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Comparing meshing approaches for groundwater modeling at a geometrically challenging mine site Volker Clausnitzer, Fabien Cornaton, Peter Schätzl DHI-WASY Robin Dufour DHI Peru
30

Clausnitzer at al comparing meshing approaches

Aug 10, 2015

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Page 1: Clausnitzer at al comparing meshing approaches

Comparing meshing approaches for groundwater modeling at a geometrically challenging mine siteVolker Clausnitzer, Fabien Cornaton, Peter SchätzlDHI-WASY

Robin DufourDHI Peru

Page 2: Clausnitzer at al comparing meshing approaches

Motivation

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Page 3: Clausnitzer at al comparing meshing approaches

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

Page 4: Clausnitzer at al comparing meshing approaches

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

Page 5: Clausnitzer at al comparing meshing approaches

3D element types

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Layered meshes

Penta- or hexahedrons with vertical quadrilateral join faces

Page 6: Clausnitzer at al comparing meshing approaches

3D element types

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Unstructured meshes / mesh parts

Tetrahedrons

Page 7: Clausnitzer at al comparing meshing approaches

3D element types

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Combined meshes

Pyramids connect layered and unstructured mesh portions

Page 8: Clausnitzer at al comparing meshing approaches

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

Page 9: Clausnitzer at al comparing meshing approaches

Tetrahedral meshing embedded in a layered

mesh

© DHI

Page 10: Clausnitzer at al comparing meshing approaches

Embedded tetrahedral mesh

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• 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, …)

Page 11: Clausnitzer at al comparing meshing approaches

Embedded tetrahedral mesh: Karstic network

© DHI

Page 12: Clausnitzer at al comparing meshing approaches

Embedded tetrahedral mesh: Karstic network

© DHI

Page 13: Clausnitzer at al comparing meshing approaches

Embedded tetrahedral mesh: Karstic network

© DHI

Page 14: Clausnitzer at al comparing meshing approaches

Fully unstructured tetrahedral meshing

© DHI

Page 15: Clausnitzer at al comparing meshing approaches

Legacy Approach

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3D GeoModeller geologic model

Layered-mesh FEFLOW model

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© DHI

Steady-state solution

22 layers; 5,380,760 pentahedral elements; 2,816,304 nodes

Page 17: Clausnitzer at al comparing meshing approaches

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

Page 18: Clausnitzer at al comparing meshing approaches

© DHI

Interfaces of geologic units

Page 19: Clausnitzer at al comparing meshing approaches

© DHI

Interfaces and geologic units

Page 20: Clausnitzer at al comparing meshing approaches

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Interfaces and geologic units

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© DHI

Tet-meshed geologic units

Page 22: Clausnitzer at al comparing meshing approaches

© DHI

Clipped tetrahedrons

Page 23: Clausnitzer at al comparing meshing approaches

© DHI

Full tetrahedral mesh

Page 24: Clausnitzer at al comparing meshing approaches

© DHI

Steady-state solution

861,685 tetrahedral elements; 195,628 nodes

Page 25: Clausnitzer at al comparing meshing approaches

Performance

© DHI

Page 26: Clausnitzer at al comparing meshing approaches

© DHI

6 cores

Page 27: Clausnitzer at al comparing meshing approaches

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

Page 28: Clausnitzer at al comparing meshing approaches

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

Page 29: Clausnitzer at al comparing meshing approaches

Summary

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• 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

Page 30: Clausnitzer at al comparing meshing approaches

Thank you

…and perhaps see you at FEFLOW 2015, September 21–25 in Berlin, Germany!

© DHI