Sukharev Sergii, Bugyna Larysa, Pallah Oleksandra, Sukhareva Tetiana, Drobnych Volodymyr, Yerem Kristina
Department of Ecology and Environment Protection, Uzhhorod National University, Uzhhorod, Ukraine.
Department of Microbiology, Virology and Epidemiology with a Course of Infectious Diseases, Uzhhorod National University, Uzhhorod, Ukraine.
Heliyon. 2020 Mar 6;6(3):e03535. doi: 10.1016/j.heliyon.2020.e03535. eCollection 2020 Mar.
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.
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).
The content of chemical elements in well water varies over a wide range, in particular for Cu: 3.27-11.6 μg⋅L, Zn: 8.16-38.2 μg⋅L; Fe: 37.9-411 μg⋅L; P: 51.4-193 μg⋅L; Ca: 85-139 mg⋅L, Mg: 10.2-18.9 mg⋅L, Mn: 22.8-78.1 μg⋅L; Mo: 2.33-8.96 μg⋅L; Co: 1.72-3.38 μg⋅L; As: 2.9-17.4 μg⋅L; Se: 0.95-3.6 μg⋅L; I: 0.94-4.4 μg⋅L; Br: 712-3098 μg⋅L; F: 71-149 μg⋅L. 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).
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).
对于外喀尔巴阡地区而言,其地域景观多样性显著,自然保护区面积广大,井水是重要的饮用水源。此前尚未对外喀尔巴阡地区饮用井水的微量元素组成进行筛查。这种井水的微量元素组成可被视为水质的自然(基线)指标。
我们对外喀尔巴阡地区(涵盖所有13个区)饮用井水的微量元素(铜、锌、铁、磷、钙、镁、锰、钼、钴、砷、硒、碘、溴和氟)组成进行了筛查。采用标准方法测定井水中化学元素的浓度:电热原子吸收光谱法(测定铜、锌、铁、锰、钼、钴)、火焰光度法(测定钙、镁)、反向伏安法(测定总碘)、电位滴定法(测定氟、溴)、荧光分析法(测定硒)以及分光光度法(测定磷、砷)。
井水中化学元素的含量变化范围广泛,尤其是铜:3.27 - 11.6μg·L,锌:8.16 - 38.2μg·L;铁:37.9 - 411μg·L;磷:51.4 - 193μg·L;钙:85 - 139mg·L,镁:10.2 - 18.9mg·L,锰:22.8 - 78.1μg·L;钼:2.33 - 8.96μg·L;钴:1.72 - 3.38μg·L;砷:2.9 - 17.4μg·L;硒:0.95 - 3.6μg·L;碘:0.94 - 4.4μg·L;溴:712 - 3098μg·L;氟:71 - 149μg·L。通过斯皮尔曼系数评估了不同景观区域井水中微量元素(铜、锌、锰、钼、钴、砷、硒、碘、溴和氟)含量的趋势。不同景观区域水中微量元素的含量按以下顺序增加:低地景观>山麓景观>山地景观(斯皮尔曼系数:铜 - 0.62,锌 - 0.85,锰 - 0.69,钼 - 0.83,钴 - 0.79,磷 - 0.74,砷 - 0.72,硒 - 0.75,碘 - 0.80,溴 - 0.91,氟 - 0.73)。
结果表明,考虑到该地区的地形和地球化学特征,井水的化学成分可被视为外喀尔巴阡地区地下水水质的自然(基线)指标。外喀尔巴阡地区饮用井水的主要问题包括铁含量相对较高(在不同景观区域均较为典型),以及硒、碘和氟含量较低。揭示了外喀尔巴阡地区饮用井水中化学元素间含量的相关性。观察到的微量元素对之间的相关性最为显著:钴 - 钼(r>0.95),碘 - 溴(r>0.92),锌 - 溴(r>0.89),铜 - 钴(r>0.84),硒 - 钴(r>0.84),钼 - 磷(r>0.84),钼 - 碘(r>0.82)以及锌 - 钼(r>0.80)。