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Molecular origin of Io's fast sodiumNeutral sodium emissions encircling Jupiter exhibit an intricate and variable structure that is well matched by a simple loss process from Io's atmosphere. These observations imply that fast neutral sodium is created locally in the Io plasma torus, both near Io and as much as 8 hours downstream. Sodium-bearing molecules may be present in Io's upper atmosphere, where thay are ionized by the plasma torus and swept downstream. The molecular ions dissociate and dissociatively recombine on a short time scale, releasing neutral fragments into escape trajectories from Jupiter. This theory explains a diverse set of sodium observations, and it implies that molecular reactions (particularly electron impact ionization and dissociation) are important at the top of Io's atmosphere.
Document ID
19910069052
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Schneider, Nicholas M.
(Colorado Univ. Boulder, CO, United States)
Wilson, Jody K.
(Colorado, University Boulder, United States)
Trauger, John T.
(Colorado Univ. Boulder, CO, United States)
Brown, David I.
(Colorado Univ. Boulder, CO, United States)
Evans, Robin W.
(JPL Pasadena, CA, United States)
Shemansky, Donald E.
(Arizona, University Tucson, United States)
Date Acquired
August 14, 2013
Publication Date
September 20, 1991
Publication Information
Publication: Science
Volume: 253
ISSN: 0036-8075
Subject Category
Lunar And Planetary Exploration
Report/Patent Number
ISSN: 0036-8075
Accession Number
91A53675
Distribution Limits
Public
Copyright
Other

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