Occurrence and Distribution of Uranium in a Hydrological Cycle around a Uranium Mill Tailings Pond, Southern China

Uranium (U) mining activities, which lead to contamination in soils and waters (i.e., leachate from U mill tailings), cause serious environmental problems. However, limited research works have been conducted on U pollution associated with a whole soil-water system. In this study, a total of 110 samp...

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Bibliographic Details
Main Authors: Wenjie Ma, Bai Gao, Yadan Guo, Zhanxue Sun, Yanhong Zhang, Gongxin Chen, Xiaojie Zhu, Chunyan Zhang
Format: Article
Language:English
Published: MDPI AG 2020-01-01
Series:International Journal of Environmental Research and Public Health
Subjects:
Online Access:https://www.mdpi.com/1660-4601/17/3/773
Description
Summary:Uranium (U) mining activities, which lead to contamination in soils and waters (i.e., leachate from U mill tailings), cause serious environmental problems. However, limited research works have been conducted on U pollution associated with a whole soil-water system. In this study, a total of 110 samples including 96 solid and 14 water samples were collected to investigate the characteristics of U distribution in a natural soil-water system near a U mining tailings pond. Results showed that U concentrations ranged from 0.09 &#177; 0.02 mg/kg to 2.56 &#215; 10<sup>4</sup>&#177; 23 mg/kg in solid samples, and varied greatly in different locations. For tailings sand samples, the highest U concentration (2.56&#215; 10<sup>4</sup> &#177; 23 mg/kg) occurred at the depth of 80 cm underground, whereas, for paddy soil samples, the highest U concentration (5.22 &#177; 0.04 mg/kg) was found at surface layers. Geo-accumulation index and potential ecological hazard index were calculated to assess the hazard of U in the soils. The calculation results showed that half of the soil sampling sites were moderately polluted. For groundwater samples, U concentrations ranged from 0.55 &#177; 0.04 mg/L to 3.36 &#177; 0.02 mg/L with a mean value of 2.36 &#177; 0.36 mg/L, which was significantly lower than that of percolating waters (ranging from 4.56 &#177; 0.02 mg/L to 12.05 &#177; 0.04 mg/L, mean 7.91 &#177; 0.98 mg/L). The results of this study suggest that the distribution of U concentrations in a soil-water system was closely associated with hydrological cycles and U concentrations decreased with circulation path.
ISSN:1660-4601