2008
DOI: 10.1190/1.2937466
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2.5D forward and inverse modeling for interpreting low-frequency electromagnetic measurements

Abstract: We present 2.5D fast and rigorous forward and inversion algorithms for deep electromagnetic (EM) applications that include crosswell and controlled-source EM measurements. The forward algorithm is based on a finite-difference approach in which a multifrontal LU decomposition algorithm simulates multisource experiments at nearly the cost of simulating one single-source experiment for each frequency of operation. When the size of the linear system of equations is large, the use of this noniterative solver is imp… Show more

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Cited by 285 publications
(185 citation statements)
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“…The utilized incident field distribution in the inversion algorithm will be the same incident field distribution that has been used to collect that scattering data set. Specifically, Sections 4.1 and 4.3 use the multiplicative-regularized Gauss-Newton inversion (MR-GNI) algorithm [23,24] to invert the data sets. Section 4.2, on the other hand, deals with shape and location reconstruction using the binary implementation of the MR-GNI algorithm as presented in [25].…”
Section: Reconstruction Resultsmentioning
confidence: 99%
“…The utilized incident field distribution in the inversion algorithm will be the same incident field distribution that has been used to collect that scattering data set. Specifically, Sections 4.1 and 4.3 use the multiplicative-regularized Gauss-Newton inversion (MR-GNI) algorithm [23,24] to invert the data sets. Section 4.2, on the other hand, deals with shape and location reconstruction using the binary implementation of the MR-GNI algorithm as presented in [25].…”
Section: Reconstruction Resultsmentioning
confidence: 99%
“…The main aim with the research presented in this paper is to develop a computationally efficient inversion methodology for CSEM data that is able to preserve prior information about geological strata, and we will therefore apply a model-based representation (see, e.g., [2][3][4][5][6][7][8][9]) of the unknown electric conductivity field. Alternatively, a pixel-based representation (see, e.g., [10][11][12][13]) could have been used, although the tendency for smoothing out the resulting conductivity field makes it less attractive. Additionally, large computational costs are associated with running second-order gradient-based optimization algorithms with a pixel-based representation, due to the large number of parameters.…”
Section: Introductionmentioning
confidence: 99%
“…Another approach is to solve an inverse-scattering problem in the frequency domain [2]. This method has a wide range of applications, e.g., underground resource detection [3]. If the investigated problem has such a geometry that is invariant in one direction, the three-dimensional (3-D) inverse-scattering problem can be transformed into a two-dimensional problem.…”
Section: Introductionmentioning
confidence: 99%