首页> 外文期刊>Journal of Hazardous Materials >Solid/solution partitioning and speciation of heavy metals in the contaminated agricultural soils around a copper mine in eastern Nanjing city, China
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Solid/solution partitioning and speciation of heavy metals in the contaminated agricultural soils around a copper mine in eastern Nanjing city, China

机译:南京市东部某铜矿附近被污染的农业土壤中重金属的固/液分配和形态

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Solid/solution partition coefficient (K_d) and speciation of soil heavy metals can be used for predicting their environmental risks. The K_d values and solution speciation of soil Cu, Cd and Zn were analyzed in 40 samples of contaminated agricultural soils around Jiuhua copper mine in eastern Nanjing city, China. The K_d ranges (and mean values) for soil Cu, Cd and Zn are 703-7418 (3453), 37.3-3963 (940) and 319-17 965 (7244) L kg~(-1), respectively, showing a large variability both for metals and soils. The results of differential pulse anodic stripping voltammetry (DPASV) indicates that 95.6% solution Cu is bound to dissolved organic ligands. About half of the dissolved Zn is DPASV-labile at pH < 6, while 92.1% solution Zn is in the form of organic complexes at pH > 6. DPASV-labile Cd is ranged from 22.6 to 98.7% with the mean value of 56.3%. Multiple linear regressions indicate that K_d, the dissolved and DPASV-labile concentrations of Cd and Zn are mostly influenced by the soil solution pH with R~2 of 0.50, 0.59 and 0.63, respectively for Cd, and 0.58, 0.72 and 0.64, respectively for Zn. Considering the second parameter of corresponding soil metal, the linear relationships of K_d with pH were improved with R~2 of 0.70 and 0.73 for Cd and Zn, respectively. However, the solubility of soil Cu was insensitive to pH. Only SOC shows a weak relationship to the dissolved Cu with R~2 of 0.21. As for its K_d, total soil Cu is the most significant factor. But for DPASV-labile Cu, no soil parameters were found to be good predictors.
机译:固/溶液分配系数(K_d)和土壤重金属的形态可用于预测其环境风险。在南京市东部九华铜矿附近的40个被污染的农业土壤样品中,分析了土壤Cu,Cd和Zn的K_d值和溶液形态。土壤Cu,Cd和Zn的K_d范围(和平均值)分别为703-7418(3453),37.3-3963(940)和319-17965(7244)L kg〜(-1),显示较大金属和土壤的变异性。差分脉冲阳极溶出伏安法(DPASV)的结果表明,95.6%的溶液Cu与溶解的有机配体结合。在pH <6时,大约一半的溶解锌对DPASV不稳定,而在pH> 6时,有92.1%的溶液Zn以有机络合物形式存在。对DPASV不稳定的Cd范围为22.6至98.7%,平均值为56.3% 。多元线性回归表明,K_d,Cd和Zn的溶解浓度以及DPASV不稳定的浓度主要受土壤溶液pH的影响,Cd的R〜2分别为0.50、0.59和0.63,Cd的R〜2分别为0.58、0.72和0.64。锌考虑到相应的土壤金属的第二参数,C_和Zn的K_d与pH的线性关系得到改善,R〜2分别为0.70和0.73。但是,土壤铜的溶解度对pH值不敏感。只有SOC与溶解的Cu的关系较弱,R〜2为0.21。至于其K_d,土壤总Cu是最重要的因素。但是对于DPASV不稳定的铜,没有发现土壤参数是好的预测指标。

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