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

机译:考虑破裂速度影响的随机有限断层模型模拟地震地震动

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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 M_w 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.
机译:有限断层随机法是地震工程中广泛应用的模拟近场高频地震动最有效的方法之一(Motazedian and Atkinson in Bull Seismol Soc Am 95(3):995-1010, 2005;Bull Seismol Soc Am 99(6):3202-3216, 2009 中的布尔)。然而,广泛使用的静态和动态转角频率是根据破裂速度与横波速度之比 0.69 得出的(Brune in J Geophys Res 75(26):4997-5009, 1970, J Geophys Res 76(20):5002-5002, 1971;中国地震局工程力学研究所,哈尔滨,2017年,王先生在《地震动高频随机模拟方法研究》中,明显消除了破裂速度对拐角频率的影响。在目前分布的随机模拟程序中,破裂速度与横波速度的比值往往设置为0.8,并作为重要的输入参数之一,这显然与推导转角频率时的假设不一致。为了保证输入参数值与推导参数的基本假设一致,本文基于位移表示理论,重新定义了与破裂速度相关的转角频率,为转角频率提供了额外的理论意义。此外,还研究了破裂速度对震源上升时间的影响,并通过2013年4月20日(当地时间)发生的6.6 M_w芦山地震验证了拐角频率的提高。静态和动态转角频率的比较表明,改进转角频率得到的模拟PGA和PSA与观测值一致。此外,本研究提出的转角频率可以进一步研究非均匀破裂速度对合成结果的影响。

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