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酸性矿山废水对碳酸盐岩侵蚀的影响
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  • 英文篇名:The effects of acid mine drainage on the erosion of carbonatite in carbonate rocks
  • 作者:夏雨 ; 吴攀 ; 张瑞雪 ; 朱健 ; 王悦竹 ; 宋传孝 ; 李玲
  • 英文作者:XIA Yu;WU Pan;ZHANG Rui-xue;ZHU Jian;WANG Yue-zhu;SONG Chuan-xiao;LI Ling;College of Resources and Environmental Engineering,Guizhou University;Key Laboratory of Process and Control of Mining Environmental Pollution,Colleges and Universities in Guizhou Province;Key Laboratory of Karst Environment and Geohazard, Ministry of Land and Resources, Guizhou University;Institute of Geochemistry,Chinese Academy of Sciences;
  • 关键词:水岩反应 ; 碳酸盐岩 ; 酸性矿山废水 ; 侵蚀速率
  • 英文关键词:water rock interaction;;carbonatite;;acid mine drainage;;erosion rate
  • 中文刊名:STXZ
  • 英文刊名:Chinese Journal of Ecology
  • 机构:贵州大学资源与环境工程学院;贵州省普通高等学校矿山环境污染过程与控制特色重点实验室;贵州大学国土资源部喀斯特环境与地质灾害重点实验室;中国科学院地球化学研究所;
  • 出版日期:2018-06-14
  • 出版单位:生态学杂志
  • 年:2018
  • 期:v.37;No.299
  • 基金:国家自然科学基金委员会-贵州省人民政府喀斯特科学研究中心项目(U1612442);; 贵州省科学技术基金(黔科合J字[2011]2353号;; 贵州省公益性、基础性地质工作项目(黔国土资地环函[2014]23);; 贵州省学科建设项目(黔学位合字ZDXK[2016]11);; 贵州省社发攻关项目(黔科合SY字[2014]3042号)资助
  • 语种:中文;
  • 页:STXZ201806013
  • 页数:6
  • CN:06
  • ISSN:21-1148/Q
  • 分类号:101-106
摘要
定量研究了酸性矿山废水对7种不同时代碳酸盐岩的侵蚀速率,以筛选出合适的被动处理填料。结果表明:酸性矿山废水对碳酸盐岩的60 d平均侵蚀速率为4.88×10~(-4)g·cm~(-2)·d~(-1),是普通岩溶水侵蚀速率的10倍以上,其中摆佐组灰质中晶白云岩的侵蚀速率高于其他灰岩;采用扫描电镜和能谱仪对岩石表面物质的微观形貌和成分分析,结果表明,不同时代的岩石表面所生成的铁氧化物均为纤铁矿;岩石表面的硫酸钙结晶速率是控制水岩反应速率的关键性因素之一,而岩石中溶出的Mg~(2+)是影响硫酸钙结晶速率的重要因素。
        We quantified the effects of acid mine drainage on the erosion rate of seven carbonate rocks with different ages,to screen for appropriate passive packing. The results showed that the mean erosion rate of carbonate rocks in response to acid mine drainage was 4.88×10~(-4) g·cm~(-2)·d~(-1) in 60 days,which is at least ten times faster than karst water erosion. The calcite Mesocrystalline dolomite in Baizuo Formation showed higher erosion rate than other limestones. The microstructure and the composition of rock surface material were measured by Scanning Electron Microscope and Energy Dispersive Spectrometer. It was found that the iron oxides on the surface of rocks from different ages were lepidocrocite. The crystallization rate of calcium sulfate on rock surface was one of the key factors controlling the erosion rate of carbonatite in carbonate rocks.Additionally,the dissolution of magnesium carbonate was an important factor driving the crystallization rate of calcium sulfate.
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