{"refrec":{"BRefID":328054,"RR":"<b>Plancke, Y.; Aragones, E.; Vos, G.; Mostaert, F.</b> (2020). Proefstortingen Westerschelde: deelrapport 3. Analyse van de sedimentatie ter hoogte van de drempel van Hansweert. Versie 3.0. <i>WL Rapporten</i>, 19_079_3. Waterbouwkundig Laboratorium: Antwerpen. VII, 12 + 21 p. bijl. pp.","BEntID":321531,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Versie 3.0. <i>WL Rapporten</i>, 19_079_3. Waterbouwkundig Laboratorium: Antwerpen.  VII, 12 + 21 p. bijl. pp.","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Plancke, Y.; Aragones, E.; Vos, G.; Mostaert, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Plancke, Y. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"In het kader van het onderzoeksprogramma Agenda voor de Toekomst werd een analyse uitgevoerd van de sedimentatie ter hoogte van de drempel van Hansweert voor de periode 2007-2016. Sinds 2016 werden er in de nabijgelegen diepe put van Hansweert 3 proefstortingen van telkens 1 Mm<sup>3</sup> uitgevoerd, waarbij een groot deel van de specie op korte termijn getransporteerd werd. De vraag rees of deze specie zorgde voor een verhoogde sedimentatie ter hoogte van de drempel van Hansweert.<br>In dit rapport werd de eerdere analyse uitgebreid in de tijd. Hiervoor werden eerst de baggervrije periodes geselecteerd waarvoor bathymetrische (MBES) opnames beschikbaar zijn. Op deze manier kunnen de natuurlijke sedimentatieprocessen vastgesteld worden. Vervolgens werd een analyse uitgevoerd waarbij gefocust wordt op 3 topics: verschilkaarten, sedimentatiesnelheden en bodemvormen.<br>De analyse van de verschilkaarten toont dat de sedimentatiepatronen in de laatste jaren gelijkaardig zijn aan de eerder vastgestelde patronen. In de sedimentatiesnelheden wordt voor alle deelgebieden een geleidelijke stijging in de tijd waargenomen. De bodemvormen zijn in het centrale en zuidelijke deel weinig gewijzigd in de tijd. In het noordelijk deel van de drempel van Hansweert kan er wel een verandering vastgesteld worden waarbij er tot 2012 eerder kleine bodemvormen aanwezig waren, terwijl in 2020 deze kleine bodemvormen gesuperponeerd zijn bovenop grote duinen.","BibLvlCode":"MS","StandardTitle":"Proefstortingen Westerschelde: deelrapport 3. 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