DEUTERIUM BURNING IN MASSIVE GIANT PLANETS AND LOW-MASS BROWN DWARFS FORMED BY CORE-NUCLEATED ACCRETION

被引:53
|
作者
Bodenheimer, Peter [1 ]
D'Angelo, Gennaro [2 ,5 ]
Lissauer, Jack J. [2 ]
Fortney, Jonathan J. [3 ]
Saumon, Didier [4 ]
机构
[1] Univ Calif Santa Cruz, Dept Astron & Astrophys, UCO Lick Observ, Santa Cruz, CA 95064 USA
[2] NASA, Ames Res Ctr, Space Sci & Astrobiol Div, Moffett Field, CA 94035 USA
[3] Univ Calif Santa Cruz, Dept Astron & Astrophys, Santa Cruz, CA 95064 USA
[4] Los Alamos Natl Lab, Los Alamos, NM 87545 USA
[5] SETI Inst, Mountain View, CA 94043 USA
来源
ASTROPHYSICAL JOURNAL | 2013年 / 770卷 / 02期
基金
美国国家科学基金会;
关键词
accretion; accretion disks; brown dwarfs; planets and satellites: formation; planets and satellites: individual (beta Pictoris b); planets and satellites: physical evolution; PROTOPLANETARY ATMOSPHERES; BETA-PICTORIS; HR; 8799; EVOLUTION; JUPITER; MODELS; OPACITIES; GRAINS; DISKS; GAS;
D O I
10.1088/0004-637X/770/2/120
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Using detailed numerical simulations, we study the formation of bodies near the deuterium-burning limit according to the core-nucleated giant planet accretion scenario. The objects, with heavy-element cores in the range 5-30 M-circle plus, are assumed to accrete gas up to final masses of 10-15 Jupiter masses (M-Jup). After the formation process, which lasts 1-5 Myr and which ends with a "cold-start," low-entropy configuration, the bodies evolve at constant mass up to an age of several Gyr. Deuterium burning via proton capture is included in the calculation, and we determined the mass, M-50, above which more than 50% of the initial deuterium is burned. This often-quoted borderline between giant planets and brown dwarfs is found to depend only slightly on parameters, such as core mass, stellar mass, formation location, solid surface density in the protoplanetary disk, disk viscosity, and dust opacity. The values for M-50 fall in the range 11.6-13.6 M-Jup, in agreement with previous determinations that do not take the formation process into account. For a given opacity law during the formation process, objects with higher core masses form more quickly. The result is higher entropy in the envelope at the completion of accretion, yielding lower values of M-50. For masses above M-50, during the deuterium-burning phase, objects expand and increase in luminosity by one to three orders of magnitude. Evolutionary tracks in the luminosity versus time diagram are compared with the observed position of the companion to Beta Pictoris.
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页数:13
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共 31 条
  • [1] THE DEUTERIUM-BURNING MASS LIMIT FOR BROWN DWARFS AND GIANT PLANETS
    Spiegel, David S.
    Burrows, Adam
    Milsom, John A.
    [J]. ASTROPHYSICAL JOURNAL, 2011, 727 (01):
  • [2] Deuterium burning in objects forming via the core accretion scenario Brown dwarfs or planets?
    Molliere, P.
    Mordasini, C.
    [J]. ASTRONOMY & ASTROPHYSICS, 2012, 547
  • [3] Connecting the dots: Low-mass stars, brown dwarfs, and planets
    Cruz, Kelle
    [J]. NEW HORIZONS IN ASTRONOMY: FRANK N. BASH SYMPOSIUM 2007, 2008, 393 : 51 - 60
  • [4] The properties of brown dwarfs and low-mass hydrogen-burning stars formed by disc fragmentation
    Stamatellos, Dimitris
    Whitworth, Anthony P.
    [J]. MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY, 2009, 392 (01) : 413 - 427
  • [5] Spitzer:: Accretion in low-mass stars and brown dwarfs in the λ orionis cluster
    Navascues, David Barrado Y.
    Stauffer, John R.
    Morales-Calderon, Maria
    Bayo, Amelia
    Fazzio, Giovanni
    Megeath, Tom
    Allen, Lori
    Hartmann, Lee W.
    Calvet, Nuria
    [J]. ASTROPHYSICAL JOURNAL, 2007, 664 (01): : 481 - 500
  • [6] A Review on Substellar Objects below the Deuterium Burning Mass Limit: Planets, Brown Dwarfs or What?
    Caballero, Jose A.
    [J]. GEOSCIENCES, 2018, 8 (10)
  • [7] A STATISTICAL ANALYSIS OF SEEDS AND OTHER HIGH-CONTRAST EXOPLANET SURVEYS: MASSIVE PLANETS OR LOW-MASS BROWN DWARFS?
    Brandt, Timothy D.
    McElwain, Michael W.
    Turner, Edwin L.
    Mede, Kyle
    Spiegel, David S.
    Kuzuhara, Masayuki
    Schlieder, Joshua E.
    Wisniewski, John P.
    Abe, L.
    Biller, B.
    Brandner, W.
    Carson, J.
    Currie, T.
    Egner, S.
    Feldt, M.
    Golota, T.
    Goto, M.
    Grady, C. A.
    Guyon, O.
    Hashimoto, J.
    Hayano, Y.
    Hayashi, M.
    Hayashi, S.
    Henning, T.
    Hodapp, K. W.
    Inutsuka, S.
    Ishii, M.
    Iye, M.
    Janson, M.
    Kandori, R.
    Knapp, G. R.
    Kudo, T.
    Kusakabe, N.
    Kwon, J.
    Matsuo, T.
    Miyama, S.
    Morino, J. -I.
    Moro-Martin, A.
    Nishimura, T.
    Pyo, T. -S.
    Serabyn, E.
    Suto, H.
    Suzuki, R.
    Takami, M.
    Takato, N.
    Terada, H.
    Thalmann, C.
    Tomono, D.
    Watanabe, M.
    Yamada, T.
    [J]. ASTROPHYSICAL JOURNAL, 2014, 794 (02):
  • [8] Atmospheric chemistry in giant planets, brown dwarfs, and low-mass dwarf stars. II. Sulfur and phosphorus
    Visscher, Channon
    Lodders, Katharina
    Fegley, Bruce, Jr.
    [J]. ASTROPHYSICAL JOURNAL, 2006, 648 (02): : 1181 - 1195
  • [9] Atmospheric chemistry in giant planets, brown dwarfs, and low-mass dwarf stars - I. Carbon, nitrogen and oxygen
    Lodders, K
    Fegley, B
    [J]. ICARUS, 2002, 155 (02) : 393 - 424
  • [10] RV survey for planets of brown dwarfs and very low-mass stars in Cha I
    Joergens, V
    Neuhäuser, R
    [J]. TOWARDS OTHER EARTHS: DARWIN/TPF AND THE SEARCH FOR EXTRASOLAR TERRESTRIAL PLANETS, PROCEEDINGS, 2003, 539 : 455 - 458