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Stratification of Flow from Channel into Deep Lake
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.
Stratification of Flow from Channel into Deep Lake
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.
Stratification of Flow from Channel into Deep Lake
Stefan, Heinz (author)
Journal of the Hydraulics Division ; 96 ; 1417-1434
2021-01-01
181970-01-01 pages
Article (Journal)
Electronic Resource
Unknown
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