An efficient 2.5D inversion of loop-loop electromagnetic data
Yoonho Song 1 3 Jung-Ho Kim 21 Groundwater and Geothermal Resources Division, Korea Institute of Geoscience and Mineral Resources (KIGAM), 30 Gajeong-Dong, Yuseong-Gu, Daejon 305-350, Korea.
2 Geoelectric Imaging Laboratory, Korea Institute of Geoscience and Mineral Resources (KIGAM), 30 Gajeong-Dong, Yuseong-Gu, Daejon 305-350, Korea.
3 Corresponding author. Email: song@kigam.re.kr
Exploration Geophysics 39(1) 68-77 https://doi.org/10.1071/EG08007
Submitted: 27 August 2007 Accepted: 8 October 2007 Published: 5 March 2008
Abstract
We have developed an inversion algorithm for loop-loop electromagnetic (EM) data, based on the localised non-linear or extended Born approximation to the solution of the 2.5D integral equation describing an EM scattering problem. Source and receiver configuration may be horizontal co-planar (HCP) or vertical co-planar (VCP). Both multi-frequency and multi-separation data can be incorporated. Our inversion code runs on a PC platform without heavy computational load.
For the sake of stable and high-resolution performance of the inversion, we implemented an algorithm determining an optimum spatially varying Lagrangian multiplier as a function of sensitivity distribution, through parameter resolution matrix and Backus-Gilbert spread function analysis. Considering that the different source-receiver orientation characteristics cause inconsistent sensitivities to the resistivity structure in simultaneous inversion of HCP and VCP data, which affects the stability and resolution of the inversion result, we adapted a weighting scheme based on the variances of misfits between the measured and calculated datasets.
The accuracy of the modelling code that we have developed has been proven over the frequency, conductivity, and geometric ranges typically used in a loop-loop EM system through comparison with 2.5D finite-element modelling results. We first applied the inversion to synthetic data, from a model with resistive as well as conductive inhomogeneities embedded in a homogeneous half-space, to validate its performance. Applying the inversion to field data and comparing the result with that of dc resistivity data, we conclude that the newly developed algorithm provides a reasonable image of the subsurface.
Key words: electromagnetic (EM), 2.5D, inversion, localised non-linear approximation.
Acknowledgments
This work was supported by Basic Research Project of Korea Institute of Geoscience and Mineral Resources (KIGAM) funded by the Ministry of Science and Technology of Korea. We also thank Dr. Jeong Sul Son of KIGAM for providing the finite element modelling results.
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