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Reservoir transport equations by compositional approach
Authors:Sorab Panday  MYavuz Corapcioglu
Institution:(1) Department of Civil and Environmental Engineering, Washington State University, 99164-3001 Pullman, WA, USA
Abstract:The objective of this paper is to present an overview of the fundamental equations governing transport phenomena in compressible reservoirs. A general mathematical model is presented for important thermo-mechanical processes operative in a reservoir. Such a formulation includes equations governing multiphase fluid (gas-water-hydrocarbon) flow, energy transport, and reservoir skeleton deformation. The model allows phase changes due to gas solubility. Furthermore, Terzaghi's concept of effective stress and stress-strain relations are incorporated into the general model. The functional relations among various model parameters which cause the nonlinearity of the system of equations are explained within the context of reservoir engineering principles. Simplified equations and appropriate boundary conditions have also been presented for various cases. It has been demonstrated that various well-known equations such as Jacob, Terzaghi, Buckley-Leverett, Richards, solute transport, black-oil, and Biot equations are simplifications of the compositional model.Notation List B reservoir thickness - B agr formation volume factor of phase agr - Ci mass of component lsquoirsquo dissolved per total volume of solution - Cagr i mass fraction of component lsquoirsquo in phase agr - Cngragr heat capacity of phase lsquoagrrsquo at constant volume - Cpagr heat capacity of phase lsquoagrrsquo at constant pressure - Dagr i hydrodynamic dispersion coefficient of component lsquoirsquo in phase agr - DMTf thermal liquid diffusivity for fluid f - F = F(x, y, z, t) defines the boundary surface - fpagr fractional flow of phase agr - g gravitational acceleration - Hpagr enthalpy per unit mass of phase agr - Jpagr volumetric flux of phase agr - krf relative permeability to fluid f - k0 absolute permeability of the medium - Mpagr i mass of component lsquoirsquo in phase agr - n porosity - N rate of accretion - Pf pressure in fluid f - pcabeta capillary pressure between phases agr and beta=pagr-pbeta - Ri agrbeta rate of mass transfer of component lsquoirsquo from phase agr to phase beta - Ri sourceagr source rate of component lsquoirsquo within phase agr - Sagr saturation of phase agr - s gas solubility - T temperature - t time - U displacement vector - u velocity in the x-direction - v velocity in the y-direction - Vagr volume of phase agr - Vs velocity of soil solids - Wi body force in coordinate direction lsquoirsquo - x horizontal coordinate - z vertical coordinate Greek Letters agrp volumetric coefficient of compressibility - agrT volumetric coefficient of thermal expansion - deltaij Kronecker delta - epsi volumetric strain - lambdam thermal conductivity of the whole matrix - ugragr internal energy per unit mass of phase agr - gf suction head - rgragr density of phase agr - sgrij tensor of total stresses - sgrprimeij tensor of effective stresses - thetaagr volumetric content of phase agr - mgrf viscosity of fluid f
Keywords:Reservoir transport  heat and mass tranfer  macroscopic equations
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