Discovery of chlorine in the Io torus

Citation
M. Kuppers et Nm. Schneider, Discovery of chlorine in the Io torus, GEOPHYS R L, 27(4), 2000, pp. 513-516
Citations number
29
Categorie Soggetti
Earth Sciences
Journal title
GEOPHYSICAL RESEARCH LETTERS
ISSN journal
00948276 → ACNP
Volume
27
Issue
4
Year of publication
2000
Pages
513 - 516
Database
ISI
SICI code
0094-8276(20000215)27:4<513:DOCITI>2.0.ZU;2-1
Abstract
We report the discovery of singly ionized chlorine in the Io plasma torus t hrough the detection of emission at 857.9 nm. The 40 Rayleigh peal; intensi ty at 857.9 nm corresponds to a Cl+ abundance of 2+/-0.5% relative to all i ons. Since Cl+ probably originates at Io, Io's atmosphere must have the hig hest proportion of chlorine of any solar system body. While Cl+ plays only a minor role in torus physics, the presence of chlorine in Io's atmosphere, surface, and interior has more profound implications. Salt as a solid or g as is probably an important source of both Na and Cl in Io's vicinity.