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arXiv 1809.09131astro-ph.HEastro-ph.SR
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大尺度磁场穿过的矮新星中湍流和风驱动的吸积

Turbulent and wind-driven accretion in dwarf novae threaded by a large scale magnetic field

Nicolas Scepi, Geoffroy Lesur, Guillaume Dubus, Mario Flock

摘要:

矮新星(DNe)是吸积白矮星,由于吸积盘中的热粘性不稳定性而爆发。爆发时间尺度限制了$α$,即粘性应力与热压力的比值,从而限制了角动量输运机制。爆发状态具有PDMATHAMN,而静止状态具有$α\approx0.03$。由于磁旋转不稳定性(MRI)引起的湍流输运通常被认为是DNe中角动量输运的来源。在这里,我们进行3D本地磁流体动力学(MHD)剪切盒模拟,包括垂直分层,辐射转移和净恒定的垂直磁通量,探讨如何运输之间的变化的爆发和静止状态的DNe。我们发现,一个恒定的$B_z$提供了一个更高的$α$在平静比爆发,在相反的预期。包括电阻率会在静止时淬灭MRI湍流,抑制传输,除非磁场足够高,这再次导致$α\approx0.1$。有净极向通量的模拟和没有净极向通量的模拟之间的一个主要区别是,在前者的角动量传输之间的湍流和风驱动的运输。我们发现,即使在低磁场$\sim 1$ G。这可能会对观测信号产生重大影响,因为风驱动的运输不会加热磁盘。此外,风输运不能简化为$α$处方。我们提供适合$α$和风扭矩与$β$,热磁压力比。我们的结论是,演化的热粘性不稳定性,其后果的爆发周期的CV,需要认真修改,考虑到大部分的吸积能量可能会被带走的风,而不是被本地消散。

英文摘要:

Dwarf novae (DNe) are accreting white dwarfs that show eruptions due to a thermal-viscous instability in the accretion disk. The outburst timescales constrain $α$, the ratio of the viscous stress to the thermal pressure, and so the mechanism of angular momentum transport. The eruptive state has $α\approx0.1$ while the quiescent state has $α\approx0.03$. Turbulent transport due to the magneto-rotational instability (MRI) is generally considered to be the source of angular momentum transport in DNe. Here, we perform 3D local magnetohydrodynamic (MHD) shearing box simulations including vertical stratification, radiative transfer and a net constant vertical magnetic flux to investigate how transport changes between the outburst and quiescent states of DNe. We find that a constant $B_z$ provides a higher $α$ in quiescence than in outburst, in opposition to what is expected. Including resistivity quenches MRI turbulence in quiescence, suppressing transport, unless the magnetic field is high enough, which again leads to $α\approx0.1$. A major difference between simulations with a net poloidal flux and simulations without is that angular momentum transport in the former is shared between turbulent and wind-driven transport. We find that wind-driven transport dominates in quiescence even for low magnetic fields $\sim 1$ G. This can have a major impact on observational signatures since wind-driven transport does not heat the disk. Furthermore, wind transport cannot be reduced to an $α$ prescription. We provide fits for $α$ and the wind torque with $β$, ratio of thermal to magnetic pressure. We conclude that the evolution of the thermal-viscous instability, and its consequences on the outburst cycles of CVs, needs to be seriously revised to take into account that most of the accretion energy may be carried away by a wind instead of being locally dissipated.

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