Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea

The role of particles for U isotope transport was investigated in the Kalix River watershed, a particle-poor, Fe/Mn-rich river in northern Sweden, and in the Baltic Sea estuary. Particles >0.45μm are strongly enriched in U and contain 20-50% of the total riverine uranium budget and <1% of the...

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Published in:Geochimica et Cosmochimica Acta
Main Authors: Andersson, P. S., Porcelli, D., Wasserburg, G. J., Ingri, J.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier 1998
Subjects:
Online Access:https://doi.org/10.1016/S0016-7037(97)00342-6
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spelling ftcaltechauth:oai:authors.library.caltech.edu:8ndgx-rkv54 2024-10-20T14:10:55+00:00 Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea Andersson, P. S. Porcelli, D. Wasserburg, G. J. Ingri, J. 1998-02 https://doi.org/10.1016/S0016-7037(97)00342-6 unknown Elsevier eprintid:42569 info:eu-repo/semantics/closedAccess Other Geochimica et Cosmochimica Acta, 62(3), 385-392, (1998-02) info:eu-repo/semantics/article 1998 ftcaltechauth https://doi.org/10.1016/S0016-7037(97)00342-6 2024-09-25T18:46:37Z The role of particles for U isotope transport was investigated in the Kalix River watershed, a particle-poor, Fe/Mn-rich river in northern Sweden, and in the Baltic Sea estuary. Particles >0.45μm are strongly enriched in U and contain 20-50% of the total riverine uranium budget and <1% of the total U in brackish waters (3-7 PSU). The particles have high δ^(234)U which is close to that of dissolved U in the associated water, indicating that U on particles is dominantly nondetrital and isotopically exchanges rapidly with the ambient dissolved U. Particles at the river mouth are dominated by nondetrital Fe-Mn oxyhydroxides. Uranium and Fe are strongly correlated, clearly demonstrating that secondary Fe-oxyhydroxide is the major carrier of U in river water. There is no evidence for significant association of U with Mn-oxyhydroxide. Apparent U distribution coefficients (K_d^(Fe)) were calculated for U between the authigenic Fe on particles and the solution. These values appear to be relatively constant throughout the year. This suggests an equilibrium between Fe in solution and authigenic Fe-oxyhydroxides on detrital particles. High values of K_d^(Fe) calculated for one summer as well as high U concentrations in brackish waters can be explained by U scavenging by biogenic phases with low authigenic Fe content. © 1998 Elsevier Science Ltd. Received June 18, 1997; accepted in revised form September 24, 1997. This work was supported by Swedish Natural Science Research Council grants G/GU 06331-311 and G/GU 06331-312 to PSA and DOE grant DE-FG-03-88ER-13851. We thank the Swedish Meteorological and Hydrological Institute for allowing us to participate in the R/V Argos cruise. Magnus Hedberg gave us invaluable support. Reviews by J. Edmond and D. Turner significantly improved the manuscript. This is Div. Contr. No. 5695 (950). Article in Journal/Newspaper Northern Sweden Caltech Authors (California Institute of Technology) Kalix ENVELOPE(23.156,23.156,65.853,65.853) Geochimica et Cosmochimica Acta 62 3 385 392
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description The role of particles for U isotope transport was investigated in the Kalix River watershed, a particle-poor, Fe/Mn-rich river in northern Sweden, and in the Baltic Sea estuary. Particles >0.45μm are strongly enriched in U and contain 20-50% of the total riverine uranium budget and <1% of the total U in brackish waters (3-7 PSU). The particles have high δ^(234)U which is close to that of dissolved U in the associated water, indicating that U on particles is dominantly nondetrital and isotopically exchanges rapidly with the ambient dissolved U. Particles at the river mouth are dominated by nondetrital Fe-Mn oxyhydroxides. Uranium and Fe are strongly correlated, clearly demonstrating that secondary Fe-oxyhydroxide is the major carrier of U in river water. There is no evidence for significant association of U with Mn-oxyhydroxide. Apparent U distribution coefficients (K_d^(Fe)) were calculated for U between the authigenic Fe on particles and the solution. These values appear to be relatively constant throughout the year. This suggests an equilibrium between Fe in solution and authigenic Fe-oxyhydroxides on detrital particles. High values of K_d^(Fe) calculated for one summer as well as high U concentrations in brackish waters can be explained by U scavenging by biogenic phases with low authigenic Fe content. © 1998 Elsevier Science Ltd. Received June 18, 1997; accepted in revised form September 24, 1997. This work was supported by Swedish Natural Science Research Council grants G/GU 06331-311 and G/GU 06331-312 to PSA and DOE grant DE-FG-03-88ER-13851. We thank the Swedish Meteorological and Hydrological Institute for allowing us to participate in the R/V Argos cruise. Magnus Hedberg gave us invaluable support. Reviews by J. Edmond and D. Turner significantly improved the manuscript. This is Div. Contr. No. 5695 (950).
format Article in Journal/Newspaper
author Andersson, P. S.
Porcelli, D.
Wasserburg, G. J.
Ingri, J.
spellingShingle Andersson, P. S.
Porcelli, D.
Wasserburg, G. J.
Ingri, J.
Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea
author_facet Andersson, P. S.
Porcelli, D.
Wasserburg, G. J.
Ingri, J.
author_sort Andersson, P. S.
title Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea
title_short Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea
title_full Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea
title_fullStr Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea
title_full_unstemmed Particle transport of ^(234)U-^(238)U in the Kalix River and in the Baltic Sea
title_sort particle transport of ^(234)u-^(238)u in the kalix river and in the baltic sea
publisher Elsevier
publishDate 1998
url https://doi.org/10.1016/S0016-7037(97)00342-6
long_lat ENVELOPE(23.156,23.156,65.853,65.853)
geographic Kalix
geographic_facet Kalix
genre Northern Sweden
genre_facet Northern Sweden
op_source Geochimica et Cosmochimica Acta, 62(3), 385-392, (1998-02)
op_relation eprintid:42569
op_rights info:eu-repo/semantics/closedAccess
Other
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