"In order to test the accuracy of Ground Penetrating Radar (GPR) in thedetectionof subsurface targets for planetary. exploration, a laboratory scale experiment is performed based on a ‘sand box’ setup using two different bistatic. GPR commercial instruments. Specific attention is paid to the challenging case of buried dielectric scatterers. whose location and dimensions are of the same order of magnitude of the GPR antenna separation and signal. wavelengths. The target depth is evaluated by using the wave propagation velocity measured with Time Domain. Reflectometry (TDR). Bymeans of a propermodeling of the different wave-propagation contributions to the gathered. signal, the position of buried targets is correctly estimated with both GPRs even for rather shallow and. small-size scatterers in near-field conditions. In this frame, relevant results for a basalt block buried in a silica. soil are discussed. The experimental configuration is also simulated with an ad-hoc numerical code, whose synthetic. radar sections fully confirm the measured results. The acquired information is of paramount importance. for the analysis of various scenarios involving GPR on-site application in future space missions."

Lauro, S., Mattei, E., Barone, P.M., Pettinelli, E., Vannaroni, G., Valerio, G., et al. (2013). Estimation of subsurface dielectric target depth for GPR planetary exploration: Laboratory measurements and modeling. JOURNAL OF APPLIED GEOPHYSICS, 99, 93-100 [10.1016/j.jappgeo.2013.04.001].

Estimation of subsurface dielectric target depth for GPR planetary exploration: Laboratory measurements and modeling

LAURO, SEBASTIAN;MATTEI, ELISABETTA;PETTINELLI, Elena;
2013-01-01

Abstract

"In order to test the accuracy of Ground Penetrating Radar (GPR) in thedetectionof subsurface targets for planetary. exploration, a laboratory scale experiment is performed based on a ‘sand box’ setup using two different bistatic. GPR commercial instruments. Specific attention is paid to the challenging case of buried dielectric scatterers. whose location and dimensions are of the same order of magnitude of the GPR antenna separation and signal. wavelengths. The target depth is evaluated by using the wave propagation velocity measured with Time Domain. Reflectometry (TDR). Bymeans of a propermodeling of the different wave-propagation contributions to the gathered. signal, the position of buried targets is correctly estimated with both GPRs even for rather shallow and. small-size scatterers in near-field conditions. In this frame, relevant results for a basalt block buried in a silica. soil are discussed. The experimental configuration is also simulated with an ad-hoc numerical code, whose synthetic. radar sections fully confirm the measured results. The acquired information is of paramount importance. for the analysis of various scenarios involving GPR on-site application in future space missions."
2013
Lauro, S., Mattei, E., Barone, P.M., Pettinelli, E., Vannaroni, G., Valerio, G., et al. (2013). Estimation of subsurface dielectric target depth for GPR planetary exploration: Laboratory measurements and modeling. JOURNAL OF APPLIED GEOPHYSICS, 99, 93-100 [10.1016/j.jappgeo.2013.04.001].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11590/267438
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