侯志强, 袁瑞甫, 李长洪, 王宇, 魏晓. 直接拉伸荷载下大理岩和砂岩的Kaiser效应与频谱特性分析[J]. 煤炭学报, 2019, 44(S1): 41-51. DOI: 10.13225/j.cnki.jccs.2018.1463
引用本文: 侯志强, 袁瑞甫, 李长洪, 王宇, 魏晓. 直接拉伸荷载下大理岩和砂岩的Kaiser效应与频谱特性分析[J]. 煤炭学报, 2019, 44(S1): 41-51. DOI: 10.13225/j.cnki.jccs.2018.1463
HOU Zhiqiang, YUAN Ruifu, LI Changhong, WANG Yu, WEI Xiao. Analysis of Kaiser effect and frequency spectrum of marble and sandstone under direct tensile load[J]. Journal of China Coal Society, 2019, 44(S1): 41-51. DOI: 10.13225/j.cnki.jccs.2018.1463
Citation: HOU Zhiqiang, YUAN Ruifu, LI Changhong, WANG Yu, WEI Xiao. Analysis of Kaiser effect and frequency spectrum of marble and sandstone under direct tensile load[J]. Journal of China Coal Society, 2019, 44(S1): 41-51. DOI: 10.13225/j.cnki.jccs.2018.1463

直接拉伸荷载下大理岩和砂岩的Kaiser效应与频谱特性分析

Analysis of Kaiser effect and frequency spectrum of marble and sandstone under direct tensile load

  • 摘要: 利用微机控制电子万能试验机,对2种大理岩和1种砂岩进行直接拉伸条件下的循环加卸载试验,分析了岩石损伤破坏全过程的声发射特性和频谱特征。结果表明:循环加卸载试验中,3种岩石表现出明显的Kaiser效应,低应力时岩石记忆滞后,高应力时岩石记忆缓慢提前。随着循环次数的增多,岩石声发射的剧烈程度在逐渐增加,Felicity比值逐渐单调下降,弹性模量逐渐减小。通过比较Felicity比值与数字“1”的大小关系,可判断该岩石所处应力状态强弱。Felicity比值远大于1时,表明承受载荷远离承载极限;Felicity比值接近1或小于1时,表明岩石承受载荷接近承载极限,所处应力状态越接近破坏应力。岩石拉伸断裂过程中,声发射信号始终存在着低频、中频和高频信号,且低频信号占比大于中频和高频信号。通过声发射信号频谱特征分析,岩石拉伸破裂存在4种声发射微观机制:第1种为晶间滑移、颗粒摩擦引起的摩擦型声发射机制,信号能量较低,主频较小; 第2种为新裂隙扩张引起的破裂型声发射机制,信号能量中等,主频较高; 第3种为裂隙微弱摩擦引起的摩擦型声发射机制,信号能量较低,主频中等; 第4种为宏观裂隙扩张与摩擦的混合型声发射机制,信号能量较大,信号频带较宽,高频与低频信号共存。本文研究获得的裂纹扩展声发射特征为岩石拉伸破坏机制和监测提供了依据。

     

    Abstract: The cyclic loading and unloading tests of two kinds of marble and one kind of sandstone were carried out under the direct tension condition by using the microcomputer controlled electronic universal testing machine, and the acoustic emission characteristics and spectrum characteristics of rock damage were analyzed.The results show that in the cyclic loading and unloading tests, three kinds of rocks show obvious Kaiser effect, the rock memory lags behind at low stress and the rock memory is slowly ahead at high stress.As the number of cycles increases, the AE intensity of rock gradually increases, Felicity ratio gradually decreases, and the elastic modulus gradually decreases.By comparing the relationship between the Felicity ratio and the number "1", the stress state of rock can be judged.When the Felicity ratio is far greater than 1, it indicates that the rock loading is far from the bearing limit, and when the Felicity ratio is close to 1 or less 1, it indicates that the rock loading is close to the bearing limit and the stress state is closer to the failure stress.In the process of rock tensile fracture, AE signals always have low-frequency, medium-frequency and high-frequency signals, and the proportion of low-frequency signals is greater than that of medium-frequency and high-frequency signals.By analyzing the spectral characteristics of AE signals, four AE microscopic mechanisms exist in the tensile fracture of rocks.The first type is the frictional acoustic emission mechanism caused by intergranular slip and particle friction, with small signal energy and low main frequency.The second type is the ruptured acoustic emission mechanism caused by the expansion of new cracks, with medium signal energy and high main frequency.The third type is the frictional acoustic emission mechanism caused by little cracks' friction, with low signal energy and medium main frequency.The fourth type is the mixed acoustic emission mechanism of macroscopic crack expansion and friction, with large signal energy wide signal frequency band, which the high frequency and low frequency signals coexist.The AE characteristics of crack propagation obtained in this paper provide a basis for the failure mechanism and monitoring of rock under tension condition.

     

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