2017
DOI: 10.1071/eg15095
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Short-offset grounded-wire TEM method for efficient detection of mined-out areas in vegetation-covered mountainous coalfields

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Cited by 18 publications
(6 citation statements)
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“…J 0 denotes the zero-order Bessel function [ 7 ]. G ( λ , t ) is a function of the variable λ and the observation time t ; moreover, it is also related to the resistivity and thickness of the formation and can be obtained using the inverse Laplace transform [ 25 ]. It can be seen from Equation (3) that larger peak value I and shorter falling time t f of the TX current contribute to a higher response amplitude.…”
Section: Detection Principlesmentioning
confidence: 99%
See 2 more Smart Citations
“…J 0 denotes the zero-order Bessel function [ 7 ]. G ( λ , t ) is a function of the variable λ and the observation time t ; moreover, it is also related to the resistivity and thickness of the formation and can be obtained using the inverse Laplace transform [ 25 ]. It can be seen from Equation (3) that larger peak value I and shorter falling time t f of the TX current contribute to a higher response amplitude.…”
Section: Detection Principlesmentioning
confidence: 99%
“…J 0 denotes the zero-order Bessel function [7]. G (λ, t) is a function of the variable λ and the observation time t; moreover, it is also related to the resistivity and thickness of the formation and can be obtained using the inverse Laplace transform [25].…”
Section: Response Analysismentioning
confidence: 99%
See 1 more Smart Citation
“…In addition, at present, most of the judgments on the target are based on the inversion of gradient class optimization, which requires the interpreter's subjective knowledge. It is impossible to infer the objective solution of the geological target entirely from the data, and it is also impossible to analyse the uncertainty of the solution (Zhou, Xue, Hou, Li, & Chen, ).…”
Section: Research Prospectsmentioning
confidence: 99%
“…The detection depth of this method can reach approximately 2,000 m. Compared with traditional LOTEM methods, the short-offset grounded-wire TEM (SOTEM) method can produce a higher signal-to-noise ratio and achieve higher detection precision at shallow depth (<2,000 m). In recent years, many research achievements have been realized with this method, and excellent deep exploration results have been obtained in the fields of mineral deposits and hydrogeological prospecting (Chen, Xue, & Khan, 2016;Xue et al, 2013Xue et al, , 2020Xue, Chen, & Cheng, 2019;Zhou, Xue, Hou, Li, & Chen, 2017;Zhou, Xue, Hou, & Lu, 2018;Zhou, Xue, & Li, 2016).…”
mentioning
confidence: 99%