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The coupled hydro-mechanical approach for fluid compressibility problems in porous media

机译:多孔介质中流体可压缩性问题的流体力学耦合方法

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Numerical modeling for geotechnics use formulations which take into consideration simplifyingrnhypotheses for porous media physical behavior. However, these simplifications neglect effects which couldrncontribute in model’s accuracy. In this paper, a fully coupled hydro-mechanical formulation considering fluidrnand solids compressibility is presented. This formulation was tested for a two-dimensional consolidation case.rnA sensitivity analysis for the fluid compressibility parameter was performed, with comparison of the simulationrnresults to Biot’s analytical solution. Results show that the values of vertical displacements are lower to casesrnwith compressible fluids than to those with incompressible fluids. Instantaneously after load application, fluidrnpressure increases to a maximum value and it dissipates as load is gradually transferred to solid matrix. Forrncompressible fluids, however, there is a delay in fluid pressure dissipation, which makes effective stress lowerrnthan expected. Therewith, stress-strain relations are affected, with low soil strain rate values, justifying verticalrndisplacement decrease.
机译:用于岩土工程的数值建模使用的公式考虑了简化多孔介质物理行为的假设。但是,这些简化忽略了可能影响模型准确性的影响。在本文中,提出了一种考虑流体和固体可压缩性的完全耦合的水力机械配方。对该配方在二维固结情况下进行了测试。对流体可压缩性参数进行了敏感性分析,并将模拟结果与Biot的分析解决方案进行了比较。结果表明,可压缩流体的垂直位移值比不可压缩流体的垂直位移值低。施加载荷后,流体压力立即增加到最大值,并且随着载荷逐渐转移到固体基质中而逐渐消散。但是,对于可压缩流体,流体压力耗散会有所延迟,这会使有效应力低于预期。因此,应力-应变关系受到影响,土壤应变率值较低,证明垂直位移减小。

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