Research Article
Jun 1975
Resistance to Flow in Alluvial Channels
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VIEW THE REPLYPublication: Journal of the Hydraulics Division
Volume 101, Issue 6
Abstract
A direct method of predicting flow resistance and uniform velocity in alluvial channels is developed. The method covers all known bed-form regimes and not only eliminates trial-and-error computations and use of rigid-boundary channel flow formulas but also avoids the difficulties associated with the use of the various existing alluvial channel flow computation techniques. The study shows that the Darcy-Weisbach friction factor can be expressed as a unique function of the ratio of the bed form and grain shear stress components for any anticipated discharge and flow geometry, the bed-form shear component being uniquely determinable from the flow and channel material characteristics. The results confirm that the friction factor is nonconstant but varies with the bed-form regime. The applicability of the method to laboratory flumes, field canals, and natural rivers is illustrated.
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Published In
Journal of the Hydraulics Division
Volume 101 • Issue 6 • June 1975
Pages: 665 - 679
Copyright
© 1975 American Society of Civil Engineers.
History
Published in print: Jun 1975
Published online: Feb 3, 2021
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Authors
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ChiEmeka G. Ilo
Prin. Agricultural Engr., Soil and Water Resources, East Central State, Nigeria; on leave as Commonwealth Research Scholar, Indian Inst. of Tech., Bombay, India
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