摘要
研究区域采区内裂隙水发育,分布变化较快,地下水变化较为复杂,并且采坑边坡已有多处滑塌破坏发生,增加了后期边坡治理的难度。利用高密度电法和地质雷达对9个断面进行勘探观察。所勘探区下部视电阻率较低存在地下裂隙水,且地下多板岩破碎带以及断层破碎带。
In the study area, the development of fissure water in the mining area, the change of the distribution is faster, the change of groundwater is more complex, and the slope of the mining pit has been destroyed, which increases the difficulty of the slope treatment. The use of high-density resistivity method and geological radar to do 9 sections of exploration and observation. By means of the above method, the underground fissure water is lower in the lower part of the exploration area, and the underground slate fracture zone and the fault fracture zone are formed.
出处
《煤炭技术》
北大核心
2017年第10期90-92,共3页
Coal Technology
基金
内蒙古科技大学创新项目基金(2015XYPYL03)
内蒙古科技大学产学研合作培育基金(PY-201406)
关键词
边坡
高密度电法
地质雷达
渗水
slope
high-density resistivity method
geological radar
water percolation
