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Multiphase flow through multilayers of thin porous media: General balance equations and constitutive relationships for a solid-gas-liquid three-phase system

机译:流经多层薄多孔介质的多相流:固-气-液三相系统的一般平衡方程和本构关系

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摘要

In this work, we propose a new approach to modeling multiphase flow and solute transport through a stack of thin porous layers. Currently, numerical simulation of thin layers involves discretization across the layer thickness. In our new approach, thin porous layers are treated as a bunch of two-dimensional (2D) interacting continua. Macroscale balance laws are formulated in terms of thickness-averaged material properties. A number of exchange terms are employed to account for exchanges of mass, momentum, energy, and entropy between two neighboring layers. The entropy inequality is then exploited for obtaining constitutive equations to close the problem under study. As an example, simplified governing equations are derived for a system of air-water flow and heat transfer through two thin porous layers. In comparison to previous macroscale models, our model possesses the following distinctive advantages: (1) it is rigorous thermodynamics-based model; (2) it is formulated in terms of layer-thickness-averaged material properties which are usually easily measurable; and (3) it reduces 3D modeling to 2D leading to a very significant reduction of computational efforts.
机译:在这项工作中,我们提出了一种新的方法来模拟通过一叠薄多孔层的多相流和溶质传输。当前,薄层的数值模拟涉及整个层厚度的离散化。在我们的新方法中,薄多孔层被视为一堆二维(2D)相互作用的连续体。宏观平衡定律是根据厚度平均材料特性制定的。许多交换项被用来解释两个相邻层之间的质量,动量,能量和熵的交换。然后利用熵不等式获得本构方程,以解决正在研究的问题。例如,针对通过两个薄多孔层的空气-水流和热传递系统,导出了简化的控制方程。与以前的宏观模型相比,我们的模型具有以下显着优势:(1)它是基于热力学的严格模型; (2)它是根据通常易于测量的平均层厚度材料特性来制定的; (3)将3D建模简化为2D,从而大大减少了计算量。

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