scholarly journals Analysis of Uncertainties in CRAC2 Calculations: Wet Deposition and Plume Rise

Author(s):  
R. C. Ward ◽  
D. C. Kocher ◽  
B. B. Hicks ◽  
R. P. Hosker ◽  
J.-Y. Ku ◽  
...  
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1987 ◽  
Vol 22 (3) ◽  
pp. 365-376
Author(s):  
C. H. Chan ◽  
L. H. Perkins

Abstract Wet deposition estimates were computed from monthly wet precipitation samples collected in the Lake Superior Basin. Sulphate and nitrogen loadings from wet precipitation corresponded to 142 and 40 thousand tonnes per year. On a percentage basis, wet deposition of sulphate and nitrogen accounted for 21% and 54%, respectively, of the total load. Atmospheric sources for other major ions ranged from 1 to 10%. Atmospheric deposition at the eastern end of Lake Superior was higher than the western end of the Basin. The relative accuracy of these estimates were examined in relation to the changes in lake chemistry in Lake Superior from 1973 to 1983.


2016 ◽  
Vol 59 (1) ◽  
pp. 1 ◽  
Author(s):  
Min Kyeong Kim ◽  
Goo Bok Jung ◽  
Jong Sik Lee ◽  
Hyun Jung Jeon ◽  
Myung Hyun Kim ◽  
...  
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Author(s):  
Mario Villalobos-Forbes ◽  
Germain Esquivel-Hernández ◽  
Ricardo Sánchez-Murillo ◽  
Rolando Sánchez-Gutiérrez ◽  
Ioannis Matiatos

Author(s):  
Shuo Li ◽  
M. R. Flynn

AbstractVisible plumes above wet cooling towers are of great concern due to the associated aesthetic and environmental impacts. The parallel path wet/dry cooling tower is one of the most commonly used approaches for plume abatement, however, the associated capital cost is usually high due to the addition of the dry coils. Recently, passive technologies, which make use of free solar energy or the latent heat of the hot, moist air rising through the cooling tower fill, have been proposed to minimize or abate the visible plume and/or conserve water. In this review, we contrast established versus novel technologies and give a perspective on the relative merits and demerits of each. Of course, no assessment of the severity of a visible plume can be made without first understanding its atmospheric trajectory. To this end, numerous attempts, being either theoretical or numerical or experimental, have been proposed to predict plume behavior in atmospheres that are either uniform versus density-stratified or still versus windy (whether highly-turbulent or not). Problems of particular interests are plume rise/deflection, condensation and drift deposition, the latter consideration being a concern of public health due to the possible transport and spread of Legionella bacteria.


2017 ◽  
Vol 223 ◽  
pp. 170-177 ◽  
Author(s):  
Ling-Chuan Guo ◽  
Lian-Jun Bao ◽  
Shao-Meng Li ◽  
Shu Tao ◽  
Eddy Y. Zeng

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