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Behavior of radium, thorium and uranium in groundwater near the Buena Lagoon in the Coastal Zone of the State of Rio de Janeiro, Brazil

机译:巴西里约热内卢州沿海地区布埃纳泻湖附近地下水中镭,th和铀的行为

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摘要

Groundwater found near the head of the Buena Lagoon in the State of Rio de Janeiro, Brazil, has high salinity and low pH values. There is a strong correlation between concentrations of radium and light rare earth elements (LREEs) that suggests the leaching of monazite as a common source. Radium is present predominantly as ~(228)Ra. The factors responsible for high radium mobility in groundwater seem to be high levels of salinity resulting in the competition for adsorption sites, and low pH values resulting in the limited adsorption of Ra~(2+) on the positively-charged surface of adsorbents. The behavior of uranium and thorium is also influenced by their speciation and low pH conditions. Uranium is present as a positively charged uranyl ion UO_2~(2+) in low pH samples and is very mobile. Similarly, the presence of positively charged Th~(4+) and thorium complexes with sulfate result in relatively high thorium concentrations at a low pH range. On the other hand, the mobility of phosphate released by dissolving monazite is probably reduced due to its adsorption and precipitation close to its source.
机译:在巴西里约热内卢州布埃纳泻湖头部附近发现的地下水盐度高,pH值低。镭和轻稀土元素(LREEs)的浓度之间存在很强的相关性,这表明独居石是一种常见的来源。镭主要以〜(228)Ra的形式存在。导致地下水中镭迁移率高的因素似乎是盐度高,导致竞争吸附位点; pH值低,导致Ra〜(2+)在带正电荷的吸附剂表面上的吸附受到限制。铀和th的行为还受到其形态和低pH条件的影响。铀在低pH值样品中以带正电荷的铀酰离子UO_2〜(2+)的形式存在,并且具有很高的移动性。类似地,带正电的Th〜(4+)和th与硫酸盐的配合物的存在会导致在低pH范围内th浓度相对较高。另一方面,溶解独居石释放的磷酸盐的迁移率可能由于其来源附近的吸附和沉淀而降低。

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