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井下泥石流物理模拟研究
引用本文:王越,明世祥,周光辉,刘志伟.井下泥石流物理模拟研究[J].中国矿业,2012,21(Z1):512-516.
作者姓名:王越  明世祥  周光辉  刘志伟
作者单位:北京科技大学土木与环境工程学院;武钢矿业有限责任公司金山店铁矿
摘    要:通过对金山店铁矿井下泥石流的调查分析,按比例建造物理实验模型并在每个分层放置一定数量的标记颗粒,以连续出矿的方式来模拟井下泥石流的发生,进而推测其成因以及形成过程,与此同时记录出矿时标记颗粒位置的变化情况,借此来观察泥石流发生的影响范围。然后利用Surfer软件来粗略的绘制出井下泥石流发生时不同分层的黄土渗入界限,为泥石流的预警提供一定的依据。

关 键 词:井下泥石流  形成过程  物理模拟

Research on physical simulation of underground debris flow
WANG Yue,MING Shi-xiang,ZhOU Guang-hui,LIU Zhi-wei.Research on physical simulation of underground debris flow[J].China Mining Magazine,2012,21(Z1):512-516.
Authors:WANG Yue  MING Shi-xiang  ZhOU Guang-hui  LIU Zhi-wei
Affiliation:1.School of Civil and Environment Engineer,University of Science and Technology Beijing,Beijing 100083,China;2.Jinshandian Iron Mine,Wuhan Iron and Steel(Group)Corp.,Daye 435100,China)
Abstract:Through the investigation and analysis of the underground debris flow in Jinshandian Iron Mine,a simulation model of physical experiment is built in proportion,and some marked particles are placed in every layer.In order to simulate the underground debris flow and conjecture its cause and formation process,the continuous drawing is adopted,at the same time the underground debris flow’s range of influence can be observed by recording the position changes of the marked particles.And then Surfer software can roughly draw the loess ’s infiltration boundary in every layer,and this can provide basis for the early warning of the underground debris flow.
Keywords:underground debris flow  formation process  physical simulation
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