2005
DOI: 10.1029/2004rs003087
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Ground‐penetrating radar land mine imaging: Two‐dimensional seismic migration and three‐dimensional inverse scattering in layered media

Abstract: [1] This paper presents two methods for ground-penetrating radar (GPR) imaging of land mines: a two-dimensional (2-D) seismic migration method and a 3-D nonlinear inverse scattering method. The seismic migration technique has been successfully applied to processing field data sets collected at a test site. The results show that the seismic migration technique is a useful real-time imaging method. To image the 3-D structure of the land mine, we have developed a full 3-D nonlinear inverse scattering algorithm on… Show more

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Cited by 16 publications
(12 citation statements)
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“…such as the assumptions of a point scatter, a homogeneous soil, and no interactions between the targets [2], [8]- [15]. The model in (1) describes a setup where a series of steppedfrequency signals of strength A, at frequency ω, are sent from a transmitter located at l s and then reflected off a target at location l t = (x t , y t , z t ) with reflection coefficient ρ.…”
Section: A Response Modelmentioning
confidence: 99%
“…such as the assumptions of a point scatter, a homogeneous soil, and no interactions between the targets [2], [8]- [15]. The model in (1) describes a setup where a series of steppedfrequency signals of strength A, at frequency ω, are sent from a transmitter located at l s and then reflected off a target at location l t = (x t , y t , z t ) with reflection coefficient ρ.…”
Section: A Response Modelmentioning
confidence: 99%
“…Once the fields for a given model are obtained, the scatterer can be reconstructed via an inversion method such as the contrast source inversion (CSI) method [14,16,20,29], the Born (BIM) and distorted Born (DBIM) iterative methods [30,38,39], among others. The CSI method constructs a sequence of contrast sources and contrasts iteratively without using a forward solver.…”
Section: Introductionmentioning
confidence: 99%
“…The forward scattering solver is required in most inversion methods [20][21][22][23][24][25][26][27][28][29][30][31][32]. For the numerical solution, the volume integral equation is an appropriate choice since the reconstruction domain is an inhomogeneous medium in most applications.…”
Section: Introductionmentioning
confidence: 99%
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“…In particular, such applications are common to geophysical exploration, environmental characterization, and subsurface sensing of landmines, through-wall-imaging, medical imaging and underground structures [1][2][3][4][5][6]. Electromagnetic inverse scattering for subsurface sensing is complicated and challenging in two-fold: one is that electromagnetic wave propagation is essentially three-dimensional wave phenomena and waves interact in a complex way with ground surface, subsurface layers, and objects; the other is that this class of inverse problems involve intensive computation and are nonlinear and ill-posed.…”
Section: Introductionmentioning
confidence: 99%