English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 80990/80990 (100%)
造訪人次 : 41633810      線上人數 : 4335
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜尋範圍 查詢小技巧:
  • 您可在西文檢索詞彙前後加上"雙引號",以獲取較精準的檢索結果
  • 若欲以作者姓名搜尋,建議至進階搜尋限定作者欄位,可獲得較完整資料
  • 進階搜尋


    請使用永久網址來引用或連結此文件: http://ir.lib.ncu.edu.tw/handle/987654321/50888


    題名: MEASUREMENTS OF ISOTOPE EFFECTS IN THE PHOTOIONIZATION OF N(2) AND IMPLICATIONS FOR TITAN'S ATMOSPHERE
    作者: Croteau,P;Randazzo,JB;Kostko,O;Ahmed,M;Liang,MC;Yung,YL;Boering,KA
    貢獻者: 天文研究所
    關鍵詞: PLANETARY-ATMOSPHERES;EXTREME-ULTRAVIOLET;CROSS-SECTIONS;ION CHEMISTRY;NITROGEN;HCN;N2;TEMPERATURE;COLLISIONS;C-12/C-13
    日期: 2011
    上傳時間: 2012-03-27 18:12:12 (UTC+8)
    出版者: 國立中央大學
    摘要: Isotope effects in the non-dissociative photoionization of molecular nitrogen (N(2) + h --> N(2)(+) + e(-)) may play a role in determining the relative abundances of isotopic species containing nitrogen in interstellar clouds and planetary atmospheres but have not been previously measured. Measurements of the photoionization efficiency spectra of (14)N(2), (15)N(14)N, and (15)N(2) from 15.5 to 18.9 eV (65.6-80.0 nm) using the Advanced Light Source at Lawrence Berkeley National Laboratory show large differences in peak energies and intensities, with the ratio of the energy-dependent photoionization cross sections, sigma((14)N(2))/sigma((15)N(14)N), ranging from 0.4 to 3.5. Convolving the cross sections with the solar flux and integrating over the energies measured, the ratios of photoionization rate coefficients are J((15)N(14)N)/J((14)N(2)) = 1.00 +/- 0.02 and J((15)N(2))/J((14)N(2)) = 1.00 +/- 0.02, suggesting that isotopic fractionation between N(2) and N(2)(+) should be small under such conditions. In contrast, in a one-dimensional model of Titan's atmosphere, isotopic self-shielding of (14)N(2) leads to values of J((15)N(14)N)/J((14)N(2)) as large as similar to 1.17, larger than under optically thin conditions but still much smaller than values as high as similar to 29 predicted for N(2) photodissociation. Since modeled photodissociation isotope effects overpredict the HC(15)N/HC(14)N ratio in Titan's atmosphere, and since both N atoms and N(2)(+) ions may ultimately lead to the formation of HCN, estimates of the potential of including N(2) photoionization to contribute to a more quantitative explanation of (15)N/(14)N for HCN in Titan's atmosphere are explored.
    關聯: ASTROPHYSICAL JOURNAL LETTERS
    顯示於類別:[天文研究所] 期刊論文

    文件中的檔案:

    檔案 描述 大小格式瀏覽次數
    index.html0KbHTML596檢視/開啟


    在NCUIR中所有的資料項目都受到原著作權保護.

    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