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Super-Earth masses sculpted by pebble isolation around stars of different masses

机译:由不同质量恒星周围的卵石隔离雕刻的超地球质量

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We developed a pebble-driven core accretion model to study the formation and evolution of planets around stars in the stellar mass range of 0.08? M _(⊙)–1? M _(⊙). By Monte Carlo sampling of the initial conditions, the growth and migration of a large number of individual protoplanetary embryos were simulated in a population synthesis manner. We tested two hypotheses for the birth locations of embryos: at the water ice line or log-uniformly distributed over entire protoplanetary disks. Two types of disks with different turbulent viscous parameters α _( t )of 10~(?3)and 10~(?4)are also investigated to shed light on the role of outward migration of protoplanets. The forming planets are compared with the observed exoplanets in terms of mass, semimajor axis, metallicity, and water content. We find that gas giant planets are likely to form when the characteristic disk sizes are larger, the disk accretion rates are higher, the disks are more metal rich, and/or their stellar hosts are more massive. Our model shows that first, the characteristic mass of super-Earth is set by the pebble isolation mass. Super-Earth masses increase linearly with the mass of its stellar host, which corresponds to one Earth mass around a late M-dwarf star and 20 Earth masses around a solar-mass star. Second, the low-mass planets, up to 20? M _(⊕), can form around stars with a wide range of metallicities, while massive gas giant planets are preferred to grow around metal rich stars. Third, super-Earth planets that are mainly composed of silicates, with relatively low water fractions, can form from protoplanetary embryos at the water ice line in weakly turbulent disks where outward migration is suppressed. However, if the embryos are formed over a wide range of radial distances, the super-Earths would end up having a distinctive, bimodal composition in water mass. Altogether, our model succeeds in quantitatively reproducing several important observed properties of exoplanets and correlations with their stellar hosts.
机译:我们开发了一个由卵石驱动的岩心积聚模型,以研究恒星质量范围为0.08?的恒星周围行星的形成和演化。 M _(⊙)–1? M _(⊙)。通过蒙特卡洛的初始条件采样,以群体合成的方式模拟了许多单个原行星胚的生长和迁移。我们针对胚胎的出生位置测试了两个假设:在水冰线处或对数均匀地分布在整个原行星盘上。还研究了两种湍流粘性参数α_(t)为10〜(?3)和10〜(?4)的圆盘,以阐明原行星向外迁移的作用。在质量,半长轴,金属性和水含量方面,将正在形成的行星与观测到的系外行星进行比较。我们发现,当特征圆盘尺寸较大,圆盘吸积率较高,圆盘的金属含量更高和/或它们的恒星主体更大时,可能会形成气体巨行星。我们的模型表明,首先,超地球的特征质量由卵石隔离质量确定。超地球质量随恒星主体的质量线性增加,相当于晚M矮星周围的一个地球质量和太阳质量恒星周围的20个地球质量。第二,低质量的行星,最多20个? M _(⊕)可以在具有广泛金属性的恒星周围形成,而大型气体巨型行星更倾向于在富含金属的恒星周围生长。第三,主要由硅酸盐组成的水含量相对较低的超地球行星可以由水冰线处的原行星胚形成在弱湍流盘中,从而抑制了向外迁移。但是,如果胚胎在宽范围的径向距离上形成,那么超级地球最终将在水团中具有独特的双峰成分。总而言之,我们的模型成功地定量再现了系外行星的几个重要观察特性以及与它们的恒星宿主的相关性。

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