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Estimation of dynamic behaviors of bedrock foundation subjected to seismic loads based on FEM and DEM simulations

机译:基于有限元和DEm模拟的地基荷载作用下岩石地基动力特性估算

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摘要

Seismic behavior of bedrock foundation remains as one of the most fundamental and important problems concerning the stability and safety of nuclear power plants. The dynamic FEM (Finite Element Method) is commonly utilized in analyzing the seismic responses of bedrock; while in recent decades, the DEM (Distinct Element Method) has attracted more and more attentions, which has a better capability of simulating the sliding and separation of discontinuities in dynamic simulations. In this study, the FEM and DEM were adopted to investigate the seismic behavior of the bedrock of a nuclear power plant located in Japan, and the differences between the two methods in dynamic simulations were illuminated. Simulation results using FEM and DEM models without discontinuities agree well with each other, exhibiting an amplification effect of intact bedrock on the seismic wave propagation. Numerical simulation results obtained from the models containing faults give similar responses of bedrock to the input seismic waves; however, the FEM model underestimates the weakening effect of discontinuities on the propagation of seismic waves due to that it cannot represent well the large deformational behavior of discontinuities. When large deformation happens due to large seismic loads, the DEM can be regarded as a better method in seismic response evaluations of bedrock with discontinuities.
机译:基岩基础的抗震性能仍然是与核电厂的稳定性和安全有关的最根本和最重要的问题之一。动态有限元法(FEM)通常用于分析基岩的地震响应。近几十年来,DEM(离散元法)引起了越来越多的关注,它在动态仿真中具有更好的模拟不连续滑动和分离的能力。在这项研究中,采用FEM和DEM来研究位于日本的核电厂的基岩的地震行为,并阐明了两种方法在动态仿真中的差异。使用不间断的FEM和DEM模型进行的模拟结果相互吻合,显示出完整的基岩对地震波传播的放大作用。从包含断层的模型中获得的数值模拟结果给出了基岩对输入地震波的相似响应。然而,有限元模型低估了不连续性对地震波传播的减弱作用,因为它不能很好地代表不连续性的大变形行为。当由于大地震载荷而发生大变形时,DEM可以被认为是不连续基岩地震响应评估中的一种更好的方法。

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