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An experimental study on impact‐induced alterations of planetary organic simulants
Author(s) -
Sekine Yasuhito,
Kodama Kenya,
Kobayashi Takamichi,
Obata Seiji,
Chang Yu,
Ogawa Nanako O.,
Takano Yoshinori,
Ohkouchi Naohiko,
Saiki Koichiro,
Sekine Toshimori
Publication year - 2018
Publication title -
meteoritics and planetary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.09
H-Index - 100
eISSN - 1945-5100
pISSN - 1086-9379
DOI - 10.1111/maps.13075
Subject(s) - organic matter , chondrite , shock (circulatory) , raman spectroscopy , chemistry , analytical chemistry (journal) , materials science , astrobiology , environmental chemistry , meteorite , organic chemistry , optics , physics , medicine
Abstract The present study systematically investigates shock‐induced alteration of organic simulants of planetary bodies ( OSPB s) as a function of peak shock pressure and temperature by impact experiments. Our results show that the composition and structure of OSPB s are unchanged upon impacts at peak pressures ≤~5 GP a and temperatures ≤~350 °C. On the other hand, these are dramatically changed upon impacts at >7–8 GPa and > ~400 °C, through loss of hydrogen‐related bonds and concurrent carbonization, regardless of the initial compositions of OSPB s. 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., <350 °C) organic matter there, which will be a target for landing to collect primordial samples in sample‐return spacecraft missions, such as Hayabusa2 and OSIRIS ‐ RE x.