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首页> 外文期刊>Journal of Iberian geology >Distribution patterns and enrichment of lead, zinc and copper in surface sediments of the central Portuguese shelf and upper slope
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Distribution patterns and enrichment of lead, zinc and copper in surface sediments of the central Portuguese shelf and upper slope

机译:葡萄牙中部陆架和上斜坡表层沉积物中铅,锌和铜的分布规律和富集

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Geographic patterns of Cu, Pb and Zn enrichment on the Lisbon-Setúbal-Sines continental shelf and upper slope (central Portuguese margin) were studied in this paper to gain insight into current pathways of trace metal dispersal. Our study is based on the analysis of elemental concentrations and mineralogy of surface sediment samples collected offshore one of the most industrialised areas of Portugal. On the Lisbon-Setúbal-Sines shelf concentrations of Al, Fe, Mg, Ti within the fine-grained sediment fraction appear to a large extent related to the amount of fine-grained fraction in the bulk sediment. The extent of enrichment of trace metals in the studied area follows the sequence: Pb Zn Cu. Generally, the enrichment of trace metals tends to decrease in offshore direction suggesting that the excess of trace metals must be derived from land. The areas of the Lisbon-Setúbal-Sines shelf most affected by enrichment of trace metals include the Tagus and Sado mud patches and the inner shelf between Tróia and Sines, including the areas close to the Sado outlet and the area adjacent to the St. André and Melides coastal lagoons, which highlights the nearby estuaries and the lagoons as likely sources for the enrichment. In addition, the more widespread enrichment of Pb in sediments points to contributions from atmospheric inputs. The similarity between the results here presented with later data from other authors allows concluding that our results provide a representative view of trace metal enrichment in surface sediments between 1980 and 2000.
机译:本文研究了里斯本-塞图巴尔-塞纳斯大陆架和上斜坡(葡萄牙中部边缘)的铜,铅和锌富集的地理模式,以了解痕量金属扩散的当前途径。我们的研究基于对葡萄牙最工业化地区之一附近海域收集的地表沉积物样品的元素浓度和矿物学分析。在里斯本-塞图巴尔-塞纳斯架子上,细颗粒沉积物中的Al,Fe,Mg,Ti浓度在很大程度上与大体积沉积物中的细颗粒含量有关。研究区域中痕量金属的富集程度遵循以下顺序:Pb> Zn> Cu。通常,痕量金属的富集趋向于在近海方向减少,这表明过量的痕量金属必须来自陆地。里斯本-Setúbal-Sines陆架受微量金属富集影响最大的地区包括塔霍河和萨多泥滩以及特洛亚和锡涅斯之间的内陆架,包括靠近萨多出口的区域和毗邻圣安德烈的区域和梅利德斯沿海泻湖,突出了附近的河口和泻湖,可能是富集的来源。此外,沉积物中铅的更广泛富集表明大气输入的贡献。这里的结果与其他作者的后续数据之间的相似性可以得出结论,即我们的结果提供了代表性的观点,即1980年至2000年之间地表沉积物中的痕量金属富集。

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