Abstract
More sophisticated discretization methods than the traditional control-volume finite-difference methods, have been proposed by Aavatsmark et al. in recent papers for solving the mass balance equations for porous media flow. These methods are based on a local representation of fluxes across cell-edges of control volumes (CVs). This paper will focus on mathematical properties of the discrete operator that arises when an elliptic term of the form −∇⋅(K∇p) is discretized based on these discretization principles.
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Eigestad, G., Aavatsmark, I. & Espedal, M. Symmetry and M-Matrix Issues for the O-Method on an Unstructured Grid. Computational Geosciences 6, 381–404 (2002). https://doi.org/10.1023/A:1021239130404
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DOI: https://doi.org/10.1023/A:1021239130404