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On the Dielectric Properties of the Martian-like Surface SedimentsWe have undertaken laboratory electromagnetic characterization of the total set of minerals identified by TES on the Martian surface in order to investigate experimentally the dielectric properties of the sediments covering it in the frequency range from 1 to 30 MHz. Volcanic Rocks with a well defined mineralogy and petrology from potential terrestrial analogues sites have also been included in the study. Our primary objective is to evaluate the range of electrical and magnetic losses that may be encountered by the various Radar sounding and imaging experiments dedicated to map the Martian subsurface searching for underground water. The electromagnetic properties of these Mars-like materials will be presented as a function of various geophysical parameters, such as porosity, bulk density and temperature. The secondary objective, is to locate regions were surface dielectric conditions are suitable for subsurface sounding.
Document ID
20040062290
Acquisition Source
Johnson Space Center
Document Type
Conference Paper
Authors
Heggy, E.
(Lunar and Planetary Inst. Houston, TX, United States)
Clifford, S. M.
(Lunar and Planetary Inst. Houston, TX, United States)
Morris, R. V.
(NASA Johnson Space Center Houston, TX, United States)
Paillou, P.
(Bordeaux 2 Univ. France)
Ruffie, G.
(Ecole National de Chimie et Physique de Bordeaux Pessac, France)
Date Acquired
August 21, 2013
Publication Date
January 1, 2004
Publication Information
Publication: Lunar and Planetary Science XXXV: Mars: Radar, Gamma Ray Spectrometer, and Cratering Mineralogy
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Public Use Permitted.
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