首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Background determination, pollution assessment and source analysis of heavy metals in estuarine sediments from Quanzhou Bay, southeast China
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Background determination, pollution assessment and source analysis of heavy metals in estuarine sediments from Quanzhou Bay, southeast China

机译:泉州湾泉州湾河口河口沉积物中重金属的背景测定,污染评价与源分析

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The concentrations of ten heavy metals (Cr, Cu, Zn, Cd, Pb, Co, Ni, Fe, Mn, and Hg) and Pb isotope compositions were investigated in two estuarine sediment cores collected in Quanzhou Bay, southeast China. The regional background levels of heavy metals in the estuarine sediments from Quanzhou Bay were established using the fine fractions (< 63 mu m) obtained from the sediment cores. The background values of Cr, Cu, Zn, Cd, Pb, Co, Ni, Mn, Hg, and Fe were 37.14 mg kg(-1), 19.79 mg kg(-1), 130.86 mg kg(-1), 0.24 mg kg(-1), 42.18 mg kg(-1), 10.31 mg kg(-1) 20.89 mg kg(-1), 612.60 mg kg(-1), 0.07 mg kg(-1) and 3.17%, respectively. The background values of most elements (Cr, Cd, Pb, Co, Ni, Mn, Hg, and Fe) detected for the estuarine sediments from Quanzhou Bay in this study were in the middle of the obtained ranges for other locations in China. However, the Pb and Zn background values in Quanzhou Bay were significantly higher than the Chinese average. The enrichment factor (EF), geoaccumulation index (I-geo), and contamination factor (CF) values indicated that sediment contamination associated with Cu, Zn, Pb, Mn, and Cd has occurred since the nineteenth century. Based on principal component analysis (PCA) and cluster analysis (CA), Cu, Zn, and Pb were clustered into a group, and their sources could be related to the mining of metallic ore deposits. The Pb isotope composition data from the dated sediment cores further suggested that the Pb sources transitioned from natural sources during 1715-1788 CE to Pb-Zn ore deposits during 1788-1935 CE and then to multiple anthropogenic sources, including Pb-Zn ore deposits and industrial and domestic emissions, in recent decades (1935-2009 CE).
机译:在中国泉州湾泉湾东南部地区收集的两种偏卤素沉积物核心,研究了十种重金属(Cr,Cu,Zn,Cd,Pb,Co,Ni,Fe,Fe,Fe,Mn和Hg)和Pb同位素组合物。使用从沉积物芯中获得的细级分(<63μm)建立了泉州海湾河口沉积物中重金属的区域背景水平。 Cr,Cu,Zn,Cd,Pb,Co,Ni,Mn,Hg和Fe的背景值为37.14mg kg(-1),19.79mg kg(-1),130.86mg kg(-1),0.24 Mg kg(-1),42.18mg kg(-1),10.31mg kg(-1)20.89mg kg(-1),612.60mg kg(-1),0.07mg kg(-1)和3.17% 。对本研究中泉州湾的河口沉积物检测到的大多数元素(Cr,Cd,Pb,Co,Ni,Mn,Hg和Fe)的背景值位于中国其他地点的所得范围的中间。然而,泉州湾的PB和Zn背景值明显高于中国平均水平。富集因子(EF),地质累积指数(I-Geo)和污染因子(CF)值表明,与十九世纪以来,与Cu,Zn,Pb,Mn和Cd相关的沉积物污染。基于主成分分析(PCA)和聚类分析(CA),Cu,Zn和Pb被聚集成一个组,它们的来源可能与金属矿床的开采有关。来自日期沉积物核心的Pb同位素组成数据进一步表明,在1715-1788 Ce期间,在1788-1935 Ce期间,从天然来源转换到Pb-Zn Ore沉积物,然后转移到多个人为沉积物,包括Pb-Zn Ore沉积物和近几十年(1935-2009 CE)的工业和国内排放量。

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