TECHNICAL NOTES
Feb 1, 1983
Antidune Movement
Publication: Journal of Hydraulic Engineering
Volume 109, Issue 2
Abstract
A new mechanism is introduced to explain the intriguing movement of antidunes. It is suggested that this mechanism may exist concurrently with sediment erosion-deposition patterns used heretofore to explain the apparent movement of antidunes. The mechanism introduced herein may be responsible for bulk movement of antidunes.
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References
1.
Kennedy, J. F., “The Mechanics of Dunes and Antidunes in Erodible‐Bed Channels,” Journal of Fluid Mechanics, Vol. 16, Part 4, 1963, pp. 521–544.
2.
Parker, G., “Sediment Inertia as Cause of River Antidunes,” Journal of the Hydraulics Division, ASCE, Vol. 101, No. HY2, Feb., 1975, pp. 211–221.
3.
Simons, D. B., and Richardson, E. V., “Forms of Bed Roughness in Alluvial Channels,” Transactions, ASCE, Vol. 128, Part 1, Paper No. 3414, 1963, pp. 284–302.
4.
Vanoni, V. A., and Kennedy, J. F., discussion of “Forms of Bed Roughness in Alluvial Channels,” by D. B. Simon & E. V. Richardson, Transactions, ASCE, Vol. 128, Part 1, 1963, pp. 311–317.
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Copyright © 1983 ASCE.
History
Published online: Feb 1, 1983
Published in print: Feb 1983
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Authors
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Subhash C. Mehrotra
Sr. Engr., Bechtel Civ. and Minerals, Inc., Gaithersburg, Md. 20877
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ASCE Library Cards let you download journal articles, proceedings papers, and available book chapters across the entire ASCE Library platform. ASCE Library Cards remain active for 24 months or until all downloads are used. Note: This content will be debited as one download at time of checkout.
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.
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.