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A preparatory study on subsurface exploration on Mars using GPR and microwave tomography
Authors:Francesco Soldovieri  Giancarlo Prisco  Svein-Erik Hamran
Institution:1. Istituto per il Rilevamento Elettromagnetico dell’Ambiente, Consiglio Nazionale delle Ricerche Via Diocleziano 328, 80124 Napoli, Italy;2. Forsvarets Forsknings Institutt-FFI, P.O. Box 25, 2007 Kjeller, Norway;1. International Space Science Institute, Bern, Switzerland;2. ESA Research and Scientific Support Department, Noordwijk, The Therlands;1. Arkansas Center for Space and Planetary Sciences, University of Arkansas Fayetteville, AR 72701, USA;2. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA;1. Istituto di Astrofisica e Planetologia Spaziali (IAPS), Istituto Nazionale di Astrofisica (INAF), Rome, Italy;2. Info Solution, Milan, Italy;3. Jet Propulsion Laboratory, Pasadena, CA, USA;4. University of Dresden, Radio Frequency and Photonics, Dresden, Germany;5. Istituto di Radioastronomia, Istituto Nazionale di Astrofisica, Bologna, Italy;1. Macau University of Science and Technology, Macau;2. Lunar and Planetary Science Laboratory, Macau University of Science and Technology, Macau;1. Edutus University, Stúdium tér, H-2800 Tatabánya, Hungary;2. Cembrit Kft., Bécsi út 7., H-2536 Nyergesújfalu, Hungary
Abstract:The exploitation of ground penetrating radar in Mars subsurface exploration is becoming assessed in remote sensing observations and is of timely interest for high resolution in situ prospecting of the first meters of the underground.In this framework, we deal with a novel processing approach based on microwave tomography. Aiming to achieve accurate and reliable “images” of the investigated subsurface region in order to detect, localize and possibly determine the extent and the geometrical features of the embedded layers while reducing at the minimum possible the “interpretation” of the diagnostics result.The feasibility of the microwave tomographic approach has been tested in realistic cases dealing with conditions analogue to the Mars subsurface ones. In particular, we will present the tomographic reconstruction results achieved by experimental data collected in a field survey at Svalbard Islands (Norway) with a time-domain GPR.
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