Research Article
Feb 1970

Formation of Dunes and Antidunes in Open Channels

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Publication: Journal of the Hydraulics Division
Volume 96, Issue 2

Abstract

The formation of dunes and antidunes on the erodible bed of an open channel is studied analytically as a problem of stability of the erodible bed. The phase lag existing between the local sediment-transport rate and the local velocity on the bed plays an essential role in the formation of the sand waves. A physical model for the transport of sediment over a wavy bed is presented and a quantitative explanation of this phase lag is developed. The regions of occurrence of dunes of those bed configurations are compared with experimental results previously summarized by Kennedy, the comparison showing a good agreement.

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Journal of the Hydraulics Division
Volume 96Issue 2February 1970
Pages: 357 - 366

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Published in print: Feb 1970
Published online: Feb 3, 2021

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Taizo Hayashi, F.ASCE
Visiting Prof., Inst. of Hydr. Res., Univ. of Iowa, Iowa City; at present, Prof. of Hydr., Chuo Univ., Tokyo, Japan

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