论文标题

带有灰尘成分的重力原理磁盘。 iii。气体,灰尘和鹅卵石的演变

Gravitoviscous protoplanetary disks with a dust component. III. Evolution of gas, dust, and pebbles

论文作者

Elbakyan, Vardan G., Johansen, Anders, Lambrechts, Michiel, Akimkin, Vitaly, Vorobyov, Eduard I.

论文摘要

我们研究了不同质量的不同质量的灰尘颗粒的动力学和生长,这些块在其进化的关键第一迈尔期间容易引起重力不稳定。灰尘成分由两个不同的组成部分组成:微米大小的灰尘和不断发展的大小的灰尘。对于灰尘成分,我们考虑了灰尘凝结,碎片化,与气体交换的动量交换以及灰尘自我重度。我们发现,在磁盘形成后不到100 kyr的情况下,微米大小的尘埃颗粒在磁盘内部的100 au中迅速生长,但前提是片段化速度为$ 30 \ rm〜ms〜ms^{ - 1} $。由于从周围的包膜中积聚了微灰尘颗粒,后者是微粉尘储层,因此在磁盘形成后,大约CM大小的灰尘颗粒继续存在于900 kyr中,并保持接近0.01的灰尘与气体比。我们表明,磁盘中的气体和卵石通量之间存在很强的相关性。我们发现,磁盘中鹅卵石的径向表面密度分布显示出与最小质量太阳星云(MMSN)相似的索引分布,而不管磁盘质量如何。我们还表明,模型中的气体表面密度与AT 209,HD 163296和DOAR 25系统的原星盘中灰尘的测量非常吻合。鹅卵石是在原球盘演化的早期阶段形成的。他们在地球形成过程中起着至关重要的作用。我们的圆盘模拟揭示了卵石大小颗粒的内向磁通的早期发作($ <10^5 $ yr),大约占气体质量通量的大约一百到十分之一,这似乎与圆盘的MM观察一致。 (简略)

We study the dynamics and growth of dust particles in circumstellar disks of different masses that are prone to gravitational instability during the critical first Myr of their evolution. The dust component is made up of two different components: micron-sized dust and grown dust of evolving size. For the dust component, we considered the dust coagulation, fragmentation, momentum exchange with the gas, and dust self-gravity. We found that the micron-sized dust particles grow rapidly in the circumstellar disk, reaching a few cm in size in the inner 100 au of the disk during less than 100 kyr after the disk formation, provided that fragmentation velocity is $30\rm~ms^{-1}$. Due to the accretion of micron dust particles from the surrounding envelope, which serves as a micron dust reservoir, the approximately cm-sized dust particles continue to be present in the disk for more than 900 kyr after the disk formation and maintain a dust-to-gas ratio close to 0.01. We show that a strong correlation exists between the gas and pebble fluxes in the disk. We find that radial surface density distribution of pebbles in the disk shows power-law distribution with an index similar to that of the Minimum-mass solar nebula (MMSN) regardless the disk mass. We also show that the gas surface density in our models agrees well with measurements of dust in protoplanetary disks of AS 209, HD 163296, and DoAr 25 systems. Pebbles are formed during the very early stages of protoplanetary disk evolution. They play a crucial role in the planet formation process. Our disc simulations reveal the early onset ($<10^5$ yr) of an inwards-drifting flux of pebble-sized particles that makes up approximately between one hundredth and one tenth of the gas mass flux, which appears consistent with mm-observations of discs. (Abridged)

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