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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 109,
A03302,
doi:10.1029/2003JA010132,
2004
Dissociative recombination of N2
+, O2
+, and NO+: Rate coefficients for ground state and vibrationally excited ions
Clint H. Sheehan
Department of Physics, Ouachita Baptist University, Arkadelphia, Arkansas, USA
J.-P. St.-Maurice
Department of Physics and Astronomy, University of Western Ontario, London, Ontario, Canada
Abstract
We review recent advances in the study of the dissociative recombination of molecular ions with electrons with a primary emphasis
on experimental studies. In particular, we focus on previous experimental measurements of recombination rates for N2
+, O2
+, and NO+ ions. In the context of this review, we present temperature dependent rate coefficients from recent merged beam studies of
the dissociative recombination of N2
+, O2
+, and NO+ ions with electrons. Identifying underlying physical differences between the various experimental techniques enables a discussion
of the effects of vibrational excitation on the dissociative recombination of these major ionospheric species of ions. For
T < 1200 K, we conclude that the recombination rates for N2
+, O2
+, and NO+ ions in the ground electronic and vibrational states respectively are 2.2 × 10−7 (Te/300)−0.39 cm3 s−1, 1.95 × 10−7(Te/300)−0.70 cm3 s−1, and (3.5 ± 0.5) × 10−7(Te/300)−0.69 cm3 s−1. Vibrational excitation is shown to play a significant role in laboratory measurements of these recombination rates. For
each of these species, vibrationally excited ions yielded a lower recombination rate than the ground state. We also discuss
the recombination of these species of ions for T > 1200 K.
Received 10
July
2003;
accepted 27
January
2004;
published 13
March
2004.
Index Terms: 2419 Ionosphere: Ion chemistry and composition (0335); 0317 Atmospheric Composition and Structure: Chemical kinetic and photochemical properties; 0335 Atmospheric Composition and Structure: Ion chemistry of the atmosphere (2419, 2427); 2407 Ionosphere: Auroral ionosphere (2704); 2459 Ionosphere: Planetary ionospheres (5435, 5729, 6026, 6027, 6028).
Read Full Article (file size: 1548088 bytes) Cited by
Citation: Sheehan, C. H., and J.-P. St.-Maurice
(2004),
Dissociative recombination of N2
+, O2
+, and NO+: Rate coefficients for ground state and vibrationally excited ions,
J. Geophys. Res.,
109,
A03302,
doi:10.1029/2003JA010132.
Copyright 2004 by the American Geophysical Union.
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