首页> 外文期刊>Environmental Geology >An application of a new method in permafrost environment assessment of Muli mining area in Qinghai-Tibet Plateau, China
【24h】

An application of a new method in permafrost environment assessment of Muli mining area in Qinghai-Tibet Plateau, China

机译:一种新方法在青藏高原木里矿区多年冻土环境评价中的应用

获取原文
获取原文并翻译 | 示例
       

摘要

The permafrost environment in the Muli mining area, an opencast mining site in the Qinghai-Tibet Plateau, China, is now undergoing significant degradation because of the ongoing mining activities. The permafrost environment in this mining site had already been evaluated by previous study, in which analytic hierarchy process was applied. Although this method can roughly characterize the permafrost environment of this mining site, it has limitations by being easily affected by man-made factors. In view of this limitation, this study attempts to employ a new method, the catastrophe progression method, to estimate the current stage of the permafrost environment in this mining area. The results show that, by catastrophe progression method, currently the calculated indexes of the permafrost freezing-thawing disintegration, permafrost thermal stability, permafrost ecological fragility, and the permafrost environment are 0.43 (general situation), 0.77 (general situation), 0.71 (bad situation) and 0.83 (general situation), respectively. These values imply that the permafrost environment has been damaged by anthropologic activities to a certain degree and potentially may be further degenerated. However, at this degree, a new equilibrium stage of permafrost environment could be achieved if the current state of environmental degradation is stabilized and treatments are constructed against further damages.
机译:由于正在进行的采矿活动,木里矿区的多年冻土环境是中国青藏高原的一个露天采矿场,目前正处于严重退化之中。先前的研究已经对该矿区的多年冻土环境进行了评估,并应用了层次分析法。尽管这种方法可以粗略地表征该矿场的多年冻土环境,但由于容易受到人为因素的影响,因此存在局限性。鉴于这种局限性,本研究试图采用一种新的方法,即巨灾渐进法,来估算该矿区的多年冻土环境的当前阶段。结果表明,利用突变级数法,目前多年冻土冻融解体,多年冻土热稳定性,多年冻土生态脆弱性和多年冻土环境的计算指标分别为0.43(一般情况),0.77(一般情况),0.71(差)。情况)和0.83(一般情况)。这些值表明,多年冻土环境已受到人类活动的一定程度的破坏,并有可能进一步退化。但是,在这种程度下,如果稳定当前的环境退化状态,并建立应对进一步破坏的措施,则可以实现永久冻土环境的新平衡阶段。

著录项

  • 来源
    《Environmental Geology》 |2011年第3期|p.609-616|共8页
  • 作者单位

    State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, Lanzhou 730000, Gansu, China;

    State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, Lanzhou 730000, Gansu, China School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210093, Jiangsu, China;

    Department of Civil and Environmental Engineering, Michigan Technological University, Houghton, MI 49931-1295, USA;

    State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, Lanzhou 730000, Gansu, China;

    State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences, Lanzhou 730000, Gansu, China;

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

    permafrost environment; catastrophe progression method; catastrophe model; muli mining area in qinghai-tibet plateau; evaluation;

    机译:多年冻土环境;突变级数法;突变模型;青藏高原木里矿区评价;
  • 入库时间 2022-08-18 03:31:25

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