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The stability of Fe-isotope signatures during low salinity mixing in subarctic estuaries

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Conrad, S, Wuttig, K ORCID: 0000-0003-4010-5918, Jansen, N, Rodushkin, I and Ingri, J 2019 , 'The stability of Fe-isotope signatures during low salinity mixing in subarctic estuaries' , Aquatic Geochemistry, vol. 25, no. 5-6 , pp. 195-218 , doi: 10.1007/s10498-019-09360-z.

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Abstract

We have studied iron (Fe)-isotope signals in particles (> 0.22 µm) and the dissolved phase (56Fe values than in the estuaries. Our data indicate the flocculation of the negative Fe-isotope signal in a low salinity environment, due to changes in the ionic strength and further the increase of pH.

Item Type: Article
Authors/Creators:Conrad, S and Wuttig, K and Jansen, N and Rodushkin, I and Ingri, J
Keywords: Fe-isotopes, Fe geochemistry, dissolved and particulate Fe, organically complexed Fe, Fe(oxy)hydroxides, salinity gradient, spring flood
Journal or Publication Title: Aquatic Geochemistry
Publisher: Kluwer Academic Publ
ISSN: 1380-6165
DOI / ID Number: 10.1007/s10498-019-09360-z
Copyright Information:

Copyright 2019 the authors. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution,and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made

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