2022
DOI: 10.1109/tgrs.2022.3187021
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Transient Electromagnetic Machine Learning Inversion Based on Pseudo Wave Field Data

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Cited by 13 publications
(3 citation statements)
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“…DL methods can learn both prior parameter relationships and structural similarity of the multiphysics data sets. Therefore, the accuracy of EM imaging may be greatly improved (Chen et al, 2022;Guo et al, 2022), and the uncertainty of imaging could be reduced (Um et al, 2022). These aspects are crucial for DL decision-making inversion and need further study (Oh and Byun, 2021).…”
Section: Potential and Challengesmentioning
confidence: 99%
“…DL methods can learn both prior parameter relationships and structural similarity of the multiphysics data sets. Therefore, the accuracy of EM imaging may be greatly improved (Chen et al, 2022;Guo et al, 2022), and the uncertainty of imaging could be reduced (Um et al, 2022). These aspects are crucial for DL decision-making inversion and need further study (Oh and Byun, 2021).…”
Section: Potential and Challengesmentioning
confidence: 99%
“…This method is an artificial source secondary field method, which has advantages such as high data signal-tonoise ratio, no interference from the primary field, less affected by topographic relief in high-resistivity surrounding rock areas, strong ability to penetrate high-resistivity overburden, and large detection depth. In recent years, it has been favored by karst researchers and applied to karst detection [20][21][22]. Since TDEM observes the electromotive force data in the time domain, it is necessary to obtain the resistivity in the depth domain through inversion and then interpret related geological problems.…”
Section: H Zmentioning
confidence: 99%
“…This method is an artificial source secondary field method, which has advantages such as high data signal-to-noise ratio, no interference from primary field, less affected by topographic relief in high-resistivity surrounding rock areas, strong ability to penetrate high-resistivity overburden, and large detection depth. In recent years, it has been favored by karst researchers and applied to karst detection [19][20][21]. Since TDEM observes the electromotive force data in time domain, it is necessary to obtain the resistivity in depth domain through inversion, and then interpret related geological problems.…”
Section: Introductionmentioning
confidence: 99%