Abstract

Two types of approximation schemes are established for incompressible miscible displacements in porous media. First, standard mixed finite element method is used to approximate the velocity and pressure. And then parallel non-overlapping domain decomposition methods combined with the characteristics method are presented for the concentration. These methods use the characteristic method to handle the material derivative term of the concentration equation in the subdomains and explicit flux calculations on the interdomain boundaries by integral mean method or extrapolation method to predict the inner-boundary conditions. Thus, the velocity and pressure can be approximated simultaneously, and the parallelism can be achieved for the concentration equation. The explicit nature of the flux prediction induces a time step limitation that is necessary to preserve stability. These schemes hold the advantages of nonoverlapping domain decomposition methods and the characteristic method. Optimal error estimates in L2-norm are derived for these two schemes, respectively.

Highlights

  • The two-phase fluid displacements in porous media is one of the most important basic problems in the oil reservoir numerical simulation

  • We have presented parallel Galerkin domain decomposition procedures for parabolic equation [18,19,20]

  • We adopt some auxiliary lemmas about the finite element spaces, which will be used

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Summary

Introduction

The two-phase fluid displacements in porous media is one of the most important basic problems in the oil reservoir numerical simulation. The pressure equation is elliptic and handled by standard mixed finite element method, which has been proven to be an effective numerical method for solving fluid problems. We have presented parallel Galerkin domain decomposition procedures for parabolic equation [18,19,20]. The main purpose is to use parallel Galerkin domain decomposition procedures in [18] combined with the characteristic method for the concentration equation of incompressible miscible displacements in porous media. These schemes hold the advantages of non-overlapping domain decomposition methods, and hold the advantages of the characteristic method

Formulation of the Methods
Auxiliary Lemmas
A Priori Error Estimates in L2-Norm
Extensions
Numerical Experiments
Full Text
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