicates that the simulated PGA and PSA obtained by the improved corner frequency are consistent with the observed values. Moreover, the corner frequency proposed in this study can further study the influence of nonuniform rupture velocity on the synthetic results.
引用
收藏
页码:2225 / 2241
页数:16
相关论文
共 61 条
  • [1] Bahrampouri M(2021)Ground motion prediction equations for arias intensity using the Kik-net database Earthq Spectra 30 428-448
  • [2] Rodriguez-Marek A(1997)Modeling finite-fault radiation from the Bull Seismol Soc Am 87 67-84
  • [3] Green R(1998) spectrum Bull Seismol Soc Am 88 1392-1401
  • [4] Beresnev IA(1992)Stochastic finite-fault modeling of ground motins from the 1994 Northridge, California, earthquake. I. Validation on rock sites Bull Seismol Soc Am 82 660-682
  • [5] Atkinson GM(1983)Acceleration source spectra anticipated for large earthquakes in northeastern North America Bull Seismol Soc Am 73 1865-1894
  • [6] Beresnev IA(2003)Stochastic simulation of high-frequency ground motion based on seismological models of the radiated spectra Pure Appl Geophys 160 635-676
  • [7] Atkinson GM(2009)Simulation of ground motion using the stochastic method Bull Seismol Soc Am 99 3202-3216
  • [8] Boatwright J(1997)Comparing stochastic point-source and finite-source ground-motion simulations: SMSIM and EXSIM Bull Seismol Soc Am 87 327-341
  • [9] Choy G(1970)Site amplifications for generic rock sites J Geophys Res 75 4997-5009
  • [10] Boore DM(1971)Tectonic stress and the spectra of seismic shear waves from earthquakes J Geophys Res 76 5002-5002