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Distribution and mobility of arsenic and antimony at mine sites in FYR Macedonia.

机译:南斯拉夫马其顿矿区砷和锑的分布和流动性。

摘要

Soils, river sediments and waters from former As-Sb mining sites in FYR Macedonia have been chemically analysed to assess their impact on the local environment. Soils and river sediments contain very high concentrations of As and Sb (medians 117 and 37 mg kg-1), but values are heterogeneously distributed. These values are far in excess of various statutory thresholds and at the largest deposit, Lojane, the area is grossly contaminated. Sequential extraction has demonstrated that a large proportion of the As (50-90%) and Sb (20-60%) in these soils is in a weakly-bound form and is thus available for further mobilization. Surface and groundwaters are neutral to alkaline because of interaction with host lithologies (e.g. serpentinite, dolomite and limestone). Surface waters appear to have higher concentrations of As (55;33) and Sb (2.1;0.6) than the groundwaters (medians, υg/l). For all samples there is a close positive correlation between As and Sb, but As contents are generally much higher than those for Sb. Most of the waters have As concentrations which exceed the 10 υg l-1 value accepted for safe drinking water whereas most Sb concentrations are much lower and appear to be within the acceptable limits for this element. The alkaline waters have been able to mobilize the As and Sb directly from the primary ore minerals and the lack of pyrite in the ores has minimized the production of secondary Fe oxides which could adsorb and immobilize these elements. These sites are environmental ‘hotspots’ and need remediation. The reservoir of As and Sb which is able to be released over a long time period threatens a much larger area. Remediation strategies would have to take the mobility of these elements under alkaline conditions into account.
机译:对马其顿前南斯拉夫联盟共和国前As-Sb采矿场的土壤,河流沉积物和水进行了化学分析,以评估其对当地环境的影响。土壤和河流沉积物中的砷和锑含量很高(中位数分别为117和37 mg kg-1),但其值分布不均。这些值远远超过了各种法定阈值,在最大的矿床Lojane,该地区受到了严重污染。连续提取表明,这些土壤中的大部分As(50-90%)和Sb(20-60%)呈弱结合形式,因此可用于进一步动员。由于与宿主岩性(例如蛇纹岩,白云岩和石灰石)相互作用,地表水和地下水对碱呈中性。地表水似乎比地下水具有更高的砷(55; 33)和锑(2.1; 0.6)浓度(中位数,μg/ l)。对于所有样品,As和Sb之间都有密切的正相关性,但As含量通常远高于Sb。大多数水的砷浓度超过安全饮用水可接受的10μgl-1值,而大多数锑的浓度则低得多,并且似乎在该元素的可接受范围内。碱性水已经能够直接从主要矿石矿物中迁移出As和Sb,并且矿石中缺乏黄铁矿已经使可以吸附和固定这些元素的次生Fe氧化物的生成减至最少。这些网站是环境的“热点”,需要补救。能够长时间释放的砷和锑的储集层威胁着更大的面积。补救策略必须考虑这些元素在碱性条件下的迁移率。

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