黎良杰, 钱鸣高, 殷有泉. 采场底板突水相似材料模拟研究[J]. 煤田地质与勘探, 1997, 25(1): 33-36.
引用本文: 黎良杰, 钱鸣高, 殷有泉. 采场底板突水相似材料模拟研究[J]. 煤田地质与勘探, 1997, 25(1): 33-36.
Li Liangjie, Qian Minggao, Yin Youquan. RESEARCH ON THE TESTS OF WATER-INRUSH FROM FLOOR SIMULATED BY SIMILAR MATERIALS[J]. COAL GEOLOGY & EXPLORATION, 1997, 25(1): 33-36.
Citation: Li Liangjie, Qian Minggao, Yin Youquan. RESEARCH ON THE TESTS OF WATER-INRUSH FROM FLOOR SIMULATED BY SIMILAR MATERIALS[J]. COAL GEOLOGY & EXPLORATION, 1997, 25(1): 33-36.

采场底板突水相似材料模拟研究

RESEARCH ON THE TESTS OF WATER-INRUSH FROM FLOOR SIMULATED BY SIMILAR MATERIALS

  • 摘要: 利用相似材料模拟试验,模拟了采场底板突水机理。实验表明,在无断层构造条件下,底板在承压水作用下呈O-X型破坏,并且在O与X的交点处最容易产生突水通道;在有断层构造条件下,断层突水的的实质是在承压水作用下断层两盘的关键层向上产生相对移差。当断层越易产生最大位移差时,越容易突水;在突水的同时还伴随着断层带充填物的冲刷。

     

    Abstract: The mechanism of water-inrush from coal floor in longwall face is simulated by the similar material tests.The results show that the O-X type failure will occur in the floor without fault but under the water-pressure of the confined aquifer,and the passage of water-inrush will be most easily formed at the point of intersection of "O" and "X";The reason for water-inrush through fault is that the difference of upward relative displacements happens at the key strata of two sides of fault under the confined water pressure,and the more easily the most difference of displacement occurs,the more easily the accident of water-inrush happens,and the fill in the fault zone is eroded by the confined water while the auident of water-inrush occurs.

     

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