Journal
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
Volume 116, Issue -, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2011JA016613
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Funding
- NASA [NNX07AN03G, NNX08AF43G]
- NASA [102571, NNX08AF43G] Funding Source: Federal RePORTER
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This paper reexamines the chemistry of N-2(+), NO+, O-2(+), and N+ by comparing densities from a photochemical model with data from the Atmosphere Explorer C satellite. These comparisons show that the measurements of N-2(+), NO+, O-2(+), and N+ density are well modeled with up-to-date reaction rates, solar EUV irradiances, and photoelectron fluxes. In particular, this study has resolved a long-standing problem wherein the previous investigations overestimated the measured N-2(+) density by a factor of 2. A new method of determining the important and controversial O+(D-2) + N-2 reaction rate from the Atmosphere Explorer C data is presented. This reaction rate determination agrees well with the latest laboratory measured reaction rate.
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