THE FORMATION OF CORES OF GIANT PLANETS AT CONVERGENCE ZONES OF PLANETARY MIGRATION

被引:0
|
作者
Sirono, Sin-iti [1 ]
Katayama, Masahumi [1 ]
机构
[1] Nagoya Univ, Earth & Planetary Sci, Tikusa Ku, Furo Cho, Nagoya, Aichi 4648601, Japan
来源
ASTROPHYSICAL JOURNAL | 2016年 / 830卷 / 02期
关键词
methods: numerical; planet-disk interactions; planets and satellites: formation; protoplanetary disks; DEAD ZONE; DISKS; ACCRETION; SIMULATIONS; BODIES; DISCS;
D O I
10.3847/0004-637X/830/2/65
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The formation of solid cores in giant planets of mass similar to 10 M-circle plus numerically simulated following the scenario of Sandor et al. In this scenario, there are two convergence zones, corresponding to the outer and inner edges of the dead zone, where the torque exerted on planetary embryos by the gas nebula is zero. At the outer edge of the dead zone, anticyclonic vortices accumulate infalling dust aggregates, and planetary embryos are continuously formed in this scenario. We performed N-body simulations and show that massive objects of similar or equal to 10 M-circle plus are formed in similar to 2.5 Myr, starting from the embryos. The largest object is formed at the inner convergence zone, although planetary embryos are placed at the outer convergence zone. This is due to the scattering of embryos from the outer to the inner convergence zone, and the shorter damping timescale of eccentricity at the inner convergence zone compared to the outer one. We varied the migration timescale due to the torque from gas by changing the gas surface density around the convergence zones. We found that there is a critical migration timescale below which 10 M-circle plus-sized objects are formed. Furthermore, we conducted simulations in which the gas surface density evolves according to viscous accretion. The largest object is also formed at the inner convergence zone irrespective of the strength of turbulence. Throughout the simulations, the location of the largest mass is the inner convergence zone. We confirmed that the formation timescale of a core of a Jovian planet can be explained in this scenario.
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页数:11
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