Rare earth elements in some bottled waters of Serbia

Twenty-one bottled mineral and spring waters from Serbia were analyzed for 16 inorganic chemical parameters, including lanthanides and yttrium which belong to the group of so-called rare earth elements (REE). REE concentrations in the bottled water samples varied over a broad range, from 5....

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Main Authors: Todorović Maja, Papić Petar, Ćuk Marina, Stojković Jana
Format: Article
Language:English
Published: Faculty of Mining and Geology, Belgrade 2013-01-01
Series:Geološki Anali Balkanskoga Poluostrva
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/0350-0608/2013/0350-06081374071T.pdf
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spelling doaj-78d1ec121bd0434ab35f7410e471c3852020-11-25T00:47:11ZengFaculty of Mining and Geology, BelgradeGeološki Anali Balkanskoga Poluostrva0350-06082406-07472013-01-01201374718110.2298/GABP1374071T0350-06081374071TRare earth elements in some bottled waters of SerbiaTodorović Maja0Papić Petar1Ćuk Marina2Stojković Jana3Faculty of Mining and Geology, Department of Hydrogeology, BelgradeFaculty of Mining and Geology, Department of Hydrogeology, BelgradeFaculty of Mining and Geology, Department of Hydrogeology, BelgradeFaculty of Mining and Geology, Department of Hydrogeology, BelgradeTwenty-one bottled mineral and spring waters from Serbia were analyzed for 16 inorganic chemical parameters, including lanthanides and yttrium which belong to the group of so-called rare earth elements (REE). REE concentrations in the bottled water samples varied over a broad range, from 5.39 to 1585.82 ng/L. Total concentrations in the bottled water samples were calculated taking into account the classification of lanthanides into heavy (HREE) and light (LREE), with yttrium added to the HREE group. The LREE concentrations ranged from 3.62 to 1449.63 ng/L, while those of the HREE were from 0 to 136.19 ng/L. Distinct REE signatures were observed in waters that drained specific rocks. The REE patterns in groundwater from granitic and related rocks showed LREE and HREE enrichment, while groundwater with mafic rock influence exhibited slightly LREE enrichment. Several bottled water samples featured naturally-occurring carbon dioxide, whose solutional capacity contributed to the highest REE concentrations in the analyzed samples. High REE concentrations are also a result of sudden changes in oxidation-reduction conditions, which particularly affect La, Ce and Eu. Aquifers developed in granitic and related rocks (methamorphic and sedimentary rocks) constitute favorable environments for HREE in groundwater, corroborated by the occurrence of HREE in bottled water samples. The bottled water samples largely exhibited a negative cerium anomaly and nearly all the samples showed a positive europium anomaly.http://www.doiserbia.nb.rs/img/doi/0350-0608/2013/0350-06081374071T.pdfrare earth elementshydrogeochemistrybottled watersSerbia
collection DOAJ
language English
format Article
sources DOAJ
author Todorović Maja
Papić Petar
Ćuk Marina
Stojković Jana
spellingShingle Todorović Maja
Papić Petar
Ćuk Marina
Stojković Jana
Rare earth elements in some bottled waters of Serbia
Geološki Anali Balkanskoga Poluostrva
rare earth elements
hydrogeochemistry
bottled waters
Serbia
author_facet Todorović Maja
Papić Petar
Ćuk Marina
Stojković Jana
author_sort Todorović Maja
title Rare earth elements in some bottled waters of Serbia
title_short Rare earth elements in some bottled waters of Serbia
title_full Rare earth elements in some bottled waters of Serbia
title_fullStr Rare earth elements in some bottled waters of Serbia
title_full_unstemmed Rare earth elements in some bottled waters of Serbia
title_sort rare earth elements in some bottled waters of serbia
publisher Faculty of Mining and Geology, Belgrade
series Geološki Anali Balkanskoga Poluostrva
issn 0350-0608
2406-0747
publishDate 2013-01-01
description Twenty-one bottled mineral and spring waters from Serbia were analyzed for 16 inorganic chemical parameters, including lanthanides and yttrium which belong to the group of so-called rare earth elements (REE). REE concentrations in the bottled water samples varied over a broad range, from 5.39 to 1585.82 ng/L. Total concentrations in the bottled water samples were calculated taking into account the classification of lanthanides into heavy (HREE) and light (LREE), with yttrium added to the HREE group. The LREE concentrations ranged from 3.62 to 1449.63 ng/L, while those of the HREE were from 0 to 136.19 ng/L. Distinct REE signatures were observed in waters that drained specific rocks. The REE patterns in groundwater from granitic and related rocks showed LREE and HREE enrichment, while groundwater with mafic rock influence exhibited slightly LREE enrichment. Several bottled water samples featured naturally-occurring carbon dioxide, whose solutional capacity contributed to the highest REE concentrations in the analyzed samples. High REE concentrations are also a result of sudden changes in oxidation-reduction conditions, which particularly affect La, Ce and Eu. Aquifers developed in granitic and related rocks (methamorphic and sedimentary rocks) constitute favorable environments for HREE in groundwater, corroborated by the occurrence of HREE in bottled water samples. The bottled water samples largely exhibited a negative cerium anomaly and nearly all the samples showed a positive europium anomaly.
topic rare earth elements
hydrogeochemistry
bottled waters
Serbia
url http://www.doiserbia.nb.rs/img/doi/0350-0608/2013/0350-06081374071T.pdf
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AT cukmarina rareearthelementsinsomebottledwatersofserbia
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