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arXiv 1402.5896physics.flu-dyn
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边界层转捩小涡产生机理的数值研究

Numerical Study on Mechanism of Small Vortex Generation in Boundary Layer Transition

Ping Lu, Chaoqun Liu

摘要:

小涡的产生是后期流动转捩和湍流产生机理的关键问题。人们普遍认为,小长度涡是由大涡破裂产生的。根据我们最近的DNS,我们发现发夹涡结构是非常稳定的,从来没有打破成小块。另一方面,我们认识到,在展向方向上,除了环颈之外,还有强的正尖峰。强正尖峰是由二次扫掠引起的,二次扫掠是由完美的圆形和垂直站立的涡环产生的。第二次扫掠将能量从无粘区下沉气流带到边界层底部,在正尖峰周围产生高剪切层。由于高剪切层不稳定,所有小尺度(湍流)都在高剪切层周围产生,特别是在壁面附近(边界层底部)。这发生在流向环颈附近和展向原来的涡腿旁边,然后小尺度从壁面上升并传播到上边界层。

英文摘要:

The small vortex generation is a key issue of the mechanism for late flow transition and turbulence generation. It was widely accepted that small length vortices were generated by large vortex breakdown. According to our recent DNS, we find that the hairpin vortex structure is very stable and never breaks down to small pieces. On the other hand, we recognize that there are strong positive spikes besides the ring neck in the spanwise direction. The strongly positive spikes are caused by second sweeps which are generated by perfectly circular and perpendicularly standing vortex rings. The second sweep brings energy from the invisid region downdraft to the bottom of the boundary layers, which generates high shear layers around the positive spikes.Since the high shear layer is not stable, all small length scales (turbulence) are generated around high shear layers especially near the wall surface (bottom of boundary layers). This happens near the ring neck in the streamwise direction and besides the original vortex legs in the spanwise direction.The small length scales then rise up from the wall surface and travel to the upper boundary layer.

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