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arXiv 0909.0505astro-ph.EP
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死区中的水动力运动

On Hydrodynamic Motions in Dead Zones

Jeffrey S. Oishi, Mordecai-Mark Mac Low

摘要:

本文研究了具有高阻中平面的垂直分层吸积盘中平面附近的流体运动。在这样的磁盘中,磁旋转不稳定性在电阻性稳定死区周围的薄层中驱动湍流。湍流层又驱动死区中的运动。我们研究这些运动的性质,使用三维的,分层的,本地的,剪切盒,非理想的,磁流体动力学模拟。虽然在活动区的湍流提供了一个源的涡的中平面,没有证据的相干涡被发现在我们的模拟。这似乎是由于死区中强烈的垂直振荡造成的。通过分析方位平均流量的时间序列,我们确定了一个轴对称波模式特有的模型与死区。通过将状态方程从等温变为理想状态,这种模式的振幅减小,但并没有完全抑制。这些波的频率太低,无法影响尘埃向中面的沉降,但可能对由此产生的中面尘埃层的引力稳定性有重要意义。

英文摘要:

We investigate fluid motions near the midplane of vertically stratified accretion disks with highly resistive midplanes. In such disks, the magnetorotational instability drives turbulence in thin layers surrounding a resistive, stable dead zone. The turbulent layers in turn drive motions in the dead zone. We examine the properties of these motions using three-dimensional, stratified, local, shearing-box, non-ideal, magnetohydrodynamical simulations. Although the turbulence in the active zones provides a source of vorticity to the midplane, no evidence for coherent vortices is found in our simulations. It appears that this is because of strong vertical oscillations in the dead zone. By analyzing time series of azimuthally-averaged flow quantities, we identify an axisymmetric wave mode particular to models with dead zones. This mode is reduced in amplitude, but not suppressed entirely, by changing the equation of state from isothermal to ideal. These waves are too low-frequency to affect sedimentation of dust to the midplane, but may have significance for the gravitational stability of the resulting midplane dust layers.

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