采矿与安全工程学报 ›› 2014, Vol. 31 ›› Issue (6): 888-895.

• 论文 • 上一篇    下一篇

断层影响下底板采动临界突水水压解析解

  

  1. 1.安徽理工大学地球与环境学院,安徽 淮南 232001; 2.中国矿业大学(北京)煤炭资源与安全开采国家重点实验室,北京 100083
  • 出版日期:2014-11-15 发布日期:2014-12-01
  • 作者简介:鲁海峰(1983—),男,安徽省合肥市人,博士,讲师,从事矿井水文地质与工程地质方面的研究。 E-mail:luhaifeng7571@126.com Tel:13625547128
  • 基金资助:

    国家自然科学基金项目(51174256);煤炭资源与安全开采国家重点实验室开放基金项目(SKLCRSM13KFB01);国家大学生创业创新训练项目(201210361006);安徽理工大学青年教师科学研究项目(QN201308)

Analytical solution of critical water inrush pressure of mining floor affected by fault

  • Online:2014-11-15 Published:2014-12-01

摘要: 考虑采动矿压和煤层隔水底板下承压含水层水压的联合作用,推导出断层影响下底板突水的水压力解析式。运用试算法搜索出最危险底板剪切破裂面及临界突水水压。在此基础上,分析了工作面开切眼到断层带距离、断层倾角、工作面推进方向以及侧压力系数等因素对底板临界突水水压的影响规律。算例显示,临界突水水压随工作面开切眼到断层带距离的加大而减小;随着断层倾角的减小,临界突水水压先减小后增加,但当断层倾角小于某一临界角度时,底板不沿断层面破坏;由断层下盘向上盘推进时的临界突水水压较由断层上盘向下盘推进时大,但无论工作面的推进方向如何,临界突水水压皆随着工作面过断层带距离的加大而逐步减小;随着侧压力系数的加大,临界突水水压先增大后逐渐减小。实例应用表明,临界突水水压计算判别结果与实际情况吻合。

关键词: 极限平衡理论, 底板突水, 断层, 临界突水水压

Abstract: Considering the combined effect of mine pressure and water pressure of confined aquifer under the water-resisting floor, water pressure expression of floor water inrush has been derived. And then the most dangerous shear fracture plane and the critical pressure of water inrush have been obtained by trial calculation. Based on the proposed analytical solutions, the effect law of distance between cut-hole and fault zone, fault dip, advancing direction of face and lateral pressure coefficient on critical pressure of water inrush have been analyzed. The results show that the critical pressure of water inrush decreases gradually with the increase of distance between cut-hole and fault zone. With the decrease of fault dip, the critical pressure of water inrush decreases firstly, and then increases gradually. However, floor failure is not along the fault surface any more when the fault dip is less than a certain critical angle. When the working face advances from the lower wall of fault to the upper, the critical pressure of water inrush is higher than the opposite, namely the working face advances from the upper of fault to the lower. But no matter in what direction the working face advances, the critical pressure is reducing with the increase of distance from working face to the fault zone gradually. The critical pressure of water inrush increases first and then decreases with the increase of lateral pressure coefficient. The application demonstrates that the calculation results of the critical pressure accord with the actual situation.

Key words: limit equilibrium theory, floor water inrush, fault, critical pressure of water inrush