Japan Geoscience Union Meeting 2018

Presentation information

[JJ] Evening Poster

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS18] Aqua planetology

Tue. May 22, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Yasuhito Sekine(Department of Earth and Planetary Science, University of Tokyo), Tomohiro Usui(Earth-Life Science Institute, Tokyo Institute of Technology), Hidenori Genda(東京工業大学 地球生命研究所, 共同), Takazo Shibuya(Japan Agency for Marine-Earth Science and Technology)

[MIS18-P12] Impact-induced alterations of planetary organic simulants: applications to space missions for small bodies

*Yasuhito Sekine1, Kenya Kodama1, Takamichi Kobayashi2, Seiji Obata1, Yu Chang1, Nanako O. Ogawa3, Yoshinori Takano3, Naohiko Ohkouchi3, Koichiro Saiki1, Toshimori Sekine4 (1.University of Tokyo, 2.National Institute for Materials Science, 3.JAMSTEC, 4.Center for High Pressure Science and Technology Advanced Research)

Keywords:organic matter, shock alteration

We systematically investigates shock-induced alteration of planetary organic simulants, which are laboratory analogues of complex organic matter found on primitive planetary bodies, as a function of peak shock pressure and temperature by impact experiments. Our results show that the composition and structure of planetary organic simulants are unchanged upon impacts at peak pressures less than ~5 GPa and temperatures less than ~350ºC. On the other hand, these are dramatically changed upon impacts at pressures higher than 7–8 GPa and temperatures higher than ~400ºC, through loss of hydrogen-related bonds and concurrent carbonization, regardless of the initial compositions of organic simulants. Compared with previous results on static heating of organic matter, we suggest that shock-induced alteration cannot be distinguished from static heating only by Raman and infrared spectroscopy. Our experimental results would provide a proxy indicator for assessing degree of shock-induced alteration of organic matter contained in carbonaceous chondrites. We suggest that a remote-sensing signature of the 3.3–3.6 μm absorption due to hydrogen-related bonds on the surface of small bodies would be a promising indicator for the presence of less-thermally-altered (i.e., temperatures less than 350°C) organic matter there, which will be a target for landing to collect primordial samples in sample-return spacecraft missions to asteroids or icy bodies.