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Dust Settling in Magnetorotationally-Driven Turbulent Discs I: Numerical Methods and Evidence for a Vigorous Streaming Instability

机译:磁力驱动湍流盘中的尘埃沉降I:数值模拟   有力的流媒体不稳定性的方法和证据

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摘要

(Abridged) In this paper we have used the RIEMANN code for computationalastrophysics to study the interaction of a realistic distribution of dustgrains with gas in a vertically stratified protostellar accretion disc. Thedisc was modeled to have the density and temperature of a minimum mass solarnebula, and was driven to a fully-developed turbulence via themagnetorotational instability (MRI). We find that the inclusion of standarddust to gas ratios does not have any significant effect on the MRI even whenthe dust sediments to the midplane of the accretion disc. The densitydistribution of the dust reaches a Gaussian profile, and the scale heights forthe dust that we derive are shown to be proportional to the reciprocal of thesquare root of the dust radius. The largest dust shows a strong tendency tosettle to the midplane of the accretion disc, and tends to organize itself intoelongated clumps of high density. The dynamics of these clumps is shown to beconsistent with a streaming instability. The streaming instability is seen tobe very vigorous and persistent once it forms. Each stream of high density dustdisplays a reduced RMS velocity dispersion, and the densest clumpings of largedust are shown to form where the streams intersect. We have also shown that themean free path and collision time for the dust that participates in thestreaming instability is reduced by almost two orders of magnitude relative tothe average mean free paths and collision times. We show that some of the largedust in our 10 au simulations should have a propensity for grain coalescence.
机译:(摘要)在本文中,我们已使用用于计算天体物理学的RIEMANN代码研究了垂直分层的原恒星吸积盘中尘埃与气体的实际分布的相互作用。对该碟片进行建模,使其具有最小质量的太阳星云的密度和温度,并通过旋转角不稳定性(MRI)将其驱使至完全发展的湍流。我们发现,即使当灰尘沉积到吸积盘的中平面时,包含标准灰尘与气体的比例对MRI也没有任何显着影响。尘埃的密度分布达到高斯分布,并且我们得出的尘埃的标度高度与尘埃半径的平方根的倒数成正比。最大的灰尘表现出强烈的趋势,使其沉降到吸积盘的中平面,并且倾向于将自身组织成高密度的细长块。这些团块的动态显示与流不稳定性一致。一旦形成流不稳定,就可以认为它非常剧烈且持久。每个高密度粉尘流显示出降低的RMS速度分散,并且显示出最密集的大粉团在流相交的地方形成。我们还表明,相对于平均平均自由程和碰撞时间,参与流不稳定性的尘埃的自由泳道和碰撞时间减少了近两个数量级。我们表明,在我们的10 au模拟中,一些大粉尘应该具有晶粒聚结的倾向。

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