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arXiv 0901.4739astro-ph.EPastro-ph.GA
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重力湍流吸积盘的性质

Properties of gravitoturbulent accretion disks

Roman R. Rafikov

摘要:

我们探索冷gravitoturbulent吸积盘的属性-非碎片盘徘徊在引力不稳定的边缘-使用一个现实的处方所造成的引力扭矩的有效粘度。这个公式是基于薄吸积盘中的角动量输运与稳定状态下吸积盘冷却之间的直接关系。假设不透明度主要是由灰尘,我们能够自洽地推导出磁盘属性为一个给定的$\dot M$假设边际引力稳定性。我们还允许外部照射的磁盘和帐户的非零背景粘度,这可能是由于MRI。不同的共存磁盘状态之间的空间转换(例如,照射和自发光或gravitoturbulent和粘性之间)的描述和磁盘必须片段的边界的位置被确定在各种情况下。我们证明,特别是在足够低的$\dot M$外部照射稳定gravitoturbulent磁盘对碎片的所有方式到无穷大,从而提供稳定的质量传输到中心对象的手段。我们的研究结果的可能性,行星形成的引力不稳定性的原行星盘和恒星形成的银河系中心和喂养的问题超大质量黑洞在星系核的影响进行了讨论。

英文摘要:

We explore the properties of cold gravitoturbulent accretion disks - non-fragmenting disks hovering on the verge of gravitational instability - using a realistic prescription for the effective viscosity caused by gravitational torques. This prescription is based on a direct relationship between the angular momentum transport in a thin accretion disk and the disk cooling in a steady state. Assuming that opacity is dominated by dust we are able to self-consistently derive disk properties for a given $\dot M$ assuming marginal gravitational stability. We also allow external irradiation of the disk and account for a non-zero background viscosity which can be due to the MRI. Spatial transitions between different co-existing disk states (e.g. between irradiated and self-luminous or between gravitoturbulent and viscous) are described and the location of the boundary at which disk must fragment is determined in a variety of situations. We demonstrate in particular that at low enough $\dot M$ external irradiation stabilizes gravitoturbulent disk against fragmentation all the way to infinity thus providing means of steady mass transport to the central object. Implications of our results for the possibility of planet formation by gravitational instability in protoplanetary disks and star formation in the Galactic Center and for the problem of feeding supermassive black holes in galactic nuclei are discussed.

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