Computing brine transport in porous media with an adaptive-grid method:

Abstract: "An adaptive-grid finite-difference method is applied to a model for non-isothermal, coupled flow and transport of brine in porous media. In the vicinity of rock salt formations the salt concentration in the fluid becomes large, giving rise to disparate scales in the salt concentratio...

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Bibliographische Detailangaben
Hauptverfasser: Trompert, Ron A. (VerfasserIn), Verwer, Jan (VerfasserIn), Blom, J. G. (VerfasserIn)
Format: Buch
Sprache:English
Veröffentlicht: Amsterdam 1992
Schriftenreihe:Centrum voor Wiskunde en Informatica <Amsterdam> / Afdeling Numerieke Wiskunde: Report NM 1992,1
Schlagworte:
Zusammenfassung:Abstract: "An adaptive-grid finite-difference method is applied to a model for non-isothermal, coupled flow and transport of brine in porous media. In the vicinity of rock salt formations the salt concentration in the fluid becomes large, giving rise to disparate scales in the salt concentration profiles. A typical situation one encounters is that of a sharp fresh-salt water interface that moves in time. In such situations adaptive-grid methods are more effective than standard fixed- grid methods, since they refine the space grid locally and hence provide for substantial reduction in number of grid points, memory use and CPU time
The adaptive-grid method of this paper is a static, local- uniform-grid-refinement method. Its main feature is that it integrates on nested sequences of locally uniformly refined cartesian space grids, which are automatically adjusted in time to follow rapid spatial transitions. Variable time steps are used to cope with rapid temporal transitions, including a fast march to possible steady-state solutions. For time stepping the implicit, second-order BDF scheme is used. Two specific example problems are numerically illustrated. The main physical properties involved here are advection and dispersion and in case of dominant advection sharp fresh-salt water interfaces arise.
Beschreibung:24 S.

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