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首页> 外文期刊>Bulletin of Environmental Contamination and Toxicology >Spatial distribution and partitioning of heavy metals in surface sediments from Yangtze Estuary and Hangzhou Bay, People's Republic of China.
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Spatial distribution and partitioning of heavy metals in surface sediments from Yangtze Estuary and Hangzhou Bay, People's Republic of China.

机译:中华人民共和国长江口和杭州湾表层沉积物中重金属的空间分布与分配

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摘要

Two neighbouring areas, Yangtze estuary and Hangzhou Bay, were investigated to establish the planar distribution patterns and fractionation of heavy metals, viz., Cu, Pb, Zn, Cd, Ni, Cr, MnO and Fe2O3, in the surface sediments. X-ray diffraction analysis showed that the mineralogical compositions of the sediments in both water bodies were similar. The average values of heavy metals in the sediments decreased in the order of Fe > Mn > Zn > Cr > Ni > Cu > Pb > Cd. The concentration of heavy metals decreased from the inner reach to the river mouth of the Yangtze estuary. In Hangzhou Bay, the concentrations of heavy metals were higher in the east than in the west. There were significant positive correlations among all metal concentrations except for Fe-Cr and Fe-Cd, while Cu and Pb were highly correlated with other metals. The distributional patterns of the 8 metals were divided into two groups according to the degree of their association with the residual fraction. Cu, Cr, Zn, Fe and Ni were assigned to a group that were mainly found in the residual fraction, while Cd, Pb and Mn were in a group with their residual fraction less than 50% of the total levels. The percentages of five fractions for Cu, Fe, Ni and Zn in the sediments followed the order as residual > Fe-Mn oxides > organic > carbonate > exchangeable, while those of Cr followed the order as residual > organic > Fe-Mn oxides > carbonate > exchangeable. A considerable proportion of Cd and Mn were found in all of the five fractions, while Pb was not detected in the exchangeable fraction. In the non-residual fraction, Cd was mainly presented in exchangeable, carbonate fraction and Fe-Mn oxides while Pb was mainly retained in Fe-Mn oxides fraction. Mn was mainly dominated in carbonate and Fe-Mn oxides. Among the five fractions, the heavy metals in exchangeable and carbonate fractions can be easily remobilized by changes in environmental conditions. The results derived from the study indicate that the study area had Cd and Mn pollution risks..
机译:研究了长江口和杭州湾两个邻近地区,以建立表层沉积物中重金属的平面分布模式和分馏,即Cu,Pb,Zn,Cd,Ni,Cr,MnO和Fe2O3。 X射线衍射分析表明,两个水体中的沉积物的矿物学组成是相似的。沉积物中重金属的平均值按Fe> Mn> Zn> Cr> Ni> Cu> Pb> Cd的顺序降低。重金属的浓度从长江口的内河段到河口下降。在杭州湾,东部地区的重金属含量高于西部地区。除Fe-Cr和Fe-Cd外,所有金属浓度之间均存在显着的正相关,而Cu和Pb与其他金属高度相关。根据8种金属与残留分数的关联程度将其分布模式分为两组。 Cu,Cr,Zn,Fe和Ni属于主要存在于残留分数中的组,而Cd,Pb和Mn属于其残留分数小于总水平的50%的组。沉积物中Cu,Fe,Ni和Zn的五个馏分的百分比顺序为:残留> Fe-Mn氧化物>有机>碳酸盐>可交换,而Cr的含量依次为残留>有机-Fe-Mn氧化物>碳酸盐>可交换。在所有五个馏分中均发现相当比例的Cd和Mn,而在可交换馏分中未检测到Pb。在非残留部分中,Cd主要存在于可交换的碳酸盐部分和Fe-Mn氧化物中,而Pb主要保留在Fe-Mn氧化物部分中。锰主要是碳酸盐和铁锰氧化物。在这五个馏分中,可交换馏分和碳酸盐馏分中的重金属可以通过环境条件的变化而容易地迁移。研究得出的结果表明,研究区存在镉和锰污染的风险。

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