IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Print this page

Sediment dynamics in the Schelde-estuary: report 1. Influence of fresh water discharge and tide on the ETM-dynamics in the Schelde-estuary using Delft3D
Plancke, Y.; Dupont, H.; Stark, J.; Kaptein, S.J. (2021). Sediment dynamics in the Schelde-estuary: report 1. Influence of fresh water discharge and tide on the ETM-dynamics in the Schelde-estuary using Delft3D. Version 3.0. FHR reports, 19_060_1. Flanders Hydraulics Research: Antwerp. VIII, 24 + 2 p. app. pp. https://dx.doi.org/10.48607/67
Part of: FHR reports. Flanders Hydraulics Research: Antwerp, more
Sediment dynamics in the Schelde-estuary: report 1 – Influence of fresh water discharge and tide on the ETM-dynamics in the Schelde-estuary using Delft3D

Available in  Authors 
Document type: Project report

Keywords
    Hydraulics and sediment > Hydrodynamics > Tides
    Hydraulics and sediment > Sediment > Cohesive sediment
    Numerical modelling
    Sediments
    ANE, Scheldt Estuary [Marine Regions]
Author keywords
    Fresh water discharge

Project Top | Authors 
  • Verkennende berekeningen slibverspreiding en seizoenale effecten, more

Authors  Top 
  • Plancke, Y., more
  • Dupont, H.
  • Stark, J., more
  • Kaptein, S.J., more

Abstract
    The Schelde-estuary is subjected to tides, (seasonal) variations in fresh water discharge and natural and manmade changes in bathymetry. These changes affect suspended sediment dynamics and therefore the formation and location of the estuarine turbidity maximum (ETM). An assessment of ETM formation and ETM location under different conditions of river discharge, tides and bathymetry is performed in this study using a Delft3D-numerical model.
    Overall results show lower maximum values of suspended sediment concentration (SSC) in the ETM and a movement of the ETM in downstream direction as fresh water discharges become higher. During exceptional high discharges no clear ETM can be discerned as SSC is distributed more evenly. ETM location does not change significantly between spring- and neap tide, however an increase in SSC can be found in the Beneden- Zeeschelde during spring tide conditions. Bathymetric changes between 2011 and 2019 show an upwards shift in ETM location and higher SSC in the ETM.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors