论文标题
在三维磁性水力动力学模拟中的灰尘颗粒的实现:崩溃的云芯中的灰尘动态
Implementation of dust particles in three-dimensional magnetohydrodynamics simulation: Dust dynamics in a collapsing cloud core
论文作者
论文摘要
这项研究的目的是大规模检查灰尘动态,并在恒星形成过程中研究灰尘与气体的耦合。我们提出了一种计算重力塌陷云中粉尘轨迹的方法,在该云中,粉尘晶粒被视为拉格朗日颗粒,并被认为是中性的。我们将粉尘轨迹计算与非理想的磁流失动力学模拟结合使用。我们的仿真表明,大小为$ \ le 10 \,{\rmμm} $的灰尘颗粒与在星形云芯中的气体结合。我们调查了尘埃气质量比和stokes数的时间演变,该数字定义为自由度时间尺度标准化的停止时间,并表明大灰尘谷物($ \ gtrsim 100 \,{\ rmμm} $)在中央区域(即接近unity)(即倾向于旋转),依靠范围(即倾向),依然繁殖。谷物($ \ Lessim 10 \,{\ rmμm} $)。因此,大谷物会显着增加磁盘周围和内部的尘埃气质量比。我们还确认,尘埃轨迹计算(追踪每个灰尘颗粒的物理量)再现了先前报道的使用Eulerian方法获得的结果。
The aim of this study is to examine dust dynamics on a large scale and investigate the coupling of dust with gas fluid in the star formation process. We propose a method for calculating the dust trajectory in a gravitationally collapsing cloud, where the dust grains are treated as Lagrangian particles and are assumed to be neutral. We perform the dust trajectory calculations in combination with non-ideal magnetohydrodynamics simulation. Our simulation shows that dust particles with a size of $\le 10\,{\rm μm}$ are coupled with gas in a star-forming cloud core. We investigate the time evolution of the dust-to-gas mass ratio and the Stokes number, which is defined as the stopping time normalized by the freefall time-scale, and show that large dust grains ($\gtrsim 100\,{\rm μm}$) have a large Stokes number (close to unity) and tend to concentrate in the central region (i.e., protostar and rotationally supported disk) faster than do small grains ($\lesssim 10\,{\rm μm}$). Thus, large grains significantly increase the dust-to-gas mass ratio around and inside the disk. We also confirm that the dust trajectory calculations, which trace the physical quantities of each dust particle, reproduce previously reported results obtained using the Eulerian approach.