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Comparing meshing approaches for groundwater modeling at a geometrically challenging mine siteVolker Clausnitzer, Fabien Cornaton, Peter SchätzlDHI-WASY
Robin DufourDHI Peru
Legacy layered meshing
© DHI #3
18 geological formations
85 numerical layers
10 million elements
5 million nodes
• 18 geological formations
• 85 numerical layers –
continuous, following the
faults
• 10 million elements
• 5 million nodes
Mesh Flexibility in 3D
© DHI
• Layered prism-based FE meshes
Excellent flexibility in 2D
Extruded to 3D
Vertical join faces restrict flexibility but simplify interactive model set-up once
mesh has been created
• Unstructured tetrahedral FE meshes
Excellent flexibility in 3D
Difficult to handle in interactive work
TetGen
© DHI
• Mesh generator for tetrahedral meshing of any 3D polyhedral domain
• Author: Hang Si (Weierstrass Institute for Applied Analysis and Stochastics,
WIAS Berlin)
tetgen.org
Embedded tetrahedral mesh
© DHI
• Strategy: Combine mesh types
Where possible, mesh with layered prisms
Where necessary, embed unstructured tetrahedral meshes
(artificial underground structures, inclined faults
karstic networks, pinch-outs, …)
Fully unstructured (tetrahedral) meshing
© DHI
• Takes spatial distribution of geologic units, 3D geometric description
of unit interfaces from dedicated geologic modelers
• 3D GeoModeller, GOCAD, (Leapfrog, MineSight, …)
• Geometric constraints passed to TetGen
• GUI-supported parameter assignment based on geologic spatial
information
Performance Comparison
© DHI
Layered Mesh Tetrahedral Mesh
Number of nodes
(Size of equation system)
2,816,304 195,628
SAMG Algebraic Multigrid Solver
Simulation time (seconds) 654.67 18.95
PARDISO Parallel Direct Solver
Simulation time (seconds) 1104.62 21.73
Performance Comparison
© DHI
Layered Mesh Tetrahedral Mesh
Number of nodes
(Size of equation system)
2,816,304 195,628
SAMG Algebraic Multigrid Solver
Simulation time (seconds) 654.67 18.95
Relative mass-balance error 2.0e-6 2.8e-8
PARDISO Parallel Direct Solver
Simulation time (seconds) 1104.62 21.73
Relative mass-balance error 1.6e-13 4.2e-14
Summary
© DHI
• Unstructured tetrahedral meshing can be
− combined with layered meshes or
− used for the entire domain
• Substantial reduction in mesh size for the same level of geologic
detail
• Direct solvers become applicable to new class of problems