论文标题
旋转cOUETTE流动中的动量运输比动量运输快得多
Much faster heat/mass than momentum transport in rotating Couette flows
论文作者
论文摘要
热和质量传输通常与剪切流中的动量传输密切相关。这种所谓的雷诺在对流热或质量传输与动量传输之间的类比阻碍了工程热和传质应用的效率提高。我通过直接的数值模拟显示,在平面和泰勒 - 库特流动旋转中,可以强烈影响壁壁的被动示踪剂传输,并且使其比动量传输更快,这显然违反了雷诺德的类比。在稳定的流动中观察到被动示踪剂传输,代表热/质量传输的代表和动量传输之间的差异,在较低的雷诺数下,在较高的雷诺数下,在较低的雷诺数字和完全湍流的流动下,在较高的反向旋转涡流中观察到了这种差异。它在中性(瑞利)稳定性极限附近特别大。当接近此极限时,旋转诱导的科里奥利力会严重抑制流向/方位速度的速度波动,而示踪剂波动的影响却大大降低。因此,动量运输比示踪剂运输要降低得多,这表明科里奥利的力打破了雷诺的类比。在较高的雷诺数下,这种强大的对流差异伴随着近似的极限循环动力学,当接近中性稳定性极限时,湍流的强烈低频爆发。该研究表明,简单的身体会在剪切流中的热量/质量和动量传输之间引起明显的异异差异。
Heat and mass transport is generally closely correlated to momentum transport in shear flows. This so-called Reynolds analogy between advective heat or mass transport and momentum transport hinders efficiency improvements in engineering heat and mass transfer applications. I show through direct numerical simulations that in plane Couette and Taylor-Couette flow rotation can strongly influence wall-to-wall passive tracer transport and make it much faster than momentum transport, clearly in violation of the Reynolds analogy. This difference between passive tracer transport, representative of heat/mass transport, and momentum transport is observed in steady flows with large counter-rotating vortices at low Reynolds numbers as well as in fully turbulent flows at higher Reynolds numbers. It is especially large near the neutral (Rayleigh's) stability limit. The rotation-induced Coriolis force strongly damps the streamwise/azimuthal velocity fluctuations when this limit is approached while tracer fluctuations are much less affected. Accordingly, momentum transport is much more reduced than tracer transport, showing that the Coriolis force breaks the Reynolds analogy. At higher Reynolds numbers this strong advective transport dissimilarity is accompanied by approximate limit cycle dynamics with intense low-frequency bursts of turbulence when approaching the neutral stability limit. The study demonstrates that simple body forces can cause clear dissimilarities between heat/mass and momentum transport in shear flows.