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  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 1992
    In:  Journal of Magnetic Resonance (1969) Vol. 100, No. 1 ( 1992-10), p. 123-138
    In: Journal of Magnetic Resonance (1969), Elsevier BV, Vol. 100, No. 1 ( 1992-10), p. 123-138
    Type of Medium: Online Resource
    ISSN: 0022-2364
    RVK:
    RVK:
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1992
    detail.hit.zdb_id: 1469665-4
    SSG: 11
    Library Location Call Number Volume/Issue/Year Availability
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1999
    In:  Journal of Geophysical Research: Planets Vol. 104, No. E10 ( 1999-10-25), p. 24111-24120
    In: Journal of Geophysical Research: Planets, American Geophysical Union (AGU), Vol. 104, No. E10 ( 1999-10-25), p. 24111-24120
    Abstract: The satellite Enceladus is obviously the main source of Saturn's E ring. Up to now, different mechanisms of how particles are delivered from this satellite have been suggested. In this paper, we try to answer the question of whether these different launch processes can be distinguished by the cosmic dust analyzer (CDA) aboard the Cassini spacecraft. To this aim, the dynamics of dust particles just launched from the surface of Enceladus is studied numerically. We have integrated the equations of motion for a wide range of initial conditions including ejecta from interplanetary and E ring impactors onto Enceladus. According to our simulations, Cassini will encounter a significant dust stream about the time of closest approach to Enceladus. The duration and intensity of this expected enhanced impact rate onto the CDA depends on the way the particles are ejected from the satellite. The counting rate yields information about the distribution of ejecta sources on the surface of Enceladus. For instance, an anisotropy of the ejecta between the leading and the trailing hemispheres of Enceladus should be detectable, and impactors of different origin should be distinguishable. Furthermore, the vertical component of the ejecta velocities can explain the vertical extent of the E ring.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1999
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    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
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    detail.hit.zdb_id: 2403298-0
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    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
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    detail.hit.zdb_id: 2016804-4
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    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
    Library Location Call Number Volume/Issue/Year Availability
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