沈欣茹,郝冰,李远东,陈珍,周正华. 2023. 河谷地形对地震动的影响分析. 地震学报,45(4):706−716. doi: 10.11939/jass.20220041
引用本文: 沈欣茹,郝冰,李远东,陈珍,周正华. 2023. 河谷地形对地震动的影响分析. 地震学报,45(4):706−716. doi: 10.11939/jass.20220041
Shen X R,Hao B,Li Y D,Chen Z,Zhou Z H. 2023. The influence of valley topography on ground motion. Acta Seismologica Sinica45(4):706−716. doi: 10.11939/jass.20220041
Citation: Shen X R,Hao B,Li Y D,Chen Z,Zhou Z H. 2023. The influence of valley topography on ground motion. Acta Seismologica Sinica45(4):706−716. doi: 10.11939/jass.20220041

河谷地形对地震动的影响分析

The influence of valley topography on ground motion

  • 摘要: 基于时域隐式动力有限元结合黏弹性人工边界的方法,实现了地震动垂直入射下三维河谷地形地震反应的数值模拟。在此基础上,针对河谷地形对地震动的影响,对峰值差异、质点运动轨迹等进行了分析,继而分析了地震动相干性及相位差等频域特性。结果表明:河谷地形对地震动强度具有显著影响,其与河谷特征及场点位置相关;河谷地形能产生明显的地震动转换,且坡度越大地震动转换越明显;河谷地形效应会减小地震动的相干性,表现为河谷两岸地震动之间相干性较好,而边坡下降会导致相干性的减小;河谷地形效应导致地震动产生相位差,相位差大小与场点位置相关,但河谷两岸地震动之间几乎不存在相位差,而斜坡及谷底相位差均较大。

     

    Abstract: Based on the time domain implicit dynamic finite element method with viscous-elastic artificial boundary, the numerical simulation of seismic response of three-dimensional valley topography under vertical incidence of ground motion is realized. The influence of valley topography on ground motion, i.e. the difference of peak value and particle motion trajectory, is analyzed firstly, and then the frequency domain characteristics of ground motion such as coherence and phase difference are analyzed. The results show that the valley topography has a significant impact on the ground motion intensity, which is related to the characteristics of the valley and the location of site points. The valley topography can produce obvious ground motion conversion, and the bigger the slope is, the more obvious the ground motion conversion is. The effect of valley topography will weaken the coherence of ground motion. The ground motion on both banks of the valley has good coherence with each other. With the descent of slope, thecoherence is worse. The effect of valley topography leads to the phase difference of ground motion, and its magnitude is related to the location of site points. There is almost no phase difference between the ground motions on both banks of the valley, but the phase differences on slope and bottom of the valley are both large.

     

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