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On Solving Groundwater Flow and Transport Models with Algebraic Multigrid Preconditioning.
1Regional Water Centre of Maghreb, LIMEN, Ecole Mohammadia d'Ingénieurs, Université Mohammed V de Rabat, B.P. 765, Agdal Rabat, Morocco.
Algebraic multigrid preconditioning significantly accelerates groundwater flow simulations. This advanced technique enhances computational efficiency for large geological models, enabling faster analysis of complex subsurface systems.
Area of Science:
- Geosciences
- Computational Hydrogeology
- Numerical Methods
Background:
- Large sparse linear systems are common in subsurface flow and transport modeling.
- Efficient solvers are crucial for handling complex geological models and reducing simulation time.
- Existing methods like MODFLOW's GMG solver have limitations in heterogeneous and anisotropic conditions.
Purpose of the Study:
- To implement and evaluate algebraic multigrid (AMG) preconditioning within the dual delineation approach for groundwater flow and transport.
- To compare the performance of AMG-based solvers against other iterative and direct solvers.
- To assess the scalability and efficiency of AMG for large-scale, complex geological models.
Main Methods:
- Implementation of AMG preconditioning for iterative solvers in the dual delineation framework.
- Comparison of AMG solvers with MODFLOW's GMG solver and direct sparse solvers.
- Testing on 2D and 3D benchmark problems with varying geological properties (homogeneous, heterogeneous, anisotropic).
Main Results:
- AMG preconditioning accelerated groundwater flow solutions by one to two orders of magnitude.
- AMG efficiency was maintained for 3D heterogeneous and anisotropic problems, outperforming MODFLOW's GMG.
- Direct sparse solvers were most efficient for pure advective transport simulations.
- The dual delineation approach with optimal solvers can process millions of grid blocks in seconds.
Conclusions:
- AMG preconditioning is a highly effective technique for accelerating groundwater flow simulations in large, complex geological models.
- The choice of solver (AMG vs. direct) depends on the specific transport processes (e.g., advection-dominated vs. advection-dispersion).
- This approach enables routine application to large geological models, significantly reducing computational time.
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