Journal
COASTAL ENGINEERING JOURNAL
Volume 55, Issue 3, Pages -Publisher
WORLD SCIENTIFIC PUBL CO PTE LTD
DOI: 10.1142/S0578563413500101
Keywords
Morphological evolution; ebb-tidal delta; inlets; Eastern Scheldt; storm surge barrier
Categories
Funding
- Subsidieregeling Innovatieketen Water [953, 17009]
- Dutch Ministry of Transport, Public Works and Water Management
- European Fund for Regional Development EFRO
- Municipality of Dordrecht
- Dr. Ir. Cornelis Lely Foundation
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The morphology of the Eastern Scheldt inlet in the southwestern Netherlands has been changing for the past 25 years in response to the construction of the Eastern Scheldt storm-surge barrier in 1986. As a result of the barrier, there has been a decrease in tidal amplitudes, tidal volumes, and average flow velocities, and there is hardly any sediment exchange through the barrier. Bathymetrical measurements of the ebb-tidal delta show multiple effects: (1) An overall decrease in sediment volume, (2) a decrease in morphological activity, (3) erosion of the shoals and sedimentation in most channels, (4) northward reorientation of channels and shoals, and (5) an increase in wave-driven features. Results from a process-based model show that the erosion is related to the wave action, and the reorientation is related to the interaction between cross-shore and alongshore tide. The steady erosive trend, combined with the decline of morphological activity, points toward a system dominated by relatively small and mostly negative bed-level changes. This system is still far from any kind of equilibrium, and is still adapting itself to the new hydraulic forcing regime, even though sediment transport capacities have decreased.
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