In a free-surface spillway, the upstream flow is non-aerated and the flow becomes a strong air-water mix downstream of the onset location of air entrapment. Field observations were conducted over a steep spillway chute, and detailed quantitative measurements were undertaken in real-world high-speed flows with strong turbulence and very high Reynolds numbers within the range 10 7 to 10 8 . The data showed that the onset of air entrapment is a complicated transient three-dimensional process in high-speed strongly-turbulent flows. A robust optical flow (OF) technique was applied and provided physically-meaningful surface velocities in the non-aerated flow region. The streamwise velocities were reasonably close to ideal fluid flow calculations, with large streamwise surface velocity fluctuations, in the non-aerated flow region. Overall, the study demonstrated the application of optical techniques to prototype spillway flows, provided that some careful validation was undertaken. Optical Flow (OF) surface velocity on the Hinze dam spillway for Q = 150 m 3 /s, Re = 4.54 × 10 7 , θ = 51.3°, steps: h = 1.5 m, q 2/3 /(g 1/3 × h) = 1.58 - Comparison between centreline OF velocity and ideal fluid flow velocity (Left), with photograph of spillway chute flow corresponding to the data (Right). • Field observations were conducted in a high-velocity prototype chute. • Flow conditions corresponded to very-high Reynolds numbers within the range 10 7 to 10 8 . • The onset of air entrapment was complicated, transient and three-dimensional. • An optical flow (OF) technique was applied to video movies. • Physically meaningful OF surface velocity data were obtained in the non-aerated region.
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