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Winter-Regime Thermal Response of Heated Streams
The increase in water temperature in natural streams due to waste heat disposal from thermal power plants leads to extensive ice-free reaches during winter periods. It is shown that the surface heat exchange between water and the atmosphere can be expressed, for most practical purposes, as a linear function of the water temperature. Using this approximation, a closed-form solution of the one-dimensional unsteady convection-diffusion equation is developed to predict temperature distributions in streams and the lengths of ice-free reaches downstream from the thermal discharge sections.
Winter-Regime Thermal Response of Heated Streams
The increase in water temperature in natural streams due to waste heat disposal from thermal power plants leads to extensive ice-free reaches during winter periods. It is shown that the surface heat exchange between water and the atmosphere can be expressed, for most practical purposes, as a linear function of the water temperature. Using this approximation, a closed-form solution of the one-dimensional unsteady convection-diffusion equation is developed to predict temperature distributions in streams and the lengths of ice-free reaches downstream from the thermal discharge sections.
Winter-Regime Thermal Response of Heated Streams
Paily, Poothrikka P. (Autor:in) / Macagno, Enzo O. (Autor:in) / Kennedy, John F. (Autor:in)
Journal of the Hydraulics Division ; 100 ; 531-551
01.01.2021
211974-01-01 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
Winter regime surface heat loss from heated streams
UB Braunschweig | 1974
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