2002
DOI: 10.1061/(asce)0733-9437(2002)128:5(305)
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Energy Dissipation and Air Entrainment in Stepped Storm Waterway: Experimental Study

Abstract: For the last three decades, research focused on steep stepped chutes. Few studies considered flat-slope stepped geometries such as stepped storm waterways or culverts. In this study, experiments were conducted in a large, flat stepped chute ͑ ϭ3.4°͒ based upon a Froude similitude. Three basic flow regimes were observed: nappe flow without hydraulic jump, transition flow, and skimming flow. Detailed air-water flow measurements were conducted. The results allow a complete characterization of the air concentratio… Show more

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Cited by 65 publications
(56 citation statements)
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“…11), as well as in terms of mean air content C mean , and dimensionless airwater flow velocity V 90 /V c . The findings were in agreement with earlier studies (Boes 2000b;Chanson and Toombes 2002b;Gonzalez and Chanson 2004;Relvas and Pinheiro 2008).…”
Section: Froude Similitudesupporting
confidence: 93%
“…11), as well as in terms of mean air content C mean , and dimensionless airwater flow velocity V 90 /V c . The findings were in agreement with earlier studies (Boes 2000b;Chanson and Toombes 2002b;Gonzalez and Chanson 2004;Relvas and Pinheiro 2008).…”
Section: Froude Similitudesupporting
confidence: 93%
“…The surface was parallel to the pseudo-bottom formed by the step edges for θ = 26.6°. For the 8.9° slope, the free-surface was not completely parallel to the pseudo-bottom and some pseudo-undular free-surface profiles were observed as previously reported on a 3.4° stepped chute (Chanson and Toombes 2002a). The amount of entrained air appeared smaller for the stepped chute with θ = 8.9° possibly linked with the different cavity shape.…”
Section: Visual Observations Of Flow Patterns Flow Regimes and Flow supporting
confidence: 58%
“…The present results were qualitatively and quantitatively comparable to these earlier findings, although Chanson and Toombes (2002b) The flow resistance on stepped waterways was characterised by significant form losses caused by the steps. Following common practice (Rajaratnam 1990, Chanson et al 2002, the DarcyWeisbach friction factor was used to quantify the dimensionless boundary shear stress in stepped spillway flows.…”
supporting
confidence: 91%