{"refrec":{"BRefID":13074,"RR":"<b>Rommets, J.W.; Postma, H.</b> (1972). Fluorescentie als natuurlijke tracer in de Waddenzee. <i>Interne verslagen Nederlands Instituut voor Onderzoek der Zee</i>, 1972(6). Nederlands Instituut voor Onderzoek der Zee: Texel. 6 pp.","BEntID":13074,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Interne verslagen Nederlands Instituut voor Onderzoek der Zee</i>, 1972(6). Nederlands Instituut voor Onderzoek der Zee: Texel.  6 pp.","DocTypID":13,"DocType":"Reports","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Rommets, J.W.; Postma, H.","OrigTitleTranslFlag":1,"Authorstringtrunc":"Rommets, J.W.; Postma, H.","Englishabstract":"While interpreting the data found in a region like the Wadden Sea, it can be of great help to dispose of fluorescent values of those samples. In the Eems estuary it is possible to calculate the addition of Westwoldse Aa. Deviations in the Western Wadden Sea indicate scour water different from the Yssel lake or a local creation of fluorescent materials from e.g. accumulated plankton. In the Easterly Wadden Sea different factors are of significance.","AbstractOtherLang":"Bij de interpretatie van gegevens gevonden in een gebied als de Waddenzee kan het een grote steun zijn om te beschikken over fluorescentiewaarden van die monsters. In het Eems estuarium is het mogelijk de bijmenging met Westerwoldse Aa water te berekenen. Afwijkingen in de Westelijke Waddenzee wijzen op spuiwater anders dan van het IJsselmeer of een plaatselijk ontstaan van fluorescerende stoffen uit bv opgehoopt plankton. 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