Macro and microelements in bottled and tap waters of Serbia

• Published in: Hemijska industrija 2012, Vol.66 (1), p.107-122
• Main Authors: Petrovic, Tanja, Zlokolica-Mandic, Milena, Veljkovic, Nebojsa, Papic, Petar, Poznanovic, Maja, Stojkovic, Jana, Magazinovic, Sava
• Format: Article
• Language: English
• Subjects: Anions; Aquifers; bottled water; Cations; Dolomite; Drinking water; Geochemistry; Groundwater; Karst; Limestone; Lithogeochemistry; Lithology; main components; Metamorphic rocks; Mineral waters; Natural resources; regulations; tap water; trace elements; Water circulation; water classification
• ISSN: 0367-598X; 2217-7426
• DOI: 10.2298/HEMIND110729062P

Comparative analysis between bottled and tap waters as well as its comparison with current Serbian regulations, European Union Directives and World Health Organization standard are shown in this paper. Thirteen bottled waters and fourteen tap waters from the territory of Serbia were analyzed in the Federal Institute for Geosciences and Natural Resources (BGR) laboratory in Berlin, for the purpose of the ?Geochemistry of European Bottled Water? project conducted by EuroGeo Survey Geochemistry (EGS). Macrocomponents (main cations and anions) of ground waters usually reflect on lithogeochemistry of the aquifer, while microcomponents indicate the circulation of ground water through the different lithological environment. Analyzed bottled waters could be classified as those with low mineral content (M500 mg/L) with prevailing HCO3 anion and Na cation. Waters with low mineral content were mainly from limestone and dolomite, while mineral waters mainly originated from magmatic and metamorphic rocks. Higher content of Cs, Li, Ge, Rb and F in bottled waters indicates the importance of the magmatic intrusions influence on their chemical composition. In some waters higher content of B, I, NH4, as well as of Tl and W has been observed which can be attributed to water?s circulation through different lithological complexes. Tap water was mostly obtained from groundwater (from Neogen and alluvial aquifers and karst springs) with rest being those of rivers and surface accumulations. Tap waters from Central Serbia were with low mineral content, with prevailing HCO3 anion and Ca and Mg cations, while waters from Vojvodina, the northern province of Serbia, were with higher mineralization, HCO3-Na. Chemical analyses of the sampled tap waters showed good quality, with exception of waters from the cities of Senta and Zrenjanin in Vojvodina. High values of B (1170 and 895 g/L), As (20.9 and 71.9 g/l), Na (208 and 275 mg/L), as well as EC (715 and 928 S/cm) have been registered in these waters. nema