Open WL Archief (OWA)

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Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.

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one publication added to basket [14850]

Marine and estuarine gradients: an overview McLusky, D.S. (1993). Marine and estuarine gradients: an overview. Neth. J. Aquat. Ecol. 27(2-4): 489-493. https://dx.doi.org/10.1007/BF02334809 In: Netherlands Journal of Aquatic Ecology. Kluwer Academic Publishers/Netherlands Society of Aquatic Ecology: Bilthoven. ISSN 1380-8427; e-ISSN 2214-7098, meer Ook verschenen in: Meire, P.; Vincx, M. (Ed.) (1993). Marine and estuarine gradients: ECSA 21: Proceedings of the 21st symposium of the Estuarine and Coastal Sciences Association held in Gent, 9-14 september 1991. Netherlands Journal of Aquatic Ecology, 27(2-4). Netherlands Society of Aquatic Ecology: Bilthoven. 496 pp., meer

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Beschikbaar in	Auteur
VLIZ: Non-open access 338764 [ aanvragen ]

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Trefwoorden

Chemical elements > Nonmetals > Atmospheric gases > Oxygen Gradients Properties > Chemical properties > Salinity Properties > Physical properties > Thermodynamic properties > Temperature Properties > Physical properties > Turbidity Marien/Kust; Brak water

Author keywords

co-variables; tidal freshwaters

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Auteur		Top
McLusky, D.S.

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Abstract

The Proceedings of the ECSA 21 symposium on Marine and Estuarine Gradients are reviewed. It is emphasised that this is probably the first time that a full set of papers on the tidal freshwater sections of estuaries has appeared. There is however some ambiguity in the terminology applied to such waters, and a more consistent terminology is proposed. In particular the estuary is defined as reaching upstream as far as the tidal limit, irrespective of salinity. A wide variety of gradients within estuaries and coastal waters are considered, but it is apparent that the crucial spatial gradients are based on salinity, oxygen and turbidity, and that many other gradients are co-variables with these parameters. Temperature is also important for temporal gradients.

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