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Determination of (210)Po and uranium in high salinity water samples

A method for the determination of uranium and (210)Po in high salinity water samples has been elaborated. Both radionuclides are preconcentrated from 0.5 dm(3) saline media by co-precipitation with hydrated manganese dioxide, followed by dissolution of the precipitate in 200 mL of 1 M HCl. Uranium i...

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Detalles Bibliográficos
Autores principales: Grabowski, Paweł, Bem, Henryk
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Netherlands 2010
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4514583/
https://www.ncbi.nlm.nih.gov/pubmed/26224904
http://dx.doi.org/10.1007/s10967-010-0720-4
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author Grabowski, Paweł
Bem, Henryk
author_facet Grabowski, Paweł
Bem, Henryk
author_sort Grabowski, Paweł
collection PubMed
description A method for the determination of uranium and (210)Po in high salinity water samples has been elaborated. Both radionuclides are preconcentrated from 0.5 dm(3) saline media by co-precipitation with hydrated manganese dioxide, followed by dissolution of the precipitate in 200 mL of 1 M HCl. Uranium isotopes (235)U and (238)U can be directly determined by ICP MS method with a detection limit of 0.01 ppb for (238)U. Prior to a selective determination of (210)Po, the majority of other naturally occurring α-emitting radionuclides (uranium, thorium and protactinium) can be stripped from this solution by their extraction with a 50% solution of HDEHP in toluene. Finally, (210)Po is simply separated by direct transfer to an extractive scintillator containing 5% of trioctylphosphine oxide in Ultima Gold F cocktail and determined by an α/β separation liquid scintillation technique with detection limit below 0.1 mBq/dm(3).
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spelling pubmed-45145832015-07-27 Determination of (210)Po and uranium in high salinity water samples Grabowski, Paweł Bem, Henryk J Radioanal Nucl Chem Article A method for the determination of uranium and (210)Po in high salinity water samples has been elaborated. Both radionuclides are preconcentrated from 0.5 dm(3) saline media by co-precipitation with hydrated manganese dioxide, followed by dissolution of the precipitate in 200 mL of 1 M HCl. Uranium isotopes (235)U and (238)U can be directly determined by ICP MS method with a detection limit of 0.01 ppb for (238)U. Prior to a selective determination of (210)Po, the majority of other naturally occurring α-emitting radionuclides (uranium, thorium and protactinium) can be stripped from this solution by their extraction with a 50% solution of HDEHP in toluene. Finally, (210)Po is simply separated by direct transfer to an extractive scintillator containing 5% of trioctylphosphine oxide in Ultima Gold F cocktail and determined by an α/β separation liquid scintillation technique with detection limit below 0.1 mBq/dm(3). Springer Netherlands 2010-08-19 2010 /pmc/articles/PMC4514583/ /pubmed/26224904 http://dx.doi.org/10.1007/s10967-010-0720-4 Text en © The Author(s) 2010 https://creativecommons.org/licenses/by-nc/4.0/ This article is distributed under the terms of the Creative Commons Attribution Noncommercial License which permits any noncommercial use, distribution, and reproduction in any medium, provided the original author(s) and source are credited.
spellingShingle Article
Grabowski, Paweł
Bem, Henryk
Determination of (210)Po and uranium in high salinity water samples
title Determination of (210)Po and uranium in high salinity water samples
title_full Determination of (210)Po and uranium in high salinity water samples
title_fullStr Determination of (210)Po and uranium in high salinity water samples
title_full_unstemmed Determination of (210)Po and uranium in high salinity water samples
title_short Determination of (210)Po and uranium in high salinity water samples
title_sort determination of (210)po and uranium in high salinity water samples
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4514583/
https://www.ncbi.nlm.nih.gov/pubmed/26224904
http://dx.doi.org/10.1007/s10967-010-0720-4
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