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Seawater inrush assessment based on hydrochemical analysis enhanced by hierarchy clustering in an undersea goldmine pit, China

机译:基于层次分析法的水化学分析方法在中国海底金矿井中的海水突涌评估

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摘要

Seawater inrush is deadly to undersea mine and it is very important to accurately assess the connectivity between seawater and the mine pit. With Xinli gold mine area as a case study, following the analysis of geological setting, a detailed hydrogeological survey and sampling were conducted and conservative ions test of mine water samples was carried out in the laboratory. Furthermore, the physical significances of ion concentration and ion ratios, such as Cl~-, γSO_4~(2-)/γCl~- and γNa~+/γCl~-, were checked. The test data analysis, enhanced by the physical significance check and hierarchy clustering analysis, was used to assess the overlying seawater inrush into the mine pit. It was determined that the undersea rock masses in the Xinli mine area bear high-mineralization brine water. The ore-controlling fault gouge and a thin layer of clay in Quaternary block the seepage of overlying seawater into the undersea mine pit to a great extent. The mine water from surrounding rock of the northeast gopher drift is closer to seawater in hydrogeochemical features, which indicates that the connectivity between the northeast of footwall of the ore-controlling fault and seawater is relatively good and should be closely monitored in future production. The mine water from the southwest gopher drift and crosscuts is similar to the brine (salty) water in chemical features, drains the net reserves of brine (salty) water in bedrock fissures and will impose few impacts on production in the near future. This approach is feasible and cost-effective.
机译:海水涌入对海底矿井是致命的,准确评估海水与矿井之间的连通性非常重要。以新里金矿区为例,在对地质环境进行分析之后,进行了详细的水文地质调查和取样,并在实验室进行了矿泉水样品的保守离子测试。此外,检查了离子浓度和离子比(如Cl〜-,γSO_4〜(2-)/γCl〜-和γNa〜+ /γCl〜-)的物理意义。通过物理重要性检查和层次聚类分析增强了测试数据分析,以评估上涌入矿井的海水。经确定,新里矿区海底岩体含有高矿化盐水。第四纪的控矿断层泥和薄层粘土在很大程度上阻止了上覆海水渗入海底矿井。在水文地球化学特征上,东北地鼠漂移的围岩中的矿水更接近海水,这表明控矿断层下盘东北面与海水之间的连通性相对较好,在未来的生产中应密切监测。来自西南地鼠漂移和横切的矿井水在化学特征上类似于盐水(咸水),排走了基岩裂缝中盐水(咸水)的净储量,并且在不久的将来不会对生产造成任何影响。这种方法是可行且具有成本效益的。

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  • 来源
    《Environmental earth sciences》 |2014年第12期|4977-4987|共11页
  • 作者单位

    Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, People's Republic of China;

    Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, People's Republic of China;

    College of Geosciences and Surveying Engineering, China University of Mining and Technology, Beijing 100083, People's Republic of China;

    Key Laboratory of Engineering Geomechanics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, People's Republic of China;

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

    Undersea mining; Hydrochemical features; Brine water; Connectivity; Desulphurization; Water-rock interaction;

    机译:海底采矿;水化学特征;盐水;连接性;脱硫;水岩相互作用;

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