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Experimental investigation of natural convective flows in slowly rotating wide spherical shells

机译:缓慢旋转的球形壳中自然对流流动的实验研究

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Experimental results are presented on natural convection in a spherical shell of inner and outer radii r_1 = 14 mm and r_2 = 35 mm, with the inner sphere cooled and the outer sphere heated. The fluids filling the shell are two different silicon oils having Prandtl numbers 39 and 233. Both spheres are fixed together and can be rotated. In the studied regime, both Coriolis and centrifugal forces become significant. For sufficiently small Rayleigh numbers the resulting flow pattern is axisymmetric and steady, consisting of a plume descending from the south pole of the inner sphere, and returning in the equatorial regions. For greater Rayleigh numbers the flow becomes non-axisymmetric, with azimuthal modes m = 2 to 4 arising. We map out the critical Rayleigh number for the onset of these different modes, and consider how they vary with increasingly rapid overall rotation. Detailed flow measurements are done by converting a standard 2D particle image velocimetry system into a scanning quasi-3D PIV system.
机译:给出了在内半径为r_1 = 14 mm和r_2 = 35 mm的球形壳中自然对流的实验结果,其中内球冷却,外球加热。填充壳体的流体是两种不同的硅油,其普朗特数分别为39和233。两个球体固定在一起并且可以旋转。在研究方案中,科里奥利力和离心力都变得很重要。对于足够小的瑞利数,所得的流型是轴对称且稳定的,由从内球南极下降并返回到赤道区域的羽状流组成。对于更大的瑞利数,流动变得非轴对称,产生方位角模m = 2到4。我们针对这些不同模式的出现绘制了关键的瑞利数,并考虑了它们如何随着整体旋转速度的加快而变化。通过将标准的2D颗粒图像测速系统转换为准3D PIV扫描系统,可以完成详细的流量测量。

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