Department of New Energy and Mining Engineering, Sangji University, Wonju, Gangwon-do, 26339, South Korea.
Institute of Mine Reclamation Technology, Korea Mine Reclamation Corporation (MIRECO), Wonju, Gangwon-do, 26464, South Korea.
Environ Geochem Health. 2021 Oct;43(10):4061-4074. doi: 10.1007/s10653-021-00820-6. Epub 2021 Mar 27.
Paddy fields near metalliferous mining area are sometimes contaminated by tailings or mine water. In the contaminated paddy fields around the abandoned Seoseong mine, South Korea, groundwater, surface water, and soil samples were assessed to infer sources (tailings and/or mine water) of soil contamination. Major contaminants in the soil included As and Pb which were not detected in the adit water. Moreover, δS values of groundwater at contaminated downstream paddy fields were higher than those of ground and surface water in the mining area, which indicated water-derived contamination is not evident. The Zn/Cd ratios of soil were assessed to verify the source (tailings) of soil contamination. Plots of the Zn/Cd ratio against Zn and As contents showed that soil samples contaminated from tailings had Zn/Cd ratios (108-247) which were similar with the Zn/Cd range of the tailings. In contrast, the ratios of the soil samples were different from the Zn/Cd range of contaminated water samples. The Zn/Cd ratios were determined using 0.1 M HCl-extractable Cd, and the fraction of 0.1 M HCl-extractable Cd in aqua regia-digestible Cd increased with increasing aqua regia-digestible Cd content. These observations suggest that Zn/Cd ratios in contaminated soil are primarily controlled by 0.1 M HCl-extractable Cd, possibly due to the greater exchangeability of 0.1 M HCl-extractable Cd than that of total Cd. This suggests that Zn/Cd ratios determined using 0.1 M HCl-extractable Cd can be especially sensitive and useful for determining sources of soil contamination in mining areas such as tailings or contaminated water.
在富含金属矿区附近的稻田有时会受到尾矿或矿井水的污染。在韩国废弃的Seoseong 矿区周围受污染的稻田中,评估了地下水、地表水和土壤样本,以推断土壤污染的来源(尾矿和/或矿井水)。土壤中的主要污染物包括砷和铅,而在入口水中未检测到这些物质。此外,受污染的下游稻田地下水的 δS 值高于矿区的地下水和地表水的 δS 值,这表明水源性污染不明显。还评估了土壤的 Zn/Cd 比值,以验证土壤污染的来源(尾矿)。土壤 Zn/Cd 比值与 Zn 和 As 含量的关系图表明,受尾矿污染的土壤样本的 Zn/Cd 比值(108-247)与尾矿的 Zn/Cd 范围相似。相比之下,土壤样本的比值与受污染的水样的 Zn/Cd 范围不同。使用 0.1 M HCl 可提取 Cd 确定 Zn/Cd 比值,而王水可消化 Cd 中 0.1 M HCl 可提取 Cd 的比例随王水可消化 Cd 含量的增加而增加。这些观察结果表明,受污染土壤中的 Zn/Cd 比值主要受 0.1 M HCl 可提取 Cd 控制,可能是因为 0.1 M HCl 可提取 Cd 的交换性大于总 Cd。这表明,使用 0.1 M HCl 可提取 Cd 确定的 Zn/Cd 比值可特别灵敏且有助于确定矿区(如尾矿或受污染的水)土壤污染的来源。