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LABORATORY OBSERVATION ON THE SPREAD OF BUBBLE PLUME IN THE WATER OF DENSITY STRATIFICATION

机译:密度分层水中气泡羽状扩散的实验室观察

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The air jet discharging upward into the stratified water is observed in the water tank. The air takes the form of bubbles which rises up owing to buoyancy and which impart an upward velocity to the surrounding water. Different air discharge rates and ambient water density stratification cases are run to observe the spread of the bubble plume. Experiments were conducted on the water tank of 67.5 cm by 60 cm with 60 cm of height. The images of bubble plume were grabbed by using the CCD camera with the resolution of 256 by 256 pixels. Observational results indicate that: (1) For the homogeneous ambient water, the air discharge rate does not significantly affect the growth of the bubble plume. (2) When the ambient water becomes density stratification, intrusion of the bubble plume occurs around the layer density difference interface. And the inhibition on the intrusion of the bubble plume increases and enlarges the intrusion length as the layer density difference increases.
机译:在水箱中观察到向上排放到分层水中的空气射流。空气采取气泡的形式,由于浮力而上升,并且使周围的水上升。运行不同的空气排放速率和环境水密度分层案例,以观察气泡羽流的扩散。在67.5厘米乘60厘米,高60厘米的水箱上进行实验。使用CCD相机以256 x 256像素的分辨率捕获气泡羽的图像。观测结果表明:(1)对于均匀的环境水,空气的排放速率不会显着影响气泡羽流的生长。 (2)当环境水变成密度分层时,在层密度差界面周围发生气泡羽流的侵入。并且随着层密度差的增加,对气泡羽流的侵入的抑制增加并且增大了侵入长度。

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