The abundances of constituents of Titan's atmosphere from the GCMS instrument on the Huygens probe

被引:735
作者
Niemann, HB [1 ]
Atreya, SK
Bauer, SJ
Carignan, GR
Demick, JE
Frost, RL
Gautier, D
Haberman, JA
Harpold, DN
Hunten, DM
Israel, G
Lunine, JI
Kasprzak, WT
Owen, TC
Paulkovich, M
Raulin, F
Raaen, E
Way, SH
机构
[1] NASA, Greenbelt, MD 20771 USA
[2] Univ Michigan, Ann Arbor, MI 48109 USA
[3] Graz Univ, Inst Meteorol & Geophys, A-8010 Graz, Austria
[4] Observ Paris, LESIA, F-92195 Meudon, France
[5] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85716 USA
[6] CNRS, Serv Aeron, F-91371 Verrieres Le Buisson, France
[7] Univ Alabama Birmingham, CMC, Birmingham, AL 35205 USA
[8] Univ Hawaii, Honolulu, HI 96822 USA
[9] Univ Paris 12, Lab Interuniv Syst Atmospher, F-94010 Creteil, France
[10] Univ Paris 07, F-94010 Creteil, France
关键词
D O I
10.1038/nature04122
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Saturn's largest moon, Titan, remains an enigma, explored only by remote sensing from Earth, and by the Voyager and Cassini spacecraft. The most puzzling aspects include the origin of the molecular nitrogen and methane in its atmosphere, and the mechanism(s) by which methane is maintained in the face of rapid destruction by photolysis. The Huygens probe, launched from the Cassini spacecraft, has made the first direct observations of the satellite's surface and lower atmosphere. Here we report direct atmospheric measurements from the Gas Chromatograph Mass Spectrometer (GCMS), including altitude profiles of the constituents, isotopic ratios and trace species ( including organic compounds). The primary constituents were confirmed to be nitrogen and methane. Noble gases other than argon were not detected. The argon includes primordial Ar-36, and the radiogenic isotope Ar-40, providing an important constraint on the outgassing history of Titan. Trace organic species, including cyanogen and ethane, were found in surface measurements.
引用
收藏
页码:779 / 784
页数:6
相关论文
共 46 条
[1]   EVOLUTION OF A NITROGEN ATMOSPHERE ON TITAN [J].
ATREYA, SK ;
DONAHUE, TM ;
KUHN, WR .
SCIENCE, 1978, 201 (4356) :611-613
[2]   TRAPPING OF GAS-MIXTURES BY AMORPHOUS WATER ICE [J].
BARNUN, A ;
KLEINFELD, I ;
KOCHAVI, E .
PHYSICAL REVIEW B, 1988, 38 (11) :7749-7754
[3]  
Bockelée-Morvan D, 2004, SPACE SCI S, P391
[4]   Lost city life [J].
Boetius, A .
SCIENCE, 2005, 307 (5714) :1420-1422
[5]   Carbon dioxide Earth degassing and seismogenesis in central and southern Italy [J].
Chiodini, G ;
Cardellini, C ;
Amato, A ;
Boschi, E ;
Caliro, S ;
Frondini, F ;
Ventura, G .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (07) :L076151-4
[6]   TITAN ATMOSPHERE FROM VOYAGER INFRARED OBSERVATIONS .2. THE CH3D ABUNDANCE AND D/H RATIO FROM THE 900-1200CM-1 SPECTRAL REGION [J].
COUSTENIS, A ;
BEZARD, B ;
GAUTIER, D .
ICARUS, 1989, 82 (01) :67-80
[7]   Titan's atmosphere from ISO mid-infrared spectroscopy [J].
Coustenis, A ;
Salama, A ;
Schulz, B ;
Ott, S ;
Lellouch, E ;
Encrenaz, T ;
Gautier, D ;
Feuchtgruber, H .
ICARUS, 2003, 161 (02) :383-403
[8]   MONODEUTERATED METHANE IN THE OUTER SOLAR-SYSTEM .2. ITS DETECTION ON URANUS AT 1.6 MICRONS [J].
DEBERGH, C ;
LUTZ, BL ;
OWEN, T ;
BRAULT, J ;
CHAUVILLE, J .
ASTROPHYSICAL JOURNAL, 1986, 311 (01) :501-510
[9]   Cassini radar views the surface of Titan [J].
Elachi, C ;
Wall, S ;
Allison, M ;
Anderson, Y ;
Boehmer, R ;
Callahan, P ;
Encrenaz, P ;
Flamini, E ;
Franceschetti, G ;
Gim, Y ;
Hamilton, G ;
Hensley, S ;
Janssen, M ;
Johnson, W ;
Kelleher, K ;
Kirk, R ;
Lopes, R ;
Lorenz, R ;
Lunine, J ;
Muhleman, D ;
Ostro, S ;
Paganelli, F ;
Picardi, G ;
Posa, F ;
Roth, L ;
Seu, R ;
Shaffer, S ;
Soderblom, L ;
Stiles, B ;
Stofan, E ;
Vetrella, S ;
West, R ;
Wood, C ;
Wye, L ;
Zebker, H .
SCIENCE, 2005, 308 (5724) :970-974
[10]   SILICATE INTERACTIONS WITH AMMONIA-WATER FLUIDS ON EARLY TITAN [J].
ENGEL, S ;
LUNINE, JI ;
NORTON, DL .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 1994, 99 (E2) :3745-3752