Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes
Multi-elemental (Ca, Mg, Na, K, Al, As, Ba, Cd, Co, Cr, Cu, Fe, Li, Mn, Mo, Ni, P, Pb, Sb, Se, Tl, V, and Zn) and stable isotope (i.e., δ2H, δ18O, and δ13CDIC) analyses were performed on 13 (8 Slovenian and 5 imported) bottled mineral and spring waters from the Slovenian market. In addition, 87Sr/86...
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ftmdpi:oai:mdpi.com:/2073-4441/12/9/2454/ 2023-08-20T04:05:53+02:00 Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes Tea Zuliani Tjaša Kanduč Rok Novak Polona Vreča agris 2020-08-31 application/pdf https://doi.org/10.3390/w12092454 EN eng Multidisciplinary Digital Publishing Institute Water and One Health https://dx.doi.org/10.3390/w12092454 https://creativecommons.org/licenses/by/4.0/ Water; Volume 12; Issue 9; Pages: 2454 bottled waters multielemental analysis 87 Sr/ 86 Sr δ 2 H δ 18 O δ 13 C DIC water quality Slovenian market Text 2020 ftmdpi https://doi.org/10.3390/w12092454 2023-08-01T00:01:05Z Multi-elemental (Ca, Mg, Na, K, Al, As, Ba, Cd, Co, Cr, Cu, Fe, Li, Mn, Mo, Ni, P, Pb, Sb, Se, Tl, V, and Zn) and stable isotope (i.e., δ2H, δ18O, and δ13CDIC) analyses were performed on 13 (8 Slovenian and 5 imported) bottled mineral and spring waters from the Slovenian market. In addition, 87Sr/86Sr isotope ratios were determined for the first time. In all analyzed bottled waters, the majority of elements were present although in low concentrations, and according to EU legislation, all were suitable for human consumption. Also, concentrations of major elements (Ca, Mg, Na, and K) were in general agreement with the values reported on the bottle labels, and any differences were the consequence of the natural variability of the water source used for bottling. The exception was one spring water, for which the source location changed, which was confirmed by the δ2H, δ18O, and δ13CDIC data. Two mineral waters had distinctive elemental compositions due to the particular geology of their recharge areas. The δ13CDIC was also investigated to decipher the carbonate contribution in the bottled waters. The results suggest that dissolution of carbonates and non-equilibrium carbonate dissolution by carbonic acid produced from soil zone CO2 are the predominant geochemical processes influencing the δ13CDIC values of bottled water. Text Carbonic acid MDPI Open Access Publishing Water 12 9 2454 |
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MDPI Open Access Publishing |
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English |
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bottled waters multielemental analysis 87 Sr/ 86 Sr δ 2 H δ 18 O δ 13 C DIC water quality Slovenian market |
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bottled waters multielemental analysis 87 Sr/ 86 Sr δ 2 H δ 18 O δ 13 C DIC water quality Slovenian market Tea Zuliani Tjaša Kanduč Rok Novak Polona Vreča Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes |
topic_facet |
bottled waters multielemental analysis 87 Sr/ 86 Sr δ 2 H δ 18 O δ 13 C DIC water quality Slovenian market |
description |
Multi-elemental (Ca, Mg, Na, K, Al, As, Ba, Cd, Co, Cr, Cu, Fe, Li, Mn, Mo, Ni, P, Pb, Sb, Se, Tl, V, and Zn) and stable isotope (i.e., δ2H, δ18O, and δ13CDIC) analyses were performed on 13 (8 Slovenian and 5 imported) bottled mineral and spring waters from the Slovenian market. In addition, 87Sr/86Sr isotope ratios were determined for the first time. In all analyzed bottled waters, the majority of elements were present although in low concentrations, and according to EU legislation, all were suitable for human consumption. Also, concentrations of major elements (Ca, Mg, Na, and K) were in general agreement with the values reported on the bottle labels, and any differences were the consequence of the natural variability of the water source used for bottling. The exception was one spring water, for which the source location changed, which was confirmed by the δ2H, δ18O, and δ13CDIC data. Two mineral waters had distinctive elemental compositions due to the particular geology of their recharge areas. The δ13CDIC was also investigated to decipher the carbonate contribution in the bottled waters. The results suggest that dissolution of carbonates and non-equilibrium carbonate dissolution by carbonic acid produced from soil zone CO2 are the predominant geochemical processes influencing the δ13CDIC values of bottled water. |
format |
Text |
author |
Tea Zuliani Tjaša Kanduč Rok Novak Polona Vreča |
author_facet |
Tea Zuliani Tjaša Kanduč Rok Novak Polona Vreča |
author_sort |
Tea Zuliani |
title |
Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes |
title_short |
Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes |
title_full |
Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes |
title_fullStr |
Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes |
title_full_unstemmed |
Characterization of Bottled Waters by Multielemental Analysis, Stable and Radiogenic Isotopes |
title_sort |
characterization of bottled waters by multielemental analysis, stable and radiogenic isotopes |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2020 |
url |
https://doi.org/10.3390/w12092454 |
op_coverage |
agris |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_source |
Water; Volume 12; Issue 9; Pages: 2454 |
op_relation |
Water and One Health https://dx.doi.org/10.3390/w12092454 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/w12092454 |
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Water |
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12 |
container_issue |
9 |
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2454 |
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1774716634936639488 |