Abstract

ABSTRACT In studying the flow of foam in unconsolidated porous media Khatib et al have shown that the destruction of foam lamellae depends on the gas/surfactant solution flowrates, fluid mobilities, and rock capillary pressure. This paper examines this flow regime, which we call the coalescence regime, in more detail. We have found that all published data referring to foam flow in consolidated media are consistent with a generalisation of Khatib's model. This new model is described in this paper. Two and three phase steady-state foam mobility models have been developed which exploit the dominant role of the foam coalescence mechanism. These models are based on published data for foam flow. The mobility models are then used in a finite difference, three phase, multi-component simulator. The simulator is applied to show that it can reproduce the generic transient foam behaviour observed in core floods. Calculations are then used to examine some of the important issues that have to be considered when designing field applications of foam flooding.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.