1985
DOI: 10.1016/0309-1708(85)90062-4
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Numerical modelling of multiphase flow in porous media

Abstract: The simultaneous flow of immiscible fluids in porous media occurs in a wide variety of applications. The equations governing these flows are inherently nonlinear, and the geometries and material properties characterizing many problems in petroleum and groundwater engineering can be quite irregular. As a result, numerical simulation often offers the only viable approach to the mathematical modeling of multiphase flows. This paper provides an overview of the types of models that are used in this field and highli… Show more

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Cited by 58 publications
(31 citation statements)
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“…Therefore, the governing equations need to account for the presence of all phases [17][18][19]. In these equations, two additional transport parameters are present-relative permeability and a capillary pressure function that includes the interaction parameters between phases [20].…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, the governing equations need to account for the presence of all phases [17][18][19]. In these equations, two additional transport parameters are present-relative permeability and a capillary pressure function that includes the interaction parameters between phases [20].…”
Section: Introductionmentioning
confidence: 99%
“…[18][19][20] For chemically reacting fluid phases, terms accounting for the interfacial transfer rate of mass I α and momentum α M must be added as sources on the right-side of Equations (1) and (2), respectively. 7 On the other hand, if heat transfer effects are important, Equations (1) and (2) must be complemented with a transport equation for the internal energy or enthalpy. However, a simplification of the above model can be obtained in the framework of continuum mixture theory.…”
Section: Fluid Flow Equationsmentioning
confidence: 99%
“…[2][3][4][5][6] Numerical models aimed at solving oil extraction problems involve mainly the solution of the nonlinear fluid equations for multiphase and multicomponent flows through a heterogeneous medium (porous rock). 3,[7][8][9] When describing the flow at a microscopic level (or pore scale), the Navier-Stokes equations coupled to the mass conservation law for multiphase flow must be solved, while at a macroscopic level Darcy´s law is employed in place of the Navier-Stokes equations to describe the flow behavior. At the microscopic scale, the fluid motion is mainly controlled by the effects of interfacial tension, viscosity, and capillary pressures.…”
Section: Introductionmentioning
confidence: 99%
“…In order to ensure convergence of a finite d•erence solution to the co•ect saturation or concentration distribution, sufficient dissipation, either physical or numefic•, must be present to satisfy the entropy (E) condition [Allen, 1985]. …”
Section: (P /3xa/i)[n+ 1/2ki +-1/2• •/ I • •/2mentioning
confidence: 99%