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首页> 外文期刊>Chinese science bulletin >Collapse ratios of buildings due to the 1995 Kobe earthquake and interference between S-wave and the second surface wave at basin edge
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Collapse ratios of buildings due to the 1995 Kobe earthquake and interference between S-wave and the second surface wave at basin edge

机译:由于1995年神户地震造成的建筑物倒塌率和盆地边缘的S波与二次面波的干扰。

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The distribution characteristics of collapse ratios of buildings in Kobe city due to the 1995 M7.2 Hyogo-ken Nanbu, Japan (Kobel earthquake and the interferences due to SH or P-SV and the second surface waves propagating in heterogeneous medium are discussed in this paper by using numerical simulation technique of wave equation. The staggered grid real value fast Fourier transform differentiation (SGRFFTD) is used in the pseudospectral method of ground motion simulations because of its speed, high stability and accuracy. The results show that the maximum amplitude of simulated acceleration waveforms on the ground coincides well with the complicated distributions of collapse ratios of buildings. The peak collapse ratio of buildings away from the earthquake fault also coincides well with the peak ground acceleration. The spatial interference process is analyzed by using the snap shots of seismic wave propagation. The peak ground acceleration is probably caused by the interferences due to the second surface wave transmitting from the bedrock to sedimentary basin and the upward body wave. Analyses of the interference process show that seismic velocity structure and geologic structure strongly influence the distribution of the maximum amplitude of acceleration waveforms. Interferences occurring near the basin boundary are probably the cause of the peak collapse ratio of buildings away from the fault. Therefore it is necessary to analyze wave propagations and interference process using numerical simulation strategy for studies on the seismic disasters.
机译:本文讨论了1995年日本兵库县南部M7.2地震造成的神户市建筑物倒塌率的分布特征(神户地震以及SH或P-SV以及在非均质介质中传播的第二面波引起的干扰)本文采用波动方程数值模拟技术,由于其速度快,稳定性高,精度高等优点,在地面运动模拟的伪谱方法中采用了交错网格实值快速傅里叶变换微分法(SGRFFTD),结果表明:模拟的地面加速度波形与建筑物倒塌率的复杂分布吻合较好,远离地震断层的建筑物的峰值倒塌率也与地面加速度峰值很好吻合,并用实测快照分析了空间干扰过程。地震波传播,地面加速度峰值可能是由于从基岩到沉积盆地的第二次面波和向上的体波。对干扰过程的分析表明,地震速度结构和地质结构强烈影响加速度波形最大振幅的分布。流域边界附近发生的干扰可能是导致远离断层的建筑物的最大倒塌率的原因。因此,有必要采用数值模拟策略来分析地震传播的波传播和干扰过程。

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