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Study on the influence of the seafloor soft soil layer on seismic ground motion

机译:海底软土层对地震地面运动的影响研究

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In the complex medium system of the sea area, the overlyingseawater and the surface soft soil have a significant impact on theseafloor ground motion, which brings great seismic risk to the safety ofoffshore-engineering structures. In this paper, four sets of typical free-field models are constructed and established, comprising a land model, landmodel with surface soft soil, sea model and sea model with surface softsoil. The dynamic finite-difference method is used to carry outtwo-dimensional seismic response analysis of a typical free field based on theinput forms of P?and SV?waves. By comparing the seismic response analysisresults of four groups of calculation models, the effects of overlyingseawater and soft soil on the peak acceleration and acceleration responsespectrum are studied. The results show that when an SV wave is input, the peakacceleration and response spectrum of the surface of soft soil on thesurface and the seabed surface can be amplified, while the overlying seawater can significantly reduce the ground motion. When the P?wave is used, theeffect of overlying seawater and soft soil on the peak acceleration and responsespectrum of the surface and seabed can be ignored. The peak accelerationdecreases first and then increases from the bottom to the surface, and thedifference of peak acceleration calculated by four free-field models is notobvious. The results show that the overlying seawater and the surface softsoil layer have little effect on the peak acceleration of ground motionbelow the surface.
机译:在海域的复杂介质系统中,综合血疏水和表面软土对该基地运动产生重大影响,这为OFFSHORE-ENGINEERS结构的安全带来了极大的地震风险。在本文中,构建并建立了四组典型的自由场模型,包括陆地模型,陆地模型,具有表面软土,海模型和海洋模型的地表软泥。动态有限差分法用于基于P?和SV的inpput形式进行典型自由场的远离尺寸地震响应分析。通过比较四组计算模型的地震反应分析,研究了综合体膜水和软土对峰值加速度和加速度应答措施的影响。结果表明,当输入SV波时,可以放大张力土壤和海底表面上的软土表面的峰值燃卡和响应谱,而覆盖海水可以显着降低地面运动。当使用P?波浪时,可以忽略覆盖海水和软土对表面和海底的峰值加速度和呼应谱的影响。峰值加速度首先,然后从底部到表面增加,并且通过四个自由场模型计算的峰值加速度的峰值是令人烦恼的。结果表明,上覆海水和表面软硅层对地面运动近距离的峰值加速度几乎没有影响。

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