A model for two-phase flow in porous media including fluid-fluid interfacial area
Abstract
We present a new numerical model for macroscale two-phase flow in porous media which is based on a physically consistent theory of multi-phase flow. The standard approach for modeling the flow of two fluid phases in a porous medium consists of a continuity equation for each phase, an extended form of Darcy's law as well as constitutive relationships for relative permeability and capillary pressure. This approach is known to have a number of important shortcomings and, in particular, it does not account for the presence and role of fluid-fluid interfaces. The alternative is to use an extended model, which is founded on thermodynamic principles and is physically consistent. In addition to the standard equations, the model uses a balance equation for specific interfacial area. The constitutive relationship for capillary pressure involves not only saturation, but also specific interfacial area. We present results of a numerical modeling study based on this extended model. We show that the extended model can capture additional physical processes compared to the standard model, such as hysteresis.
- Publication:
-
Water Resources Research
- Pub Date:
- August 2008
- DOI:
- 10.1029/2007WR006721
- Bibcode:
- 2008WRR....44.8439N
- Keywords:
-
- Hydrology: Groundwater hydraulics;
- Hydrology: Modeling;
- Hydrology: Computational hydrology;
- Hydrology: Groundwater transport;
- Two-phase flow;
- porous media;
- interfacial area