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Seismic response analysis of the reef-seawater system under incident SV wave

机译:SV波入射时礁海系统的地震响应分析

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摘要

The seismic response analysis of a reef engineering site is the foundation for the seismic design of artificial islands and other upper constructions. This study proposes a two-dimensional seismic analysis model for the reef-seawater system, where the fluid-solid coupling effect is considered and the wave radiation effects of infinite fluid and solid domains are simulated by corresponding artificial boundary conditions. Meanwhile, the seismic wave input method based on the substructure of artificial boundaries is modified to accomplish the process of inputting the seismic waves with arbitrary incident angles into the calculation region. The accuracy of the proposed model is verified by numerical examples. Afterwards, we conduct the parametric studies and the seismic analysis of a series of practical layered reef models. The results indicate that the least favorable slope gradient for the seismic response is generally at approximately 30 degrees, and the feature of wave velocity reduction along the vertical direction significantly magnifies the seismic response on the reef flat. The peak acceleration ratio near the edges of the reef flat distributes between 3 and 4. While in the middle area, it is usually between 1.5 and 2.5, and can reach up to 4 when the width of reef flat decreases.
机译:礁石工程现场的地震响应分析是人工岛和其他上部建筑的抗震设计的基础。这项研究提出了一种针对礁石-海水系统的二维地震分析模型,其中考虑了流固耦合效应,并通过相应的人工边界条件模拟了无限大的流体和固体域的波辐射效应。同时,修改了基于人工边界子结构的地震波输入方法,以完成将任意入射角的地震波输入计算区域的过程。数值例子验证了所提模型的准确性。之后,我们对一系列实用的分层礁石模型进行参数研究和地震分析。结果表明,对于地震响应最不利的坡度通常在大约30度,并且沿垂直方向波速降低的特征显着放大了礁滩上的地震响应。礁滩边缘附近的峰值加速比分布在3到4之间。而在中间区域,峰值加速比通常在1.5到2.5之间,当礁滩的宽度减小时,峰值加速比可以达到4。

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