{"refrec":{"BRefID":352840,"RR":"<b>Stark, J.; Smolders, S.; Plancke, Y.</b> (2022). IMMERSE Work Package 3.2: model simulations for scenario 4. Version 3.0. <i>FHR reports</i>, 20_098_01. Flanders Hydraulics Research: Antwerp. III, 25 + 7 app. pp. <a href=\"https://dx.doi.org/10.48607/103\" target=\"_blank\">https://dx.doi.org/10.48607/103</a>","BEntID":350549,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Version 3.0. <i>FHR reports</i>, 20_098_01. Flanders Hydraulics Research: Antwerp.  III, 25 + 7 app. pp. <a href=\"https://dx.doi.org/10.48607/103\" target=\"_blank\">https://dx.doi.org/10.48607/103</a>","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Stark, J.; Smolders, S.; Plancke, Y.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Stark, J.; Smolders, S.; Plancke, Y.","Englishabstract":"Flanders Hydraulics Research was asked to apply a recently improved version of the cohesive sediment transport model in Delft3D-NeVla to analyze the impact of the bathymetric changes in the so-called Scenario 4 on the SSC distribution along the Scheldt estuary. In Scenario 4, developed by IMDC as part of the Interreg project IMMERSE’s Work Package 3.2, the bathymetry of the river banks in between Burcht and Rupelmonde just upstream of Antwerp (Lower Sea Scheldt) are raised to a maximum elevation of -1,0 m TAW. 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