Article ID Journal Published Year Pages File Type
4526493 Advances in Water Resources 2008 13 Pages PDF
Abstract

In this paper we extend to three-phase flow the nonequilibrium formalism proposed by Barenblatt and co-workers for two-phase porous media flow. The underlying idea is to include nonequilibrium effects by introducing a pair of effective water and gas saturations, which are linked to the actual saturations by a local evolution equation. We illustrate and analyze how nonequilibrium effects lead to qualitative and quantitative differences in the solution of the three-phase flow equations.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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