Rothman T, Ledbetter J O
Environ Lett. 1975;10(3):191-203. doi: 10.1080/00139307509435821.
Fog from cooling towers causes problems of visibility and icing along roadways adjacent to the towers; moreover, the visible plume from the towers offers difficulty in that it is equated by much of the public with air pollution. It is desirable to know the size of the fog droplets in order to plan abatement procedures and to determine the airborne lifetimes of such fogs. The methodology involved capturing the droplets on slides coated with a vaseline-mineral oil mixture, making photomicrographs of the droplets, counting and sizing the droplets into eight droplet diameter increments; namely less than 5 mum, 5-10 mum, 10-20 mum, 20-40 mum, 40-60 mum, 60-80 mum, 80-100 mum, and greater than 100 mum. The resulting distribution was similar to that for natural fogs and clouds; i.e., it was bi-modal, the first mode at less than 5 mum containing the vast majority of the droplets, and the second at 20-40 mum. This study agrees with others that the size distribution of a fog in a saturated environment is continuously changing, with the smaller droplets tending to evaporate and the larger ones tending to grow, thus shifting the second mode toward larger sizes.
冷却塔产生的雾气会导致冷却塔附近道路出现能见度问题和结冰现象;此外,冷却塔可见的羽状物也带来了麻烦,因为大部分公众将其等同于空气污染。为了规划减排措施并确定此类雾气在空气中的持续时间,了解雾滴的大小是很有必要的。所采用的方法是将雾滴捕获在涂有凡士林 - 矿物油混合物的载玻片上,拍摄雾滴的显微照片,将雾滴计数并按八个液滴直径增量进行尺寸测量;即小于5微米、5 - 10微米、10 - 20微米、20 - 40微米、40 - 60微米、60 - 80微米、80 - 100微米以及大于100微米。所得分布与自然雾气和云层的分布相似;也就是说,它是双峰的,第一个峰在小于5微米处,包含绝大多数雾滴,第二个峰在20 - 40微米处。这项研究与其他研究一致,即在饱和环境中雾的尺寸分布是不断变化的,较小的雾滴倾向于蒸发,而较大的雾滴倾向于增长,从而使第二个峰向更大尺寸移动。