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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 85, NO. A5,
PAGES 2171–2176,
1980
Comparison of the N2 + Photochemistry at Different Phases of the Solar Cycle
Marsha R. Torr
Space Physics Research Laboratory, The University of Michigan, Ann Arbor, Michigan 48109
D. G. Torr
Space Physics Research Laboratory, The University of Michigan, Ann Arbor, Michigan 48109
R. A. Ong
Space Physics Research Laboratory, The University of Michigan, Ann Arbor, Michigan 48109
Abstract
Over the increasing phase of solar activity from 1974 to 1978 the F 10.7 index increased from ∼70 to ∼180. Earlier studies of the N2 + ion based on the Atmosphere Explorer satellite measurements used data gathered in 1974. A study of N2 + using 1978 measurements made during significantly higher solar EUV fluxes reveals a change in the relative importance of
the major chemical processes. Photoionization of N2 is found to be the major source of N2 + in the F 2 layer, by contrast with the charge exchange reaction of O+(2 D) with N2, which was dominant for the lower solar activity. The increased electron concentrations enhance the importance of reactions
involving electrons, thus permitting good determinations of the relevant reaction rate coefficients, which could not be done
in the earlier studies. As such, the 1978 data provide a useful opportunity to confirm the photochemical scheme established
earlier and to improve the accuracy of the determination of the rate coefficients for certain processes. Specifically, we
determine the rate coefficient for dissociative recombination of N2 + with electrons, confirming laboratory measurements; we refine an earlier determination of the charge exchange rate coefficient
for O+(2 D) with N2 to (7 ± 3) × 10−11 cm3 s−1; and we determine the rate coefficient for quenching of O+(2 D) by electrons, confirming a theoretical calculation.
Received 14
September
1979;
accepted 2
January
1980.
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Citation: Torr, M. R., D. G. Torr, and R. A. Ong
(1980),
Comparison of the N2 + Photochemistry at Different Phases of the Solar Cycle,
J. Geophys. Res.,
85(A5),
2171–2176.
Copyright 1980 by the American Geophysical Union.
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