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 inComputers & geosciences Vol. 158; p. 104975
Main Authors Bai, Ningbo, Zhou, Junjun, Hu, Xiangyun, Han, Bo
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.01.2022
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ISSN0098-3004
1873-7803
DOI10.1016/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.
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
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  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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Snippet Research on the magnetotelluric (MT) forward modeling response in anisotropic media has been important since the discovery of anisotropic electric fields in...
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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
URI https://dx.doi.org/10.1016/j.cageo.2021.104975
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