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The effects of weathering and diagenetic processes on the geochemical stability of uranium mill tailings

机译:风化和成岩作用对铀矿尾矿地球化学稳定性的影响

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摘要

Uranium mill tailings from the Ranger mine, located in the Alligator Rivers Region of theNorthern Territory, Australia, were examined to assess the effects of weathering and diagenesison their long-term geochemical stability. Run of mill uranium tailings are a complex heterogeneous mixture of lithogenic ( primary gangue minerals and weathering products ) andsecondary ( components that form during milling ) minerals, residual process chemicals and biogenic ( products of biological activity ) phases. Following transfer to the tailings storage facility, post depositional reactions alter the mineralogical and hydrochemical characteristics of the tailings solids and pore waters in accordance with weathering and diagenetic processes.In this thesis, a detailed examination of tailings cores and pore waters, kinetic column test work and geochemical modelling was combined with results from earlier studies to examine the key processes governing the geochemical stability of the Ranger tailings. Conclusions drawn fromthe work clearly demonstrates that the solid state speciation and mobility of metals andradionuclides in the tailings pile are governed by the processes of oxidative dissolution ofsulfide minerals, weathering of phyllosilicates and organic matter diagenesis. The processes arespatially dependent, evolve over time and are influenced by the following key factors :1. Tailings water content or degree of saturation ;2. The nature and content of organic matter in the tailings ;3. Redox potential of the tailings solid - pore water interface ; and4. The specific reactivity of precursor minerals ( primary / secondary ) from the millingprocess and pore water solutes.Combined, these processes lead to the formation of authigenic minerals, which control thesolubility of pore water constituents. These mechanisms will also have a profound impact onthe long-term geochemical stability of the tailings pile and, as such, will need to be taken into account in the design, management and closure of the final tailings repositories at the Ranger site.
机译:检查了位于澳大利亚北部领土鳄鱼河地区的游侠矿的铀厂尾矿,以评估风化作用和成岩作用对其长期地球化学稳定性的影响。碾磨铀尾矿是一种复杂的非均质混合物,包括成岩(主要的脉石矿物和风化产物)和次生的(碾磨过程中形成的成分)矿物,残留的加工化学品和生物(生物活性的产物)相。转移到尾矿存储设施后,沉积后的反应会根据风化和成岩作用改变尾矿固体和孔隙水的矿物学和水化学特性。本文详细研究了尾矿的岩心和孔隙水,动力学柱测试工作并将地球化学模型与早期研究的结果相结合,以研究控制游骑兵尾矿地球化学稳定性的关键过程。这项工作得出的结论清楚地表明,尾矿堆中金属和放射性核素的固态形态和迁移率受硫化物矿物的氧化溶解,层状硅酸盐的风化和有机质成岩作用的过程控制。这些过程是空间相关的,随着时间的推移而发展,并受到以下关键因素的影响:1。尾矿中的水含量或饱和度; 2。尾矿中有机质的性质和含量; 3。尾矿固-孔水界面的氧化还原势;和4。研磨过程中的前体矿物(主要/次要矿物)与孔隙水溶质的比反应性。这些过程共同导致自生矿物的形成,从而控制孔隙水成分的溶解度。这些机制还将对尾矿桩的长期地球化学稳定性产生深远影响,因此,在流浪者基地的最终尾矿储存库的设计,管理和关闭中需要考虑这些因素。

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    Sinclair, Gregory;

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  • 年度 2004
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  • 原文格式 PDF
  • 正文语种 en
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