On the survival of cool clouds in the circumgalactic medium

On the survival of cool clouds in the circumgalactic medium
复制标题

DOI:
10.1093/mnras/stz3567
复制
发表时间:
2019-09
影响因子:
4.8
通讯作者:
Zhihui Li;P. Hopkins;J. Squire;C. Hummels
Zhihui Li;P. Hopkins;J. Squire;C. Hummels
中科院分区:
物理与天体物理2区
文献类型:
--
作者:
Zhihui Li;P. Hopkins;J. Squire;C. Hummels

文献摘要

被引文献

相似文献

我们探讨了冷云在多相环星系介质中的生存。我们重新审视的“云破碎问题”在一个大的调查模拟,包括辐射冷却,自屏蔽,自重力,磁场,各向异性Braginskii传导和粘度(饱和)。我们探索了广泛的参数,包括云的大小,速度,环境温度和密度,以及各种磁场配置和云湍流。我们发现,现实的磁场和湍流对云的生存有较弱的影响,最重要的物理是辐射冷却和传导。自引力和自屏蔽对于最初是吉恩不稳定的云很重要,但在其他方面基本上无关紧要。非自引力的、实际磁化的云分为四种状态:(1)在低柱密度下,云通过传导迅速蒸发;(2)“失效压力约束”状态,即周围的热气体冷却得太快而不能为云提供压力约束;(3)“无限长寿命”状态,在这个状态下,云的寿命变得比在弓形激波中被扫过的气体的冷却时间长,因此云开始吸积和增长;(4)云最终被不稳定性破坏的“经典云破坏”机制。在最后的制度,云的寿命可以超过天真的云粉碎时间,由于传导诱导的压缩。然而,小的和/或缓慢移动的云也可以比云破碎时间更快地蒸发。我们开发了简单的分析模型,解释了模拟云破坏时间在这个政权。
We explore the survival of cool clouds in multiphase circumgalactic media. We revisit the ‘cloud-crushing problem’ in a large survey of simulations including radiative cooling, self-shielding, self-gravity, magnetic fields, and anisotropic Braginskii conduction and viscosity (with saturation). We explore a wide range of parameters including cloud size, velocity, ambient temperature and density, and a variety of magnetic field configurations and cloud turbulence. We find that realistic magnetic fields and turbulence have weaker effects on cloud survival; the most important physics is radiative cooling and conduction. Self-gravity and self-shielding are important for clouds that are initially Jeans-unstable, but largely irrelevant otherwise. Non-self-gravitating, realistically magnetized clouds separate into four regimes: (1) at low column densities, clouds evaporate rapidly via conduction; (2) a ‘failed pressure confinement’ regime, where the ambient hot gas cools too rapidly to provide pressure confinement for the cloud; (3) an ‘infinitely long-lived’ regime, in which the cloud lifetime becomes longer than the cooling time of gas swept up in the leading bow shock, so the cloud begins to accrete and grow; and (4) a ‘classical cloud destruction’ regime, where clouds are eventually destroyed by instabilities. In the final regime, the cloud lifetime can exceed the naive cloud-crushing time owing to conduction-induced compression. However, small and/or slow-moving clouds can also evaporate more rapidly than the cloud-crushing time. We develop simple analytic models that explain the simulated cloud destruction times in this regime.