Abstract

River ice complicates river hydraulics and morphodynamics by adding a new boundary layer to the top of the flow. This boundary layer affects the velocity distribution throughout the depth due to increased flow resistance, and varies the local boundary shear stress on the bed (lower boundary) by adding new shear stress on the upper boundary (under surface of the ice). Variation of shear stress plays an important role in incipient motion of upper and lower boundary materials: sediment motion and transport are directly affected by local boundary shear stress, as are ice cover thickness, condition, and progression. This paper provides estimates of upper and lower boundary shear stress during stable ice cover and the important stage of ice cover breakup using available methods based on continuous field measurements of velocity profiles obtained with a bottom-mounted acoustic Doppler current profiler in the Nelson River, Canada. Boundary shear stresses varied dynamically with transformation of the ice cover, including the presence and removal of slush ice and formation of the ice jams. Estimated upper boundary shear stress varied between 0.52 and 23.87N/m2, whereas lower boundary shear stress varied between 1.51 and 2.40N/m2, with the highest values observed during breakup. These values are compared with estimates from previous laboratory experiments.

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Acknowledgments

The authors would like to thank Nathan Lambkin and his crew from Manitoba Hydro for all their help and contributions during field measurements, including deployment and retrieval of instruments. We also acknowledge Mark Lapointe at University of Ottawa Civil Engineering Hydraulic Laboratory for building the deployment mount. This work was funded by Manitoba Hydro (R&D grant), Hatch corporation Ltd., and the Natural Sciences and Engineering Research Council of Canada (CRD grant).

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Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 142Issue 4April 2016

History

Received: Sep 10, 2014
Accepted: Jul 15, 2015
Published online: Dec 28, 2015
Published in print: Apr 1, 2016
Discussion open until: May 28, 2016

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Soheil Ghareh Aghaji Zare, S.M.ASCE [email protected]
Ph.D. Candidate, Dept. of Civil Engineering, Faculty of Engineering, Univ. of Ottawa, 161 Louise Pasteur, Ottawa, ON, Canada K1N 6N5 (corresponding author). E-mail: [email protected]
Stephanie A. Moore [email protected]
Postdoctoral Fellow, Dept. of Civil Engineering, Faculty of Engineering, Univ. of Ottawa, 161 Louise Pasteur, Ottawa, ON, Canada K1N 6N5. E-mail: [email protected]
Colin D. Rennie [email protected]
Professor, Dept. of Civil Engineering, Faculty of Engineering, Univ. of Ottawa, 161 Louise Pasteur, Ottawa, ON, Canada K1N 6N5. E-mail: [email protected]
Ousmane Seidou [email protected]
Associate Professor, Dept. of Civil Engineering, Faculty of Engineering, Univ. of Ottawa, 161 Louise Pasteur, Ottawa, ON, Canada K1N 6N5. E-mail: [email protected]
Habib Ahmari [email protected]
Senior Engineer, Golder Associates Ltd., 146 Commerce Dr., Winnipeg, MB, Canada R3P 0Z6. E-mail: [email protected]
Jarrod Malenchak [email protected]
Section Head, Ice and Environmental Engineering, Water Resources Engineering Dept., Manitoba Hydro, 360 Portage Ave., 15th Floor, Winnipeg, MB, Canada R3C 0G8. E-mail: [email protected]

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