Lee Minhee
Department of Environmental Geosciences, Pukyong National University, Namgu, Pusan, South Korea.
Water Res. 2002 Apr;36(8):2140-6. doi: 10.1016/s0043-1354(01)00421-3.
Oxygen concentration fields in a water body were visualized by the fluorescence oxygen visualization (FOV) method. Pyrenebutyric acid (PBA) was used as a fluorescent indicator of oxygen, and an intensive charge coupled-device (ICCD) camera as an image detector. Sequential images (over 2000 images) of the oxygen concentration field around the surface water of the tank (1 x 1 x 0.75 m3) were produced during the 3 h experiment. From image processing, the accurate pathway of oxygen-rich, cold water at the water surface was also visualized. The amount of oxygen transferred through the air-water interface during the experiment was measured and the oxygen transfer coefficient (K(L)) was determined as 0.22 m/d, which was much higher than that is expected in molecular diffusion. Results suggest that vertical penetration of cold water was the main pathway of oxygen in the water body in the tank. The average velocity of cold water penetrating downward in water body was also measured from consecutive images and the value was 0.3-0.6 mm/s. The FOV method used in this research should have wide application in experimental fluid mechanics and can also provide a phenomenological description of oxygen transfer under physically realizable natural conditions in lakes and reservoirs.
采用荧光氧可视化(FOV)方法对水体中的氧浓度场进行了可视化。使用芘丁酸(PBA)作为氧的荧光指示剂,并使用增强型电荷耦合器件(ICCD)相机作为图像探测器。在3小时的实验过程中,生成了水箱(1×1×0.75立方米)地表水周围氧浓度场的序列图像(超过2000张图像)。通过图像处理,还可视化了水面富氧冷水的精确路径。测量了实验过程中通过气-水界面转移的氧量,并确定氧转移系数(K(L))为0.22米/天,这远高于分子扩散预期的值。结果表明,冷水的垂直渗透是水箱水体中氧的主要传输途径。还从连续图像中测量了冷水在水体中向下渗透的平均速度,其值为0.3-0.6毫米/秒。本研究中使用的FOV方法在实验流体力学中应具有广泛的应用,并且还可以对湖泊和水库中物理上可实现的自然条件下的氧转移提供现象学描述。