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Determination of permeability tensors for two-phase flow in homogeneous porous media: Theory
Authors:Didier Lasseux  Michel Quintard  Stephen Whitaker
Institution:(1) L.E.P.T.-ENSAM (UA CNRS), Esplanade des Arts et Métiers, 33405 Talence cedex, France;(2) Department of Chemical Engineering and Material Science, University of California at Davis, 95616 Davis, CA, USA
Abstract:In this paper we continue previous studies of the closure problem for two-phase flow in homogeneous porous media, and we show how the closure problem can be transformed to a pair of Stokes-like boundary-value problems in terms of lsquopressuresrsquo that have units of length and lsquovelocitiesrsquo that have units of length squared. These are essentially geometrical boundary value problems that are used to calculate the four permeability tensors that appear in the volume averaged Stokes' equations. To determine the geometry associated with the closure problem, one needs to solve the physical problem; however, the closure problem can be solved using the same algorithm used to solve the physical problem, thus the entire procedure can be accomplished with a single numerical code.Nomenclature aagrkappa a vector that maps mgragrlangVkapparangkappa onto 
$$\tilde p_\alpha  $$
, m-1. - A agrkappa a tensor that maps langVkapparangkappa onto 
$$\tilde v_\alpha  $$
. - A agrkappa area of the agr-kappa interface contained within the macroscopic region, m2. - A agrescr area of the agr-phase entrances and exits contained within the macroscopic region, m2. - A agrkappa area of the agr-kappa interface contained within the averaging volume, m2. - A agrescr area of the agr-phase entrances and exits contained within the averaging volume, m2. - Bo Bond number (= (=(rgrbetargrgamma)gell2/sgr). - Ca capillary number (= mgrlangvrang/sgr). - g gravitational acceleration, m/s2. - H mean curvature, m-1. - I unit tensor. - Kgr agr permeability tensor for the agr-phase, m2. - Kgr agrkappa viscous drag tensor that maps langVkapparang onto langVagrrang. - Kgr agragr * dominant permeability tensor that maps 
$$\left( {\frac{{\nabla \langle p_\alpha  \rangle ^\alpha   - \rho _\alpha  g}}{{\mu _\alpha  }}} \right)c$$
onto langv agrrang, m2. - Kgr agrkappa * coupling permeability tensor that maps 
$$\left( {\frac{{\nabla \langle p_\kappa  \rangle ^\kappa   - \rho _\kappa  g}}{{\mu _\kappa  }}} \right)$$
onto langv agrrang, m2. - ellagr characteristic length scale for the agr-phase, m. - l characteristic length scale representing both ellbeta and ellgamma, m. - L characteristic length scale for volume averaged quantities, m. - n agrkappa unit normal vector directed from the agr-phase toward the kappa-phase. - n beta unit normal vector representing both n betasgr and n betagamma. - n gamma unit normal vector representing both n gammasgr and n gammabeta. - P agr pressure in the agr-phase, N/m2. - langp agrrang superficial average pressure in the agr-phase, N/m2. - langp agrrangagr intrinsic average pressure in the agr-phase, N/m2. - 
$$\tilde p_\alpha  $$
p agrlangp agrrangagr, spatial deviation pressure for the agr-phase, N/m2. - r 0 radius of the averaging volume, m. - r position vector, m. - t time, s. - v agr fluid velocity in the agr-phase, m/s. - langv agrrang superficial average velocity in the agr-phase, m/s. - langv agrrangagr intrinsic average velocity in the agr-phase, m/s. - 
$$\tilde v_\alpha  $$
v agrlangv agrrangagr, spatial deviation velocity in the agr-phase, m/s. - V agr volume of the agr-phase contained within the averaging volmue, m3. - ngr averaging volume, m3. Greek Symbols epsiagr V agr/ngr, volume fraction of the agr-phase. - mgragr viscosity of the agr-phase, Ns/m2. - rgragr density of the agr-phase, kg/m3. - sgr surface tension, N/m. - tauagr mgr(nablav agr+nablav agr T ), viscous stress tensor for the agr-phase, N/m2.
Keywords:homogeneous porous media  two-phase flow  volume averaging  permeability tensors
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