科研之友
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摘要
This paper reviews the distribution of methane (CH4) in our Solar System, as well as its sources and sinks in the atmospheres of the main Solar System bodies. Methane is widely distributed in the Solar System. In general, the inner planets are methane-poor, being Earth a unique exception, whereas the outer planets have CH4-rich atmospheres. In general, the atmospheric chemistry of this compound is dominated by the solar radiation although in O-2-rich atmospheres this compound participates in a reaction system that removes atmospheric CH4. In our planet most of the atmospheric CH4 is produced by lifeforms, reason why scientists have proposed that the simultaneous detection of methane signal along with oxygen (O-2) or ozone (O-3) signals in the atmospheric spectra of planets may be good evidence of life. Therefore, the study of this gas at planetary level is important for understanding the chemical reactions that control its abundance on the exoplanetary atmospheres and to classify possible inhabited planets.
- 出版日期2015
