TECHNICAL PAPERS
Feb 1, 2001

Spatially Averaged Open-Channel Flow over Rough Bed

Publication: Journal of Hydraulic Engineering
Volume 127, Issue 2

Abstract

In this paper it is suggested that the double-averaged (in temporal and in spatial domains) momentum equations should be used as a natural basis for the hydraulics of rough-bed open-channel flows, especially with small relative submergence. The relationships for the vertical distribution of the total stress for the simplest case of 2D, steady, uniform, spatially averaged flow over a rough bed with flat free surface are derived. These relationships explicitly include the form-induced stresses and form drag as components of the total stress. Using this approach, we define three types of rough-bed flows: (1) Flow with high relative submergence; (2) flow with small relative submergence; and (3) flow over a partially inundated rough bed. The relationships for the double-averaged velocity distribution and hydraulic resistance for all three flow types are derived and compared with measurements where possible. The double-averaged turbulent and form-induced intensities and stresses for the case of regular spherical-segment-type roughness show the dominant role of the double-averaged turbulence stresses and form drag in momentum transfer in the near-bed region.

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Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 127Issue 2February 2001
Pages: 123 - 133

History

Received: Jun 7, 1999
Published online: Feb 1, 2001
Published in print: Feb 2001

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Authors

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Sci., Nat. Inst. of Water and Atmospheric Res., P.O. Box 8602, Christchurch, New Zealand.
Sci., Nat. Inst. of Water and Atmospheric Res., P.O. Box 8602, Christchurch, New Zealand.
Sr. Lect., Dept. of Engrg., Univ. of Aberdeen AB24 3UE, U.K.
Sci., Environment Canterbury, P.O. Box 345, Christchurch, New Zealand.

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