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arXiv 0902.4487physics.flu-dyn
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湍流Rayleigh-B{é}nard对流大尺度环流振荡的原因

The cause of oscillations of the large-scale circulation of turbulent Rayleigh-B{é}nard convection

Eric Brown, Guenter Ahlers

摘要:

与最近的实验发现夏等。(2009),我们还在纵横比为1的圆柱形样品中湍流瑞利-贝纳德对流的大尺度环流(LSC)实验中发现了晃动模式。晃动模式与Funfschilling和Ahlers(2004)发现的扭转振荡具有相同的频率。我们表明,这两种模式都可以通过以前开发的模型的扩展来描述[Brown和Ahlers(2008)],该模型包括允许LSC循环平面远离样品垂直中心线的横向位移以及位移随高度的变化(原始模型中排除了这种位移)。由容器的侧壁产生的压力梯度平均地使LSC的平面居中,使得其优选地达到其最长直径。如果LSC远离该直径移位,则壁提供回复力。湍流波动驱动LSC远离中心对准,并且与回复力结合,它们导致振荡。这些振荡与LSC一起平流。该模型预测正确的波数和相位的振荡,以及频率,振幅和位移的概率分布的估计。

英文摘要:

In agreement with a recent experimental discovery by Xia et. al. (2009), we also find a sloshing mode in experiments on the large-scale circulation (LSC) of turbulent Rayleigh-Benard convection in a cylindrical sample of aspect ratio one. The sloshing mode has the same frequency as the torsional oscillation discovered by Funfschilling and Ahlers (2004). We show that both modes can be described by an extension of a model developed previously [Brown and Ahlers (2008)] which consists of permitting a lateral displacement of the LSC circulation plane away from the vertical center line of the sample as well as a variation in displacements with height (such displacements had been excluded in the original model). Pressure gradients produced by the side wall of the container on average center the plane of the LSC so that it prefers to reach its longest diameter. If the LSC is displaced away from this diameter, the walls provide a restoring force. Turbulent fluctuations drive the LSC away from the central alignment, and combined with the restoring force they lead to oscillations. These oscillations are advected along with the LSC. This model predicts the correct wavenumber and phase of the oscillations, as well as estimates of the frequency, amplitude, and probability distributions of the displacements.

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