杨小刚, 刘洋, 张壮路. 数值模拟在回坡底煤矿底板突水防治中的应用[J]. 煤田地质与勘探, 2008, 38(5): 58-61.
引用本文: 杨小刚, 刘洋, 张壮路. 数值模拟在回坡底煤矿底板突水防治中的应用[J]. 煤田地质与勘探, 2008, 38(5): 58-61.
YANG Xiao-gang, LIU Yang, ZHANG Zhuang-lu. Numerical simulation in the floor inrush water control of Huipodi coal mine[J]. COAL GEOLOGY & EXPLORATION, 2008, 38(5): 58-61.
Citation: YANG Xiao-gang, LIU Yang, ZHANG Zhuang-lu. Numerical simulation in the floor inrush water control of Huipodi coal mine[J]. COAL GEOLOGY & EXPLORATION, 2008, 38(5): 58-61.

数值模拟在回坡底煤矿底板突水防治中的应用

Numerical simulation in the floor inrush water control of Huipodi coal mine

  • 摘要: 随着煤矿开采深度的不断增加,将面临高承压水的严重威胁,带压开采已成为深部煤炭资源开采的主要方式。应用RFPA2D-Flow系统对煤层底板破坏深度进行了数值模拟,得出了回坡底煤矿采煤工作面煤层底板岩层的破坏深度约为12 m;同时,当回采到110 m处时,自切眼向掘进方向50~80 m处出现漏斗状底板破坏区,该破坏区将可能导通底部奥灰水,使煤层底板发生突水。

     

    Abstract: As the coal mining depth is increasing gradually,the mine will face the serious threat of the high pres-sure water,mining above aquifer has already become main way in which the deep coal resources are mined.The paper employs RFPA2D-Flow analytical system to simulate the coal seam floor destructive depth,and educes the 12 m destructive depth of the coal seam floor of mining working face,meanwhile,when coal extraction to 110 m,there is a tundish form to appear in 50 ~80 m range from cutting to driving direction,the destructive area will switch into conduction Ordovician period calcareousness water,and make inrush water from coal seam floor take place.

     

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