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Mineralogical attenuation for metallic remediation in a passive system for mine water treatment

机译:用于矿井水处理的被动系统中金属修复的矿物学衰减

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Passive systems with constructed wetlands have been consistently used to treat mine water from abandoned mines. Long-term and cost-effective remediation is a crucial expectation for these water treatment facilities. To achieve that, a complex chain of physical, chemical, biological, and mineralogical mechanisms for pollutants removal must be designed to simulate natural attenuation processes. This paper aims to present geochemical and mineralogical data obtained in a recently constructed passive system (from an abandoned mine, Jales, Northern Portugal). It shows the role of different solid materials in the retention of metals and arsenic, observed during the start-up period of the treatment plant. The mineralogical study focused on two types of materials: (1) the ochre-precipitates, formed as waste products from the neutralization process, and (2) the fine-grained minerals contained in the soil of the wetlands. The ochre-precipitates demonstrated to be poorly ordered iron-rich material, which gave rise to hematite upon artificial heating. The heating experiments also provided mineralogical evidence for the presence of an associated amorphous arsenic-rich compound. Chemical analysis on the freshly ochre-precipitates revealed high concentrations of arsenic (51,867 ppm) and metals, such as zinc (1,213 ppm) and manganese (821 ppm), indicating strong enrichment factors relative to the water from which they precipitate. Mineralogical data obtained in the soil of the wetlands indicate that chlorite, illite, chlorite–vermiculite and mica–vermiculite mixed-layers, vermiculite, kaolinite and goethite are concentrated in the fine-grained fractions (20 and 2 μm). The chemical analyses show that high levels of arsenic (up to 3%) and metals are also retained in these fractions, which may be enhanced by the low degree of order of the clay minerals as suggested by an XRD study. The obtained results suggest that, although the treatment plant has been receiving water only since 2006, future performance will be strongly dependent on these identified mineralogical pollutant hosts.
机译:带有人工湿地的被动系统一直被用来处理废弃矿井的矿井水。对于这些水处理设施而言,长期且具有成本效益的修复是至关重要的期望。为此,必须设计复杂的物理,化学,生物和矿物学机制来去除污染物,以模拟自然衰减过程。本文旨在介绍在最近建造的被动系统(从废弃的矿山,葡萄牙北部的贾勒斯)中获得的地球化学和矿物学数据。它显示了在处理厂启动期间观察到的不同固体材料在金属和砷保留方面的作用。矿物学研究集中在两种类型的材料上:(1)och色沉淀物,是中和过程中产生的废物,(2)湿地土壤中所含的细粒矿物。 och色沉淀物证明是有序的富铁材料,在人工加热时会生成赤铁矿。加热实验还为相关无定形富含砷的化合物的存在提供了矿物学证据。对新鲜石沉淀物的化学分析显示,砷(51,867 ppm)和金属(例如锌(1,213 ppm)和锰(821 ppm))高浓度,表明相对于其沉淀的水而言,浓集因子很高。在湿地土壤中获得的矿物学数据表明,绿泥石,伊利石,绿泥石-ver石和云母-ver石混合层,ver石,高岭石和针铁矿集中在细粒级分(<20和<2μm)中。化学分析表明,这些馏分中还保留了高含量的砷(高达3%)和金属,这可以通过XRD研究表明,粘土矿物的有序度较低而得到增强。所获得的结果表明,尽管污水处理厂仅从2006年起才开始取水,但是未来的性能将在很大程度上取决于这些确定的矿物污染物宿主。

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