Research Article
May 1973
The Dissipation of Excess Heat from Water Systems
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VIEW THE REPLYAbstract
A model for the prediction of excess temperature is shown to have the form of the classical diffusion equation. The excess temperature in this model is defined as the difference between the actual water temperature and the water temperature which would have occurred provided that a particular heat source, such as a power plant, had never existed. This definition of excess temperature is convenient because it directly represents the incremental effect that a heat source has on a water system and, provided that historical water temperature records are available, the excess temperature can be predicted without the use of solar or atmospheric radiation data. A prediction equation for the surface transfer coefficient for excess heat illustrates that this coefficient is primarily dependent upon the water temperature and wind speed, and that it is almost independent of the humidity and temperature of the air.
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Information
Published In
Journal of the Power Division
Volume 99 • Issue 1 • May 1973
Pages: 89 - 103
Copyright
© 1973 American Society of Civil Engineers.
History
Published in print: May 1973
Published online: Feb 11, 2021
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Authors
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Harvey E. Jobson, M.ASCE
Research Hydrologists, U.S. Geological Survey, Bay St. Louis, Miss
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ASCE Library Cards let you download journal articles, proceedings papers, and available book chapters across the entire ASCE Library platform. ASCE Library Cards remain active for 24 months or until all downloads are used. Note: This content will be debited as one download at time of checkout.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.