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Background levels of heavy metals in surficial sediments of the Gulf of Lions (NW Mediterranean): An approach based onud133Cs normalization and lead isotope measurements

机译:狮子湾(西北地中海)表层沉积物中重金属的背景水平:一种基于 ud的方法133Cs归一化和铅同位素测量

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摘要

This paper presents an attempt to reach natural background levels of heavy metals in surficial sediments of the Gulf of Lions(NW Mediterranean). To correct for the grain-size effect, normalization procedures based on a clay mineral indicator element are commonly used, after a first grain size separation by sieving. In our study, we tested the applicability of this method with respect to commonly used normalizer elements, and found that stable Cs shows the best ability to reflect the fine sediment fraction. Background levels were successfully reached for Co, Cr, Cu, Ni and Pb, compared to various literature references. Nevertheless, in the case of lead, the normalized data depicted a general enrichment in all samples, and the natural levels could only be reached when concentrations were corrected for the atmospheric contribution by analysing lead isotope ratios. Also for Zn, a general enrichment was found in our samples, although less important.
机译:本文提出了一种尝试达到狮子湾(西北地中海)表层沉积物中自然重金属含量的尝试。为了校正晶粒尺寸效应,在通过筛分进行第一次晶粒尺寸分离之后,通常使用基于粘土矿物指示剂元素的归一化程序。在我们的研究中,我们测试了该方法对常用归一化元素的适用性,并发现稳定的Cs具有最佳的反映细颗粒沉积物含量的能力。与各种文献参考相比,成功达到了Co,Cr,Cu,Ni和Pb的背景水平。然而,在铅的情况下,归一化数据描述了所有样品的总体富集,只有通过分析铅同位素比校正大气贡献的浓度后才能达到自然水平。同样对于锌,在我们的样品中发现了一般富集,尽管重要性不高。

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