地球自转阻碍了实验室中流体的精确固体旋转

P. Cortet, J. Boisson, D. C. 'ebron, F. Moisy
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引用次数: 26

摘要

我们报告了在一个以恒定旋转速率旋转的充满水的球形容器中,地球旋转所激发的二次流的直接证据。这种所谓的倾斜流动本质上是围绕一个轴的旋转,这个轴相对于球体的旋转轴略微倾斜。在天体物理学的背景下,它对应于行星旋转轴进动所迫使的行星液体核心的流动,并且已经提出它有助于行星磁场的产生。我们使用安装在旋转框架中的粒子图像测速系统来检测这种弱二次流。这种二次流包括微弱的旋转,比球体旋转小一千倍,围绕一个固定在实验室框架中的水平轴。它的振幅和方向与旋进激发的倾斜流理论在数量上是一致的。这些结果表明,在实验室实验中使流体处于完美的固体旋转状态是不可能的——除非将实验的旋转轴倾斜,使之与地球的旋转轴平行。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Earth rotation prevents exact solid-body rotation of fluids in the laboratory
We report direct evidence of a secondary flow excited by the Earth rotation in a water-filled spherical container spinning at constant rotation rate. This so-called tilt-over flow essentially consists in a rotation around an axis which is slightly tilted with respect to the rotation axis of the sphere. In the astrophysical context, it corresponds to the flow in the liquid cores of planets forced by precession of the planet rotation axis, and it has been proposed to contribute to the generation of planetary magnetic fields. We detect this weak secondary flow using a particle image velocimetry system mounted in the rotating frame. This secondary flow consists in a weak rotation, thousand times smaller than the sphere rotation, around a horizontal axis which is stationary in the laboratory frame. Its amplitude and orientation are in quantitative agreement with the theory of the tilt-over flow excited by precession. These results show that setting a fluid in a perfect solid-body rotation in a laboratory experiment is impossible —unless by tilting the rotation axis of the experiment parallel to the Earth rotation axis.
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