Uranium biogeochemistry across the redox transition zone of a permanently stratified fjord: Framvaren, Norway

During August 1995, the vertical concentration profile of dissolved and particulate uranium exhibited strong non-conservative characteristics in the upper 30 m of Framvaren Fjord. There was a pronounced peak in both particulate (>0.2 μm; 1.09 nM) and dissolved (

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Bibliographic Details
Published in:Marine chemistry 1999-11, Vol.67 (3), p.181-198
Main Authors: Swarzenski, P.W., McKee, B.A., Skei, J.M., Todd, J.F.
Format: Article
Language:English
Subjects:
Earth sciences
Earth, ocean, space
Exact sciences and technology
External geophysics
Framvaren Fjord
Geochemistry
Marine
microbial mobilization
Mineralogy
oxidation–reduction
Physical and chemical properties of sea water
Physics of the oceans
Silicates
U oxidation states
uranium biogeochemistry
Water geochemistry
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Description
Summary:During August 1995, the vertical concentration profile of dissolved and particulate uranium exhibited strong non-conservative characteristics in the upper 30 m of Framvaren Fjord. There was a pronounced peak in both particulate (>0.2 μm; 1.09 nM) and dissolved (
ISSN:0304-4203
1872-7581
DOI:10.1016/S0304-4203(99)00058-4