College of Horticulture and Landscape, Yunnan Agriculture University, Kunming 650201, China.
BIOSE Department, Soil-Water-Plant Exchanges, University of Liège, Gembloux Agro-Bio Tech, 2 Passage des Déportés, 5030 Gembloux, Belgium.
Int J Environ Res Public Health. 2019 Nov 25;16(23):4686. doi: 10.3390/ijerph16234686.
The largest lead/zinc mine in China is located in Lanping mining valley. The real impact of mining activity on the Lanping mining valley has not been studied to date. This study aims to characterize the geochemical baseline values and risk assessment of heavy metal contamination in soils of a study area located in the Lanping mining valley including upstream, mining and downstream areas. The results showed that the mean soil pH value was 6.8, and organic matter was 34.3%, in surface layer of the mining area. The mean soil pH value in the upstream and downstream areas was less than 5.5. The concentrations of Pb and Zn in the mining area were 56 and 47 times above the world average, the concentrations of Pb, Zn and Cd in the upstream area were six, seven, and six times above the world average, and the concentrations of Pb, Zn and Cd in the downstream area were eight, eight, and 18 times above the world average, respectively. The proposed geochemical baseline values of Pb, Cu, Zn and Cd were 169.93, 31.81, 569.06 and 4.13 mg·kg, respectively. The pseudo total and ethylene diamine tetraacetic acid (EDTA)-extractable concentrations of Pb, Zn and Cd showed similar tendency as follows: mining area > downstream area > upstream area. The contamination degree with the geoaccumulation index (I) and the improved Nemerow index (I) in the upstream and mining areas was non-contamination or slight contamination with low or moderate risk with the individual ecological risk index (E) and the comprehensive potential ecological risk index (RI), although moderate or heavy contamination with pollution factor (Pi) and the Nemerow index (I). The contamination degree with I and I in the downstream area was non-contamination or extreme contamination with low or extreme risk with E and RI. The results suggest that the I should be recommended to assess the soil contamination of heavy metals and the geochemical baseline values would be important for the environmental management and remediation of soils contaminated by heavy metals.
中国最大的铅/锌矿位于兰坪矿区。迄今为止,尚未对采矿活动对兰坪矿区的实际影响进行研究。本研究旨在对位于兰坪矿区(包括上游、矿区和下游地区)的研究区域土壤的重金属污染的地球化学基线值和风险评估进行特征描述。结果表明,矿区表层土壤的平均 pH 值为 6.8,有机质含量为 34.3%。上游和下游地区的土壤 pH 值均小于 5.5。矿区 Pb 和 Zn 的浓度分别是世界平均值的 56 倍和 47 倍,上游地区 Pb、Zn 和 Cd 的浓度分别是世界平均值的 6 倍、7 倍和 6 倍,下游地区 Pb、Zn 和 Cd 的浓度分别是世界平均值的 8 倍、8 倍和 18 倍。提出的 Pb、Cu、Zn 和 Cd 的地球化学基线值分别为 169.93、31.81、569.06 和 4.13mg·kg。Pb、Zn 和 Cd 的拟总量和乙二胺四乙酸(EDTA)可提取浓度表现出相似的趋势,如下:矿区>下游地区>上游地区。基于地质累积指数(I)和改进的内梅罗指数(I),上游和矿区的污染程度为无污染或轻度污染,风险较低或中等,而基于个体生态风险指数(E)和综合潜在生态风险指数(RI),污染程度为中度或重度污染,污染因子(Pi)和内梅罗指数(I)较高。下游地区的污染程度为无污染或极度污染,E 和 RI 的风险较低或极高。结果表明,I 可用于评估重金属污染土壤,而地球化学基线值对于重金属污染土壤的环境管理和修复非常重要。