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Total mercury, organic mercury and mercury fractionation in soil profiles from the Almaden mercury mine area

机译:Almaden汞矿区土壤剖面中的总汞,有机汞和汞分馏

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Soil profiles located in the mining district of Almaden were investigated for total Hg, organic Hg fraction and Hg distribution by selective sequential extraction. A four-step sequential extraction method (labile Hg species, humic and futvic complexes, elemental Hg and bound to crystalline oxides and Hg sulfide and refractory species) was performed. Total Hg concentrations ranged from 13 to 64 mg per kg dry mass. A clear relationship between the depth and Hg content was found since Hg concentration decreases downwards, which is indicative of anthropogenic contamination via deposition processes from nearby mine waste. Significant organic Hg concentrations were found in all the tested soil profiles ranging from 79 to 287 μg kg~(-1) (dry weight). It seems that organic Hg was strongly influenced by elemental Hg (r = 0.79) and to a lesser extent by the organic carbon content (r = 0.57). The fractionation revealed that Hg exists mainly as cinnabar in the studied soils, which is one of the least available and mobile Hg species, and as elemental Hg as well. The most mobile Hg fractions only accounted for 3.2 to 7.7% of the total Hg content, with the main contribution being the humic and fulvic complexes fraction. The elemental Hg fraction increased with depth indicating a migration to deeper soil layers. In contrast, the surface layers showed an enrichment in the fraction bound to sulfide, which means that Hg is mostly deposited as cinnabar particles from non-processed ore in this area.
机译:通过选择性顺序提取,对位于阿尔玛登(Almaden)矿区的土壤剖面进行了总汞,有机汞含量和汞分布的调查。进行了四个步骤的顺序萃取方法(不稳定的Hg物种,腐殖酸和富特维克络合物,元素Hg并结合到晶体氧化物和Hg硫化物及难熔物种)。汞的总浓度为每千克干重13至64毫克。由于汞浓度向下下降,因此发现了深度与汞含量之间的明确关系,这表明来自附近矿山废物的沉积过程造成了人为污染。在所有测试的土壤剖面中,从79至287μgkg〜(-1)(干重),均发现了显着的有机汞浓度。似乎有机汞受到元素汞的强烈影响(r = 0.79),而有机碳含量受到的影响较小(r = 0.57)。分馏表明,Hg主要以朱砂的形式存在于被研究的土壤中,这是最缺乏的和可移动的Hg物种之一,也以元素Hg的形式存在。流动性最高的汞馏分仅占总汞含量的3.2%至7.7%,主要贡献是腐殖质和黄腐复合物的分数。元素汞含量随深度增加而增加,表明迁移到更深的土壤层。相比之下,表层显示出与硫化物结合的馏分富集,这意味着汞主要以朱砂颗粒的形式沉积在该区域的未加工矿石中。

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