冲击能量和长宽比对积水中粒子云运动的影响

Maliheh Sabershahraki, Amir Azimi
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摘要

为了研究冲击能量和其他初始控制参数对颗粒云在死水中运动的影响,我们进行了一系列实验室实验。实验针对两种中值砂直径(D50 = 0.52 毫米和 0.74 毫米)和喷嘴直径(do = 6 毫米和 8 毫米)进行。沙粒质量被转换为与喷嘴直径相同的等效管道长度(Lo),并测试了 2 至 93 之间的宽高比(Lo/do)。沙粒的冲击能量由沙粒的释放高度控制,并用非尺寸释放高度 η 量化,范围在 1 到 21.5 之间。研究发现,冲击能量越高的颗粒云的浓度和速度衰减率越小。这表明,随着释放高度的增加,沙粒与环境水之间的动量传递会减小。利用沙粒瞬时速度的时间序列来确定沙粒的速度波动和湍流强度,发现沙粒速度波动与颗粒云的长宽比直接相关。本研究还考察了冲击能量对所产生的颗粒云解剖结构的影响。研究发现,当高纵横比(即 Lo/do > 39)沙粒的冲击能量增加时,沙粒云的宽度急剧增加。此外,随着沙粒在水面的动能增加,沙粒的分散开始得更早。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of Impact Energy and Aspect Ratio on the Motion of Particle Clouds in Stagnant Water
A series of laboratory experiments was conducted to investigate the effects of impact energy and other initial controlling parameters on the motion of particle clouds in stagnant water. Experiments were performed for two median sand diameters of D50 = 0.52 mm and 0.74 mm and nozzle diameters of do = 6 mm and 8 mm. Sand masses were converted to an equivalent pipe length with the same diameter as the nozzle, Lo, and a wide range of aspect ratios, Lo/do, between 2 and 93 was tested. The impact energy of sand particles was controlled by the release height of sand particles, and it was quantified by the non-dimensional release height, η, ranging from 1 to 21.5. It was found that particle clouds with higher impact energy had smaller concentration and velocity decay rates. This indicated that by increasing the release height, the momentum transfer between sand particles and the ambient water decreases. The time-series of instantaneous sand velocity were used to determine velocity fluctuations and turbulence intensity of sand particles and a direct correlation was found between sand velocity fluctuations and aspect ratio in particle clouds. The effects of impact energy on the anatomy of the resulted particle clouds were examined in this study. It was found that the cloud width increased dramatically when the impact energy of sand particles with high aspect ratios (i.e., Lo/do > 39) increased. Furthermore, the dispersion of sand particle began earlier as the kinetic energy of sand particles increased at the water surface.
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