不同岩石单轴压缩破裂全过程声发射序列分形特征研究
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  • 英文篇名:Fractal Feature of Acoustic Emission Sequences of Different Rocks Unloading Failure Process under Uniaxial Compression
  • 作者:王创业 ; 常新科 ; 刘沂琳
  • 英文作者:WANG Chuangye;CHANG Xinke;LIU Yilin;School of Civil and Resource Engineering, University of Science and Technology Beijing;Institute of Mining Engineering, Inner Mongolia University of Science and Technology;
  • 关键词:岩石力学 ; 声发射 ; 破裂失稳 ; 分形
  • 英文关键词:rock mechanics;;acoustic emission(AE);;failure instability;;fractal
  • 中文刊名:ZGWU
  • 英文刊名:China Tungsten Industry
  • 机构:北京科技大学土木与资源工程学院;内蒙古科技大学矿业研究院;
  • 出版日期:2018-10-26
  • 出版单位:中国钨业
  • 年:2018
  • 期:v.33;No.267
  • 基金:国家自然科学基金项目(51464036);; 内蒙古自治区自然科学基金项目(2018MS05037)
  • 语种:中文;
  • 页:ZGWU201805004
  • 页数:8
  • CN:05
  • ISSN:11-3236/TF
  • 分类号:26-33
摘要
通过对青砂岩和花岗岩两种岩性岩石的单轴压缩声发射试验,获取岩石破裂全过程的基本力学特征及声发射时域特征参数,观察两种岩石破裂时的破坏情况,着重对比了两种岩石的声发射事件率及能率时域特征,并探讨了声发射事件率及能率的分形特征。试验结果表明:声发射事件率及能率均可很好地描述岩石破裂损伤的整个过程,青砂岩事件率变化特征有明显的"上升期"和"下降期",花岗岩则无明显变化特征,两种岩石能率变化特征均存在两个"活跃期(Ⅰ,Ⅱ)"和一个"缓慢释放期";青砂岩事件率分形特征与花岗岩差异明显,相比较花岗岩而言,青砂岩分形维数D值存在多处转折点;能率分形特征,两种岩石较为相似,分形维数D值均表现为随着加载应力比的增大而波动增加,在试样破裂前又突降至最低值。
        Through the uniaxial compression acoustic emission test of two lithologic rocks of blue sandstone and granite, the basic mechanical characteristics and acoustic emission time domain characteristic parameters of rock failure process are obtained. By observing the failure of two kinds of rocks during fracture, the time domain characteristics of AE event rate and energy rate of two kinds of rocks are compared emphatically, and the fractal characteristics of AE event rate and energy rate are discussed. The experimental results show that the acoustic emission event rate and energy rate can well describe the whole process of rock rupture damage. The variation characteristics of the blue sandstone event rate have obvious "rise period" and "down period", and the granite has no obvious change characteristics. There are two"active periods(I, II)"and a"slow release period"for the variation of rock energy rate. The fractal characteristics of the sandstone event rate are significantly different from those of granite. Compared with granite, there are many turning points in the fractal dimension of blue sandstone fractal dimension. The fractal characteristics of the energy rate are similar. The D values of the fractal dimension are all fluctuated with the increase of the load stress ratio, and then drop to the lowest value before the sample breaks.
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