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Propagation of seismic waves through liquefied soils

机译:地震波在液化土壤中的传播

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To predict the earthquake response of saturated porous media it is essential to correctly simulate the generation, redistribution, and dissipation of excess pore water pressure during and after earthquake shaking. To this end, a reliable numerical tool requires a dynamic, fully coupled formulation for solid-fluid interaction and a versatile constitutive model. Presented in this paper is a 3D finite element framework that has been developed and utilized for this purpose. The framework employs fully coupled dynamic field equations with a u-p-U formulation for simulation of pore fluid and solid skeleton interaction and a SANISAND constitutive model for response of solid skeleton. After a detailed verification and validation of the formulation and implementation of the developed numerical tool, it is employed in the seismic response of saturated porous media. The study includes examination of the mechanism of propagation of the earthquake-induced shear waves and liquefaction phenomenon in uniform and layered profiles of saturated sand deposits.
机译:要预测饱和多孔介质的地震响应,必须正确模拟地震震动期间和之后多余孔隙水压力的产生,重新分布和消散。为此,可靠的数值工具需要用于固-液相互作用的动态,完全耦合的公式和通用的本构模型。本文介绍的是为此目的而开发和利用的3D有限元框架。该框架采用具有u-p-U公式的完全耦合动态场方程来模拟孔隙流体和固体骨架相互作用,并使用SANISAND本构模型来响应固体骨架。在对开发的数值工具的公式和实现进行详细验证和确认后,将其用于饱和多孔介质的地震响应。这项研究包括检查地震引起的剪切波的传播机理以及饱和砂沉积物的均匀分层分布中的液化现象。

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