摘要
As a result of electron impact dissociation and electron dissociative recombination, nitrogen atoms could be ejected from the exosphere of Titan representing an efficient way of non-thermal atmospheric escape. In this study, the corresponding formation of a nitrogen torus in the magnetospheric system of Saturn is simulated. The number density of the nitrogen atoms in a narrow gas ring near the orbit of Titan is estimated to be on the order of 3-20 atoms cm-3 while a much more diffuse nitrogen cloud covers the whole Saturnian system. Because of the small kinetic energy of the atomic nitrogen fragments at production, only a very small density can be maintained in most parts of the magnetosphere. The ionization of the nitrogen atoms in this extended gas torus could nevertheless introduce an appreciable amount of N+ ions into the Saturnian magnetosphere. A similar extended structure of an atomic nitrogen cloud is produced in the Neptunian system as a result of the nonthermal escape of nitrogen atoms from Triton. The peak density near Triton's orbit is estimated to be 10-20 atoms cm-3.
原文 | ???core.languages.en_GB??? |
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頁(從 - 到) | 73-79 |
頁數 | 7 |
期刊 | Advances in Space Research |
卷 | 12 |
發行號 | 8 |
DOIs | |
出版狀態 | 已出版 - 8月 1992 |