Research Article
Jun 1982
Origin of Step-Pool Systems in Mountain Streams
Publication: Journal of the Hydraulics Division
Volume 108, Issue 6
Abstract
Mountain streams very often present a step-pool aspect. Antidune formation alone; dispersion and sorting theory or velocity reversal as advocated for the origin of riffle-pool sequences do not explain how steps and pools form. Experiments have been conducted to clarify their origin. It was found that the step-pool aspect appears after high flows had deformed the bed. During the presented tests a self armoring process occurred which resulted in a stabilization of the bed. When coarsening of the top layer was little classic antidunes resulted. An important coarsening was accompanied by a structuring of the bed into roughness elements whose spacing did correspond to maximum flow resistance. The substantial increase in resistance was an essential factor in bed-stabilization.
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Published In
Journal of the Hydraulics Division
Volume 108 • Issue 6 • June 1982
Pages: 758 - 773
Copyright
© 1982 American Society of Civil Engineers.
History
Published in print: Jun 1982
Published online: Feb 3, 2021
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Jeffrey G. Whittaker
Research Fellow, Dept. of Agr. Engrg., Univ. of Canterbury, Lincoln Coll., Canterbury, New Zealand
Martin N. R. Jaeggi
Sr. Research Engr., Lab. of Hydr., Hydrology, and Glaciology, Federal Inst. of Tech., Zurich, Switzerland
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Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.