2014
DOI: 10.1186/bf03351574
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Domain decomposition for 3D electromagnetic modeling

Abstract: Using the staggered grid full domain 3D modeling schemes of various accuracies have been developed. This study focuses on the second order finite difference method with the 13-point rule for meshes extending into the air. Tests with Krylov space iterative solvers indicate that the restarted Bi-CG Stablised method offers the best convergence for our problems. Because the air and the conductive earth have distinctive physical properties which greatly broaden the spectra of the whole matrix system, the whole mesh… Show more

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Cited by 6 publications
(11 citation statements)
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“…The coordinate relationship between master cell and slave cell can be described as Eqn. (7), and the differential relationship between master cell and slave cell can be described as Eqn. (8).…”
Section: Finite Element Methodsmentioning
confidence: 99%
“…The coordinate relationship between master cell and slave cell can be described as Eqn. (7), and the differential relationship between master cell and slave cell can be described as Eqn. (8).…”
Section: Finite Element Methodsmentioning
confidence: 99%
“…Xiong (1999) demonstrates an overlapping approach for 3D controlledsource problems using finite-difference methods. Zyserman and Santos (2000) apply a nonoverlapping approach to magnetotelluric (MT) problems using nodal-based shape functions and structured elements (rectangular cuboids).…”
Section: Introductionmentioning
confidence: 99%
“…However, the convergence rate of this iterative procedure is a serious issue. To obtain accurate and trustworthy results, large numbers of iterations are normally required, which seriously impairs performance (Xiong, 1999). For approaches using nonoverlapping subdomains, abutting subdomains only share common internal surfaces (Butrylo et al, 2004).…”
Section: Introductionmentioning
confidence: 99%
“…In many problems, when the model domain becomes very large, particularly in 3‐D problems, solving the system of equations with the direct method is impractical due to the large memory requirement (see Ben‐Hadj‐Ali et al 2008 for 3‐D frequency‐domain full‐waveform tomography; Streich 2009 for 3‐D MT). Instead, the system is solved using iterative solvers such as the Bi‐Conjugate Gradient method (Smith 1996; Xiong 1999), Quasi Minimum Residual (Siripunvaraporn et al 2002), Preconditioned Conjugate Gradient (PCG) (Siripunvaraporn & Egbert 2000), Minimum Residual Method (Mackie et al 1994). In many practical MT cases, the electrical resistivity model can be geologically complicated resulting in a large condition number and hence a very long computational time when used repeatedly inside the inversion (Patro & Egbert 2008).…”
Section: Introductionmentioning
confidence: 99%
“…Bitzarakis et al 1997; Lu & Shen 1997; Larsson 1999; Yin et al 2002; Basermann et al 2005; Lu et al 2008; Wang et al 2008) and also in various multidimensional geophysical problems (e.g. Xiong 1999; Zyserman et al 1999; Xie et al 2000; Zyserman & Santos 2000; Pain et al 2002; Ben‐Hadj‐Ali et al 2008; Sourbier et al 2008; Takei et al 2010).…”
Section: Introductionmentioning
confidence: 99%