论文标题

将光流体运动分析带入现场:使用开源ROV作为摄像头系统的方法,作为示踪剂升起的气泡

Bringing optical fluid motion analysis to the field: a methodology using an open source ROV as camera system and rising bubbles as tracers

论文作者

Løken, Trygve K., Ellevold, Thea J., de la Torre, Reyna G. Ramirez, Rabault, Jean, Jensen, Atle

论文摘要

详细的水运动学对于理解北极中的大气 - 冰山能量传递过程很重要。边缘冰区的2D速度场的原位观察很少。粒子跟踪速度法和粒子图像速度法是用于测量2D速度场的众所周知的实验室技术,但它们通常依靠脆弱的设备和轮询性塑料示踪剂。因此,为了将这些方法带入现场,我们开发了一个新系统,该系统将紧凑的开源远程操作的车辆与成像装置相结合,并将气泡作为追踪颗粒。然后,可以使用对极地区域中的现场测量的图像处理技术分析获得的数据。在受控条件下已经研究了生成的气泡的性质,例如末端速度和直径之间的关系。速度测量值的准确性和扩散已在波罐中量化,并与理论溶液进行了比较。在10%的精度范围内测量了周期性波的水平速度分量。偏离理论溶液的偏差归因于由于流动加速而导致的气泡惯性。我们包括来自北极野外探险的一个例子,在该探险中,该系统被部署并从ICE Floe进行了成功测试。这项工作是在北极冰下进行详细的2D流量测量的重要里程碑,我们预计这将有助于直接观察到海冰下发生的动态。

Detailed water kinematics are important for understanding atmosphere-ice-ocean energy transfer processes in the Arctic. There are few in situ observations of 2D velocity fields in the marginal ice zone. Particle tracking velocimetry and particle image velocimetry are well known laboratory techniques for measuring 2D velocity fields, but they usually rely on fragile equipment and pollutive plastic tracers. Therefore, in order to bring these methods to the field, we have developed a new system which combines a compact open-source remotely operated vehicle as an imaging device, and air bubbles as tracing particles. The data obtained can then be analyzed using image processing techniques tuned for field measurements in the polar regions. The properties of the generated bubbles, such as the relation between terminal velocity and diameter, have been investigated under controlled conditions. The accuracy and the spread of the velocity measurements have been quantified in a wave tank and compared with theoretical solutions. Horizontal velocity components under periodic waves were measured within the order of 10% accuracy. The deviation from theoretical solutions is attributed to the bubble inertia due to the accelerated flow. We include an example from an Arctic field expedition where the system was deployed and successfully tested from an ice floe. This work is an important milestone towards performing detailed 2D flow measurements under the ice in the Arctic, which we anticipate will help perform much needed direct observations of the dynamics happening under sea ice.

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