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Two-fluid mathematical model for compressible flow in fractured porous media

机译:裂隙多孔介质中可压缩流动的双流体数学模型

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A three-dimensional isothermal transient compressible two phase flow of liquid and gas in a low permeability fractured porous media model has been developed from the general mass and momentum balances using volume averaging techniques. The emphasis of the paper is on the available analytical and semi-empirical correlations and closure relations. The interfacial mass and momentum transfer terms in the averaged formulation are explained. The assumptions used in the model's formulation are that a condition of capillary equilibrium exists throughout the media, momentum transfer between mobile fluid phases is negligible in the porous media and exists in the fracture, and fluid phase change has been neglected. The pore size distribution of the studied porous media was represented by three mean pore diameters: liquid pore network, gas pore network, and fractures. An average pore diameter and length for each network were determined using the gamma distribution function. The model was validated and solved for a hypothetical porous media and fractured domain.
机译:利用体积平均技术,根据一般的质量和动量平衡,开发了低渗透压裂多孔介质模型中液体和气体的三维等温瞬态可压缩两相流。本文的重点是可用的分析和半经验相关性和闭合关系。解释了平均配方中的界面质量和动量传递项。模型公式中使用的假设是,在整个介质中都存在毛细管平衡的条件,在多孔介质中流动相之间的动量转移可忽略不计,而在裂缝中则存在,流体相的变化已被忽略。研究的多孔介质的孔径分布用三个平均孔径表示:液体孔网,气体孔网和裂缝。使用γ分布函数确定每个网络的平均孔径和长度。对假设的多孔介质和裂缝域进行了模型验证和求解。

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