Effective interface conditions for the forced infiltration of a viscous fluid into a porous medium using homogenization

It is generally accepted that the effective velocity of a viscous flow over a porous bed satisfies the Beavers-Joseph slip law. To the contrary, in the case of a forced infiltration of a viscous fluid into a porous medium the interface law has been a subject of controversy. In this paper, we prove r...

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Bibliographic Details
Main Authors: Carraro, Thomas (Author) , Goll, Christian (Author) , Marciniak-Czochra, Anna (Author) , Mikelić, Andro (Author)
Format: Article (Journal)
Language:English
Published: 2015
In: Computer methods in applied mechanics and engineering
Year: 2015, Volume: 292, Pages: 195-220
ISSN:1879-2138
DOI:10.1016/j.cma.2014.10.050
Online Access:Verlag, Volltext: http://dx.doi.org/10.1016/j.cma.2014.10.050
Verlag, Volltext: http://www.sciencedirect.com/science/article/pii/S0045782514004204
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Author Notes:Thomas Carraro, Christian Goll, Anna Marciniak-Czochra, Andro Mikelić
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Summary:It is generally accepted that the effective velocity of a viscous flow over a porous bed satisfies the Beavers-Joseph slip law. To the contrary, in the case of a forced infiltration of a viscous fluid into a porous medium the interface law has been a subject of controversy. In this paper, we prove rigorously that the effective interface conditions are: (i) the continuity of the normal effective velocities; (ii) zero Darcy’s pressure and (iii) a given slip velocity. The effective tangential slip velocity is calculated from the boundary layer and depends only on the pore geometry. In the next order of approximation, we derive a pressure slip law. An independent confirmation of the analytical results using direct numerical simulation of the flow at the microscopic level is given, as well.
Item Description:Available online 13 November 2014
Gesehen am 08.08.2017
Physical Description:Online Resource
ISSN:1879-2138
DOI:10.1016/j.cma.2014.10.050