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Chemical availability of arsenic and heavy metals in sediments from abandoned cinnabar mine tailings

机译:废弃朱砂矿尾矿沉积物中砷和重金属的化学利用率

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摘要

The understanding of the solid-phase speciation of arsenic in soils and sediments is important in the evaluations of its potential mobility and availability in the environment. The spoil heaps of abandoned mercury mines contain waste materials with high arsenic and heavy metals concentrations. The weathering of these tailings can cause their mobilization to the surroundings. In this work, the mobility and availability of arsenic and some heavy metals were evaluated in sediments from two heavily polluted mercury mining districts in Asturias (NW Spain). For this purpose, a slightly modified version of the Bureau Community of Reference sequential extraction scheme was applied to sediments. The total contents in the operationally defined fractions were analysed by inductively coupled plasma-atomic emission spectrometry. Extremely high total arsenic concentrations were found in all sediments ranging from 4,000 to 24,800 mg kg~(-1). High easily mobilizable arsenic contents were found in the first mining area, related to the solubilization of Ca-bearing phases, supported by extracts analyses, X-ray diffraction results and the positive correlation found among the As and Ca fractionations. Ni and Zn were the most mobile among heavy metals, being Cr the least mobile, suggesting an anthropogenic origin due to the metallurgical processes, transport or dispersion generated from neighbour spoil heaps. In the second mining area, the bulk of As was concentrated in the residual phase, as well as Cr, Cu, Fe, Pb, Ti, indicating a mineralogical origin and the low availability of these elements. The strong correlations established between As and Fe and Ti distributions support the hypothesis that As is mainly associated to structural mineral phases in these sediments.
机译:了解土壤和沉积物中砷的固相形态对于评估其在环境中的潜在迁移率和可利用性非常重要。废弃汞矿的废料堆中含有高砷和重金属的废料。这些尾矿的风化会导致它们动员到周围环境中。在这项工作中,评估了阿斯图里亚斯(西班牙西北部)两个污染严重的汞矿区的沉积物中砷和一些重金属的迁移率和有效性。为此,对沉积物采用了稍作修改的“科技局参考序列提取方案”。通过电感耦合等离子体原子发射光谱法分析可操作定义的馏分中的总含量。在所有沉积物中发现的最高总砷浓度范围为4,000至24,800 mg kg〜(-1)。在第一个矿区发现了易迁移的高砷含量,这与含钙相的增溶有关,提取物分析,X射线衍射结果与砷和钙的分馏之间存在正相关关系。 Ni和Zn在重金属中的流动性最高,而Cr的流动性最低,这表明人为起源是由于冶金过程,邻近弃渣堆产生的运输或分散。在第二个矿区,大部分砷以及剩余的铬,铜,铁,铅,钛都集中在残留相中,表明这些元素的矿物学成因和可用性较低。 As与Fe和Ti分布之间建立的强相关性支持以下假设:As主要与这些沉积物中的结构矿物相有关。

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  • 来源
    《Environmental earth sciences》 |2013年第2期|535-546|共12页
  • 作者单位

    Unidad de Espectroscopfa, Division de Qufmica, Departamento de Tecnologfa, CIEMAT, Av. Complutense, 40, Madrid, Spain;

    Unidad de Espectroscopfa, Division de Qufmica, Departamento de Tecnologfa, CIEMAT, Av. Complutense, 40, Madrid, Spain;

    Dpto. de Explotacion y Prospeccion de Minas, Universidad de Oviedo, Escuela de Minas. C/Independencia, 13, Oviedo, Spain;

    Unidad de Espectroscopfa, Division de Qufmica, Departamento de Tecnologfa, CIEMAT, Av. Complutense, 40, Madrid, Spain;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    fractionation; sediments; BCR; mobility; heavy metals; arsenic; mine sites;

    机译:分馏沉积物BCR;流动性重金属;砷;矿场;

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