A sharp-interface interpretation of a continuous density model for homogenization of gravity-driven flow in porous media

DOI10.1016/j.physd.2010.06.009zbMath1198.76110OpenAlexW1977979108WikidataQ57540918 ScholiaQ57540918MaRDI QIDQ602699

Daniel M. Anderson, Cass T. Miller, Richard M. McLaughlin

Publication date: 5 November 2010

Published in: Physica D (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.physd.2010.06.009

zbMATH Keywords

homogenizationsharp interfacediffuse interface

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Liquid-gas two-phase flows, bubbly flows (76T10) Homogenization applied to problems in fluid mechanics (76M50)

Related Items (2)

Homogenization of one-dimensional draining through heterogeneous porous media including higher-order approximations ⋮ Solving Nonlinear Parabolic Equations by a Strongly Implicit Finite Difference Scheme

Cites Work

• Modelling carbon dioxide sequestration in layered strata
• The effect of a fissure on storage in a porous medium
• The averaging of gravity currents in porous media
• Homogenization of linear and nonlinear transport equations
• DIFFUSE-INTERFACE METHODS IN FLUID MECHANICS
• Large scale front dynamics for turbulent reaction-diffusion equations with separated velocity scales
• A phase-field model with convection: sharp-inerface asymptotics.
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