The Influence Of Freshwater Distribution On SPM Transport In The Dutch Coastal Zone
Price
Free (open access)
Transaction
Volume
58
Pages
16
Published
2001
Size
1,988 kb
Paper DOI
10.2495/CE010281
Copyright
WIT Press
Author(s)
J.M. de Kok
Abstract
The influence of fresh water distribution on SPM transport in the Dutch coastal zone J. M. de Kok National Institute for Coastal and Marine Management/RIKZ NL-2500 EX The Hague Abstract The rivers Rhine and Meuse - interconnected in the Dutch delta - flow into the North Sea through two outlets: the Rotterdam Waterway and the Haringvliet. The distribution of fresh water between the Rotterdam Waterway and the Haringvliet can be controlled by the management of sluices in the Haringvliet. A change in the management of the Haringvliet sluices can cause a different distribution of river run off over the two outlets and consequently a different salinity pattern around the mouths of Haringvliet and Rotterdam Waterway. This results also in a different transport pattern of cohesive sediment in the area, as it is strongly influenced by the salinity distribution. A case study with a high resolution 3D baroclinic tidal model combined with a cohesive sediment transport model was conducted to
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