Ice surface reactions: A key to chemical evolution in space

被引:199
作者
Watanabe, Naoki [1 ]
Kouchi, Akira [1 ]
机构
[1] Hokkaido Univ, Inst Low Temp Sci, Kita Ku, Sapporo, Hokkaido 0600819, Japan
基金
日本学术振兴会;
关键词
Cosmic dust; Amorphous solid waters; Surface reaction; Chemical evolution; Interstellar molecular cloud; Hydrogen atom; Tunneling reaction;
D O I
10.1016/j.progsurf.2008.10.001
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Chemical reactions on the surface of cosmic ice dust play an important role in chemical evolution in space. Arnong the many kinds of molecules observed, the abundances of some major species such as hydrogen molecules cannot be explained by gas-phase synthesis; therefore, surface reactions oil cosmic dust are considered for the synthesis of such molecules. Experimental research on surface reactions relevant to cosmic ice dust has been conducted since the late 1980s. Early experiments were rather qualitative, and so the details of reactions were not clear. In the last decade, many scientists from various fields including surface science have been motivated to extend the knowledge in this area of research, and have performed sophisticated experiments regarding surface reactions on cosmic ice dust. The aim of this article is to review the recent progress in surface astrochemistry. In particular, focus is made on experiments concerning the synthesis of abundant molecules such as H-2, H2O, CO2, H2CO and CH3OH oil ice surfaces at very low temperatures. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:439 / 489
页数:51
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