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Fully homogenized model for immiscible incompressible two-phase flow through heterogeneous porous media with thin fractures

机译:用于不混溶的不可压缩两相流的完全均匀化模型   通过具有薄裂缝的非均质多孔介质

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摘要

In this paper we discuss a model describing global behavior of the two phaseincompressible flow in fractured porous media. The fractured media is regardedas a porous medium consisting of two superimposed continua, a connectedfracture system, which is assumed to be thin of order $\varepsilon\delta$, andan $\varepsilon$-periodic system of disjoint matrix blocks. We derive globalbehavior of the fractured media by passing to the limit as$\varepsilon\rightarrow 0$ and then as the relative fracture thickness$\delta\rightarrow 0$, taking into account that the permeability of the blocksis proportional to $(\varepsilon\delta)^2$, while permeability of the fracturesis of order one. The macroscopic model obtained is then a fully homogenizedmodel, i.e., where all the coefficients are calculated in terms of given dataand do not depend on the additional coupling or cell problems.
机译:在本文中,我们讨论描述描述多孔多孔介质中两相不可压缩流动的整体行为的模型。破裂介质被认为是由两个叠加的连续体组成的多孔介质,一个连接的断裂系统被假定为稀薄的$ \ varepsilon \ delta $阶,以及一个$ \ varepsilon $-不连续矩阵块的周期系统。考虑到块体的渗透率与$(\ varepsilon成比例),我们通过将极限介质传递为$ \ varepsilon \ rightarrow 0 $,然后将其作为相对裂缝厚度$ \ delta \ rightarrow 0 $,得出了裂缝介质的整体特性。 \ delta)^ 2 $,而一阶断裂的渗透率。然后,所获得的宏观模型是完全同质化的模型,即,其中所有系数都是根据给定的数据计算的,并且不取决于附加的耦合或单元问题。

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