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Simulation of the Jiuzhaigou, China, earthquake by stochastic finite-fault method based on variable stress drop

机译:基于可变应力下降的九寨沟挖掘,中国九寨沟地震

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摘要

An improved stochastic finite-fault method was used to simulate theM(w)6.6 earthquake that occurred on August 8, 2017, in Jiuzhaigou, Sichuan, China. A variation of the stochastic finite-fault method, considering the dynamic corner frequency, was used to overcome the corner frequency. It explains the effect of a given slip distribution on the corner frequency of each subfault. A comparison of the response spectra (damping ratio 5%), spectral ratio (simulated values/observed values), and model deviation demonstrated that the improved corner frequency performs well for the whole periods, especially in short periods from 0.2 to 1 s. Similarly, the revised duration model and the site-amplification factor were applied to simulate the ground motion during the Jiuzhaigou earthquake, and then the response spectra were obtained. The duration of the nine near-field station recordings matched well with the simulated ground motions, and the peak ground acceleration (PGA) of most of the stations matched well with the observed PGA. In the short periods (T < 1 s), a small difference is observed between the simulated response spectra and the observed spectra for most of the stations. However, the response spectra were overestimated within the period range (0.05-10 s). Generally, the simulated ground motions obtained by using the improved model matched well with the observed ground motions, which could be considered the basis for earthquake-resistant design during the postdisaster recovery and the structural dynamic analysis of the Jiuzhaigou region.
机译:改进的随机有限故障方法用于模拟2017年8月8日发生的6.6地震,在中国四川九寨沟发生。考虑动态角频率的随机有限故障方法的变化用于克服角频率。它解释了给定滑动分布对每个子故障的角频率的影响。响应光谱(阻尼比5%),光谱比(模拟值/观察值)和模型偏差的比较表明,改进的角频率在整个时段中表现良好,特别是在0.2至1秒的短时间内。类似地,修订后的持续时间模型和站点放大因子被应用于模拟九寨沟地震期间的地面运动,然后获得响应光谱。九个近场录制的持续时间与模拟地面运动相匹配,并且大多数站的峰接地加速度(PGA)与观察到的PGA匹配良好。在短时间内(T <1 s)中,在模拟响应光谱和大多数站的观察光谱之间观察到小差异。然而,响应光谱在期间范围内估量(0.05-10秒)。通常,通过使用改进的模型获得的模拟地面运动与观察到的地面运动相匹配,这可以被认为是在邮政恢复期间抗震设计的基础和九寨沟地区的结构动态分析。

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