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contributor authorGuo, Dong-Peng
contributor authorYao, Ren-Tai
contributor authorFan, Dan
date accessioned2017-06-09T16:49:47Z
date available2017-06-09T16:49:47Z
date copyright2014/02/01
date issued2013
identifier issn1558-8424
identifier otherams-74884.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217158
description abstracthis paper introduces a wind tunnel experiment to study the effect of the cooling tower of a nuclear power plant on the flow and the characteristics of visible plume regions. The relevant characteristics of the flow field near the cooling tower, such as the plume rise and the visible plume region, are compared with the results of previous experimental data from Électricité de France (EDF) and the Briggs formulas. The results show that the wind tunnel experiment can simulate the top backflow of the cooling tower and the rear cavity regions among others. In the near-wake region, including the recirculation cavity, mean velocity decreases and turbulence intensity increases significantly. The maximum turbulence intensity observed is 0.5. In addition, the disturbed flow extent of the cooling tower top reaches 1.5 times the cooling tower height. Analysis of the visible plume region shows that the wind tunnel experiment can simulate the variation of a visible plume region. The results are consistent with the wind tunnel experiment of EDF. Moreover, the plume rise analysis shows that the wind tunnel experiment data are in agreement with the Briggs formulas for 50?200 m. As a whole, the proposed wind tunnel experiment can simulate the flow field variation of the visible plume region and the plume rise around the buildings with reasonable accuracy.
publisherAmerican Meteorological Society
titleWind Tunnel Experiment for Predicting a Visible Plume Region from a Nuclear Power Plant Cooling Tower
typeJournal Paper
journal volume53
journal issue2
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/JAMC-D-13-0153.1
journal fristpage234
journal lastpage241
treeJournal of Applied Meteorology and Climatology:;2013:;volume( 053 ):;issue: 002
contenttypeFulltext


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