论文标题

交错山后醒来的发夹涡之间的干扰和传热

Interference and heat transfer between hairpin vortices in wakes behind staggered hills

论文作者

Yanaoka, Hideki, Yomogida, Yoshiyuki

论文摘要

本研究对在层状边界层的交错山丘后面的唤醒中形成的发夹涡流之间的干扰和传热进行了数值模拟。在一排丘陵之后,发夹涡流定期脱落,导致发夹涡流之间的干扰。随着山丘之间的跨度距离减小,干扰增加,发夹涡流变得强大。当时,由于发夹涡旋和Q2弹出的腿之间的干扰变得强大,因此每个发夹涡旋的头部都急剧上升。当山间距减小时,第二排山的头部和发夹涡流的两条腿引起的湍流会显着增加。另外,次级涡流还会产生湍流。发夹涡流和次级涡流被吸引到相邻的发夹涡流中,从而在墙壁表面附近的跨度方向上引起广泛的高湍流。无论山间距如何,出发发夹涡流引起的Q2射出和Q4扫描,并且在发夹涡旋周围形成二次涡旋,激活热传输并增加热传递系数。当山间距变窄时,发夹涡流之间的干扰增强了每个发夹涡旋和次级涡旋的腿,墙壁表面附近的热传输变得非常活跃。热传递在唤醒的广泛范围内增加,因为向下游流动的发夹涡旋的腿沿跨度方向扩散。

The present study performs a numerical simulation of the interference and heat transfer between hairpin vortices formed in wakes behind staggered hills in a laminar boundary layer. Hairpin vortices are periodically shed in the wake of a row of hills, causing interference between the hairpin vortices. As the spanwise distance between the hills decreases, interference increases and the hairpin vortices become strong. At that time, because the interference between the legs of the hairpin vortex and the Q2 ejection becomes strong, the head of each hairpin vortex rises sharply. When the hill spacing decreases, the turbulence caused by the head and both legs of the hairpin vortex generated from a hill in the second row increases remarkably. In addition, the secondary vortex also generates turbulence. The hairpin vortex and the secondary vortex are attracted to adjacent hairpin vortices, causing widespread high turbulence in the spanwise direction near the wall surface. Regardless of the hill spacing, Q2 ejection and Q4 sweep due to the hairpin vortex occur, and the secondary vortex forms around the hairpin vortex, activating heat transport and increasing the heat transfer coefficient in the wake. When the hill spacing becomes narrower, the interference between the hairpin vortices strengthens the legs of each hairpin vortex and secondary vortex, and heat transport near the wall surface becomes very active. The heat transfer increases over a wide range of the wake because the legs of hairpin vortices flowing downstream are spread in the spanwise direction.

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