{"refrec":{"BRefID":418838,"RR":"<b>Van Goethem, S.; Michielsen, S.; Nguyen, D.; Hemelaer, J.; Thant, S.; Bertels, J.; Meire, D.; Plancke, Y.; Vereecken, H.</b> (2025). Monitoring Effecten Ontwikkelingsschets (MONEOS) – Jaarboek monitoring 2024: data rapportage monitoring waterbeweging en fysische parameters in Zeeschelde en bijrivieren. Versie 4.0. <i>WL Rapporten</i>, PA047_14. Waterbouwkundig Laboratorium: Antwerpen. XV, 100 + 31 p. bijl. pp. <a href=\"https://dx.doi.org/10.48607/359\" target=\"_blank\">https://dx.doi.org/10.48607/359</a>","BEntID":416668,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Versie 4.0. <i>WL Rapporten</i>, PA047_14. Waterbouwkundig Laboratorium: Antwerpen.  XV, 100 + 31 p. bijl. pp. <a href=\"https://dx.doi.org/10.48607/359\" target=\"_blank\">https://dx.doi.org/10.48607/359</a>","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Van Goethem, S.; Michielsen, S.; Nguyen, D.; Hemelaer, J.; Thant, S.; Bertels, J.; Meire, D.; Plancke, Y.; Vereecken, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Van Goethem, S. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"Voorliggend MONEOS jaarboek presenteert de resultaten van de systeemmonitoring in het Schelde &nbsp;estuarium uitgevoerd door het Waterbouwkundig Laboratorium in het jaar 2024. De uitgevoerde monitoring &nbsp;betreft de continue metingen van waterstand, debiet, stroming, saliniteit en sedimentconcentratie, &nbsp;alsook vaarten (halftij-eb en 13-uursmetingen) en periodieke metingen zwevende stof. &nbsp;Tevens is een inschatting gemaakt van de fluviatiele aanvoer van sediment, alsook van de PFAS-vrachten &nbsp;doorheen de Zeeschelde. Tenslotte worden ook de morfologische veranderingen van de Zeeschelde &nbsp;beschreven op basis van de topo-bathymetrische metingen.<br>Het enige stormtij in 2024 trad op op 15 januari 2024, te Antwerpen werd een waterstand van +6,68 mTAW &nbsp;bereikt. Op 23 december werd er een zeer hoog laagwater gemeten (+2,29 mTAW). Dat was niet meer &nbsp;gebeurd sinds 5 januari 2012 (+2,28 mTAW).<br>Het jaargemiddelde bovendebiet van 2024 voor Schelle bedraagt 172 m³/s. Dit is de hoogste waarde sinds &nbsp;2002. Over de periode 1949-2021 is er in slechts 5% van de jaren een jaardebiet hoger dan deze waarde. &nbsp;De aanvoer via de Rupel vormt bijna het hele jaar door het grootste aandeel van de bovenafvoer in Schelle. &nbsp;Gemiddeld 58 % van de aanvoer in Schelle wordt langs de Rupel aangevoerd. Volgens het KMI was 2024 het &nbsp;natste jaarsinds het begin van de metingen in 1833. Logischerwijs zorgt dat voor hoge afvoeren in de rivieren.<br>De gemiddelde stroomsnelheden bij Oosterweel tijdens vloed en eb zijn vergelijkbaar met elkaar, hoewel &nbsp;de gemiddelde waarden voor eb iets hoger liggen dan bij vloed. Dit is voornamelijk het geval voor de &nbsp;periode juni-november. Er ontwikkelt zich gedurende de springtijcondities en in beperktere mate bij &nbsp;gemiddelde tijcondities een duidelijke piek in stroomsnelheid tijdens de vloedfase, ongeveer 1 tot 2 uur &nbsp;voor het optreden van kentering hoogwater. Het stroomsnelheidsverloop van 2024 is, in vergelijking &nbsp;met de voorgaande jaren, gekenmerkt door eerder lagere snelheden.<br>In vergelijking met voorgaande jaren is de saliniteit in 2024 heel laag. In Oosterweel en Prosperpolder wordt &nbsp;de saliniteit het langst gemeten en de saliniteit was er sinds 2003 niet meer zo laag, resp. &lt; 5 PSU en &lt; 10 PSU.<br>In 2024 worden de hoogste gemiddelde SSC waarden waargenomen ter hoogte van Oosterweel-Boven en Melle.<br>De jaarstatistieken voor de sedimentconcentratie bij respectievelijk kentering hoogwater en kentering laagwater vallen binnen de range met voorgaande jaren maar eerder aan de lage kant, mogelijks als gevolg &nbsp;van de hogere aanvoer.<br>De methode voor de bepaling van de sedimentvracht is geactualiseerd. Ondanks de vernieuwde methode &nbsp;voor de correctie a.h.v. (EWI)ijkmetingen blijven de grootste jaarlijkse vrachten aangevoerd worden vanuit &nbsp;het Zennebekken. De sedimentaanvoer van de Leie en Bovenschelde is vergelijkbaar met die van de Dender. &nbsp;Via de Grote Nete wordt het minste sediment aangevoerd, de aanvoer is er 30x kleiner dan die van de Zenne. &nbsp;De totale sedimentvracht richting Schelde estuarium voor het jaar 2024 bedraagt 9,2 * 105 ton.<br>&nbsp;Voor de vijf geobserveerde PFAS-componenten is er een toename van de vracht van stroomopwaarts naar &nbsp;stroomafwaarts. 4 componenten vertonen min of meer dezelfde evolutie doorheen het stroomgebied.","BibLvlCode":"MS","StandardTitle":"Monitoring Effecten Ontwikkelingsschets (MONEOS) – Jaarboek monitoring 2024: data rapportage monitoring waterbeweging en fysische parameters in Zeeschelde en bijrivieren","OrigTitleLangCode":"nl","OrigTitleLangCodeExtended":"dut","OrigTitleLangID":41,"DateLastModified":{"date":"2026-04-19 01:39:16.211860","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":null,"MonPub":2025,"DateUpdate":"2026-03-27","DateCreate":"2025-10-08","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":null,"monrec":{"MonID":418838,"ISBN":null,"PubliDate":2025,"IssueDate":null,"Volume":"PA047_14","Issue":null,"Pagination":"XV, 100 + 31 p. bijl.","Place":"Antwerpen","Edition":"Versie 4.0","BRefXtra":null,"BRefXtraRR":null,"SerID":24938,"SerRR":"WL Rapporten. 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