期刊导航

论文摘要

单轴压缩条件下花岗岩声发射事件空间分布的分维特征研究

Fractal Study on Spatial Distribution of Acoustic Emission Events of Granite Specimens Under Uniaxial Compression

作者:裴建良(四川大学水电学院);刘建锋(四川大学 水利水电学院);张茹(四川大学 水利水电学院);尹贤刚(四川大学 水利水电学院;长沙矿砂研究院)

Author:Pei Jianliang();Liu Jianfeng(School of Water Resource and Hydropower, Sichuan Univ.);Zhang Ru(School of Water Resource and Hydropower, Sichuan Univ.);Yin Xiangang(School of Water Resource and Hydropower, Sichuan Univ.;Changsha Inst. of Mining Research)

收稿日期:2009-10-30          年卷(期)页码:2010,42(6):51-55

期刊名称:工程科学与技术

Journal Name:Advanced Engineering Sciences

关键字:岩石破坏;声发射;分维模型;空间分布

Key words:rock failure; Acoustic Emission (AE); fractal model; spatial distribution

基金项目:国家重点基础研究发展计划资助项目(2010CB226802;2011CB201201);国家自然科学基金重点资助项目(50639100);国家自然科学基金面上资助项目(50974091)

中文摘要

基于声发射事件空间分布的柱覆盖分形模型,利用MTS815 Flex Test GT岩石力学试验系统和PCI-2声发射(AE)3维定位实时监测系统,对瀑布沟水电站地下厂房花岗岩单轴压缩损伤破坏过程中声发射事件空间分布的分形特征进行了研究。结果表明,声发射事件随应力增加逐渐活跃,加载初期声发射数量较少,应力接近峰值强度时,声发射事件累计数曲线呈指数上升;声发射事件的空间分布随应力增加是一个降维过程,其空间分维D在3~2内变化,峰值强度时,其值最小;弹性阶段后期,岩石内部微破裂开始向破坏面集聚,声发射空间分维D下降幅度明显增大;声发射空间分维恰当地表征了声发射事件空间分布的复杂程度。研究结论揭示了岩石声发射事件空间分布的分形特征,室内试验结果与文献对岩爆研究结果相吻合,可为现场监测应用提供理论指导。

英文摘要

The granite samples collected from the underground powerhouse of Pubugou Hydropower Station were tested on MTS815 Flex Test GT rock mechanics test system under uniaxial compression condition. During the whole test process, the acoustic emission events were monitored by PCI-2 based AE system. Based on the cylinder-covering spatial fractal model, the spatial distribution features of AE events and the changing law of spatial fractal dimensions at different stress levels were studied. The experimental results showed that there are little AE events at low stress stage. The AE events become gradually active as the stress increasing and the cumulative number of AE events raises exponentially when the stress is close to the peak strength. The fractal dimension values gradually decrease from 3 to 2 with the increase of stress and reach the minimum value when the loading is equal to the peak strength. At the later stage of elastic deformation, the spatial fractal dimension values decrease obviously with the microcracks in granite sample gathering in the nearby field of failure surface. The complexity of AE events spatial distribution can be characterized properly by its fractal dimension, and these results agree with the research results of rock burst in references.

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