TECHNICAL PAPERS
Apr 13, 2011

Secondary Currents and Corresponding Surface Velocity Patterns in a Turbulent Open-Channel Flow over a Rough Bed

Publication: Journal of Hydraulic Engineering
Volume 137, Issue 11

Abstract

River and open-channel flows present complex three-dimensional (3D) structures in the water column and on the surface as a result of the existence of secondary currents driven by either centrifugal force or turbulence. This paper experimentally investigates secondary currents in a straight, turbulent, rough-bed open-channel flow; the effect of different channel width to flow depth ratios (12.25, 15, and 20) on secondary currents; and surface boils associated with secondary currents at moderate Reynolds numbers. Nearly instantaneous profiles of three components of flow velocity and turbulence characteristics in the water column were measured by using an acoustic Doppler velocity profiler (ADVP). Simultaneously, large-scale particle image velocimetry was used to measure the water surface velocities and turbulence structures. Mean velocity patterns in the water undulate across the channel, indicating the presence of secondary currents in the long-term average flow structure. Secondary currents affect the distribution of bed shear stress, Reynolds stress, and turbulence intensities across the channel. The aspect ratio determines the number of secondary cells in the water column. A mean multiband undulating surface velocity pattern in the transverse direction correlates with the secondary cell distribution in the water column below. The instantaneous position of the upwelling and downwelling regions on the surface may deviate from their long-term mean position, indicating a meandering of the surface pattern. Vortex structures are detected from instantaneous surface velocity maps, and vortex boil lines are identified. Boil vortices mainly occur in upwelling areas with high vorticity. The simultaneous detailed velocity measurements in the water column and on the free surface have shown a good agreement between the secondary cell patterns obtained by the two methods.

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Acknowledgments

The writers are grateful for the financial support that was provided by the Swiss National Science Foundation (grant NSF200020-100383) for this study. We would like to thank to the anonymous reviewers for their constructive comments.

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Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 137Issue 11November 2011
Pages: 1318 - 1334

History

Received: Dec 15, 2009
Accepted: Apr 11, 2011
Published online: Apr 13, 2011
Published in print: Nov 1, 2011

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I. Albayrak [email protected]
Laboratory of Hydraulics, Hydrology and Glaciology (VAW), Swiss Federal Institute of Technology (ETH) Zürich, VAW E 35, Gloriastrasse 37/39, 8092 Zürich, Switzerland; formerly, School of Engineering, Fraser Noble Building, Univ. of Aberdeen, AB24 3UE Aberdeen, UK (corresponding author). E-mail: [email protected]
Laboratory of Environmental Hydraulics (LHE), Ecole Polytechnique Fédérale de Lausanne (EPFL), Switzerland. E-mail: [email protected]

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