中大學術數位典藏-NCU Institutional Repository-提供博碩士論文、考古題、期刊論文、研究計畫等下載:Item 987654321/101081
English  |  正體中文  |  简体中文  |  全文笔数/总笔数 : 94274/94274 (100%)
造访人次 : 82915352      在线人数 : 2317
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜寻范围 查询小技巧:
  • 您可在西文检索词汇前后加上"双引号",以获取较精准的检索结果
  • 若欲以作者姓名搜寻,建议至进阶搜寻限定作者字段,可获得较完整数据
  • 进阶搜寻


    jsp.display-item.identifier=請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/101081


    题名: A sublimation-driven exospheric model of ceres
    作者: 葉永烜;Tu, L.;Ip, W.-H.;Wang, Y.-C.
    贡献者: 理學院天文研究所
    关键词: Assessments;Ballistic transport;Ceres;Cold trap;Cold traps;Dawn mission;Exosphere;Hard surfacing;Implantation;Meteoroids;Micrometeoroid bombardment;Outgassing;Surface chemistry;Thermal model;Water vapor
    日期: 2014-01-01
    上传时间: 2026-04-21 14:22:48 (UTC+8)
    出版者: Elsevier Ltd.;Elsevier Ltd
    摘要: 摘要: After Vesta, the NASA Dawn spacecraft will visit the dwarf planet Ceres to carry out in-depth observations of its surface morphology and mineralogical composition in 2015. One of the important questions is whether Ceres has any outgassing activity that would lead to the formation of a thin atmosphere. The recent detection of water vapor emitted from localized source regions by Herschel (Küppers et al., 2014) has only underscored this point. If the localized outgassing activity observed by Herschel is totally switched off, could a sizable surface-bounded exosphere still be maintained by other source mechanisms? Our preliminary assessment is that chemical sputtering via solar wind interaction and meteoroid impact are probably not adequate because of the large injection speed of the gas at production relative to the surface escape velocity of Ceres. One potential source is a low-level outgassing effect from its subsurface due to thermal sublimation with a production rate of the order of 1024 molecules s−1 as first considered by Fanale and Salvail (1989). If the water plumes are active, the fall-back of some of the water vapor onto Ceres’ surface would provide an additional global source of water molecules on the surface with a production rate of about 1025 molecules s−1. In this work, different scenarios of building up a tenuous exosphere by ballistic transport and the eventual recycling of the water molecules to the polar cold trap are described. It turns out that a large fraction of the exospheric water could be transferred to the polar caps area as originally envisaged for the lunar polar ice storage. •Description of the global exospheric structures during Ceres׳ active outgassing condition and inactive outgassing condition, respectively.•The ballistic transport of the emitted water molecules to the polar regions could be effective in forming ice caps on Ceres.
    出版者: Elsevier Ltd
    出版日期: 2014-12
    出處: Planetary and space science, 2014-12, Vol.104, p.157-162
    資源來源: Elsevier ScienceDirect Journals Complete
    版權: 2014 Elsevier Ltd
    識別號: ISSN: 0032-0633
    識別號: EISSN: 1873-5088
    識別號: DOI: 10.1016/j.pss.2014.09.002
    显示于类别:[天文研究所] 期刊論文

    文件中的档案:

    档案 描述 大小格式浏览次数
    index.html0KbHTML17检视/开启


    在NCUIR中所有的数据项都受到原著作权保护.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明