TY - JOUR
T1 - Assessing the debris generated by the small carry-on impactor operated from the Hayabusa2 mission
AU - Hayabusa2 project team
AU - Ito, Motoo
AU - Takano, Yoshinori
AU - Kebukawa, Yoko
AU - Ohigashi, Takuji
AU - Matsuoka, Moe
AU - Kiryu, Kento
AU - Uesugi, Masayuki
AU - Nakamura, Tomoki
AU - Yuzawa, Hayato
AU - Yamada, Keita
AU - Naraoka, Hiroshi
AU - Yada, Toru
AU - Abe, Masanao
AU - Hayakawa, Masahiko
AU - Saiki, Takanao
AU - Tachibana, Shogo
N1 - Funding Information:
Acknowledgments—We are grateful to Dr. Conel M.O’D. Alexander, anonymous reviewer, and the associated editor Dr. Yoshihiro Furukawa of Tohoku University for constructive comments and an editorial handing, which helped to improve an earlier version of the manuscript. We thank Drs. H. Yano, H. Imanaka, H. Sawada (ISAS/JAXA), R. Okazaki (Kyushu Univ.), M. Arakawa (Kobe Univ.), K. Tanaka (AIST), N. Tomioka (JAMSTEC) and Ms. R. Hiyoshi (National Res. Inst. Police Sci.) for the discussion. We thank Dr. T. Shibuya and Dr. M. Igisu (JAMSTEC) for Raman analysis and Nissan ARC for SEM analyses. The authors would like to thank Enago (www.enago.jp) for the English edit. Preliminary results of this work have been presented at the Hayabusa Symposium 2014. This research was supported in part by the JSPS KAKENHI (18K18795 and 18H04468 to MI, 16H04083 to YT, 17H06458 and 19H05073 to YK, 20H00188 to TN).
Funding Information:
We are grateful to Dr. Conel M.O?D. Alexander, anonymous reviewer, and the associated editor Dr. Yoshihiro Furukawa of Tohoku University for constructive comments and an editorial handing, which helped to improve an earlier version of the manuscript. We thank Drs. H. Yano, H. Imanaka, H. Sawada (ISAS/JAXA), R. Okazaki (Kyushu Univ.), M. Arakawa (Kobe Univ.), K. Tanaka (AIST), N. Tomioka (JAMSTEC) and Ms. R. Hiyoshi (National Res. Inst. Police Sci.) for the discussion. We thank Dr. T. Shibuya and Dr. M. Igisu (JAMSTEC) for Raman analysis and Nissan ARC for SEM analyses. The authors would like to thank Enago (www.enago.jp) for the English edit. Preliminary results of this work have been presented at the Hayabusa Symposium 2014. This research was supported in part by the JSPS KAKENHI (18K18795 and 18H04468 to MI, 16H04083 to YT, 17H06458 and 19H05073 to YK, 20H00188 to TN).
Publisher Copyright:
Copyright © 2021 by The Geochemical Society of Japan.
PY - 2021
Y1 - 2021
N2 - We have analyzed the carbonaceous materials generated by the explosion of an High-melting explosive mixture in an Ar atmosphere in a laboratory simulation of the small carry-on impactor experiment. We used both non-destructive and destructive analytical techniques to identify the chemical nature of the materials. From SEM-EDS, we found the materials to be composed mainly of carbon, nitrogen, and oxygen, with a detectable amount of metals. Suitable parameters for identifying these materials are a FTIR peak at 1520 cm−1, low reflectance and gentle red slope of FTIR spectrum compared with the Murchison CM2 chondrite, the Raman D and G bands, and the hydrogen, carbon, and nitrogen isotopic compositions and their spatial distributions. The scanning transmission X-ray microscopy (STXM)-XANES results provided information about the molecular nature of these highly aromatic materials, which was supported by results from TD-GC/MS. These results suggest that it is possible to distinguish Ryugu samples from SCI potential contaminants in a sample container by using proper combinations of analytical techniques. This assessment provides information that will be useful for the analysis of the Ryugu asteroidal samples.
AB - We have analyzed the carbonaceous materials generated by the explosion of an High-melting explosive mixture in an Ar atmosphere in a laboratory simulation of the small carry-on impactor experiment. We used both non-destructive and destructive analytical techniques to identify the chemical nature of the materials. From SEM-EDS, we found the materials to be composed mainly of carbon, nitrogen, and oxygen, with a detectable amount of metals. Suitable parameters for identifying these materials are a FTIR peak at 1520 cm−1, low reflectance and gentle red slope of FTIR spectrum compared with the Murchison CM2 chondrite, the Raman D and G bands, and the hydrogen, carbon, and nitrogen isotopic compositions and their spatial distributions. The scanning transmission X-ray microscopy (STXM)-XANES results provided information about the molecular nature of these highly aromatic materials, which was supported by results from TD-GC/MS. These results suggest that it is possible to distinguish Ryugu samples from SCI potential contaminants in a sample container by using proper combinations of analytical techniques. This assessment provides information that will be useful for the analysis of the Ryugu asteroidal samples.
UR - http://www.scopus.com/inward/record.url?scp=85120817224&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85120817224&partnerID=8YFLogxK
U2 - 10.2343/geochemj.2.0632
DO - 10.2343/geochemj.2.0632
M3 - Article
AN - SCOPUS:85120817224
SN - 0016-7002
VL - 5
SP - 223
EP - 239
JO - Geochemical Journal
JF - Geochemical Journal
IS - 4
ER -