3D edge-based and nodal finite element modeling of magnetotelluric in general anisotropic media
Research on the magnetotelluric (MT) forward modeling response in anisotropic media has been important since the discovery of anisotropic electric fields in the Earth's interior. In this study, we presented an edge-based and nodal finite-element method (FEM) for three-dimensional (3D) MT forwar...
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| Published in | Computers & geosciences Vol. 158; p. 104975 |
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| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier Ltd
01.01.2022
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0098-3004 1873-7803 |
| DOI | 10.1016/j.cageo.2021.104975 |
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| Abstract | Research on the magnetotelluric (MT) forward modeling response in anisotropic media has been important since the discovery of anisotropic electric fields in the Earth's interior. In this study, we presented an edge-based and nodal finite-element method (FEM) for three-dimensional (3D) MT forward modeling problems in general anisotropic media. Partial differential equations are derived using the Coulomb-gauged approach from Maxwell's equation and discretized by the edge-based and nodal FEM. The magnetic vector A was discretized by an edge-based FEM and the electric scalar ψ was discretized by nodal FEM. The computational domain was refined using a hexahedral mesh. The Galerkin variant of the weighted residuals method was used to obtain a sparse linear system for magnetic vector A and electric scalar ψ. Three models were designed to validate and analyze our forward modeling code by comparing it with a one-dimensional analytical solution and with the results from codes developed by other scholars. A direct solver and iterative solvers with preprocessors were used to evaluate the performance of our code. Numerical experiments showed that our forward modeling code is accurate and robust and converges faster. In addition, the stiffness matrix assembled by our algorithm was smaller than that assembled by the nodal FEM, which further demonstrates the advantage of our algorithm in terms of computational memory.
•3D MT anisotropy forward code using edge-based and nodal FEM is presented.•It solves the low frequency convergence problem of direct EM method.•The algorithm has good robustness in wide frequency range.•The non-zero elements of stiffness matrix are reduced and the cost is saved. |
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| AbstractList | Research on the magnetotelluric (MT) forward modeling response in anisotropic media has been important since the discovery of anisotropic electric fields in the Earth's interior. In this study, we presented an edge-based and nodal finite-element method (FEM) for three-dimensional (3D) MT forward modeling problems in general anisotropic media. Partial differential equations are derived using the Coulomb-gauged approach from Maxwell's equation and discretized by the edge-based and nodal FEM. The magnetic vector A was discretized by an edge-based FEM and the electric scalar ψ was discretized by nodal FEM. The computational domain was refined using a hexahedral mesh. The Galerkin variant of the weighted residuals method was used to obtain a sparse linear system for magnetic vector A and electric scalar ψ. Three models were designed to validate and analyze our forward modeling code by comparing it with a one-dimensional analytical solution and with the results from codes developed by other scholars. A direct solver and iterative solvers with preprocessors were used to evaluate the performance of our code. Numerical experiments showed that our forward modeling code is accurate and robust and converges faster. In addition, the stiffness matrix assembled by our algorithm was smaller than that assembled by the nodal FEM, which further demonstrates the advantage of our algorithm in terms of computational memory. Research on the magnetotelluric (MT) forward modeling response in anisotropic media has been important since the discovery of anisotropic electric fields in the Earth's interior. In this study, we presented an edge-based and nodal finite-element method (FEM) for three-dimensional (3D) MT forward modeling problems in general anisotropic media. Partial differential equations are derived using the Coulomb-gauged approach from Maxwell's equation and discretized by the edge-based and nodal FEM. The magnetic vector A was discretized by an edge-based FEM and the electric scalar ψ was discretized by nodal FEM. The computational domain was refined using a hexahedral mesh. The Galerkin variant of the weighted residuals method was used to obtain a sparse linear system for magnetic vector A and electric scalar ψ. Three models were designed to validate and analyze our forward modeling code by comparing it with a one-dimensional analytical solution and with the results from codes developed by other scholars. A direct solver and iterative solvers with preprocessors were used to evaluate the performance of our code. Numerical experiments showed that our forward modeling code is accurate and robust and converges faster. In addition, the stiffness matrix assembled by our algorithm was smaller than that assembled by the nodal FEM, which further demonstrates the advantage of our algorithm in terms of computational memory. •3D MT anisotropy forward code using edge-based and nodal FEM is presented.•It solves the low frequency convergence problem of direct EM method.•The algorithm has good robustness in wide frequency range.•The non-zero elements of stiffness matrix are reduced and the cost is saved. |
| ArticleNumber | 104975 |
| Author | Zhou, Junjun Bai, Ningbo Hu, Xiangyun Han, Bo |
| Author_xml | – sequence: 1 givenname: Ningbo surname: Bai fullname: Bai, Ningbo organization: China University of Geosciences, Key Laboratory of Geological Survey and Evaluation of Ministry of Education, Wuhan, China – sequence: 2 givenname: Junjun surname: Zhou fullname: Zhou, Junjun organization: China University of Geosciences, Institute of Geophysics and Geomatics, Wuhan, China – sequence: 3 givenname: Xiangyun surname: Hu fullname: Hu, Xiangyun email: xyhu@cug.edu.cn organization: China University of Geosciences, Key Laboratory of Geological Survey and Evaluation of Ministry of Education, Wuhan, China – sequence: 4 givenname: Bo surname: Han fullname: Han, Bo organization: China University of Geosciences, Institute of Geological Survey, Wuhan, 430074, China |
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| Keywords | Edge-based finite element method Nodal finite element method Magnetotelluric Coulomb-gauged approach Forward modeling |
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| SubjectTerms | algorithms anisotropy Coulomb-gauged approach Edge-based finite element method finite element analysis Forward modeling magnetism Magnetotelluric memory Nodal finite element method |
| Title | 3D edge-based and nodal finite element modeling of magnetotelluric in general anisotropic media |
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