Tidal Hydraulics

Keyword(s):  
2020 ◽  
Vol 125 (12) ◽  
Author(s):  
L. Fernando Pareja‐Roman ◽  
Robert J. Chant ◽  
Christopher K. Sommerfield

1980 ◽  
Vol 1 (17) ◽  
pp. 96
Author(s):  
Bruce M. Druery

Between mid 1974 and mid 1975,760,000 m3 of sand was dredged from the bed of the Tweed River for the purpose of nourishing cyclone damaged beaches of the Gold Coast (Queensland). A comprehensive field data programme was established in 1976 to record the changes in the hydraulic processes of the Tweed River brought about by the dredging. The field measurements demonstrated that the dredged area was being infilled with sediments of both marine and estuarine origin. The dredging increased tidal ranges throughout the lower estuary, the effect being more pronounced at low water. Sediment bedload rates were estimated from detailed measurements of bedforms and used to calibrate a sediment transport formula. The formula was used in conjunction with a 1 Dim. numerical model of tidal hydraulics to simulate estuarine shoal dynamics by means of a simple sediment routing technique. The results showed that the dredging had altered the tidal hydrodynamics so as to enhance the ebb transport of sediment towards the dredged hole. In the long term it was found that the sediment transport switched to a weak net upstream movement of sediment. The detailed hydraulic mechanisms involved are discussed. The study demonstrates that the impact of dredging can be minimised by location upstream of the entrance plug of marine sand.


2011 ◽  
Vol 1 (8) ◽  
pp. 34
Author(s):  
E.A. Weiser ◽  
Jack Armstrong

It was in July 1956 when the senior writer of this paper was requested to prepare a program for investigations and studies required in connection with the proposed deep-draft channel from the Gulf of Mexico to Point Comfort. During 1938 to 19^0, the senior writer had attempted to analyze the available field and model study data which were then available on Galveston Bay in the hope of thus being able to reduce the shoaling in the various deep draft channels in Galveston Bay. In 19^0, the senior writer had been in charge of two field parties one of which measured the flow of water in the Colorado River and the Gulf Intracoastal Waterway near their crossing near Matagorda, Texas. A peak discharge of about 80,000 cubic feet per second was measured in the Colorado River at the Palacios Road bridge, about 15 miles upstream from its mouth during this period. At that time there were no locks nor gates in the Intracoastal Waterway adjacent to the Colorado River. It was found then that about one third of this peak river discharge flowed southwest through the Intracoastal Waterway. On the basis of the above experience and the information obtained from a review of the Matagorda Ship Channel, Texas, project report (l) and other literature, then, available (2) thru (5) a program was formulated in June 1958 and submitted to the Division Engineer in Dallas with the request that the Office of the Chief of Engineers, the Southwestern Division Engineer Office, the Beach Erosion Board and the Committee on Tidal Hydraulics review the program.


2000 ◽  
Vol 1 (4) ◽  
pp. 19
Author(s):  
J. B. Schijf

The reconstruction of the damage to the dikes by the flood of February 1953 presented an enormous task. From the hydraulic engineer's point of view the most interesting part was the closing of the major or tidal breaches, that is to say, the places where a dike for a certain length was totally destroyed and where, therefore, the tides had free entrance to the inundated interior, scouring out deep gullies. This called into action the resources of tidal hydraulics, theoretical considerations, and model experiments.


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