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arXiv 0812.0365astro-ph
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几何薄黑洞吸积过程的时变性研究II:粘性诱导的全局振荡模

On the Time Variability of Geometrically-Thin Black Hole Accretion Disks II: Viscosity-Induced Global Oscillation Modes in Simulated Disks

Sean M. O'Neill, Christopher S. Reynolds, M. Coleman Miller

摘要:

我们研究了模拟黑洞吸积盘中粘性诱导盘震模的演化和影响。了解这种振荡的起源和行为将有助于我们评估它们在产生天文观测到的吸积黑洞双星系统的高频准周期振荡中的潜在作用。我们模拟的圆盘是几何上薄的,具有恒定的半厚度,为最内层稳定圆形轨道半径的5%。伪牛顿势再现了广义相对论的相关效应,α模型粘性实现了角动量输运和正交速度分量的耦合,否则理想的流体动力学数值处理。我们发现,我们模拟的粘性磁盘的特性发展和保持捕获的全球模式振荡的特性类似于预期的捕获的g-模式和内部p-模式在一个狭窄的范围内的频率低于最大径向周转频率。虽然模式驱动的内部部分的磁盘,他们产生的波传播的陷阱模式的频率到更大的磁盘半径。这一发现与全球磁流体动力学磁盘模拟的结果相比,这种振荡不容易识别。这样的例子强调吸积系统驱动的磁旋转不稳定性和那些α粘度作为代理的物理过程,驱动吸积之间的根本物理差异,我们探索潜在的方法来搜索diskoseismic模式在全磁流体动力磁盘。

英文摘要:

We examine the evolution and influence of viscosity-induced diskoseismic modes in simulated black hole accretion disks. Understanding the origin and behavior of such oscillations will help us to evaluate their potential role in producing astronomically observed high-frequency quasi-periodic oscillations in accreting black hole binary systems. Our simulated disks are geometrically-thin with a constant half-thickness of five percent the radius of the innermost stable circular orbit. A pseudo-Newtonian potential reproduces the relevant effects of general relativity, and an alpha-model viscosity achieves angular momentum transport and the coupling of orthogonal velocity components in an otherwise ideal hydrodynamic numerical treatment. We find that our simulated viscous disks characteristically develop and maintain trapped global mode oscillations with properties similar to those expected of trapped g-modes and inner p-modes in a narrow range of frequencies just below the maximum radial epicyclic frequency. Although the modes are driven in the inner portion of the disk, they generate waves that propagate at the trapped mode frequencies out to larger disk radii. This finding is contrasted with the results of global magnetohydrodynamic disk simulations, in which such oscillations are not easily identified. Such examples underscore fundamental physical differences between accretion systems driven by the magneto-rotational instability and those for which alpha viscosity serves as a proxy for the physical processes that drive accretion, and we explore potential approaches to the search for diskoseismic modes in full magnetohydrodynamic disks.

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