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Heavy metal concentrations in soils from a remote oceanic island, Fernando de Noronha, Brazil

机译:来自巴西费尔南多·迪诺罗尼亚群岛一个偏远海洋岛屿的土壤中的重金属含量

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This paper examines the role of parent rock, pedogenetic processes and airborne pollution in heavy metal accumulation in soils from a remote oceanic island, Fernando de Noronha, Brazil. We studied five soil profiles developed from different volcanic rocks. Mineralogical composition and total concentrations of major and trace elements were determined in 43 samples. The obtained concentrations range for heavy metals were: Co: 26-261 ppm; Cu: 35-97 ppm; Cr: 350-1446 ppm; Ni: 114-691 ppm; Zn: 101-374 ppm; Hg: 2-150 ppb. The composition of soils is strongly affected by the geochemical character of the parent rock. Pedogenesis appears to be responsible for the accumulation of Zn, Co, and, to a lesser extent, of Ni and Cu, in the upper, Mn- and organic carbon-enriched horizons of the soil profiles. Pedogenic influence may also explain the relationship observed between Cr and the Fe. Hg is likely to have been added to the soil profile by long-range atmospheric transport. Its accumulation in the topsoil was further favoured by the formation of stable complexes with organic matter. Clay minerals do not appear to play an important role in the fixation of heavy metals.
机译:本文研究了来自遥远的海洋岛屿费尔南多·德·诺罗尼亚(Fernando de Noronha),巴西的母岩,成岩过程和空气传播污染在土壤重金属积累中的作用。我们研究了从不同火山岩中发育的五种土壤剖面。确定了43个样品的矿物学组成以及主要和微量元素的总浓度。获得的重金属浓度范围为:Co:26-261 ppm;铜:35-97 ppm; Cr:350-1446 ppm; Ni:114-691 ppm;锌:101-374 ppm;汞:2-150 ppb。土壤组成受母岩地球化学特征的强烈影响。在土壤剖面的上部,富含锰和有机碳的地层中,成岩作用似乎是造成锌,钴以及少量镍和铜积累的原因。受成岩作用的影响也可以解释Cr和Fe之间的关系。汞可能是通过远程大气迁移而添加到土壤中的。稳定的有机物络合物的形成进一步促进了其在表土中的积累。粘土矿物质似乎在重金属固着中不发挥重要作用。

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