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Dynamic wave propagation in infinite saturated porous media half spaces

机译:无限饱和多孔介质半空间中的动态波传播

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From a macroscopic perspective, saturated porous materials like soils represent volumetrically interacting solid–fluid aggregates. They can be properly modelled using continuum porous media theories accounting for both solid-matrix deformation and pore-fluid flow. The dynamic excitation of such multi-phase materials gives rise to different types of travelling waves, where it is of common interest to adequately describe their propagation through unbounded domains. This poses challenges for the numerical treatment and demands special solution strategies that avoid artificial and numerically-induced perturbations or interferences. The present paper is concerned with the accurate and stable numerical solution of dynamic wave propagation problems in infinite half spaces. Proceeding from an isothermal, biphasic, linear poroelasticity model with incompressible constituents, finite elements are used to discretise the near field and infinite elements to approximate the far field. The transient propagation of the poroacoustic body waves to the infinity is thereby modelled by a viscous damping boundary, which, for stability reasons, necessitates an appropriate treatment of the included velocity-dependent damping forces.
机译:从宏观的角度看,饱和的多孔材料(例如土壤)代表了体积相互作用的固液聚集体。可以使用考虑固体基质变形和孔隙流体流动的连续多孔介质理论对它们进行正确建模。这种多相材料的动态激发会引起不同类型的行波,其中充分描述它们通过无界域的传播是人们普遍关注的问题。这给数值处理带来了挑战,并要求采取特殊的解决方案策略,以避免人为和数字引起的扰动或干扰。本文涉及无限半空间中动态波传播问题的精确和稳定的数值解。从具有不可压缩成分的等温,双相,线性多孔弹性模型开始,有限元被用来离散近场,而无限元被用来近似远场。因此,通过粘性阻尼边界来模拟孔隙声体波向无穷大的瞬态传播,出于稳定性的原因,该边界必须对包含的与速度有关的阻尼力进行适当处理。

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