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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Distribution of arsenic and nickel in uranium mill tailings, Rabbit Lake, Saskatchewan, Canada
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Distribution of arsenic and nickel in uranium mill tailings, Rabbit Lake, Saskatchewan, Canada

机译:加拿大萨斯喀彻温省Rabbit Lake铀矿尾矿中砷和镍的分布

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The Rabbit Lake U mine in-pit tailings management facility (TMF) is located in northern Saskatchewan, Canada. The tailings body is approximately 425 m long x 300 m wide and 91 m thick at its centre. An investigation of the TMF was performed to collect tailings samples from depth to quantify the distribution of As and Ni in the tailings with respect to ore type and assess the distribution of As and Ni with respect to tailings mineralogy. The tailings body consists of alternating layers of ice, frozen tailings and unfrozen tailings which varied in texture from a slurry to a firm silty sand. The tailings solids are predominately composed of quartz (16-36%), calcium sulphate (0.3-54%) and illite (3 and 14%). Arsenic and Ni concentrations in the tailings show similar patterns with depth which were strongly related to historical changes in As and Ni concentrations in the mill feed. Mineralogy of the ore bodies indicated that As and Ni in the mill feed occurred primarily as 1:1 molar ratio arsenides such as niccolite and gersdorffite. Arsenic and Ni concentrations in the tailings were also measured at a near 1:1 molar ratio. Mill process records showed that an average of 71% pf the As in the mill feed was solubilized during leaching. SEM analysis suggested that solubilized As is precipitated as Ca2+, Fe3+ and Ni2+ arsenates during the neutralization process. Mill records indicated that 17,000 tonnes of As were discharged to the TMF of which approximately 88% was as arsenates and 12% as primary arsenides. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 25]
机译:Rabbit Lake U矿的矿山尾矿管理设施(TMF)位于加拿大萨斯喀彻温省北部。尾矿体长约425 m x宽300 m,中心约91 m厚。进行了TMF的调查,从深处收集尾矿样品,以定量确定尾矿中As和Ni相对于矿石类型的分布,并评估As和Ni相对于尾矿矿物学的分布。尾矿体由交替的冰层,冷冻的尾矿和未冻结的尾矿组成,其质地从泥浆到坚硬的粉砂。尾矿中的固体主要由石英(16-36%),硫酸钙(0.3-54%)和伊利石(3%和14%)组成。尾矿中的砷和镍浓度在深度上显示出相似的模式,这与磨粉厂进料中砷和镍浓度的历史变化密切相关。矿体的矿物学表明,磨机进料中的砷和镍主要以摩尔比为1:1的砷化物(如烟碱和硅藻土)出现。还以接近1:1的摩尔比测量了尾矿中的砷和镍浓度。磨机过程记录显示,在浸出过程中,平均溶解了磨机进料中71%的As。 SEM分析表明,在中和过程中,可溶解的As以Ca2 +,Fe3 +和Ni2 +砷的形式沉淀出来。造纸厂的记录表明,有17,000吨的As排放到TMF中,其中约88%是砷,而12%是初级砷。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:25]

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