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Two-scale computational modelling of water flow in unsaturated soils containing irregular-shaped inclusions

机译:含异形夹杂物的非饱和土壤水流的两尺度计算模型

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摘要

The focus of this paper is two-dimensional computational modelling of water flow in unsaturated soils consisting of weakly conductive disconnected inclusions embedded in a highly conductive connected matrix. When the inclusions are small, a two-scale Richards’ equation-based model has been proposed in the literature taking the form of an equation with effective parameters governing the macroscopic flow coupled with a microscopic equation, defined at each point in the macroscopic domain, governing the flow in the inclusions. This paper is devoted to a number of advances in the numerical implementation of this model. Namely, by treating the micro-scale as a two-dimensional problem, our solution approach based on a control volume finite element method can be applied to irregular inclusion geometries, and, if necessary, modified to account for additional phenomena (e.g. imposing the macroscopic gradient on the micro-scale via a linear approximation of the macroscopic variable along the microscopic boundary). This is achieved with the help of an exponential integrator for advancing the solution in time. This time integration method completely avoids generation of the Jacobian matrix of the system and hence eases the computation when solving the two-scale model in a completely coupled manner. Numerical simulations are presented for a two-dimensional infiltration problem.
机译:本文的重点是对非饱和土壤中水流的二维计算建模,该模型由嵌入高导电连接基质中的弱导电不连续夹杂物组成。当夹杂物较小时,文献中已经提出了一种基于尺度的基于理查兹方程的两尺度模型,该方程的形式为具有有效参数的方程,该有效参数控制宏观流动,并结合了微观方程,该微观方程定义在宏观域的每个点上,控制内含物的流动。本文致力于该模型的数值实现方面的许多进展。也就是说,通过将微观尺度视为二维问题,我们基于控制体积有限元方法的求解方法可以应用于不规则的夹杂物几何形状,并在必要时进行修改以解决其他现象(例如施加宏观现象)通过沿着微观边界对宏观变量进行线性逼近,在微观尺度上实现最大梯度)。这需要借助指数积分器来及时解决该问题。这种时间积分方法完全避免了系统的雅可比矩阵的生成,因此在以完全耦合的方式求解两尺度模型时简化了计算。提出了二维渗透问题的数值模拟。

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    Carr E.J.; Turner I.W.;

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  • 年度 2014
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