On the incipient aerated flow in chutes and spillways

Natural self-aeration of water flows in open channels protects surfaces in contact with the flow from cavitation damage if enough air content is reached (Falvey [6] [7], Peterka [10], Russel & Sheenan [11]), although it could lead to an increase in both flow depth and velocity. Also, self-aerate...

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Bibliographic Details
Published inJournal of hydraulic research Vol. 40; no. 1; pp. 95 - 97
Main Authors Monino Ferrando, Antonio, Riera Rico, Jaime
Format Journal Article
LanguageEnglish
Published Delft Taylor & Francis Group 01.01.2002
International Association for Hydraulic Research
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Summary:Natural self-aeration of water flows in open channels protects surfaces in contact with the flow from cavitation damage if enough air content is reached (Falvey [6] [7], Peterka [10], Russel & Sheenan [11]), although it could lead to an increase in both flow depth and velocity. Also, self-aerated flow enhance the process of atmospheric gases exchange within the fluid, improving water quality downstream of hydraulic structures (Chanson [5]). So it is of great interest to evaluate accurately the critical point where air entrainment begins, that is, the location of the inception point. The note first shows a review on some methods to evaluate the inception point location. Second, a brief explanation on calculation development is made and an expression is obtained which enables to compute the point of incipient self-aeration as a function of unit discharge, bottom slope of the chute and uniform surface roughness in a more simple and accurate way. Finally, comparison with results provided by other methods is made and conclusions are obtained.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
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ISSN:0022-1686
1814-2079
DOI:10.1080/00221680209499877