用户名: 密码: 验证码:
华北型煤矿底板断层突水水文地质分类研究
详细信息    查看官网全文
摘要
华北型煤矿由于特殊的水文地质条件,主要受底板灰岩突水威胁,断层是灰岩突水最重要的突水通道之一。以断层的水文地质特征为主综合考虑突水时空与动态特征,进行底板断层突水水文地质分类,通过统计典型华北型煤矿断层突水实例,进行验证分析。研究成果可以为华北型煤矿底板灰岩突水防治提供借鉴。
Due to special hydro-geological condition,North China-type mines are mainly threatened by water inrush of limestone aquifer of floor.Fault is one of main channels of water inrush.Based on the hydro-geological features of the fault,time-space and dynamic features of water inrush are integrated to classify the hydro-geology of the floor fault.Typical fault water inrush accidents were calculated and verified in North China-type mines.The results could provide guidance to prevent the water inrush of limestone aquifer.
引文
[1]彭苏萍,王金安.承压水体上安全采煤—对拉工作面开采底板破坏机理与突水预测防治[M].北京:煤炭工业出版社,2001
    [2]中国统配煤矿总公司生产局,煤炭科技情报研究所.煤矿水害事故典型案例汇编[G].北京:煤炭科学技术出版社,1992.
    [3]黎良杰.采场底板突水机理的研究[D].徐州:中国矿业大学,1995.
    [4]李白英.预防矿井底板突水的“下三带”理论及其发展与应用[J].山东矿业学院学报,1999,18(4):11-18.
    [5]施龙青,韩进.底板突水机理及预测预报[M].徐州:中国矿业大学出版社,2004.
    [6]王作宇,刘鸿泉.承压水上采煤[M].北京:煤炭工业出版社,1993.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700