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Determination of macro-scale soil properties from pore-scale structures: model derivation

机译:从孔隙尺度结构确定宏观尺度土壤特性:模型推导

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摘要

In this paper, we use homogenization to derive a set of macro-scale poro-elastic equations for soils composed of rigid solid particles, air-filled pore space and a poro-elastic mixed phase. We consider the derivation in the limit of large deformation and show that by solving representative problems on the micro-scale we can parametrize the macro-scale equations. To validate the homogenization procedure, we compare the predictions of the homogenized equations with those of the full equations for a range of different geometries and material properties. We show that the results differ by  ≲ 2% for all cases considered. The success of the homogenization scheme means that it can be used to determine the macro-scale poro-elastic properties of soils from the underlying structure. Hence, it will prove a valuable tool in both characterization and optimization.
机译:在本文中,我们使用均质化推导了由刚性固体颗粒,充气孔隙空间和孔隙弹性混合相组成的土壤的宏观孔隙弹性方程组。我们考虑了大变形极限的推导,并表明通过解决微观尺度上的代表性问题,我们可以对宏观尺度方程进行参数化。为了验证均质化过程,我们针对一系列不同的几何形状和材料特性,将均质化方程的预测与完整方程的预测进行了比较。我们显示,对于所有考虑的案例,结果相差≲2%。均质化方案的成功意味着它可用于从基础结构确定土壤的宏观孔隙弹性特性。因此,它将在表征和优化方面被证明是有价值的工具。

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