{"refrec":{"BRefID":12996,"RR":"<b>van Beusekom, J.E.E.</b> (1983). Opgelost silicaat en aluminium in de Groenlandzee, Noorse Zee en IJslandzee. <i>Interne verslagen Nederlands Instituut voor Onderzoek der Zee</i>, 1983(8). NIOZ: Texel. 45 pp.","BEntID":12996,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Interne verslagen Nederlands Instituut voor Onderzoek der Zee</i>, 1983(8). NIOZ: Texel.  45 pp.","DocTypID":13,"DocType":"Reports","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van Beusekom, J.E.E.","OrigTitleTranslFlag":1,"Authorstringtrunc":"van Beusekom, J.E.E.","Englishabstract":"During the Meteor cruise 61 Al- and Si-data have been gathered. Results show that two processes influence the Al- and Si concentration. Due to diatom growth the Al- and Si-concentration decreases. In the Deep Water the Al- and Si concentration increases due to the flux from the sediment. A flux calculation shows that not Atlantic Water but a different watermass with higher Si-concentration is the major direct source for Greenland Sea Deep Water. It is suggested that this watermass is part of the Polar Ocean Deep Water. This part of the Polar Ocean Deep Water moves southward along the east of Greenland at depth of 1000-2000 meter. Al/Si- plots show the existence of a surface watermass, an intermediate watermass with a core depth of 1000-2000 meters and a bottom watermass and suggest that Polar Ocean Deep Water is the source of not only the intermediate water in the west of the Greenland Sea but of all the intermediate water in the Greenland Sea, Iceland Sea and Norwegian Sea. Bottom water is formed in the south of the Greenland Sea as a mixture of an Arctic Water type that can be found in the winter at the surface of the Greenland Sea and of Polar Ocean Deep Water. Part of this new-formed Greenland Sea Deep Water mixes in the north of the Greenland Sea with the Intermediate Water and is thus transformed to Norwegian Sea Deep Water. It fills the Lofoten basin from the north. Another part of the Greenland Sea Deep Water enters the south of the Lofoten basin through gaps in the Mohn-ridge. The Norwegian basin and Lofoten basin exchange Norwegian Sea Deep Water through gaps in the east - Jan Mayen fracture zone.","AbstractOtherLang":"Tijdens de Meteor tocht 61 zijn Al- en Si- gegevens verzameld. De resultaten laten zien dat zowel de Al- als de Si-concentratie door twee processen beïnvloedt wordt. Door diatomeeëngroei wordt zowel aluminium als silicaat uit het water opgenomen en ingebouwd in hun silicaatskeletjes. In het Diepe Water wordt de Al- en Si-concentratie verhoogd door een flux uit het bodemsediment. Een fluxberekening laat zien dat niet Atlantisch water maar een andere watermassa met hogere Si-concentratie de belangrijkste directe bron voor Groenland Zee Diepte Water is. Het wordt gesuggereerd dat deze watermassa een component is van het Poolzee Diep Water die zich op diepten van 1000-2000 meter langs oost-Groenland zuidwaart beweegt. Al/Si-plots laten het bestaan van een oppervlakte watermassa, een middelste watermasa met een kerndiepte van 1000-2000 meter en een bodemwatermassa zien en suggereren dat Poolzee Diep Water behalve in het westen van de Groenlandzee overal de middelste watermassa vormt. Het bodemwater ontstaat in het zuiden van de Groenlandzee als mengsel van een Arctisch Watertype dat in de winter aan de oppervlakt kan worden aangetroffen en van Poolzee Diep Water. Van dit nieuwe Groenland Zee Diep Water mengt zich een deel in het noorden van de Groenlandzee met Poolzee Diep Water tot Norwegian Sea Deep Water en vult vanuit het noorden het Lofotenbekken. Een ander deel stroomt via de Mohn-rug in het zuidelijk deel van het Lofotenbekken. Het Noorse bekken en het Lofotenbekken wisselen door dalen in de Jan Mayen breukzone Norwegian Sea Deep Water uit.","BibLvlCode":"MS","StandardTitle":"Opgelost silicaat en aluminium in de Groenlandzee, Noorse Zee en IJslandzee","OrigTitleLangCode":"nl","OrigTitleLangCodeExtended":"dut","OrigTitleLangID":41,"DateLastModified":{"date":"2025-07-25 01:33:49.256478","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":null,"MonPub":1983,"DateUpdate":"2025-07-18","DateCreate":"2001-07-06","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":null,"monrec":{"MonID":12996,"ISBN":null,"PubliDate":1983,"IssueDate":null,"Volume":"1983","Issue":"8","Pagination":"45","Place":"Texel","Edition":null,"BRefXtra":null,"BRefXtraRR":null,"SerID":5036,"SerRR":"Interne verslagen Nederlands Instituut voor Onderzoek der Zee. 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