Composition of jovian dust stream particles

被引:55
|
作者
Postberg, Frank
Kempf, Sascha
Srama, Ralf
Green, Simon F.
Hillier, Jon K.
McBride, Neil
Gruen, Eberhard
机构
[1] MPI Kernphys, D-69117 Heidelberg, Germany
[2] Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England
[3] Univ Hawaii, Hawaii Inst Geophys & Planetol, Honolulu, HI 96822 USA
关键词
Jupiter; interplanetary dust; Io; volcanism; satellites; atmospheres;
D O I
10.1016/j.icarus.2006.02.001
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The Cassini spacecraft encountered Jupiter in late 2000. Within more than 1 AU of the gas giant the Cosmic Dust Analyser onboard the spacecraft recorded the first ever mass spectra of jovian stream particles. To determine the chemical composition of particles, a comprehensive statistical analysis of the dataset was performed. Our results imply that the vast majority ( > 95%) of the observed stream particles originate from the volcanic active jovian satellite to from where they are sprinkled out far into the Solar System. Sodium chloride (NaCl) was identified as the major particle constituent, accompanied by sulphurous as well as potassium bearing components. This is in contrast to observations of gas in the ionian atmosphere, its co-rotating plasma torus, and the neutral cloud, where sulphur species are dominant while alkali and chlorine species are only minor components. to has the largest active volcanoes of the Solar System with plumes reaching heights of more than 400 km above the moons surface. Our in situ measurements indicate that alkaline salt condensation of volcanic gases inside those plumes could be the dominant formation process for particles reaching the ionian exosphere. (c) 2006 Elsevier Inc. All rights reserved.
引用
收藏
页码:122 / 134
页数:13
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