Determination of the Mechanism of Droplets Post-impact Atomisation in Water Sprays at Temperatures Bellow the Critical Nukiyama and Leidenfrost Values

V. Stamatov, L. Stamatova
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Abstract

Several non-intrusive laser diagnostic techniques (PIV, Marker Nephelometry and PLIF) were applied to study spray impact morphology: droplets velocity and size prior and after the impact, the number of droplets in the impact and post-impact zones, and the presence of vorticity fields in the impact area, at a temperature lower than the critical Nukiyama and Leidenfrost temperatures. The experimental results suggest that the process of droplet post-impact atomisation follows a hydrodynamic mechanism in which the first droplets that hit the wall form a liquid film. Later, the film breaks up because of the impact of the next incident dropletsm.  As a result, a small number of relatively large post-impact droplets of low velocity is formed and pushed away from the zone of impact.
在低于Nukiyama和Leidenfrost临界值的温度下,水喷雾中液滴撞击后雾化机理的测定
在低于Nukiyama和Leidenfrost临界温度的条件下,采用几种非侵入式激光诊断技术(PIV、Marker浊度测定法和PLIF)研究了喷雾撞击形态:撞击前后液滴的速度和大小,撞击区和撞击区液滴的数量,以及撞击区涡度场的存在。实验结果表明,液滴撞击后雾化过程遵循流体动力学机制,其中第一批液滴撞击壁面形成液体膜。后来,影片因为下一个水滴事件的影响而破裂。因此,形成了少量相对较大的低速撞击后液滴,并将其推离撞击区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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