Research Article
Jul 1970
Stratification of Flow from Channel into Deep Lake
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VIEW THE REPLYPublication: Journal of the Hydraulics Division
Volume 96, Issue 7
Abstract
The flow of heated water from an open channel into a reservoir containing colder and essentially stagnant water has been studied in a laboratory flume. The basic mechanisms which can produce a variety of substantially different flow patterns are considered. The combined effects of buoyancy, viscosity, and stratification conditions in the reservoir on the flow are shown qualitatively in the case of a two-layered system. The information obtained has a relationship to the design and operation of heated water outlets into lakes and ocean outfalls.
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Published In
Journal of the Hydraulics Division
Volume 96 • Issue 7 • July 1970
Pages: 1417 - 1434
Copyright
© 1970 American Society of Civil Engineers.
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Published in print: Jul 1970
Published online: Feb 3, 2021
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Authors
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Heinz Stefan, AM.ASCE
Asst. Prof., Dept. of Civ. Engrg. and Hydr., St. Anthony Falls Hydr. Lab., Univ. of Minn., Minneapolis, M. N
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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.