2014
DOI: 10.1190/geo2014-0043.1
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Fast multimodel finite-difference controlled-source electromagnetic simulations based on a Schur complement approach

Abstract: We have developed an efficient numerical scheme for fast multimodel 3D electromagnetic simulations by applying a Schur complement approach to a frequency-domain finite-difference method. The scheme is based on direct solvers and developed with constrained inversion algorithms in view. Such algorithms normally need many forward modeling jobs with different resistivities for the target zone and/or background formation. We geometrically divide the computational domain into two subdomains: an anomalous subdomain, … Show more

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Cited by 40 publications
(11 citation statements)
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“…In all simulations the system matrix was generated using the finite-difference modelling code presented in Jaysaval et al (2014). The simulations were carried out on either (1) the CALMIP supercomputer EOS (https://www.calmip.univ-toulouse.fr/), which is a BULLx DLC system composed of 612 computing nodes, each composed of two Intel Ivybridge processors with 10 cores (total 12 240 cores) running at 2.8 GHz per node and 64 GB/node, or (2) a computer FARAD with 16-core Intel Xeon CPU E5-2690 processors running at 2.90 GHz and 264 GB memory.…”
Section: R E S U Lt Smentioning
confidence: 99%
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“…In all simulations the system matrix was generated using the finite-difference modelling code presented in Jaysaval et al (2014). The simulations were carried out on either (1) the CALMIP supercomputer EOS (https://www.calmip.univ-toulouse.fr/), which is a BULLx DLC system composed of 612 computing nodes, each composed of two Intel Ivybridge processors with 10 cores (total 12 240 cores) running at 2.8 GHz per node and 64 GB/node, or (2) a computer FARAD with 16-core Intel Xeon CPU E5-2690 processors running at 2.90 GHz and 264 GB memory.…”
Section: R E S U Lt Smentioning
confidence: 99%
“…In the padded regions the gridding was severely non-uniform and followed the rules described by Jaysaval et al (2014), where the air was discretized with 15 cells and the other boundaries with 7 cells. Apart from the padded regions, we used finite-difference grids that were uniform in all three directions.…”
Section: Models and System Matricesmentioning
confidence: 99%
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“…This is especially important for EM inversion requiring sequential solution of multiple forward problems. Recently, significant advances have been made in developing the direct solvers for forward EM problems (e.g., Grayver et al 2013;Jaysaval et al 2014). However, the direct solvers still impose challenging memory requirements for large-scale 3D problems, which makes the iterative solvers more attractive in geophysical applications.…”
Section: Introductionmentioning
confidence: 99%
“…Direct solvers have tradition- ally been considered to be too computationally demanding for 3D problems compared to iterative solvers. However, gradual advancement of direct-solution algorithms, along with the availability of resources for parallel computation, makes it possible to apply these algorithms for solving large-scale 3D problems very efficiently (Streich, 2009;da Silva et al, 2012;Yang and Oldenburg, 2012;Grayver et al, 2013;Schwarzbach and Haber, 2013;Jaysaval et al, 2014). In particular, in the case of multisource problems such as marine CSEM, the direct solvers may perform more efficiently than the iterative solvers because the direct solvers reuse the decomposed system matrix for multiple sources whereas the iterative solvers need to solve the problem for each source separately (Chung et al, 2014).…”
Section: Introductionmentioning
confidence: 99%