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Low-frequency Topographic Amplification Effect of Lushan Earthquake Based on Three-dimensional Numerical Simulation

机译:基于三维数值模拟的庐山地震低频地形放大效应

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The study of the influence of terrain on ground motion is quantified as the amplification effect of terrain on ground motion. In this paper, we use the spectral element method to simulate the three-dimensional real terrain model, and select the aftershocks of the station ground motion observation records in the Lushan area as the source, and analyze the amplification effect of the three-dimensional topography on the ground motion of the Lushan earthquake in the low frequency range (1-5hz). In this paper, the Fourier model of the real terrain of Lushan and the half-space free model are used to calculate the Fourier amplitude spectrum. The results show that in the low frequency range, the ground fluctuations have a large variation, which will have complex effects on the propagation of seismic waves. Especially in the bulging mountain and depression terrain, the time course peak is large. In addition, this paper selects the mountain near the BXD station from the calculation area, and analyzes the terrain magnifying effect of the convex mountain. Under 2-3hz, the mountain slope near the source side has a magnification effect of 3-4 times.
机译:将地形对地震动的影响研究量化为地形对地震动的放大作用。本文采用谱元法对三维真实地形模型进行了模拟,以庐山地区台站地面运动观测记录的余震为源,分析了三维地形的放大效应。在低频范围(1-5hz)内的庐山地震的地震动。本文利用庐山真实地形的傅里叶模型和半空间自由模型计算傅里叶振幅谱。结果表明,在低频范围内,地面起伏变化较大,会对地震波的传播产生复杂的影响。特别是在崎mountain的山地和低洼地带,时程高峰很大。此外,本文从计算区域中选择了BXD站附近的山脉,并分析了凸山的地形放大效果。在2-3hz下,靠近源侧的山坡具有3-4倍的放大效果。

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