Ion sputtering and surface erosion at Europa

W. H. Ip, D. J. Williams, R. W. McEntire, B. H. Mauk

研究成果: 雜誌貢獻期刊論文同行評審

63 引文 斯高帕斯(Scopus)

摘要

New results from the energetic particle detector (EPD) experiment on the Galileo mission are used to update the ion sputtering rate at Europa. It is found that the resultant gas emission rates are 5.7×1027 O2 s-1 and 9.5×1027 H2O s-1 in total if the maximum self-sputtering effect of the exospheric pickup ions is taken into consideration. This means that the surface number density of O2 molecules could be as much as 1.8×109 cm-3 and the average column density is 3.4×1015 O2 molecules cm-2. The corresponding ion production rate is on the order of 1.3×1027 ions s-1 probably leading to a plasma density of about 2000 ions cm-3 in the ionospheric wake region. The magnetospheric particle bombardment effect is also effective in redistributed mass across Europa's surface. The maximum mass redistribution rate can be estimated to be ≈80 m per 100 Myrs with the associated net erosion rate ≈20 m/100 Myrs. At the same time, mass resurfacing rate by liquid water or out-gassing could reach similar magnitude.

原文???core.languages.en_GB???
頁(從 - 到)829-832
頁數4
期刊Geophysical Research Letters
25
發行號6
DOIs
出版狀態已出版 - 15 3月 1998

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