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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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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 (, 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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