1997
DOI: 10.1006/jcph.1997.5779
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Adaptive Mesh Refinement and Multilevel Iteration for Flow in Porous Media

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Cited by 76 publications
(55 citation statements)
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“…These applications include single-phase flow in heterogeneous porous media (Cao and Kitanidis, 1999), unsaturated flow (Li et al, 2007), multispecies reactive transport (Wolfsberg and Freyberg, 1994), coupled density-dependent flow and transport (Trompert, 1993;van Esch, 2002), and multiphase flow and multicomponent transport (Hornung and Trangenstein, 1997;Pau et al, 2008). All these applications are limited to capability demonstration.…”
Section: Actual Phase I Accomplishmentsmentioning
confidence: 99%
“…These applications include single-phase flow in heterogeneous porous media (Cao and Kitanidis, 1999), unsaturated flow (Li et al, 2007), multispecies reactive transport (Wolfsberg and Freyberg, 1994), coupled density-dependent flow and transport (Trompert, 1993;van Esch, 2002), and multiphase flow and multicomponent transport (Hornung and Trangenstein, 1997;Pau et al, 2008). All these applications are limited to capability demonstration.…”
Section: Actual Phase I Accomplishmentsmentioning
confidence: 99%
“…Structured grids with patches of refinement have been used for time dependent and time independent problems in applications such as fluid flow [3], [8], [10], [12], electromagnetics [11], [14], [17], [21], and plasma physics [6], [18]. The missing values of the solution at the interfaces are determined by interpolation.…”
Section: Introductionmentioning
confidence: 99%
“…Our approach is similar to the approach introduced by Hornung & Trangenstein (1997) and to the approach discussed by Propp (1998). In these approaches, the solution is represented on a hierarchical sequence of nested grids with successively finer spacing in both time and space.…”
Section: Introductionmentioning
confidence: 99%
“…The method presented here uses subcycling in time so that all levels are advanced at the same Courant-Friedrichs-Levy (CFL) number, thus reducing the numerical dissipation of the explicit upwind advection scheme used to advance the solution. The major difference between the approach adopted here and that of Hornung & Trangenstein (1997) is that the current method does not require a global, multilevel pressure solve at each fine-grid time step. Instead, when advancing a given level, we solve the pressure on that level only with boundary conditions obtained from the coarser levels.…”
Section: Introductionmentioning
confidence: 99%
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