Three-dimensional magnetotelluric modeling in a mixed space-wavenumber domain

Author:

Dai Shikun1,Zhao Dongdong2ORCID,Wang Shunguo3ORCID,Li Kun4,Jahandari Hormoz5

Affiliation:

1. Central South University, School of Geosciences and Info-physics, Changsha, China.

2. Guilin University of Electronic Technology, School of Electronic Engineering and Automation, Guilin, China.

3. Norwegian University of Science and Technology, Department of Electronic Systems, Trondheim, Norway. (corresponding author)

4. Southwest Petroleum University, School of Geoscience and Technology, Chengdu, China.

5. Memorial University of Newfoundland, Department of Earth Science, St. John’s, Canada.

Abstract

We have developed a new 3D magnetotelluric modeling scheme in a mixed space-wavenumber domain. The modeling scheme is based on using a 2D Fourier transform along two horizontal directions to solve a vector-scalar potential formula derived from Maxwell’s equations based on the primary-secondary potential separation. The derived 1D governing equations in a mixed space-wavenumber domain are solved by using the finite-element method (FEM) together with a chasing method, and then the 2D inverse Fourier transform is used to recover the final solution of the electromagnetic (EM) fields in the 3D spatial domain. An iterative scheme is applied to approximate the true solution by repeating the previous steps because the governing equations cannot be solved directly due to an unusual primary-secondary potential field separation used. Nevertheless, the new method is capable of reducing the memory requirement and computational time in the mixed domain, and the 1D governing equations are highly parallel among different wavenumbers. For each of the 1D equations, the two- or four-node Gaussian quadrature rule can be used in both horizontal directions for Gauss fast Fourier transform. It is worth mentioning that the linear matrix equation to be solved is a fixed bandwidth system, and the chasing method is more efficient and convenient than solvers with preconditioners for the 1D matrix equations. The reliability and efficiency of the newly proposed method are verified with three synthetic 3D models by comparisons with a classical integral equation solution, an adaptive FEM solution, and a nonadaptive FEM solution. The proposed algorithm will be used in electrical resistivity tomography and controlled-source EM methods in future studies.

Funder

Norges Forskningsråd

Natural Science Foundation of Guangxi Province

Natural Science Foundation of China

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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