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Uranium isotopes as a tracer of groundwater transport studies

The activity concentrations of (234)U and (238)U in thermal groundwater, deep well water and river water samples from Central Poland were determined. Concentration of (234)U and (238)U in the examined waters varied from <0.013 (LLD) to 16.8 mBq/dm(3) and from <0.013 (LLD) to 45.5 mBq/dm(3) res...

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Detalles Bibliográficos
Autores principales: Grabowski, P., Bem, H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Netherlands 2011
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4513905/
https://www.ncbi.nlm.nih.gov/pubmed/26224922
http://dx.doi.org/10.1007/s10967-011-1558-0
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author Grabowski, P.
Bem, H.
author_facet Grabowski, P.
Bem, H.
author_sort Grabowski, P.
collection PubMed
description The activity concentrations of (234)U and (238)U in thermal groundwater, deep well water and river water samples from Central Poland were determined. Concentration of (234)U and (238)U in the examined waters varied from <0.013 (LLD) to 16.8 mBq/dm(3) and from <0.013 (LLD) to 45.5 mBq/dm(3) respectively. The highest uranium activity concentrations were measured in the thermal groundwater from Mszczonow and Cieplice, while the lowest were observed in thermal ground water from Uniejow and Poddebice. In thermal groundwater from Skierniewice, uranium activity concentrations were below lower limit of detection (0.013 mBq/dm(3)). The (234)U/(238)U activity ratio varied from 0.37 (Cieplice) to 1.30 (Poddebice well water).
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spelling pubmed-45139052015-07-27 Uranium isotopes as a tracer of groundwater transport studies Grabowski, P. Bem, H. J Radioanal Nucl Chem Article The activity concentrations of (234)U and (238)U in thermal groundwater, deep well water and river water samples from Central Poland were determined. Concentration of (234)U and (238)U in the examined waters varied from <0.013 (LLD) to 16.8 mBq/dm(3) and from <0.013 (LLD) to 45.5 mBq/dm(3) respectively. The highest uranium activity concentrations were measured in the thermal groundwater from Mszczonow and Cieplice, while the lowest were observed in thermal ground water from Uniejow and Poddebice. In thermal groundwater from Skierniewice, uranium activity concentrations were below lower limit of detection (0.013 mBq/dm(3)). The (234)U/(238)U activity ratio varied from 0.37 (Cieplice) to 1.30 (Poddebice well water). Springer Netherlands 2011-12-17 2012 /pmc/articles/PMC4513905/ /pubmed/26224922 http://dx.doi.org/10.1007/s10967-011-1558-0 Text en © The Author(s) 2011 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, P.
Bem, H.
Uranium isotopes as a tracer of groundwater transport studies
title Uranium isotopes as a tracer of groundwater transport studies
title_full Uranium isotopes as a tracer of groundwater transport studies
title_fullStr Uranium isotopes as a tracer of groundwater transport studies
title_full_unstemmed Uranium isotopes as a tracer of groundwater transport studies
title_short Uranium isotopes as a tracer of groundwater transport studies
title_sort uranium isotopes as a tracer of groundwater transport studies
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4513905/
https://www.ncbi.nlm.nih.gov/pubmed/26224922
http://dx.doi.org/10.1007/s10967-011-1558-0
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