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Numerical modelling of landslide-generated waves with the particle finite element method (PFEM) and a non-Newtonian flow model

机译:利用粒子有限元法(pFEm)和非牛顿流动模型对滑坡产生的波浪进行数值模拟

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摘要

Landslide-generated impulse waves may have catastrophic consequences. The physical phenomenon is difficult to model because of the uncertainties in the kinematics of the mobilised material and to the intrinsic complexity of the fluid–soil interaction. The particle finite element method (PFEM) is a numerical scheme that has successfully been applied to fluid–structure interaction problems. It uses a Lagrangian description to model the motion of nodes (particles) in both the fluid and the solid domains (the latter including soil/rock and structures). A mesh connecting the particles (nodes) is re-generated at every time step, where the governing equations are solved. Various constitutive laws are used for the sliding mass, including rigid solid and the Newtonian and non-Newtonian fluids. Several examples of application are presented, corresponding both to experimental tests and to actual full-scale case studies. The results show that the PFEM can be a useful tool for analysing the risks associated with landslide phenomena, providing a good estimate to the potential hazards even for full-scale events.
机译:滑坡产生的脉冲波可能会带来灾难性的后果。由于动员材料的运动学不确定性以及流体与土壤相互作用的内在复杂性,很难对物理现象进行建模。粒子有限元法(PFEM)是一种数值方案,已成功地应用于流固耦合问题。它使用拉格朗日描述对流体域和固体域(后者包括土壤/岩石和结构)中的节点(粒子)运动进行建模。在每个时间步都会重新生成连接粒子(节点)的网格,在此求解控制方程。滑动质量使用各种本构定律,包括刚性固体以及牛顿流体和非牛顿流体。给出了几个应用示例,分别对应于实验测试和实际的全面案例研究。结果表明,PFEM可以作为分析与滑坡现象相关的风险的有用工具,即使对于全面事件,也可以很好地估计潜在危害。

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