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Simulating Martian regolith in the laboratory
Authors:Karsten Seiferlin  Pascale Ehrenfreund  Kurt Gunderson  Günter Kargl  Jonathan Peter Merrison
Institution:a Physikalisches Institut, Universität Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
b Astrobiology Laboratory, Leiden Institute of Chemistry, P.O. Box 9502, 2300 RA Leiden, The Netherlands
c Institut für Weltraumforschung, Graz, Österreichische Akademie der Wissenschaften, Austria
d German Aerospace Centre (DLR), Institute for Planetary Research, Rutherfordstr. 2, 12489 Berlin-Adlershof, Germany
e Aarhus Mars Simulation Laboratory, Aarhus University, Denmark
Abstract:Regolith and dust cover the surfaces of the Solar Systems solid bodies, and thus constitute the visible surface of these objects. The topmost layers also interact with space or the atmosphere in the case of Mars, Venus and Titan. Surface probes have been proposed, studied and flown to some of these worlds. Landers and some of the mechanisms they carry, e.g. sampling devices, drills and subsurface probes (“moles”) will interact with the porous surface layer. The absence of true extraterrestrial test materials in ample quantities restricts experiments to the use of soil or regolith analogue materials. Several standardized soil simulants have been developed and produced and are commonly used for a variety of laboratory experiments. In this paper we intend to give an overview of some of the most important soil simulants, and describe experiments (penetrometry, thermal conductivity, aeolian transport, goniometry, spectroscopy and exobiology) made in various European laboratory facilities.
Keywords:Martian soil  Lunar soil  Soil simulants  JSC-1  Salten Skov  Thermal conductivity
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