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...
Published in: | Geochimica et Cosmochimica Acta |
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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 |
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Open Polar |
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Caltech Authors (California Institute of Technology) |
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ftcaltechauth |
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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 |
op_doi |
https://doi.org/10.1016/S0016-7037(97)00342-6 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
62 |
container_issue |
3 |
container_start_page |
385 |
op_container_end_page |
392 |
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1813450994204278784 |