Uranium content and uranium isotopic disequilibria as a tool to identify hydrogeochemical processes. (February 2021)

• Record Type: Journal Article
• Authors: Milena-Pérez, A.; Piñero-García, F.; Benavente, J.; Expósito-Suárez, V.M.; Vacas-Arquero, P.; Ferro-García, M.A.
• Is Part Of: Journal of environmental radioactivity. Volume 227(2021)
• Publication Date: 2021-02
• Subjects: Uranium natural isotopes -- 234U/238U -- Groundwater -- Hydrogeochemistry -- Betic cordillera; Radioactivity -- Periodicals; Radiation, Background -- Periodicals; Radioecology -- Periodicals; Radioactive pollution -- Periodicals; Environmental Pollutants -- Periodicals; Radioactive Pollutants -- Periodicals; Radioactivity -- Periodicals; Radioécologie -- Périodiques; Pollution radioactive -- Périodiques; Fond de rayonnement -- Périodiques; 539.752
• DOI: 10.1016/j.jenvrad.2020.106503
• Languages: English
• ISSNs: 0265-931X

Abstract

Abstract: This paper studies the uranium content and uranium isotopic disequilibria as a tool to identify hydrogeochemical processes from 52 groundwater samples in the province of Granada (Betic Cordillera, southeastern Spain). According to the geological complexity of the zone, three groups of samples have been considered. In Group 1 (thermal waters; longest residence time), the average uranium content was 2.63 ± 0.16 μg/L, and 234 U/ 238 U activity ratios (AR) were the highest of all samples, averaging 1.92 ± 0.30. In Group 2 (mainly springs from carbonate aquifers; intermediate residence time), dissolved uranium presented an average value of 1.34 ± 0.13 μg/L, while AR average value was 1.38 ± 0.25. Group 3 comes from pumping wells in a highly anthropized alluvial aquifer. In this group, where the residence time of the groundwater is the shortest of the three, average uranium content was 5.28 ± 0.26 μg/L, and average AR is the lowest (1.17 ± 0.12). In addition, the high dissolved uranium value and the low AR brought to light the contribution of fertilizers (Group 3). In the three groups, 235 U/ 238 U activity ratios were similar to the natural value of 0.046. Therefore, 235 U detected in the samples comes from natural sources. This study is completed with the determination of major ions and physicochemical parameters in the groundwater samples and the statistical analysis of the data by using the Principal Component Analysis. This calculation indicates the correlation between uranium isotopes and bicarbonate and nitrate anions. Highlights: Natural uranium isotopic ratios have been calculated and used as a prospecting tool in hydrogeochemical processes in groundwater samples. Anthropogenic contribution to the presence of uranium has been found. 234 U/ 238 U activity ratio has demonstrated to be a key factor to distinguish different geological environments. A statistical study has been performed and some chemical processes that take place in water have been remarked.