Macroscopic Equations of Motion for Two Phase Flow in Porous Media

Abstract

The established macroscopic equations of motion for two phase immiscible displacement in porous media are known to be physically incomplete because they do not contain the surface tension and surface areas governing capillary phenomena. Therefore a more general system of macroscopic equations is derived here which incorporates the spatiotemporal variation of interfacial energies. These equations are based on the theory of mixtures in macroscopic continuum mechanics. They include wetting phenomena through surface tensions instead of the traditional use of capillary pressure functions. Relative permeabilities can be identified in this approach which exhibit a complex dependence on the state variables. A capillary pressure function can be identified in equilibrium which shows the qualitative saturation dependence known from experiment. In addition the new equations allow to describe the spatiotemporal changes of residual saturations during immiscible displacement.

15 pages, Phys. Rev. E (1998), in print

References in corpus (2)

• Temporal Scaling of Interfaces Propagating in Porous Media
• Sedimentation and Flow Through Porous Media: Simulating Dynamically Coupled Discrete and Continuum Phases

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