{"title":"Scheldt Estuary and its alluvial plains - Belgium","id":{"prefix":"https:\/\/deims.org\/","suffix":"f64f5541-c6a5-45ff-a996-bb4e799d6736"},"type":"site","created":"2014-09-19T16:28:03+02:00","changed":"2025-01-07T11:14:56+01:00","attributes":{"affiliation":{"networks":[{"network":{"name":"GERI","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"c3abdc60-49f1-49db-81fe-863b7dbb21d3"}},"siteCode":null,"verified":true},{"network":{"name":"ILTER","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"1aa7ccb2-a14b-43d6-90ac-5e0a6bc1d65b"}},"siteCode":null,"verified":true},{"network":{"name":"LTER Belgium","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"735946e0-4e9e-484a-acee-85e31f4e2a2e"}},"siteCode":"LTER_EU_BE_06","verified":true},{"network":{"name":"LTER Europe","id":{"prefix":"https:\/\/deims.org\/networks\/","suffix":"4742ffca-65ac-4aae-815f-83738500a1fc"}},"siteCode":null,"verified":true}],"projects":[{"label":"Natura 2000","uri":"https:\/\/natura2000.eea.europa.eu\/"},{"label":"Ramsar Convention on Wetlands","uri":"https:\/\/www.ramsar.org"}]},"contact":{"siteManager":[{"type":"person","name":"Gunther Van Ryckegem","email":"Gunther.Van.Ryckegem@inbo.be","orcid":null}],"operatingOrganisation":null,"metadataProvider":[{"type":"person","name":"Gunther Van Ryckegem","email":"Gunther.Van.Ryckegem@inbo.be","orcid":null}],"fundingAgency":null,"siteUrl":null},"general":{"abstract":"The study site starts at the mouth of the river (Vlissingen, the Netherlands) and extends to Gent, 160 km from the mouth, where tidal influence is stopped by sluices. The tributaries the Durme and the Rupel, with the Nete , Dijle and Zenne are also under tidal influence and are considered part of the estuary. The natural inundated areas around the river and the valleys up to 5m TAW are also part of the study system.","citation":null,"relatedIdentifiers":null,"status":{"label":"Operational","uri":"http:\/\/vocabs.lter-europe.net\/elter_cl\/10772"},"yearEstablished":1991,"yearClosed":null,"relatedSites":[{"typeOfRelationship":{"label":"contains","uri":"null"},"listOfSites":[{"type":"site","title":"Durme debouchment - Belgium","id":{"prefix":"https:\/\/deims.org\/","suffix":"091be706-4e09-43d6-8523-c9cfe829176a"},"changed":"2023-07-25T09:57:09+0200"},{"type":"site","title":"Ketenisse - Belgium","id":{"prefix":"https:\/\/deims.org\/","suffix":"22709233-3029-435e-968d-0c201d88daa8"},"changed":"2023-07-25T09:58:02+0200"},{"type":"site","title":"Lippenbroek - Belgium","id":{"prefix":"https:\/\/deims.org\/","suffix":"3b6e9142-e09b-4467-8faf-299a3fe03bee"},"changed":"2023-07-25T09:57:12+0200"},{"type":"site","title":"Notelaar - Belgium","id":{"prefix":"https:\/\/deims.org\/","suffix":"506339be-afca-4dd2-86e7-b5ae17d32af5"},"changed":"2023-07-25T09:57:58+0200"},{"type":"site","title":"Paardenschor - Belgium","id":{"prefix":"https:\/\/deims.org\/","suffix":"d0a8b449-d5e5-4902-8790-d8fc9d111d15"},"changed":"2023-07-25T09:57:30+0200"}]}],"siteName":"Scheldt Estuary and its alluvial plains","shortName":"Scheldt estuary","siteType":"Platform","protectionLevel":null,"landUse":null,"images":[{"url":"https:\/\/deims.org\/sites\/default\/files\/photos\/LTER_EU_BE_06_Scheldt.JPG","alt":"not defined"},{"url":"https:\/\/deims.org\/sites\/default\/files\/photos\/LTER_EU_BE_06_Durme_Schelde.png","alt":"not defined"}]},"environmentalCharacteristics":{"airTemperature":{"yearlyAverage":10.5,"monthlyAverage":null,"unit":"\u00b0C","referencePeriod":null},"precipitation":{"yearlyAverage":852.4,"monthlyAverage":null,"unit":"mm","referencePeriod":null},"biogeographicalRegion":"atlantic","biome":"marine","ecosystemType":[{"label":"Large river deltas","uri":null},{"label":"Rivers","uri":null}],"eunisHabitat":[{"label":"Coastal saltmarshes and saline reedbeds (A2.5)","uri":null},{"label":"Littoral mud (A2.3)","uri":null},{"label":"Littoral sand and muddy sand (A2.2)","uri":null},{"label":"Littoral sediment (A2)","uri":null},{"label":"Marine habitats (A)","uri":null}],"landforms":null,"geoBonBiome":["Marine"],"geology":"The Scheldt estuary as we know it now is only formed 700 years ago, when mayor flood connected the Easter and Westerscheldt . The latter would become the only entry of the Scheldt. The river it self dates from a much older period (Pliocene).","hydrology":"The Scheldt is rain fed river with a macro tidal estuary (maximum tidal amplitude 5.4 m). 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