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Thermal and mechanical properties of the near-surface layers of comet 67P/Churyumov-Gerasimenko

Spohn, T.; Knollenberg, J.; Ball, A. J.; Banaszkiewicz, M.; Benkhoff, J.; Grott, M.; Grygorczuk, J.; Hüttig, C.; Hagermann, A.; Kargl, G.; Kaufmann, E.; Kömle, N.; Kuhrt, E.; Kossacki, K. J.; Marczewski, W.; Pelivan, I.; Schrödter, R. and Seiferlin, K. (2015). Thermal and mechanical properties of the near-surface layers of comet 67P/Churyumov-Gerasimenko. Science, 349(6247), article no. aab0464.

DOI (Digital Object Identifier) Link: https://doi.org/10.1126/science.aab0464
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Abstract

Thermal and mechanical material properties determine comet evolution and even solar system formation because comets are considered remnant volatile-rich planetesimals. Using data from the Multipurpose Sensors for Surface and Sub-Surface Science (MUPUS) instrument package gathered at the Philae landing site Abydos on comet 67P/Churyumov-Gerasimenko, we found the diurnal temperature to vary between 90 and 130 K. The surface emissivity was 0.97, and the local thermal inertia was 85 ± 35 J m-2 K-1s-1/2. The MUPUS thermal probe did not fully penetrate the near-surface layers, suggesting a local resistance of the ground to penetration of >4 megapascals, equivalent to >2 megapascal uniaxial compressive strength. A sintered near-surface microporous dust-ice layer with a porosity of 30 to 65% is consistent with the data.

Item Type: Journal Item
Copyright Holders: 2015 American Association for the Advancement of Science
ISSN: 1095-9203
Project Funding Details:
Funded Project NameProject IDFunding Body
Astronomy and Planetary Sciences at the Open University (SP-12-089-MG)ST/L000776/1STFC
Academic Unit/School: Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
Item ID: 43916
Depositing User: Axel Hagermann
Date Deposited: 04 Aug 2015 09:47
Last Modified: 07 Dec 2018 10:33
URI: http://oro.open.ac.uk/id/eprint/43916
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