Physics
Scientific paper
Mar 1977
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977jgr....82.1008b&link_type=abstract
Journal of Geophysical Research, vol. 82, Mar. 1, 1977, p. 1008-1012.
Physics
6
Atmospheric Ionization, Ionospheric Ion Density, Oxygen Ions, Photochemical Reactions, Thermosphere, Charge Exchange, Explorer 51 Satellite, Photoionization, Reaction Kinetics, Solar X-Rays, X Ray Density Measurement
Scientific paper
Measurements of O(++) concentrations made by the Atmosphere Explorer C satellite are analyzed for altitudes where photochemical equilibrium conditions prevail in order to determine the photochemical sources and sinks of the doubly charged ion. The major loss process is found to be through partial charge exchange with neutral atomic oxygen with a rate coefficient of 1 x 10 to the -11th cu cm/s with an uncertainty of 40%. Above 220 km the major source is photo-ionization of O(+). However, X ray ionization of O (at not greater than 23.3 A) producing O(++) directly through the Auger process provides a better fit to the observed profile at lower altitudes.
Breig Edward L.
Hanson William B.
Hoffman John H.
Nier Alfred O.
Torr Douglas G.
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