周瑞光, 成彬芳, 叶贵钧, 武强. 2000: 断层破碎带突水的时效特性研究. 工程地质学报, 8(4): 411-415.
    引用本文: 周瑞光, 成彬芳, 叶贵钧, 武强. 2000: 断层破碎带突水的时效特性研究. 工程地质学报, 8(4): 411-415.
    ZHOU Rui guang, CHENG Bin fang, YE Gui jun, Wu Qiang. 2000: TIME EFFECT OF WATER BURSTING IN FAULT RUPTURE ZONE. JOURNAL OF ENGINEERING GEOLOGY, 8(4): 411-415.
    Citation: ZHOU Rui guang, CHENG Bin fang, YE Gui jun, Wu Qiang. 2000: TIME EFFECT OF WATER BURSTING IN FAULT RUPTURE ZONE. JOURNAL OF ENGINEERING GEOLOGY, 8(4): 411-415.

    断层破碎带突水的时效特性研究

    TIME EFFECT OF WATER BURSTING IN FAULT RUPTURE ZONE

    • 摘要: 突水属重大地质灾害 ,一直引起人们的关注。本文认为突水瞬间表现一个综合效应下的瞬时地质事件。突水前表现一个与时间有关的地质作用过程。事件与过程都受多因素的影响 ,而且工程地质作用过程和突水瞬间与岩体由弹性变形 -阻尼变形 -常速流动变形 -加速流动变形相对应。突水具有时效特征。

       

      Abstract: WT5,5BZBy study of the mechanical characteristics of fault rocks, the authors consider that the water bursting is an instant aneous geologic event under a combined effect. The process before water bursting acts as a geological activation related to time of exploitation. The geological process and the instancy of water bursting correspond to multi factors: rockmass elastic deformation, damping deformation, steady state flow deformation, and accelerated flow deformation. So the water bursting has time effect characteristic.

       

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