A sand transport model for the Scheldt estuary was made in the framework of the integrated plan “Upper Sea Scheldt”. This model is called “Scaldis Sand” and was able to reproduce sand transport rates measured along the Sea Scheldt and was as such validated. In this report the Scaldis sand model is adopted to evaluate the effects of the C-alternatives on the sand transport with a focus on the Upper Sea Scheldt.
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