The dissociative recombination of O2/+/ in the ionosphere

Computer Science – Sound

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Aeronomy, Atmospheric Chemistry, Gas Dissociation, Ion Recombination, Ionospheric Composition, Oxygen Ions, Recombination Coefficient, Charge Exchange, Ionospheric Electron Density, Ionospheric Ion Density, Oxygen Recombination, Reaction Kinetics, Satellite Sounding

Scientific paper

Aeronomical determinations of the dissociative recombination reaction rate coefficient for O2(+) and alpha depend directly on a knowledge of the rate coefficient for the charge exchange of O(+) with O2 and k. The aeronomical determination of alpha is reevaluated using Atmosphere Explorer satellite data in light of a subsequent laboratory measurement of k (Chen et al., 1978). The results are found to be in good agreement with laboratory determinations of the coefficient for night-time conditions. For data obtained under sunlit conditions, however, the results differed significantly with those of the laboratory measurements. These results imply that the state of the O2(+) molecule major thermospheric processes needs to be examined in greater detail.

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