SPE Symposium on Reservoir Simulation 1989
DOI: 10.2118/18412-ms
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Modeling Reservoir Geometry With Irregular Grids

Abstract: The widely used Cartesian coordinate grid has some disadvantages in the description of boundaries, faults and discontinuities. In addition, a five-point scheme can cause significant grid orientation effects. A ninepoint scheme reduces this effect but makes the treatment of boundaries and heterogeneities more difficult.Orthogonal curvilinear coordinate systems have improved the modeling of reservoir shape and flow geometry. Mathematically they are based on a coordinate transformation and discretization of the t… Show more

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Cited by 67 publications
(51 citation statements)
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“…Other gridding methods have been proposed with the express purpose of reducing GOE such as Pruess and Bodvarsson (1983) and Heinemann et al (1991). Currently, irregular grids are often suggested for handling GOE in the literature since they can seemingly reduce directionally preferred transport directions.…”
Section: Past Approaches To Alleviate Grid Orientation Effectsmentioning
confidence: 99%
“…Other gridding methods have been proposed with the express purpose of reducing GOE such as Pruess and Bodvarsson (1983) and Heinemann et al (1991). Currently, irregular grids are often suggested for handling GOE in the literature since they can seemingly reduce directionally preferred transport directions.…”
Section: Past Approaches To Alleviate Grid Orientation Effectsmentioning
confidence: 99%
“…In general a full tensor equation arises whenever the computational grid is non-aligned with the principal axes of the local tensor field. A full tensor can occur when representing cross bedding, modeling any anisotropic medium that is non-aligned with the computational grid [10], using non K-orthogonal [11,12] or unstructured grids and when upscaling rock properties from fine scale diagonal tensor simulation to the grid block scale [13]. Consequently, the standard diagonal tensor simulator will suffer from an inconsistent O(1) error in flux when applied to cases involving these major features.…”
Section: Introductionmentioning
confidence: 99%
“…Finite volume difference method (FVDM) is used in spatial discretization of the governing equations (Heinemann et al, 1989;Pruess and Moridis, 1999). The discretized grid blocks are arranged with the standard method described by .…”
Section: Governing Equationsmentioning
confidence: 99%