Chen Zeng, Wang Ping, Shi Feng
BGRIMM Technology Group, Building 23, Zone 18 of ABP, No. 188, South 4th Ring Road West, Beijing, 100160, People's Republic of China.
China-South Africa Joint Research Center for Development and Utilization on Mineral Resources, Beijing, 102628, People's Republic of China.
Sci Rep. 2023 Oct 20;13(1):17961. doi: 10.1038/s41598-023-45276-z.
Understanding the evolution mechanism of cracks helps to evaluate the behavior and performance of rock masses and provides a theoretical basis for the mechanism of crack propagation and instability. For this purpose, a rock mechanics testing system and an acoustic emission monitoring system were used to conduct acoustic emission positioning experiments on coal samples under uniaxial compression. According to clustering theory, the distribution pattern of microcracks and the dynamic evolution process of multiple cracks were studied. Subsequently, the reasons for the change in the spatio-temporal entropy (H) and fractal dimension (D) of a single crack were revealed. The research results show that microcracks present a statistical equilibrium distribution, the Gaussian distribution model is applicable to cluster crack distribution patterns, and a machine learning method can effectively identify cracks. The fractal dimension reflects the spatial characteristics of three-dimensional elliptical cracks, and low-dimensional cluster cracks are more likely to develop into macroscopic cracks. The change of H is related to the formation process of cracks, and an abnormal H (sudden increase and sudden decrease) could provide precursor information for the instability of coal samples. This research provides a new method to study crack distributions and formations and shows the competitiveness of the method in evaluating the damage state of coal.
了解裂纹的演化机制有助于评估岩体的行为和性能,并为裂纹扩展和失稳机制提供理论依据。为此,采用岩石力学试验系统和声发射监测系统对煤样进行单轴压缩下的声发射定位实验。依据聚类理论,研究了微裂纹的分布模式和多条裂纹的动态演化过程。随后,揭示了单条裂纹时空熵(H)和分形维数(D)变化的原因。研究结果表明,微裂纹呈现统计平衡分布,高斯分布模型适用于簇状裂纹分布模式,机器学习方法能有效识别裂纹。分形维数反映三维椭圆形裂纹的空间特征,低维簇状裂纹更易发展为宏观裂纹。H的变化与裂纹形成过程有关,H的异常(突然增大和突然减小)可为煤样失稳提供前兆信息。本研究为研究裂纹分布和形成提供了一种新方法,并展示了该方法在评估煤体损伤状态方面的竞争力。