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arXiv 1402.4162astro-ph.EP
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原行星盘浮力共振的解析模型

An Analytic Model for Buoyancy Resonances in Protoplanetary Disks

Stephen H. Lubow, Zhaohuan Zhu

摘要:

Zhu,Stone和Rafikov(2012)在3D剪切箱模拟中发现了一种新形式的行星-磁盘相互作用,他们将其归因于磁盘中的垂直浮力共振。我们描述了这种相互作用的分析线性模型。我们采用了一个简化的模型,涉及方位强迫产生的共振,并允许其结构的分析描述。我们推导出的浮力扭矩的解析表达式,并表明,垂直扭矩分布与雅典娜模拟和傅立叶方法进行线性数值计算的结果一致,具有相同的迫使。浮力共振与经典的Lindblad共振和共转共振的不同之处在于共振沿着倾斜的平面。它的宽度取决于阻尼效应,与气体声速无关。共振不激发传播波。在给定的大方位波数k_y > 1/h(对于圆盘厚度h)下,浮力共振在径向上比Lindblad共振更靠近共转半径的区域上施加力矩。由于转矩局部化到激励区域,因此它潜在地受到非线性饱和的影响。此外,可以通过谐振区域与其周围环境之间的辐射热传递的效应来减小扭矩。对于每个方位波数,共振在盘中的平面中建立大尺度密度波图案。

英文摘要:

Zhu, Stone, and Rafikov (2012) found in 3D shearing box simulations a new form of planet-disk interaction that they attributed to a vertical buoyancy resonance in the disk. We describe an analytic linear model for this interaction. We adopt a simplified model involving azimuthal forcing that produces the resonance and permits an analytic description of its structure. We derive an analytic expression for the buoyancy torque and show that the vertical torque distribution agrees well with results of Athena simulations and a Fourier method for linear numerical calculations carried out with the same forcing. The buoyancy resonance differs from the classic Lindblad and corotation resonances in that the resonance lies along tilted planes. Its width depends on damping effects and is independent of the gas sound speed. The resonance does not excite propagating waves. At a given large azimuthal wavenumber k_y > 1/h (for disk thickness h), the buoyancy resonance exerts a torque over a region that lies radially closer to the corotation radius than the Lindblad resonance. Because the torque is localized to the region of excitation, it is potentially subject to the effects of nonlinear saturation. In addition, the torque can be reduced by the effects of radiative heat transfer between the resonant region and its surroundings. For each azimuthal wavenumber, the resonance establishes a large scale density wave pattern in a plane within the disk.

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