Uranium and Nickel Partitioning in a Contaminated Riparian Wetland

Uranium (U) and nickel (Ni) released 50 years ago have been immobilized in the Tims Branch wetlands located on the Savannah River Site in the United States. Sediments were collected from seven locations to identify the factors responsible for this attenuation. Ni and U contents in the solids were si...

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Main Authors: Peng Lin, Maxim I. Boyanov, Edward J. O’Loughlin, Wei Xing, Kenneth M. Kemner, John Seaman, Steven P. Simner, Daniel I. Kaplan
Format: Article
Language:English
Published: MDPI AG 2024-03-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/16/7/966
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author Peng Lin
Maxim I. Boyanov
Edward J. O’Loughlin
Wei Xing
Kenneth M. Kemner
John Seaman
Steven P. Simner
Daniel I. Kaplan
author_facet Peng Lin
Maxim I. Boyanov
Edward J. O’Loughlin
Wei Xing
Kenneth M. Kemner
John Seaman
Steven P. Simner
Daniel I. Kaplan
author_sort Peng Lin
collection DOAJ
description Uranium (U) and nickel (Ni) released 50 years ago have been immobilized in the Tims Branch wetlands located on the Savannah River Site in the United States. Sediments were collected from seven locations to identify the factors responsible for this attenuation. Ni and U contents in the solids were significantly correlated, suggesting that depositional as opposed to chemical processes contributed to their spatial distribution. Based on sequential extractions, 63 ± 16% of the U was partitioned into the organic fraction, whereas Ni was distributed between several sediment fractions. An inverse pH-organic matter (OM) correlation and positive correlations of OM with total U and organic-bound U/Ni suggest that increased OM preservation and binding to the mineral surfaces were likely responsible for Ni- and especially U-sediment retention (Tims Branch pH = 4.84 ± 0.68). EXAFS analysis indicated the predominance of U(VI) coordinated with clay minerals (~65%), together with ~35% coordinated to either OM (in areas with elevated OM levels) or iron oxides. The desorption-<i>K<sub>d</sub></i> coefficients of U (3972 ± 1370 L/kg) and Ni (30 ± 8 L/kg) indicate that dissolved Ni poses a greater long-term risk than dissolved U for migrating downstream. This study suggests that a delicate balance of geochemical properties controls whether wetlands behave as sinks or sources of contaminants.
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spelling doaj.art-65b6b8f4e845421ba49607dfe90c92cc2024-04-12T13:27:04ZengMDPI AGWater2073-44412024-03-0116796610.3390/w16070966Uranium and Nickel Partitioning in a Contaminated Riparian WetlandPeng Lin0Maxim I. Boyanov1Edward J. O’Loughlin2Wei Xing3Kenneth M. Kemner4John Seaman5Steven P. Simner6Daniel I. Kaplan7Savannah River Ecology Laboratory, University of Georgia, Aiken, SC 29803, USABiosciences Division, Argonne National Laboratory, Lemont, IL 60439, USABiosciences Division, Argonne National Laboratory, Lemont, IL 60439, USASavannah River Ecology Laboratory, University of Georgia, Aiken, SC 29803, USABiosciences Division, Argonne National Laboratory, Lemont, IL 60439, USASavannah River Ecology Laboratory, University of Georgia, Aiken, SC 29803, USASavannah River Mission Completion, Aiken, SC 29803, USASavannah River Ecology Laboratory, University of Georgia, Aiken, SC 29803, USAUranium (U) and nickel (Ni) released 50 years ago have been immobilized in the Tims Branch wetlands located on the Savannah River Site in the United States. Sediments were collected from seven locations to identify the factors responsible for this attenuation. Ni and U contents in the solids were significantly correlated, suggesting that depositional as opposed to chemical processes contributed to their spatial distribution. Based on sequential extractions, 63 ± 16% of the U was partitioned into the organic fraction, whereas Ni was distributed between several sediment fractions. An inverse pH-organic matter (OM) correlation and positive correlations of OM with total U and organic-bound U/Ni suggest that increased OM preservation and binding to the mineral surfaces were likely responsible for Ni- and especially U-sediment retention (Tims Branch pH = 4.84 ± 0.68). EXAFS analysis indicated the predominance of U(VI) coordinated with clay minerals (~65%), together with ~35% coordinated to either OM (in areas with elevated OM levels) or iron oxides. The desorption-<i>K<sub>d</sub></i> coefficients of U (3972 ± 1370 L/kg) and Ni (30 ± 8 L/kg) indicate that dissolved Ni poses a greater long-term risk than dissolved U for migrating downstream. This study suggests that a delicate balance of geochemical properties controls whether wetlands behave as sinks or sources of contaminants.https://www.mdpi.com/2073-4441/16/7/966radionuclidesmonitored natural attenuationorganic matterXANESEXAFSiron oxides
spellingShingle Peng Lin
Maxim I. Boyanov
Edward J. O’Loughlin
Wei Xing
Kenneth M. Kemner
John Seaman
Steven P. Simner
Daniel I. Kaplan
Uranium and Nickel Partitioning in a Contaminated Riparian Wetland
Water
radionuclides
monitored natural attenuation
organic matter
XANES
EXAFS
iron oxides
title Uranium and Nickel Partitioning in a Contaminated Riparian Wetland
title_full Uranium and Nickel Partitioning in a Contaminated Riparian Wetland
title_fullStr Uranium and Nickel Partitioning in a Contaminated Riparian Wetland
title_full_unstemmed Uranium and Nickel Partitioning in a Contaminated Riparian Wetland
title_short Uranium and Nickel Partitioning in a Contaminated Riparian Wetland
title_sort uranium and nickel partitioning in a contaminated riparian wetland
topic radionuclides
monitored natural attenuation
organic matter
XANES
EXAFS
iron oxides
url https://www.mdpi.com/2073-4441/16/7/966
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