论文标题
朝着磁盘和行星的种群综合I.灰尘的演变,夹带在风和辐射压力中
Toward a Population Synthesis of Disks and Planets I. Evolution of Dust with Entrainment in Winds and Radiation Pressure
论文作者
论文摘要
毫米天文学提供了有关行星系统出生地的宝贵信息。为了将理论模型与观测进行比较,必须仔细计算灰尘成分。在这里,我们旨在研究光蒸发风中灰尘夹带的影响,以及由于中央恒星辐射引起的效果而引起的灰尘的弹出和阻力。我们改进并扩展了全球伯尔尼/海德堡星球形成和进化模型中两人群尘埃和卵石描述的现有实施。使用了光蒸发风的现代处方,在计算夹带率时,我们考虑了灰尘的沉降和对流。为了为未来的人口研究做准备,我们探索了广泛的磁盘,光蒸发 - 和尘埃参数。我们发现,如果灰尘可以生长到卵石尺寸,即,如果它们抵抗碎裂或湍流较弱,则漂移会占主导地位,并且夹带的质量小,但比在没有气流的晶粒垂直对流的情况下大。对于在实验室实验中指出的1 m/s的脆弱粉尘碎裂的情况下,将夹带更多的灰尘,这成为主要的灰尘去除过程。辐射压力效应在数量100 MYR的时间尺度上分散大量的尘土。这些结果突出了尘埃夹带在风中的重要性,这是固体质量去除过程。此外,该模型的扩展是对行星在其出生环境中形成的未来统计研究的基础。
Millimeter astronomy provides valuable information on the birthplaces of planetary systems. In order to compare theoretical models with observations, the dust component has to be carefully calculated. Here, we aim to study the effects of dust entrainment in photoevaporative winds and the ejection and drag of dust due to effects caused by radiation from the central star. We improved and extended the existing implementation of a two-population dust and pebble description in the global Bern/Heidelberg planet formation and evolution model. Modern prescriptions for photoevaporative winds were used and we account for settling and advection of dust when calculating entrainment rates. In order to prepare for future population studies with varying conditions, we explore a wide range of disk-, photoevaporation-, and dust-parameters. We find that if dust can grow to pebble sizes, that is, if they are resistant to fragmentation or turbulence is weak, drift dominates and the entrained mass is small but larger than under the assumption of no vertical advection of grains with the gas flow. For the case of fragile dust shattering at velocities of 1 m/s - as indicated in laboratory experiments -, an order of magnitude more dust is entrained which becomes the main dust removal process. Radiation pressure effects disperse massive, dusty disks on timescales of a few 100 Myr. These results highlight the importance of dust entrainment in winds as a solid mass removal process. Furthermore, this model extension lies the basis for future statistical studies of planet formation in their birth environment.