Models of the protosatellite disk of Saturn: Conditions for Titan’s formation

被引:0
|
作者
A. B. Makalkin
V. A. Dorofeeva
机构
[1] Russian Academy of Sciences,Schmidt Institute of Physics of the Earth
[2] Russian Academy of Sciences,Vernadsky Institute of Geochemistry and Analytical Chemistry
来源
Solar System Research | 2006年 / 40卷
关键词
96.10.+I; 96.12.Bc; 96.25.Vt; 96.30.nd;
D O I
暂无
中图分类号
学科分类号
摘要
Models of the protosatellite accretion disk of Saturn are developed that satisfy cosmochemical constraints on the volatile abundances in the atmospheres of Saturn and Titan with due regard for the data obtained with the Cassini orbiter and the Huygens probe, which landed on Titan in January 2005. All basic sources of heating of the disk and protosatellite bodies are taken into account in the models, namely, dissipation of turbulence in the disk, accretion of gaseous and solid material onto the disk from the feeding zone of Saturn in the solar nebula, and heating by the radiation of young Saturn and thermal radiation of the surrounding region of the solar nebula. Two-dimensional (axisymmetric) temperature, pressure, and density distributions are calculated for the protosatellite disk. The distributions satisfy the cosmochemical constraints on the disk temperature, according to which the temperature at the stage of the satellite formation ranged from 60–65 K to 90–100 K at pressures from 10−7 to −10−4 bar in the zone of Titan’s formation (according to estimates, r = 20–35RSat). Variations of the basic input parameters (the accretion rate onto the protosatellite disk of Saturn from the feeding zone of the planet Ṁ; the parameter α characterizing turbulent viscosity of the disk; and the mass concentration ratio in the solid/gas system) satisfying the aforementioned temperature constraint are found. The spectrum of models satisfying the cosmochemical constraints covers a considerable range of consistent parameters. A model with a rather small flux of Ṁ = 10−8MSat/ yr and a tenfold depletion of Saturn’s disk in gas due to gas scattering from the solar nebula is at one side of this range. A model with a much higher flux of Ṁ = 10−6MSat/yr and a hundredfold decrease in opacity of the disk matter owing to decreased concentration of dust particles and/or their agglomeration into large aggregates and sweeping up by planetesimals is at the other side of the range.
引用
收藏
页码:441 / 455
页数:14
相关论文
共 50 条
  • [41] Simulation of tides in hydrocarbon lakes on Saturn’s moon Titan
    Tetsuya Tokano
    Ocean Dynamics, 2010, 60 : 803 - 817
  • [42] Erosion on saturn's moon Titan - Analyses of the distribution, morphology, and spectral properties of Titan's fluvial valleys
    Langhans, Mirjam
    DLR Deutsches Zentrum fur Luft- und Raumfahrt e.V. - Forschungsberichte, 2011, (07): : 1 - 118
  • [43] Radarclinometry of the sand seas of Africa's Namibia and Saturn's moon Titan
    Neish, Catherine D.
    Lorenz, Ralph D.
    Kirk, Randolph L.
    Wye, Lauren C.
    ICARUS, 2010, 208 (01) : 385 - 394
  • [44] Formation of terrestrial planets in a dissipating gas disk with Jupiter and Saturn
    Kominami, J
    Ida, S
    ICARUS, 2004, 167 (02) : 231 - 243
  • [45] Phase Trapping in Acetonitrile, a Metastable Mineral for Saturn's Moon Titan
    Choi, Ka Yik
    Duyker, Samuel G.
    Maynard-Casely, Helen E.
    Kennedy, Brendan J.
    ACS EARTH AND SPACE CHEMISTRY, 2020, 4 (08): : 1324 - 1331
  • [46] Titan interaction with Saturn's magnetosphere:: mass loading and ionopause location
    Sittler, EC
    Hartle, RE
    Viñas, AF
    Johnson, RE
    Smith, HT
    Mueller-Wodard, I
    PROCEEDINGS OF THE INTERNATIONAL CONFERENCE TITAN: FROM DISCOVERY TO ENCOUNTER, 2004, : 377 - 394
  • [47] GEOC 11-Lakes of hydrocarbons on Saturn's moon Titan
    Lorenz, Ralph D.
    ABSTRACTS OF PAPERS OF THE AMERICAN CHEMICAL SOCIETY, 2009, 238
  • [48] Challenges and approaches to the robotic detection of enantioenrichment on Saturn's Moon, Titan
    Welch, CJ
    Lunine, JI
    ENANTIOMER, 2001, 6 (2-3): : 69 - +
  • [49] The Origin and Evolution of Saturn's Earth-like Moon, Titan
    Atreya, Sushil K.
    SERENDIPITIES IN THE SOLAR SYSTEM AND BEYOND, 2018, 513 : 149 - 161
  • [50] Saturn's Titan: Surface change, ammonia, and implications for atmospheric and tectonic activity
    Nelson, R. M.
    Kamp, L. W.
    Matson, D. L.
    Irwin, P. G. J.
    Baines, K. H.
    Boryta, M. D.
    Leader, F. E.
    Jaumann, R.
    Smythe, W. D.
    Sotin, C.
    Clark, R. N.
    Cruikshank, D. P.
    Drossart, P.
    Pearl, J. C.
    Hapke, B. W.
    Lunine, J.
    Combes, M.
    Bellucci, G.
    Bibring, J. -P.
    Capaccioni, F.
    Cerroni, P.
    Coradini, A.
    Formisano, V.
    Filacchione, G.
    Langevin, R. Y.
    McCord, T. B.
    Mennella, V.
    Nicholson, P. D.
    Sicardy, B.
    ICARUS, 2009, 199 (02) : 429 - 441