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arXiv 0902.4659physics.flu-dyn
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湍流Rayleigh-Benard对流中大尺度环流的方位不对称性

Azimuthal asymmetries of the large-scale circulation in turbulent Rayleigh-Benard convection

Eric Brown, Guenter Ahlers

摘要:

以前,我们发表了一个动力学模型(E。Brown和G. Ahlers,Phys. Fluids,20,075101(2008)),用于圆柱形容器中瑞利-贝纳德对流的大尺度循环(LSC)动力学。该模型由一对随机常微分方程组成,由纳维-斯托克斯方程驱动,分别用于LSC的强度δ和方向θ_0。在这里,我们将其扩展到的情况下,系统的旋转不变性被打破的几个物理相关的扰动之一。作为一个例子,我们提出了实验测量的LSC动态容器倾斜相对于重力。在这种情况下,该模型预测,热边界层的浮力促使流体沿着最陡的斜坡行进,它将LSC锁定在这个方向上,并且它加强了流动,如实验所示。LSC强度的增加被证明是负责所观察到的cessations和方位角波动的抑制。我们预测并观察到,对于足够大的倾斜角,使流动与斜坡对齐的回复力足够强,以引起LSC围绕该方向的振荡。这种平面振荡模式不同于先前观察到的相干扭转振荡。该模型也适用于椭圆形横截面的容器,并预测,由于侧壁的压力迫使流到一个优选的方向上的最长直径。当椭圆率足够大时,预测围绕该取向的振荡。

英文摘要:

Previously we published a dynamical model (E. Brown and G. Ahlers, Phys. Fluids, 20, 075101 (2008)) for the large-scale-circulation (LSC) dynamics of Rayleigh-Benard convection in cylindrical containers. The model consists of a pair of stochastic ordinary differential equations, motivated by the Navier-Stokes equations, one each for the strength delta and the orientation theta_0 of the LSC. Here we extend it to cases where the rotational invariance of the system is broken by one of several physically relevant perturbations. As an example we present experimental measurements of the LSC dynamics for a container tilted relative to gravity. In that case the model predicts that the buoyancy of the thermal boundary layers encourages fluid to travel along the steepest slope, that it locks the LSC in this direction, and that it strengthens the flow, as seen in experiments. The increase in LSC strength is shown to be responsible for the observed suppression of cessations and azimuthal fluctuations. We predict and observe that for large enough tilt angles, the restoring force that aligns the flow with the slope is strong enough to cause oscillations of the LSC around this orientation. This planar oscillation mode is different from coherent torsional oscillations that have been observed previously. The model was applied also to containers with elliptical cross-sections and predicts that the pressure due to the side walls forces the flow into a preferred orientation in the direction of the longest diameter. When the ellipticity is large enough, then oscillations around this orientation are predicted.

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