Estimation of the reaction rate for the formation of CH3O from H + H2CO - Implications for chemistry in the solar system

Computer Science

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Carbon Monoxide, Cosmochemistry, Methane, Methoxy Systems, Reaction Kinetics, Solar System, Carbon Dioxide, Hydrogen Atoms, Organic Compounds, Planetary Atmospheres, Planetary Systems, Solar Corona

Scientific paper

Troe's (1977) approximate theory is presently used in conjunction with transition state theory to estimate the rate coefficient of the reaction by which CO is reduced to CH4; attention is given to the role that may be played in the reduction process by the formation of the CH3O radical from H + H2CO. Attention is given to the implications of such a reaction (1) for the CO chemistry on Jupiter and within the solar nebula, (2) for the interpretation of such experimental results as those of Bar-Nun and Shaviv (1975) and Bar-Nun and Chang (1983), and (3) for organic synthesis in the prebiotic terrestrial atmosphere.

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