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

机译:中国南部铀厂尾矿池水文循环中铀的赋存与分布

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摘要

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 ± 0.02 mg/kg to 2.56 × 10 ± 23 mg/kg in solid samples, and varied greatly in different locations. For tailings sand samples, the highest U concentration (2.56× 10 ± 23 mg/kg) occurred at the depth of 80 cm underground, whereas, for paddy soil samples, the highest U concentration (5.22 ± 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 ± 0.04 mg/L to 3.36 ± 0.02 mg/L with a mean value of 2.36 ± 0.36 mg/L, which was significantly lower than that of percolating waters (ranging from 4.56 ± 0.02 mg/L to 12.05 ± 0.04 mg/L, mean 7.91 ± 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.
机译:铀的开采活动导致土壤和水体的污染(即,铀厂尾矿中的渗滤液),这会造成严重的环境问题。然而,关于与整个土壤-水系统有关的U污染的研究很少。在这项研究中,总共收集了110个样品,包括96个固体样品和14个水样品,以研究U采矿尾矿池附近天然土壤-水系统中U的分布特征。结果表明,固体样品中的U浓度范围从0.09±0.02 mg / kg到2.56×10±23 mg / kg,并且在不同位置有很大差异。尾矿砂样品的最高U浓度(2.56×10±23 mg / kg)发生在地下80 cm深度,而稻田土壤样品的U浓度最高(5.22±0.04 mg / kg)表面层。计算了土壤累积指数和潜在生态危害指数,以评估土壤中U的危害。计算结果表明,一半的土壤采样点受到中度污染。对于地下水样品,U浓度范围为0.55±0.04 mg / L至3.36±0.02 mg / L,平均值为2.36±0.36 mg / L,显着低于渗滤水的浓度(范围为4.56±0.02 mg / L)。 L至12.05±0.04 mg / L,平均值7.91±0.98 mg / L)。这项研究的结果表明,土壤水系统中U浓度的分布与水文循环密切相关,U浓度随循环路径而降低。

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