从孔隙到岩心的升级:强毛细力和润湿性现象的影响

M. Hoffmann, J. P. D. Plessis
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引用次数: 0

摘要

在从孔隙到岩心的升级过程中,使用了不同的技术。本文介绍了体积平均法的一种新应用。基本发展遵循杜·普莱西斯(1988)提出的代表性单位细胞概念(RUC)。这个RUC概念被扩展到多相流。借助多孔介质的概念几何微观模型,推导了描述多相流的有效方程。由于流动过程的强非线性,方程中引入了非局部地形。在强毛细力和多孔介质内部不同润湿性条件下,对这些放大方程进行了分析。毛细力的存在强烈地改变了流动特性,并在平均方程中引入了非局部地形。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Upscaling from pore to core : effects of strong capillary forces and wettability phenomena
In the upscaling process from pore to core different techniques are being used. In this presentation a novel application of Volume Averaging is described. The basic development follows the representative unit cell concept (RUC) developed by du Plessis (1988). This RUC concept is extended to multiphase flow. With the aid of a conceptual geometrical micro-model of a porous medium effective equations are derived which describe multiphase flow. Due to the strong nonlinearity of the flow proces non-local terras are introduced into the equations. These upscaled equations are analyzed in the presence of strong capillary forces and different wettability conditions inside the porous medium. The presente of capillary forces modifies the flow behaviour strongly and introduces non-local terras in the averaged equations.
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