Please use this identifier to cite or link to this item: http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/5854
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dc.contributor.authorDEHIYA, RAHULen_US
dc.date.accessioned2021-05-03T06:46:22Z
dc.date.available2021-05-03T06:46:22Z
dc.date.issued2021-05en_US
dc.identifier.citationGeophysics, 86(3), WB79–WB88.en_US
dc.identifier.issn0016-8033en_US
dc.identifier.issn1942-2156en_US
dc.identifier.urihttp://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/5854
dc.identifier.urihttps://doi.org/10.1190/geo2020-0372.1en_US
dc.description.abstractI have examined the possibility of using a 3D modeling algorithm in studying tunnel detectability using the electromagnetic gradiometer (EMG) response. A detailed comparison of different source-receiver configurations reveals that the EMG response is stronger for a configuration when the transmitter and receiver are orthogonal to each other than the parallel configurations. Orthogonal configurations perform better at a relatively lower frequency than the parallel configuration. The EMG response is enhanced with the broadside offset defined as the distance between transmitter and receiver pair. The response of a tunnel is generally weak; consequently, deviation from the configuration in which both receivers are equidistant from the transmitter masks the response of a tunnel. The impact analysis of tunnel-floor conductivity revealed that a one-order-higher conductive floor does not change the behavior of response compared to a tunnel without a conductive floor. However, the two-order-higher conductive floor changes the shape of the response curves, yet the change in the magnitude is not significant. The presence of a metal conductor substantially enhances the response of an EMG system. The parallel configuration is more suitable for the depth estimation of the tunnel than the orthogonal configuration. The distortion in the EMG response due to the heterogeneity in the case of an orthogonal configuration depends on the broadside offset. For a zero broadside offset, the response is severely distorted by the small-scale inhomogeneity. For a broadside offset such as 20 m, the impact of small-scale inhomogeneity is almost invisible.en_US
dc.language.isoenen_US
dc.publisherSociety of Exploration Geophysicistsen_US
dc.subjectElectromagneticsen_US
dc.subjectGradiometryen_US
dc.subjectModelingen_US
dc.subjectNear surfaceen_US
dc.subjectTOC-APR-2021en_US
dc.subject2021en_US
dc.subject2021-APR-WEEK4en_US
dc.title3D modeling of electromagnetic gradiometer data — A numerical study on tunnel detectionen_US
dc.typeArticleen_US
dc.contributor.departmentDept. of Earth and Climate Scienceen_US
dc.identifier.sourcetitleGeophysicsen_US
dc.publication.originofpublisherForeignen_US
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