Unattenuated ionization rates for the dissociative photoionization of SO2 producing SO2+, SO+, S+, O+, and O2+ ions are reported during solar minimum and maximum conditions. It is found that in the atmosphere of Io the photodissociation-ionization of SO2 could be an important source of the production of SO+, S+, O+, and O2+ ions and that its contribution is much greater (factor of 5-10) compared with that due to direct photoionization of, respectively, SO, S, O, and O2 gases. Role of photoelectron impact ionization of SO2 in producing SO2+, SO+, S+, O+, and O2+ ions in the Io's atmosphere is investigated using a Monte Carlo model. It is recommended that the models of Io's ionosphere-atmosphere should include the dissociative ionization of SO2. Copyright 1997 by the American Geophysical Union.
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Michael, M., & Bhardwaj, A. (1997). On the dissociative ionization of so2 in Io’s atmosphere. Geophysical Research Letters, 24(16), 1971–1974. https://doi.org/10.1029/97GL02056