Formation of terrestrial planet cores inside giant planet embryos

被引:42
|
作者
Nayakshin, Sergei [1 ]
机构
[1] Univ Leicester, Dept Phys & Astron, Leicester LE1 7RH, Leics, England
关键词
planets and satellites: formation; planet-disc interactions; RADIATION HYDRODYNAMIC MODEL; PROTOPLANETARY DISKS; SOLAR NEBULA; GRAVITATIONAL-INSTABILITY; PROTOSTELLAR COLLAPSE; GRAIN SEDIMENTATION; GASEOUS PROTOPLANET; DISCS; FRAGMENTATION; ACCRETION;
D O I
10.1111/j.1365-2966.2011.18230.x
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Giant planet embryos are believed to be spawned by gravitational instability in massive extended (R similar to 100 au) protostellar discs. In a recent paper, we have shown that dust can sediment inside the embryos, as argued earlier by Boss in a slightly different model. Here we study numerically the next stage of this process - the formation of a solid core. If conditions are conducive to solid core formation, the centre of the gas cloud goes through the following sequence of phases: (i) becomes grain (and metal) rich; (ii) forms a terrestrial mass solid core via a rapid collapse driven by self-gravity of the grains; (iii) starts to accrete a gaseous atmosphere when the solid core reaches mass of a few to 10 Earth masses. This sequence of events may build either terrestrial planet cores or metal-rich giant planets inside the larger gas reservoir of the giant planet embryo. In a companion letter we argue that tidal and irradiation effects from the parent star should disrupt the outer metal-poor layers of the embryo, releasing nearly 'ready to use' planets. We propose this as an alternative way to build planets.
引用
收藏
页码:1462 / 1478
页数:17
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