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中国山东省焦家金矿周边土壤中微量元素的地球化学形态及风险评估

Geochemical fractions and risk assessment of trace elements in soils around Jiaojia gold mine in Shandong Province, China.

作者信息

Cao Feifei, Kong Linghao, Yang Liyuan, Zhang Wei

机构信息

School of Resources and Environment, University of Jinan, Jinan, 250022, China.

出版信息

Environ Sci Pollut Res Int. 2015 Sep;22(17):13496-505. doi: 10.1007/s11356-015-4618-0. Epub 2015 May 6.

Abstract

Soils located adjacent to the Jiaojia gold mine were sampled and analyzed to determine the degree of which they were contaminated by trace elements (Hg, As, Cd, Pb, Cu, and Zn) in Shandong Province, China. All 18 samples exhibited mean Hg, As, Cd, and Pb concentrations in excess of local background values, while the mean concentrations of Cu and Zn were below the background values. In addition, the concentrations of trace elements in gold smelter (GS) soils were higher than in the gold mine (GM) soils. The result from a modified Tessier sequential extraction procedure was that with the exception of Cu in soils near the smelter, the trace elements were predominantly associated with the residual fraction. After residual fraction, most Hg was mainly humic acid and strong organic fraction, while most As was the humic acid. Cd was associated with the water soluble, ion exchange, and carbonate fractions compared with the other trace elements. Furthermore, Cu, Pb, and Zn were more concentrated in the humic acid and Fe/Mn oxide fraction. The fractions of trace elements were affected by soil pH and Ec (Electrical conductivity). The humic acid fraction of Hg as well as the ion exchange fraction of Cd and Zn displayed negative correlations with soil pH. The strong organic fraction of Hg, the Fe/Mn oxide fraction of Cd, and the carbonate fraction of Zn were positively related to the soil Ec. The strong organic fraction and ion exchange fraction of Zn were negatively related to soil Ec. However, the ion exchange and carbonate fractions of As showed significant positive correlations with soil pH. A calculated individual availability factor (A f (i) ) is used; the values of each trace element in the soils are in the following order: Cu > Cd > Pb > Zn > As > Hg. When combined with a risk assessment code, data suggest that Hg, As, Pb, and Zn levels showed low risk for the environment, whereas Cd levels in soils adjacent to the GM and Cu levels in soils adjacent to the GS showed medium risk to the environment, and Cd levels in soils adjacent to the GS exhibited higher environment risk.

摘要

对位于焦家金矿附近的土壤进行了采样和分析,以确定中国山东省土壤中微量元素(汞、砷、镉、铅、铜和锌)的污染程度。所有18个样品的汞、砷、镉和铅平均浓度均超过当地背景值,而铜和锌的平均浓度低于背景值。此外,金冶炼厂(GS)土壤中的微量元素浓度高于金矿(GM)土壤。改进的 Tessier 连续提取程序的结果表明,除冶炼厂附近土壤中的铜外,微量元素主要与残留部分相关。在残留部分之后,大多数汞主要与腐殖酸和强有机部分相关,而大多数砷与腐殖酸相关。与其他微量元素相比,镉与水溶性、离子交换和碳酸盐部分相关。此外,铜、铅和锌在腐殖酸和铁/锰氧化物部分中更为集中。微量元素的各部分受土壤pH值和电导率(Ec)的影响。汞的腐殖酸部分以及镉和锌的离子交换部分与土壤pH值呈负相关。汞的强有机部分、镉的铁/锰氧化物部分和锌的碳酸盐部分与土壤电导率呈正相关。锌的强有机部分和离子交换部分与土壤电导率呈负相关。然而,砷的离子交换和碳酸盐部分与土壤pH值呈显著正相关。使用计算得出的个体有效性因子(Af(i));土壤中各微量元素的值顺序如下:铜>镉>铅>锌>砷>汞。结合风险评估代码,数据表明汞、砷、铅和锌水平对环境显示低风险,而GM附近土壤中的镉水平和GS附近土壤中的铜水平对环境显示中等风险,GS附近土壤中的镉水平显示更高的环境风险。

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