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The dynamic response of fluid-saturated porous materials with application to seismically induced soil liquefaction

机译:流体饱和多孔材料的动力响应及其在地震诱发土液化中的应用

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摘要

The numerical simulation of liquefaction phenomena in fluid-saturated porous materials within a continuum-mechanical framework is the aim of this contribution. This is achieved by exploiting the Theory of Porous Media (TPM) together with thermodynamically consistent elasto-viscoplastic constitutive laws. Additionally, the Finite Element Method (FEM) besides monolithic time-stepping schemes is used for the numerical treatment of the arising coupled multi-field problem. Within an isothermal and geometrically linear framework, the focus is on fully saturated biphasic materials with incompressible and immiscible phases. Thus, one is concerned with the class of volumetrically coupled problems involving a potentially strong coupling of the solid and fluid momentum balance equations and the algebraic incompressibility constraint. Applying the suggested material model, two important liquefaction-related incidents in porous media dynamics, namely the flow liquefaction and the cyclic mobility, are addressed, and a seismic soil-structure interaction problem to reveal the aforementioned two behaviors in saturated soils is introduced.
机译:在连续力学框架内的流体饱和多孔材料中液化现象的数值模拟是这一贡献的目的。这是通过利用多孔介质理论(TPM)与热力学一致的弹粘塑性本构关系来实现的。此外,除了单片时间步长方案外,有限元方法(FEM)还用于数值计算所引起的耦合多场问题。在等温和几何线性框架内,重点是具有不可压缩和不可混溶相的完全饱和的两相材料。因此,人们关注一类体积耦合问题,涉及固体和流体动量平衡方程与代数不可压缩约束的潜在强耦合。应用建议的材料模型,研究了多孔介质动力学中两个重要的与液化有关的事件,即流动液化和循环迁移率,并介绍了地震土-结构相互作用问题以揭示上述两种在饱和土壤中的行为。

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