Aeration performance of a hydraulic jump

S. Kucukali*, S. Cokgor

*Corresponding author for this work

Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

4 Citations (Scopus)

Abstract

Hydraulic jump is occurred at the transition from supercritical to subcritical flow which is characterized with energy dissipation due to highly turbulent flow, air entrainment, and macro-scale vortices. In this study self-aeration performance of a classical hydraulic jump beyond a sluice gate, has been investigated in a 0.5 m wide flume. Experiments were conducted for a range of upstream Froude numbers 2-6, and unit discharges 2×10 -2 -5.3×10 -2 m 3/sm. It was appeared that the aeration efficiency of a hydraulic jump was mostly dependent on head loss, and then to the unit discharge positively. Further, turbulence structure of the hydraulic jump, which ensures the entrainment of air into water, was highlighted by using an Acoustic Doppler velocimeter at low Froude numbers. An empirical formula predicting aeration efficiency for hydraulic jumps was developed by using non-linear regression analysis. Good agreement between measured and predicted aeration efficiency values was obtained.

Original languageEnglish
Title of host publicationExamining the Confluence of Environmental and Water Concerns - Proceedings of the World Environmental and Water Resources Congress 2006
DOIs
Publication statusPublished - 2007
EventWorld Environmental and Water Resources Congress 2006: Examining the Confluence of Environmental and Water Concerns - Omaha, NE, United States
Duration: 21 May 200625 May 2006

Publication series

NameExamining the Confluence of Environmental and Water Concerns - Proceedings of the World Environmental and Water Resources Congress 2006

Conference

ConferenceWorld Environmental and Water Resources Congress 2006: Examining the Confluence of Environmental and Water Concerns
Country/TerritoryUnited States
CityOmaha, NE
Period21/05/0625/05/06

Keywords

  • Aeration
  • Hydraulic jump
  • Turbulent flow

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