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Hunton et al. 1991
Hunton, D.E., Viggiano, A.A., Morris, R.A., Paulson, J.F., Smith, D. and Adams, N.G. (1991). The O++ CO2 reaction: New results and atmospheric implications. Journal of Geophysical Research 96: doi: 10.1029/91JA01175. issn: 0148-0227.

The vibrational distribution of the O2 + product ion in the reaction of O+ with CO2 has been measured in a selected ion flow tube using the monitor ion technique. At 300 K the measured vibrational distribution is 45% of the ions in v=1, 32% in v≥2 and 23% in v=0. However, it is possible that vibrational quenching by the monitor gas may affect the distribution, and the nascent population may be entirely in v>0. The branching ratio between the O2 ++CO and the CO2 ++O product channels has also been measured as a function of ion drift velocity. The implications of these experiments for terrestrial releases of CO2 into the ionosphere and for the ionospheres of Mars and Venus are considered. ¿ American Geophysical Union 1991

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Keywords
Atmospheric Composition and Structure, Ion chemistry of the atmosphere, Ionosphere, Active experiments, Planetology, Solid Surface Planets and Satellites, Atmospheric composition and chemistry, Planetology, Solid Surface Planets and Satellites, Ionospheres, Ionosphere
Journal
Journal of Geophysical Research
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American Geophysical Union
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