Abstract
Uranium is a radioactive element normally present in hexavalent form as U(VI) in solution and elevated levels in drinking water cause health hazards. Representative groundwater samples were collected from different litho-units in this region and were analyzed for total U and major and minor ions. Results indicate that the highest U concentration (113 µg l−1) was found in granitic terrains of this region and about 10 % of the samples exceed the permissible limit for drinking water. Among different species of U in aqueous media, carbonate complexes [UO2(CO3) 2−2 ] are found to be dominant. Groundwater with higher U has higher pCO2 values, indicating weathering by bicarbonate ions resulting in preferential mobilization of U in groundwater. The major minerals uraninite and coffinite were found to be supersaturated and are likely to control the distribution of U in the study area. Nature of U in groundwater, the effects of lithology on hydrochemistry and factors controlling its distribution in hard rock aquifers of Madurai district are highlighted in this paper.
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The authors express their sincere thanks to University Grants Commission (UGC), India, for providing the necessary financial support to this research project with wide reference to UGC Letter No. F: 39-143/2010 (SR) dated December 27, 2010.
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Thivya, C., Chidambaram, S., Keesari, T. et al. Lithological and hydrochemical controls on distribution and speciation of uranium in groundwaters of hard-rock granitic aquifers of Madurai District, Tamil Nadu (India). Environ Geochem Health 38, 497–509 (2016). https://doi.org/10.1007/s10653-015-9735-7
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DOI: https://doi.org/10.1007/s10653-015-9735-7