Environmental Studies Center (CEA) and Basin Studies Laboratory, São Paulo State University, UNESP, Rio Claro, SP 13506-900, Brazil.
Environmental Studies Center (CEA), São Paulo State University, UNESP, Rio Claro, SP 13506-900, Brazil.
Sci Total Environ. 2021 Feb 25;757:143917. doi: 10.1016/j.scitotenv.2020.143917. Epub 2020 Dec 3.
On January 25, 2019, a tailings dam at the Córrego do Feijão iron ore mine (Brumadinho, Minas Gerais, southern Brazil) ruptured and released ~12 million m of mine tailings into the Paraopeba River, which is an important source of drinking water to a populous region. While water potability due to a strong increase in turbidity has been well documented, possible effects of metal contamination are yet to be addressed. We investigated the speciation of metals in the river water and desorption of metals from sediments as a means of supporting risk assessment, using the diffusive gradient in thin films (DGT) technique, desorption experiments and chemical speciation calculations. The results of the in-situ DGT monitoring revealed that the labile concentrations of metals were low in relation to the respective total and dissolved concentrations. Chemical speciation calculations showed that the heavy metals were not stable in the Paraopeba River. The desorption experiments suggested that sediments may release a limited amount of As and Cu, but large amounts of Mn into the river water. Higher concentrations of Fe and Mn indicated a possible association with the impact of mine tailings. In general, the total metal concentrations during the rainy season were higher than those during the dry season, whereas the reverse was generally the case for labile forms. This pattern reveals that metal speciation is intrinsically dependent on the seasonal variation of the hydrological conditions.
2019 年 1 月 25 日,巴西南部米纳斯吉拉斯州布鲁马迪尼奥的铁矿区 Feijão 尾矿坝发生溃坝事件,约 1200 万立方米的尾矿流入帕拉奥佩巴河,该河是人口稠密地区的重要饮用水源。尽管由于浊度急剧增加导致水的饮用性已得到充分记录,但金属污染的可能影响仍有待解决。我们使用扩散梯度薄膜(DGT)技术、解吸实验和化学形态计算,研究了河水中金属的形态和金属从沉积物中的解吸,以支持风险评估。原位 DGT 监测的结果表明,相对于总浓度和溶解浓度,金属的生物可利用浓度较低。化学形态计算表明,重金属在帕拉奥佩巴河中不稳定。解吸实验表明,沉积物可能会向河水中释放有限量的砷和铜,但会释放大量的锰。Fe 和 Mn 的浓度较高表明可能与尾矿的影响有关。一般来说,雨季的总金属浓度高于旱季,而生物可利用形态则相反。这种模式表明金属形态在本质上取决于水文条件的季节性变化。