Formation of chiral CO polyhedral crystals on icy interstellar grains

Author:

Kouchi Akira1ORCID,Tsuge Masashi1ORCID,Hama Tetsuya2,Niinomi Hiromasa3,Nakatani Naoki4,Shimonishi Takashi5,Oba Yasuhiro1ORCID,Kimura Yuki1,Sirono Sin-iti6,Okuzumi Satoshi7,Momose Munetake8,Furuya Kenji9ORCID,Watanabe Naoki1

Affiliation:

1. Institute of Low-Temperature Science, Hokkaido University, Sapporo, Hokkaido 060–0819, Japan

2. Komaba Institute for Science, The University of Tokyo, Meguro, Tokyo 153–8902, Japan

3. Institute for Materials Research, Tohoku University, Sendai, Miyagi 980–8577, Japan

4. Department of Chemistry, Graduate School of Science and Engineering, Tokyo Metropolitan University, Hachioji, Tokyo 192–0397, Japan

5. Center for Transdisciplinary Research, Niigata University, Niigata 950–2181, Japan

6. Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya, Aichi 464–8601, Japan

7. Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152–8551, Japan

8. College of Science, Ibaraki University, Mito, Ibaraki 310–8512, Japan

9. National Astronomical Observatory of Japan, Osawa 2-21-1, Mitaka, Tokyo 181–8588, Japan

Abstract

ABSTRACT The crystallinity and morphology of solid carbon monoxide (CO) on icy interstellar grains were examined by observing the deposition, crystallization, and UV and electrons irradiation of solid CO using transmission electron microscopy. Herein, we found that solid CO deposited in molecular clouds was crystalline, and that even if amorphous CO was deposited, amorphous CO crystallized within 103 yr at 10 K. Conversely, crystalline CO was not amorphized by UV rays or electron beam at 10 K. These results indicated the occurrence of chiral crystalline CO instead of amorphous CO in space. Furthermore, the large surface diffusion coefficients of CO on eamorphous H2O and crystalline CO at 10 K facilitated the morphological equilibration of crystalline CO. Bad wetting of crystalline CO with amorphous H2O proved that the morphology of the ice grains was not spherical with an onion-like structure, as hitherto assumed, but rather it was a polyhedral crystalline CO attached to amorphous H2O. This has important implications for phenomena associated with the collision and subsequent sticking between ice grains, surface chemical reactions, non-thermal desorption of molecules and the origin of homochirality in interstellar biomolecules.

Funder

Hokkaido University

Ministry of Education, Culture, Sports, Science and Technology

Japan Society for the Promotion of Science

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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