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Published October 1982 | Published
Journal Article Open

Erosion of frozen sulfur dioxide by ion bombardment: Applications to Io

Abstract

The erosion of frozen SO_2 due to bombardment by both light and heavy ions (He and F) was measured for bombarding energies of 0.08 to 1.3 MeV/amu. The number of SO_2 molecules ejected from the target per incident ion (i.e., the sputtering yield) was 50 for 1.5 MeV He ions and 7300 for 6 MeV F ions. Ion bombardment followed by heating produced an oxygen/sulfur residue which was much more stable against subsequent ion bombardment than the initial frozen SO_2. The erosion rate of SO_2 frost on Jupiter's moon Io depends strongly on the elemental composition and energy spectra of the magnetospheric ion flux which bombards the surface. The combined effects of ion bombardment and heating which produced residues on our target substrates may also occur on Io from magnetospheric ion bombardment and heating by volcanism. Our experimental results compare favorably with a new model of the sputtering process which considers the energy loss of the incident ion to electronic excitation in the target.

Additional Information

Copyright 1982 by the American Geophysical Union. (Received April 29, 1982; accepted August 24, 1982.) Paper number 2L1328. We are grateful for discussions with P. K. Haff and C. C. Watson. This work was supported in part by NASA [NAGW-148, NAGW-202] and the NSF [PHY79-23638, CHE81-13273].

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