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Multiphase flow modeling in multiscale porous media: An open-source micro-continuum approach
Francisco J. Carrillo, Ian C. Bourg, Cyprien Soulaine

Multiphase flow modeling in multiscale porous media: An open-source micro-continuum approach

Science & Mathematics Published 2020 Verification Pending

Overview & Synopsis

A multiphase Darcy-Brinkman approach is proposed to simulate two-phase flow in hybrid systems containing both solid-free regions and porous matrices. This micro-continuum model is rooted in elementary physics and volume averaging principles, where a unique set of partial differential equations is used to represent flow in both regions and scales. The crux of the proposed model is that it tends asymptotically towards the Navier-Stokes volume-of-fluid approach in solid-free regions and towards the multiphase Darcy equations in porous regions. Unlike existing multiscale multiphase solvers, it can match analytical predictions of capillary, relative permeability, and gravitational effects at both the pore and Darcy scales. Through its open-source implementation, hybridPorousInterFoam, the proposed approach marks the extension of computational fluid dynamics (CFD) simulation packages into porous multiscale, multiphase systems. The versatility of the solver is illustrated using applications to two-phase flow in a fractured porous matrix and wave interaction with a porous coastal barrier.

Indexed from repository: HAL Open Science (hal.science)
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Document Information

Document Title Multiphase flow modeling in multiscale porous media: An open-source micro-continuum approach
Author / Organization Francisco J. Carrillo, Ian C. Bourg, Cyprien Soulaine
Subject & Discipline Multidisciplinary Academic Open Research
Categories Science & Mathematics
Publication Year 2020
License / Rights Open Access / Creative Commons
Resource Verification Listed PDF (Verification Pending)
Original Host Website HAL Open Science (hal.science)
File Format application/pdf (Portable Document Format)
Language EN
Catalog ID DOC-238179
Original Source Link Visit Source Page on hal.science »