Jiang Yimin, Wang Zhenyi, Jin Xiaoliang, Wang Yalei
School of Architectural Engineering, Zhengzhou University of Industrial Technology, Zhenzhou, 451100, China.
Department of Civil Engineering, Shanghai University, Shanghai, 200444, China.
Heliyon. 2024 Mar 3;10(5):e27385. doi: 10.1016/j.heliyon.2024.e27385. eCollection 2024 Mar 15.
In order to investigate the acoustic emission (AE) features of rocks in different (medium and strong) rockburst areas, the Sangzhuling Railway Tunnel granite in China was taken as an example, the mineral composition of rocks in different rockburst areas was analyzed by using XRD (X-ray diffraction) method. The Original rock cores of different rockburst areas were processed into standard rock specimens (diameter 50 mm, height 100 mm) in different directions (transverse, oblique and longitudinal). AE feature parameters (event number, ringing count and energy) of standard rock specimens during indoor uniaxial compression test were obtained by using AE technique. The variation law of AE feature parameters of rocks in different rockburst grade areas was then analyzed. The AE features of failure precursor of rocks in different rockburst areas were therefore discussed. It shows that compared with rocks in medium rockburst area, the content of quartz and feldspar of rocks in strong rockburst area is high, while the content of biotite is low; the rock in the strong rock burst area released more energy during the failure process with about 2-3 times that of the rock in the medium rock burst area; the cumulative ringing curve of rock in medium burst area is a stepped type, while the cumulative ringing curve of rock in strong burst area is the smoothed type; the end of the second and first AE quiet period may be regarded as the failure precursor of rocks in medium and strong rockburst area, respectively. The results presented herein are important for understanding the mechanisms of rockburst.
为了研究不同(中强)岩爆区域岩石的声发射(AE)特征,以中国桑珠岭铁路隧道花岗岩为例,采用XRD(X射线衍射)方法分析了不同岩爆区域岩石的矿物成分。将不同岩爆区域的原始岩芯加工成不同方向(横向、斜向和纵向)的标准岩石试件(直径50mm,高100mm)。利用声发射技术获得了标准岩石试件在室内单轴压缩试验过程中的声发射特征参数(事件数、振铃计数和能量)。进而分析了不同岩爆等级区域岩石声发射特征参数的变化规律。因此,探讨了不同岩爆区域岩石破坏前兆的声发射特征。结果表明,与中岩爆区域的岩石相比,强岩爆区域岩石的石英和长石含量较高,而黑云母含量较低;强岩爆区域的岩石在破坏过程中释放的能量更多,约为中岩爆区域岩石的2 - 3倍;中岩爆区域岩石的累积振铃曲线为阶梯型,而强岩爆区域岩石的累积振铃曲线为平滑型;第二和第一声发射平静期的结束分别可视为中、强岩爆区域岩石的破坏前兆。本文给出的结果对于理解岩爆机制具有重要意义。