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INTERFACIAL AREA TRANSPORT OF BUBBLY FLOW IN A SMALL DIAMETER PIPE UNDER MICROGRAVITY ENVIRONMENT

机译:微匍匐环境下小直径管道在小直径管中的界面区域传输

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Axial developments of one-dimensional void fraction, bubble number density, interfacial area concentration, and Sauter mean diameter of adiabatic nitrogen-water bubbly flows in a 9-mm-diameter pipe were measured under a microgravity environment using an image-processing method. The interfacial area transport mechanism was determined based on visual observation. Marked bubble coalescence occurred when fast-moving bubbles near the channel center overtook and swept up slower-moving bubbles in the vicinity of the channel wall (velocity profile entrainment). Negligible bubble breakup was observed because of weak turbulence under tested flow conditions. Axial changes of measured interfacial area concentrations were compared with the interfacial area transport equation considering the bubble expansion and wake entrainment as observed under a normal gravity environment. The velocity profile entrainment effect under microgravity was likely to be comparable to the wake entrainment effect under normal gravity in the tested flow conditions. This apparently led to insignificant differences between measured interfacial area concentrations and those predicted by the interfacial area transport equation with the wake entrainment model under normal gravity. Possible bubble coalescence mechanisms would differ, however, between normal gravity and microgravity conditions.
机译:使用图像处理方法在微匍匐环境下测量一维空隙部分,气泡数密度,界面区域浓度,气泡数密度,界面区域浓度和绝热氮气泡泡的流动的轴向开发。基于视觉观察确定界面区域传输机制。当通道中心附近的快速移动泡沫超越并扫过沟道壁附近的快速移动气泡时,发生了标记的泡沫聚焦,在通道墙附近(速度夹材夹带)。由于经过测试的流动条件下的湍流疲软,观察到可忽略的泡泡分解。将测量的界面区域浓度的轴向变化与考虑到在正常重力环境下观察到的气泡膨胀和唤醒夹带的界面区域输送方程。在经过测试流动条件下的正常重力下,微刻度下的速度曲线夹带效果可能与在正常重力下的尾螺母夹带效果相当。这显然导致测量的界面区域浓度与界面区域传送方程在正常重力下与Xke夹夹层模型预测的那些之间的微不足道的差异。然而,可能的气泡聚结机制会在正常重力和微重力条件之间不同。

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