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    請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/101397


    題名: The organic-rich surface of comet 67P/Churyumov-Gerasimenko as seen by VIRTIS/Rosetta
    作者: 葉永烜;Capaccioni, F.;Coradini, A.;Filacchione, G.;Erard, S.;Arnold, G.;Drossart, P.;De Sanctis, M. C.;Bockelee-Morvan, D.;Capria, M. T.;Tosi, F.;Leyrat, C.;Schmitt, B.;Quirico, E.;Cerroni, P.;Mennella, V.;Raponi, A.;Ciarniello, M.;McCord, T.;Moroz, L.;Palomba, E.;Ammannito, E.;Barucci, M. A.;Bellucci, G.;Benkhoff, J.;Bibring, J. P.;Blanco, A.;Blecka, M.;Carlson, R.;Carsenty, U.;Colangeli, L.;Combes, M.;Combi, M.;Crovisier, J.;Encrenaz, T.;Federico, C.;Fink, U.;Fonti, S.;Ip, W. H.;Irwin, P.;Jaumann, R.;Kuehrt, E.;Langevin, Y.;Magni, G.;Mottola, S.;Orofino, V.;Palumbo, P.;Piccioni, G.;Schade, U.;Taylor, F.;Tiphene, D.;Tozzi, G. P.;Beck, P.;Biver, N.;Bonal, L.;Combe, J.-Ph;Despan, D.;Flamini, E.;Fornasier, S.;Frigeri, A.;Grassi, D.;Gudipati, M.;Longobardo, A.;Markus, K.;Merlin, F.;Orosei, R.;Rinaldi, G.;Stephan, K.;Cartacci, M.;Cicchetti, A.;Giuppi, S.;Hello, Y.;Henry, F.;Jacquinod, S.;Noschese, R.;Peter, G.;Politi, R.;Reess, J. M.;Semery, A.
    貢獻者: 理學院天文研究所
    關鍵詞: Absorption;Albedo;Astrophysics;Chemical compounds;Comet nuclei;Comets;Hydrogen;image analysis;Micrometers;minerals;Physics;Planetology;reflectance;Slopes;Spacecraft;Spectra;Spectrometers;Surface chemistry
    日期: 2015-01-23
    上傳時間: 2026-04-21 14:32:37 (UTC+8)
    出版者: American Association for the Advancement of Science;Washington: American Association for the Advancement of Science (AAAS)
    摘要: 摘要: The VIRTIS (Visible, Infrared and Thermal Imaging Spectrometer) instrument on board the Rosetta spacecraft has provided evidence of carbon-bearing compounds on the nucleus of the comet 67P/Churyumov-Gerasimenko. The very low reflectance of the nucleus (normal albedo of 0.060 ± 0.003 at 0.55 micrometers), the spectral slopes in visible and infrared ranges (5 to 25 and 1.5 to 5% kÅ−1), and the broad absorption feature in the 2.9-to-3.6–micrometer range present across the entire illuminated surface are compatible with opaque minerals associated with nonvolatile organic macromolecular materials: a complex mixture of various types of carbon-hydrogen and/or oxygen-hydrogen chemical groups, with little contribution of nitrogen-hydrogen groups. In active areas, the changes in spectral slope and absorption feature width may suggest small amounts of water-ice. However, no ice-rich patches are observed, indicating a generally dehydrated nature for the surface currently illuminated by the Sun.
    出版者: Washington: American Association for the Advancement of Science (AAAS)
    出版日期: 2015-01-23
    出處: Science, 2015-01, Vol.347 (6220), p.aaa0628--aaa0628
    資源來源: American Association for the Advancement of Science
    版權: Copyright © 2015, American Association for the Advancement of Science
    版權: CC0 1.0 - Universal
    識別號: ISSN: 0036-8075
    識別號: ISSN: 1095-9203
    識別號: EISSN: 1095-9203
    識別號: DOI: 10.1126/science.aaa0628
    識別號: CODEN: SCIEAS
    顯示於類別:[天文研究所] 期刊論文

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