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首页> 外文期刊>Journal of Environmental Engineering >Speciation and Bioavailability of Heavy Metals in Sediments Taken from Wetland in the Huaihe River Basin
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Speciation and Bioavailability of Heavy Metals in Sediments Taken from Wetland in the Huaihe River Basin

机译:淮河流域湿地沉积物中重金属的形态及生物利用度

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The fractions of heavy metals in sediment cores taken from the riverine wetland located in the Huaihe River Basin, China, were analyzed using BCR (European Communities Bureau of Reference) sequential extraction techniques. The results revealed that the total concentrations of Cd, Cr, Cu, Pb, and Zn ranged from 0.09-0.38, 47.6-70.2, 14.0-92.1, 19.6-35.9, and 53.8-227.0mgkg-1, respectively. The significant increase in the values of enrichment factors (EF) and the geoaccumulation index (Igeo) from about 4cm depth layer and maximum values approaching 5 and 1 near the surface, respectively, indicated the rapid growth of pollutant discharge especially for Cd, Cu, and Zn in recent years. Furthermore, the proportions of the different fractions (i.e.,acid extractable, reducible, oxidizable, and residual fractions) of Cd, Cr, Cu, Pb, and Zn had changed drastically. The significant increases in the proportions of reactive forms (acid extractable, reducible, and oxidizable fractions) of heavy metals from about 4cm depth layer to top layer suggested a marked increase in the mobility and bioavailability of Cd, Pb, Cu, and Cr. Finally, significant positive correlations between total organic carbon (TOC) and reactive fractions suggested that heavy metals, especially reactive fractions, tended to be absorbed by organic materials. The most significant trend in increases indicated that Cd and Cu possessed the most conspicuous mobility and bioavailability. In addition, larger proportions of reactive fractions of Zn indicated that Zn had constant mobility and posed a significant ecological risk to aquatic organisms in the riverine wetland.
机译:使用BCR(欧洲共同体参考局)连续萃取技术分析了来自位于中国淮河流域的河流湿地的沉积物芯中的重金属含量。结果表明,Cd,Cr,Cu,Pb和Zn的总浓度范围为0.09-0.38、47.6-70.2、14.0-92.1、19.6-35.9和53.8-227.0mg kg - 1,分别。富集因子(EF)和地质累积指数(Igeo)的值分别从约4cm的深度层显着增加,并且最大值分别接近地表5和1,表明污染物排放迅速增长,尤其是对于Cd,Cu,和锌。此外,Cd,Cr,Cu,Pb和Zn的不同部分(即,可酸提取的,可还原的,可氧化的和残留的部分)的比例发生了巨大变化。重金属的反应形式(可酸提取,可还原和可氧化的馏分)的比例从约4cm深度到顶层显着增加,表明Cd,Pb,Cu和Cr的迁移率和生物利用度显着提高。最后,总有机碳(TOC)与反应性馏分之间存在显着的正相关关系,表明重金属,尤其是反应性馏分倾向于被有机材料吸收。增长的最显着趋势表明,镉和铜具有最明显的迁移率和生物利用度。此外,较大比例的锌反应性组分表明锌具有恒定的迁移率,并且对河流湿地中的水生生物构成了重大的生态风险。

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