ISSN 1003-8035 CN 11-2852/P

    三点弯曲加载下灰岩临界破裂特征及其失稳前兆识别研究

    Critical fracture behavior and instability precursors of limestone under three-point bending

    • 摘要: 岩溶区域的工程活动中普遍存在着岩体弯曲断裂现象,影响岩体结构完整性及工程安全性,亟需开展岩体弯曲临界破裂特征及其失稳前兆识别研究。文章以灰岩试样为对象,开展岩体三点弯曲试验,并借助声发射(AE, acoustic emission)和数字图像相关方法(DIC,digital image correlation ),提出灰岩三点弯临界破坏前兆的多参数识别方法。研究结果表明:(1)灰岩弯曲破坏呈明显脆断特征,峰值荷载与断裂能随加载速率呈先增后减趋势,在速率为0.05~0.1 mm/min范围内变化较快;(2)声发射信号在不稳定裂纹扩展阶段最为活跃,累计撞击数增加38%以上并达到峰值。在该峰值之后,形成平行于载荷方向的主裂纹。裂纹在加载过程中主要以拉伸裂纹的形式扩展,并伴有一些剪切裂纹;(3)剪切裂纹占比、声发射b值和临界慢化指标可作为识别灰岩弯曲临界破坏预兆的指标,其中剪切裂纹占比具有更大的前兆响应系数和更早的响应时间,可靠性更高。研究对深入认识灰岩弯曲变形破坏特性及指导工程岩体灾变前兆识别具有重要的参考价值。

       

      Abstract: Rock bending fractures are common in engineering activities in karst areas and can affect rock-mass integrity and engineering safety. To investigate the critical fracture behavior of rock masses and identify instability precursors, three-point bending tests were conducted on limestone specimens. Acoustic emission (AE) monitoring and digital image correlation (DIC) were used to develop a multi-parameter method for identifying precursors of critical failure in limestone under three-point bending. The results show that: (1) limestone bending failure exhibits clear brittle-fracture characteristics. Peak load and fracture energy first increase and then decrease with loading rate, and they vary rapidly within the range of 0.05-0.1 mm/min. (2) AE signals are most active during unstable crack propagation, when cumulative hits increase by more than 38% and reach a peak. After this peak, a main crack parallel to the loading direction forms. Cracks propagate mainly as tensile cracks during loading, accompanied by some shear cracks. (3) The shear-crack proportion, AE b-value, and critical-slowing-down index can be used as indicators for identifying precursors of critical bending failure in limestone. Among them, the shear-crack proportion shows a larger precursor response coefficient, an earlier response time, and higher reliability. This study provides an important reference for understanding the bending deformation and failure characteristics of limestone and for identifying disaster precursors in engineering rock masses.

       

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