论文标题
超级地球的保存和气体巨人的祖细胞岩心进入卵石隔离阶段的出现
The Preservation of Super Earths and the Emergence of Gas Giants after Their Progenitor Cores have Entered the Pebble Isolation Phase
论文作者
论文摘要
超级毕业一文的无所不能表明,它们能够保留在低质量恒星周围的出生盘中,而系外行星的质量分布表明,某些核心通过太阳能型星的1AU中的1AU促进气体促进了气体巨人。在本文中,我们表明,在获得足够的质量(通常为10mearth)进入卵石 - 分离阶段之后,岩心的过渡可能会因其信封中的谷物不透明度的增加而自我影响。 MM-M大小鹅卵石在其迁移屏障中的积累提高了其局部破碎率。新鲜产生的亚MM晶粒穿过屏障,提高有效的灰尘不透明度,并减少岩心膜中的辐射通量。仅这些影响就足以抑制向失控积聚的过渡并保留恒星接近(0.1 au)的超收入,尽管包膜和磁盘之间的熵对流可以进一步降低积聚率。在与宿主恒星的中间距离(1AU)处,尘埃不透明度的升级在熵的距离上占主导地位,从而使过渡到失控的卵石相粘的核心的过渡。除了几个AU之外,在磁盘气体的严重消耗之前,可以将更大的核心转化为天然气巨头。可以通过有序地积分迁移的卵石或通过寡头原球网胚的合并来满足具有较大高度的扩展磁盘的需求,并且可以解释长期周期气体巨头和近距离超级货币的相关性。
The omnipresence of super-Earths suggests that they are able to be retained in natal disks around low-mass stars, whereas exoplanets' mass distribution indicates that some cores have transformed into gas giants through runaway gas accretion at 1AU from solar-type stars. In this paper, we show that transition to runaway gas accretion by cores may be self-impeded by an increase of the grain opacity in their envelope after they have acquired sufficient mass (typically 10Mearth) to enter a pebble-isolation phase. The accumulation of mm-m size pebbles in their migration barriers enhances their local fragmentation rates. The freshly produced sub-mm grains pass through the barrier, elevate the effective dust opacity and reduce the radiative flux in the cores envelope. These effects alone are adequate to suppress the transition to runaway accretion and preserve super-Earths in the stellar proximity (0.1 AU), albeit entropy advection between the envelope and the disk can further reduce the accretion rate. At intermediate distance (1AU) from their host stars, the escalation in the dust opacity dominates over entropy advection in stalling the transition to runaway accretion for marginally pebble-isolated cores. Beyond a few AU, the transformation of more massive cores to gas giants is reachable before severe depletion of disk gas. This requirement can be satisfied either in extended disks with large scale height via orderly accretion of migrating pebbles or through the mergers of oligarchic protoplanetary embryos, and can account for the correlated occurrence of long-period gas giants and close-in super-Earths.