首页> 外文期刊>Science of the total environment >The impact of cemented layers and hardpans on oxygen diffusivity in mining waste heaps A field study of the Halsbrucke lead-zinc mine tailings (Germany)
【24h】

The impact of cemented layers and hardpans on oxygen diffusivity in mining waste heaps A field study of the Halsbrucke lead-zinc mine tailings (Germany)

机译:胶结层和硬壳对采矿废料堆中氧气扩散性的影响Halsbrucke铅锌矿尾矿的现场研究(德国)

获取原文
获取原文并翻译 | 示例
       

摘要

This article reports fibre-optic oxygen measurements on a reactive mine waste heap located in the polymetallic sulphide mine district of Freiberg in south-eastern Germany. The heaped material consists of sulphide-bearing tailings from a processing plant of a lead-zinc mine. Mine waste material was deposited in the water phase after separation of mining ores in a flotation process. The tailing impoundment is partly covered with coarse sand and topsoil. Oxygen profiles were monitored during one year at eleven locations showing different physical and mineralogical compositions. At each location a borehole was drilled where the optic sensors were installed at 2-5 different depths. After installation the oxygen profiles were monitored seven times during one year from 2006-2007 and three to five oxygen profiles at each location were obtained. Oxygen measurements were accompanied by physical, chemical and mineralogical data of the tailing material. Additionally, a detailed mineralogical profile was analysed at a location representative for the central part of the heap, where the cemented layers show lateral continuity. Results showed that cemented layers have a significant influence on natural attenuation of the toxic As and Pb species owing to their capacity of water retention. The measured oxygen profiles are controlled by the zone of active pyrite weathering as well as by the higher water content in the cemented layers which reduces gaseous atmospheric oxygen supply. In contrast, gypsum bearing hardpans detected at three other locations have no detectable influence on oxygen profiles. Furthermore, the grain size distribution was proved to have a major effect on oxygen diffusivity due to its control on the water saturation. Temporal changes of the oxygen profiles were only observed at locations with coarse sediment material indicating also an important advective part of gas flux.
机译:本文报告了位于德国东南部弗赖贝格(Freiberg)多金属硫化物矿区的反应性矿山废料堆上的光纤氧气测量结果。堆积的物料由铅锌矿加工厂的含硫尾矿组成。在浮选过程中分离矿砂后,矿山废料沉积在水相中。尾矿库部分被粗砂和表土覆盖。一年中在十一个位置监测了氧气分布,显示出不同的物理和矿物组成。在每个位置都钻了一个钻孔,将光学传感器安装在2-5个不同的深度。安装后,从2006年至2007年,在一年中对氧气分布进行了七次监测,并在每个位置获得了三到五个氧气分布。氧气测量伴随着尾矿物质的物理,化学和矿物学数据。此外,在代表堆中部的位置分析了详细的矿物学剖面,在该处胶合层显示出横向连续性。结果表明,胶结层由于其保水能力而对有毒As和Pb物种的自然衰减有很大影响。测得的氧分布由活性黄铁矿风化带以及胶结层中较高的水含量控制,这减少了气态大气氧的供应。相反,在其他三个位置检测到的带有石膏的硬质涂层对氧分布没有可检测到的影响。此外,由于其对水饱和度的控制,已证明晶粒尺寸分布对氧扩散率具有主要影响。氧分布的时间变化仅在沉积物较粗的位置观察到,这也是气体通量的重要对流部分。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号