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U.S. Department of Energy
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A microscopic model of fluid flow in porous media

Conference ·
OSTI ID:6975432

A model to describe microscopic fluid flow in porous media is proposed. It offers the potential to predict relative permeability curves from microscopic rock and fluid properties. Conventional descriptions of fluid flow in porous media are based on Darcy's equations which require relative permeabilities and capillary pressure curves to be measured on macroscopic porous material. Prior to 1980, these macroscopically measured parameters could not be quantitatively related to microscopic rock properties. Recently, percolation theory has been used to relate macroscopic rock properties to relative permeabilities in the limit of capillary flow. Diffusion Limited Aggregation has been shown to simulate microscopic flow in the limit of infinite mobility ratios. The model described in this paper is a new approach to simulating flow through porous media on a microscopic scale. It is based on a variation of diffusion limited aggregation. The model can match coreflood average saturation profiles and production histories as predicted by Darcy's equations while generating saturation distributions resembling viscous fingering. The model can also simulate the limiting cases of infinite mobility ratio and zero flow rates as previously modeled by diffusion limited aggregation and percolation theory. With some simplifying assumptions, differential equations very similar to Darcy's equations can be derived from the microscopic interpretation of fluid behavior in porous media used in this model.

Research Organization:
Conoco Inc.
OSTI ID:
6975432
Report Number(s):
CONF-861080-
Country of Publication:
United States
Language:
English