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海洋近岸沉积物芯中重金属的分布与化学分馏:来自中国连云港墟沟的案例研究。

Distribution and chemical partitioning of heavy metals in marine near-shore sediment cores: a case study from the Xugou, Lianyungang, China.

机构信息

School of Chemical Engineering, Huaihai Institute of Technology, Lianyungang, Jiangsu 222005, China.

出版信息

Environ Monit Assess. 2011 Jun;177(1-4):263-72. doi: 10.1007/s10661-010-1632-z. Epub 2010 Aug 10.

Abstract

The concentrations and chemical partitioning of heavy metals (Co, Cr, Ni, Zn, Cu, and Pb) in the marine near-shore sediment cores were investigated. Typically, the mean concentrations from Core B sediment samples were 98.6, 21.1, 47.0, 46.4, 107.6, and 31.9 mg kg( - 1) for Cr, Co, Ni, Cu, Zn, and Pb, respectively. The heavy metal concentrations were normalized to commonly used reference elements Al, Li, Sc, and total organic carbon. Based on Pearson coefficients, Li was found to be a good normalizer for Co (r = 0.974), Cr (r = 0.967), Ni (r = 0.898), and Zn (r = 0.929) in 80 sediment samples from three sampling sites. However, the correlation coefficients between Li and Cu, and Li and Pb were relatively low. Multivariate statistic approaches (Principal Component Analysis and Cluster Analysis) were adopted for data treatment, allowing the identification of two main factors controlling the heavy metal variability in the sediments. Heavy metals in the enrichment sections were evaluated by a sequential extraction method for possible chemical forms in sediments. The results showed that the residual, Fe/Mn oxides and Organic/sulfide fractions were dominant geochemical phases in the enriched sections, indicating low bioavailability of heavy metals in sediments.

摘要

研究了海洋近岸沉积物岩芯中重金属(Co、Cr、Ni、Zn、Cu 和 Pb)的浓度和化学分配。通常,B 岩芯沉积物样品的平均浓度分别为 Cr、Co、Ni、Cu、Zn 和 Pb 的 98.6、21.1、47.0、46.4、107.6 和 31.9 mg kg(-1)。重金属浓度与常用的参考元素 Al、Li、Sc 和总有机碳进行了归一化。基于 Pearson 系数,发现 Li 是 Co(r = 0.974)、Cr(r = 0.967)、Ni(r = 0.898)和 Zn(r = 0.929)在三个采样点的 80 个沉积物样品中的良好归一化元素。然而,Li 与 Cu 和 Li 与 Pb 之间的相关系数相对较低。采用多元统计方法(主成分分析和聚类分析)进行数据处理,确定了控制沉积物中重金属变化的两个主要因素。采用连续提取法对富集段中的重金属进行评估,以确定沉积物中重金属的可能化学形态。结果表明,在富集段中,残余物、Fe/Mn 氧化物和有机/硫化物是主要的地球化学相,表明沉积物中重金属的生物可利用性较低。

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