An efficient multigrid solver based on a four-color cell-block Gauss-Seidel smoother for 3D magnetotelluric forward modeling

Author:

Guo Rongwen1ORCID,Wang Yongfei1ORCID,Egbert Gary D.2ORCID,Liu Jianxin1,Liu Rong3ORCID,Pan Kejia4ORCID,Li Jian1ORCID,Chen Hang5ORCID

Affiliation:

1. Central South University, School of Geosciences and Info-Physics, Changsha 410083, China; Central South University, Laboratory of Non-ferrous Resources and Geological Hazard Detection, Changsha 410083, China; and Central South University, Ministry of Education, Key Laboratory of Metallogenic Prediction of Nonferrous Metals, Changsha 410083, China.

2. Oregon State University, School of Earth, Ocean, and Atmospheric Sciences, Corvallis, Oregon 97331, USA.

3. Central South University, School of Geosciences and Info-Physics, Changsha 410083, China; Central South University, Laboratory of Non-ferrous Resources and Geological Hazard Detection, Changsha 410083, China; and Central South University, Ministry of Education, Key Laboratory of Metallogenic Prediction of Nonferrous Metals, Changsha 410083, China. (corresponding author)

4. Central South University, School of Mathematics and Statistics, HNP-LAMA, Changsha 410083, China.

5. Boise State University, Department of Geosciences, Boise, Idaho 83725, USA.

Abstract

Practical application of 3D magnetotelluric inversion requires efficient forward modeling of electromagnetic (EM) fields in the earth. To resolve realistic 3D structures, large computational domains and extremely large linear systems of equations are required. The iterative solvers, which are almost exclusively used to solve these systems, can be inefficient due to the abundant null space of the curl-curl operator. Multigrid (MG) solvers are considered a potentially efficient technique for solving such problems. However, due to the abundant null solution space and existence of the air layer, MG solvers can still converge slowly or even diverge. We have developed an efficient MG solver for finite-difference frequency-domain EM solution. In this algorithm, the excellent smoothing property of an efficient four-color cell-block Gauss-Seidel (GS) is exploited to remove the short-range errors effectively, and the interpolation and prolongation operators are used to handle the long-range errors. They work as a whole to speed the convergence of our algorithm remarkably. Because all of the nodes for the four-color cell-block GS are grouped into four colors and the edge components attached to different nodes in each color are completely decoupled, this can be used to develop a highly vectorized or parallelized algorithm. Another important property is that our algorithm is locally current divergence free, effectively eliminating spurious solutions in the null space of the curl-curl operator. The accuracy and efficiency of the algorithm are verified by comparing the numerical solutions obtained with our MG solver to those from the biconjugate gradient stabilized solver with different preconditioners based on synthetic models and a model from 3D inversion. Comparisons, in terms of iteration number and computational time, indicate that our algorithm is extremely stable and efficient relative to the other solvers. Our MG algorithm will be suitable for massively parallel computing as well.

Funder

National Natural Science Foundation of China

Guangxi Natural Science Foundation

Innovation-driven Plan from Hunan province

Hunan Natural Science Foundation

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Cited by 26 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Fast 3D magnetotelluric modelling using Yee's scheme and extrapolation multigrid solver;International Workshop on Gravity, Electrical & Magnetic Methods and Their Applications, Shenzhen, China, May 19–22, 2024;2024-08-23

2. An Edge-based cascadic multigrid method for $$H(\textbf{curl})$$ problems;Numerical Algorithms;2024-08-15

3. Natural source electromagnetic survey for geothermal application in industrial area with strong electromagnetic noise;Frontiers in Energy Research;2024-02-12

4. Three-Dimensional Magnetotelluric Forward Modeling Through Deep Learning;IEEE Transactions on Geoscience and Remote Sensing;2024

5. Three-Dimensional Unstructured Finite Element Modeling of Magnetotelluric Problems Allowing for Continuous Variation of Conductivity in Each Block;IEEE Transactions on Geoscience and Remote Sensing;2024

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