TECHNICAL PAPERS
Jul 1, 1991

Wake Vortex Scour at Bridge Piers

Publication: Journal of Hydraulic Engineering
Volume 117, Issue 7

Abstract

At most bridges, wake vortex scour is insignificant and confluence scour does not exist. In clear‐water rivers flowing on fine sand, these two forms of local scour can be very large. The deep scour holes downstream from the large circular piers (10 and 15 m in diameter) at the Tahrir and Imbaba Bridges over the Nile River in Cairo, Egypt were produced by the conflicting velocity fields at the intersection of the wake vortex streams from adjacent piers. The depths of scour due to these wake vortices are now 8 to 11 m where the normal depth of flow is approximately 8 m. Confluence scour where the main and side channel join upstream from the Imbaba Bridge was 9 m in 1981 and 1987 and was aligned with the bisector of the intersection angle of the two channels. These depths of scour can be considered nearly clear‐water scour as the bridges are in the backwater of the Delta Barrages, the velocity is less than 1 m/s, and sediment transport is very low.

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Published In

Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 117Issue 7July 1991
Pages: 891 - 904

History

Published online: Jul 1, 1991
Published in print: Jul 1991

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Authors

Affiliations

Michael A. Stevens
Consultant, P.O. Box 3263, Boulder, CO 80307 and Affiliate Faculty, Civil Engineering, Colorado State Univ., Fort Collins, CO 80523
Mohamed M. Gasser
Dir., The Hydr. and Sediment Res. Inst., Delta Barrage, Egypt
Mohamed B. A. M. Saad
Sr. Researcher, The Hydr. and Sediment Res. Inst., Delta Barrage, Egypt

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