Wiley Encyclopedia of Electrical and Electronics Engineering 2016
DOI: 10.1002/047134608x.w3602.pub2
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Electromagnetic Subsurface Remote Sensing

Abstract: Fundamental principles and several applications of electromagnetic (EM) subsurface remote sensing methods are outlined and illustrated. Physical insight is emphasized rather than mathematical analysis. The various methods are classified according to the practical embodiment and their range of applications. These include borehole EM methods, ground‐penetrating radar, magnetotelluric methods, airborne methods, inductive EM methods, time‐domain EM methods, and marine EM methods.

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Cited by 10 publications
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“…In general, TR invariance can be exploited for detection and localization of obscured targets in noisy and rich-scattering environments, with high resolution. Timereversal (TR) techniques were first developed for acoustics (Fink et al, 1989) (Fink, 1992), being later successfully used in several applications including non-destructive testing and evaluation (Liu et al, 2014), sound quality enhancement (Lin & Too, 2014), atmospherics studies (Mora et al, 2012), subsurface geophysics (Fink, 2006;Leuschen & Plumb, 2001;Saillard et al, 2004;Cresp et al, 2008;Artman et al, 2010;Foroozan & Asif, 2010;Yavuz et al, 2014;Chen et al, 2016), microwave remote sensing (Reyes-Rodríguez et al, 2014), wireless communications (Fouda et al, 2012) and medicine 1 Backpropagation can be effected either physically by transmitting the time-reversed signals into the original medium, or synthetically by means of a forward simulation engine, such as the finite-difference time-domain (FDTD) method. Synthetic backpropagation is done for imaging purposes, as considered here.…”
Section: Introductionmentioning
confidence: 99%
“…In general, TR invariance can be exploited for detection and localization of obscured targets in noisy and rich-scattering environments, with high resolution. Timereversal (TR) techniques were first developed for acoustics (Fink et al, 1989) (Fink, 1992), being later successfully used in several applications including non-destructive testing and evaluation (Liu et al, 2014), sound quality enhancement (Lin & Too, 2014), atmospherics studies (Mora et al, 2012), subsurface geophysics (Fink, 2006;Leuschen & Plumb, 2001;Saillard et al, 2004;Cresp et al, 2008;Artman et al, 2010;Foroozan & Asif, 2010;Yavuz et al, 2014;Chen et al, 2016), microwave remote sensing (Reyes-Rodríguez et al, 2014), wireless communications (Fouda et al, 2012) and medicine 1 Backpropagation can be effected either physically by transmitting the time-reversed signals into the original medium, or synthetically by means of a forward simulation engine, such as the finite-difference time-domain (FDTD) method. Synthetic backpropagation is done for imaging purposes, as considered here.…”
Section: Introductionmentioning
confidence: 99%
“…Ground penetrating radar (GPR) finds a large number of applications related to detection and imaging of subsurface targets and anomalies such as underground utilities, pipes, chemical spills, groundwater levels, etc. Historically, GPR data has been typically analyzed and interpreted based on a "visual" analysis of the radargram [1], [2]; however, this analysis is able to provide reliable interpretation only in simple scenarios. In order to improve the interpretability of GPR data, inverse scattering and migration algorithms [3]- [8], including microwave tomography (MT) techniques [9]- [11], have also been used in different scenarios related to GPR surveys.…”
Section: Introductionmentioning
confidence: 99%