Please use this identifier to cite or link to this item: https://dspace.uzhnu.edu.ua/jspui/handle/lib/31631
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dc.contributor.authorSukharev, Sergii-
dc.contributor.authorBugyna, Larysa-
dc.contributor.authorPallah, Oleksandra-
dc.contributor.authorSukhareva, Tetiana-
dc.contributor.authorDrobnych, Volodymyr-
dc.contributor.authorYerem, Kristina-
dc.contributor.authorПаллаг, Олександра Володимирівнаuk
dc.date.accessioned2020-11-30T12:24:41Z-
dc.date.available2020-11-30T12:24:41Z-
dc.date.issued2020-
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S2405844020303807-
dc.identifier.urihttps://dspace.uzhnu.edu.ua/jspui/handle/lib/31631-
dc.description.abstractBackground For Transcarpathian region, with a pronounced landscape diversity of territories and significant areas of nature reserves, well water is an important source of drinking water. Screening of the microelement composition of drinking well water in Transcarpathia has not been carried out before. The microelement composition of such well water can be considered as the natural (baseline) indicator of quality. Methods We screened of the microelement (Cu, Zn, Fe, P, Ca, Mg, Mn, Mo, Co, As, Se, I, Br and F) composition of drinking well water in Transcarpathian region (for all 13 districts). Standard methods were used to determination the concentration of chemical elements in well water: electrothermal atomic absorption spectroscopy (Cu, Zn, Fe, Mn, Mo, Co), flame photometry (Ca, Mg), inverse voltammetry (total iodine), potentiometry (F, Br), fluorimetric (Se) and spectrophotometric methods (P, As). Results The content of chemical elements in well water varies over a wide range, in particular for Cu: 3.27–11.6 μg⋅L−1, Zn: 8.16–38.2 μg⋅L−1; Fe: 37.9–411 μg⋅L−1; P: 51.4–193 μg⋅L−1; Ca: 85–139 mg⋅L−1, Mg: 10.2–18.9 mg⋅L−1, Mn: 22.8–78.1 μg⋅L−1; Mo: 2.33–8.96 μg⋅L−1; Co: 1.72–3.38 μg⋅L−1; As: 2.9–17.4 μg⋅L−1; Se: 0.95–3.6 μg⋅L−1; I: 0.94–4.4 μg⋅L−1; Br: 712–3098 μg⋅L−1; F: 71–149 μg⋅L−1. The tendency that the content of microelements (Cu, Zn, Mn, Mo, Co, As, Se, I, Br, and F) in well waters of different landscape zones was evaluated through Spearman's coefficients. The content of trace elements in the waters of different landscape zones increases in the series: lowland landscape > foothill landscape > mountainous landscape (Spearman's coefficients: Cu – 0.62, Zn – 0.85, Mn – 0.69, Mo – 0.83, Co – 0.79, P – 0.74, As – 0.72, Se – 0.75, I – 0.80, Br – 0.91, F – 0.73). Conclusion It is shown that the chemical composition of well water can be considered as the natural (baseline) indicator of quality of groundwater in Transcarpathia, taking into account topographic and geochemical features of the territories. Among the main problems of drinking well water in Transcarpathia are the relatively high content of Fe (typical for different landscape zones), as well as the low content of Se, I and F. The correlation of inter-elements content of chemical elements in drinking well waters of Transcarpathia has been revealed. The most pronounced correlations are observed for such pairs of microelements: Co–Mo (r > 0.95), I–Br (r > 0.92), Zn–Br (r > 0.89), Cu–Co (r > 0.84), Se–Co (r > 0.84), Mo–P (r > 0.84), Mo–I (r > 0.82) and Zn–Mo (r > 0.80).uk
dc.description.sponsorshipThis work was supported by the Ministry of Education and Science of Ukraine, registration number 0117U000379.uk
dc.language.isoenuk
dc.publisherHeliyonuk
dc.relation.ispartofseries6;3-
dc.subjectWater qualityuk
dc.subjectWell watersuk
dc.subjectMicroelements compositionuk
dc.subjectGeochemical featuresuk
dc.subjectPearson's and Spearman's correlation coefficientsuk
dc.subjectLandscape diversityuk
dc.subjectAnalytical chemistryuk
dc.subjectEnvironmental analysisuk
dc.subjectEnvironmental chemistryuk
dc.subjectEnvironmental geochemistryuk
dc.subjectGeochemistryuk
dc.subjectEnvironmental scienceuk
dc.titleScreening of the microelements composition of drinking well water of Transcarpathian region, Ukraineuk
dc.typeTextuk
dc.pubTypeСтаттяuk
Appears in Collections:Наукові публікації НДНЦ молекулярної мікробіології та імунології слизових оболонок

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