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Measurement of spray-cloud characteristics with bubble image velocimetry for braking wave impact

机译:用气泡图像测速仪测量雾气特性,以测量制动波的冲击

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The process of spray-cloud production and flow kinematics arising from breaking wave impact on a fixed flatshaped plate and a bow-shaped plate models were investigated based on the image velocimetry method. During wave impact and water sheet formation on a flat surface, an enormous amount of aerated flow is created in front of the surface. This process produces a significant number of bubbles in the resulting flow. The Bubble Image Velocimetry (BIV) was used to measure the wave run-up velocity. The BIV method uses these bubbles as a tracer and measures bubble velocity by correlating the texture in the bubble images. A high-speed camera was employed to record images for calculating fluid velocity. Instead of using a laser light sheet, a diffused LED backlight illuminated the bubble images. Two perpendicular plane views were used to capture the footages: a side and a front view. The wave run-up velocity measurements at the moment of impact are compared with the results of several published experimental results. Aside from the BIV method, spray characteristics were examined based on the Digital Particle Image Velocimetry (DPIV) method. This method was used for the area that the concentration of bubbles is low or no bubbles are present. Measurements of droplet size, and velocity, as well as wave run-up velocity, were major concerns in this study. Results of velocimetry from both views were compared, and a satisfactory agreement was achieved among> 90% of the data. The highly transient process of spray formation from the liquid sheet breakup was discussed, and the drag coefficients and drag forces were calculated in two different stages of spray formation. Several pressure sensors were used to measure the impact pressure and three capacitive wave probes to measure the free surface profile. It was observed that higher impact pressure leads to the production of more dense and finer spray with a higher transition velocity. Moreover, it was illustrated that smaller size droplets have a higher velocity in compare with the medium and large size droplets, however, because of the effect of drag force these small size droplets cannot reach the maximum spray heights.
机译:基于图像测速方法,研究了破碎波对固定平板和弓形板模型产生的喷云产生过程和流动运动学。在波浪冲击和在平坦表面上形成水床的过程中,在表面的前面会产生大量的充气流。此过程在生成的流中产生大量气泡。气泡图像测速(BIV)用于测量波上升速度。 BIV方法使用这些气泡作为示踪剂,并通过关联气泡图像中的纹理来测量气泡速度。使用高速相机记录图像以计算流体速度。代替使用激光片,漫射的LED背光照明了气泡图像。两个垂直的平面视图用于捕获素材:侧视图和正视图。将撞击时的波浪起伏速度测量结果与几个已发表的实验结果进行比较。除了BIV方法外,还基于数字粒子图像测速(DPIV)方法检查了喷雾特性。该方法用于气泡浓度低或不存在气泡的区域。液滴尺寸,速度以及波上升速度的测量是这项研究的主要关注点。比较了两种方法测速的结果,并在> 90%的数据中获得了令人满意的一致性。讨论了由液膜破裂引起的喷雾形成过程的高瞬变过程,并在喷雾形成的两个不同阶段计算了阻力系数和阻力。几个压力传感器用于测量冲击压力,三个电容波探头用于测量自由表面轮廓。观察到较高的冲击压力导致产生更高密度和更细的喷雾,并具有更高的转变速度。此外,已经说明,与中等和大尺寸液滴相比,较小尺寸的液滴具有较高的速度,但是,由于拖曳力的作用,这些较小尺寸的液滴不能达到最大喷雾高度。

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