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Effect of relative depth in physical models of sediment transport in unidirectional flows / by B.G. Krishnappan, [Peter Engel]. : En13-5/86-102E-PDF

"In establishing scaling laws for physical models to simulate sediment transport rate in the vicinity of the bed in unidirectional flows, it has been a common practice to neglect the effect of the relative depth and consider only the shear Reynolds number and the mobility number. As a result, scale effects are introduced in the model because of the influence of flow depth on bed form geometry which in turn affects the friction factor and the sediment transport rate. This paper describes an experimental study to systematically measure the effect of the relative depth on sediment transport rate"--Abstract.

Lien permanent pour cette publication :
publications.gc.ca/pub?id=9.849511&sl=1

Renseignements sur la publication
Ministère/Organisme
  • Canada. Environment Canada.
  • National Water Research Institute (Canada)
TitreEffect of relative depth in physical models of sediment transport in unidirectional flows / by B.G. Krishnappan, [Peter Engel].
Titre de la série
  • NWRI contribution ; 86-102
Type de publicationMonographie - Voir l'enregistrement principal
Langue[Anglais]
FormatTexte numérique
Document électronique
Note(s)
  • Title from cover.
  • "June 1986".
  • "This paper is to be published in the Proceedings of the IAHR Symposium '86 on Scale Effects in Modelling Sediment Transport Phenomena, Toronto, Ontario, August 25-28, 1986 and the contents are subject to change".
  • Digitized edition from print [produced by Environment and Climate Change Canada].
  • Includes bibliographical references: p. 11.
  • Includes abstract in French.
Information sur la publication
  • Burlington, Ont. : Hydraulics Division, National Water Research Institute, Canada Centre for Inland Waters, 1986.
Auteur / Contributeur
  • Krishnappan, B. G., 1943-
  • Engel, Peter, 1938-
Description12 p. : ill.
Numéro de catalogue
  • En13-5/86-102E-PDF
Descripteurs
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