Failure Characteristic Analysis and Warning Method of Sandstone Based on Catastrophe Theory

被引:2
|
作者
Zhang, Erhui [1 ]
Zhou, Baokun [2 ]
Yang, Lei [2 ]
Li, Changfeng [2 ]
Li, Ping [3 ,4 ]
机构
[1] China Univ Min & Technol Beijing, Sch Emergency Management & Safety Engn, Ding 11,Xueyuan Rd, Beijing 100083, Peoples R China
[2] China Univ Min & Technol Beijing, Sch Energy & Min Engn, Beijing 100083, Peoples R China
[3] Capital Univ Econ & Business, Sch Management & Engn, Beijing 100071, Peoples R China
[4] Beijing Qidi Registered Safety Engineer Off Co LTD, Beijing 101601, Peoples R China
关键词
Damage evolution; Multi-field monitoring; Energy evolution; Cusp catastrophe theory; Early warning; ACOUSTIC-EMISSION; INSTABILITY; ROCK; IDENTIFICATION; EVOLUTION; FRACTURE; MODEL;
D O I
10.1007/s42461-023-00830-1
中图分类号
TF [冶金工业];
学科分类号
0806 ;
摘要
A uniaxial compression experiment was conducted on standard sandstone specimens to explore the sandstone's mutation characteristics and early warning interval during deformation and failure. Meanwhile, acoustic emission (AE) and digital image correlation (DIC) techniques were introduced to realize multi-field analysis and cross-validation from the stress field, deformation field, and elastic wave field. The mutation characteristics of rock failure were investigated based on the cusp catastrophe theory. The results showed four mutation points in the destabilization process of sandstone: compressional density, yielding, destruction, and residual retention. As an internal activity characteristic of the sandstone failure process, AE directly reflected the dynamic failure process of sandstone. The stress variation was closely related to the evolution of AE characteristics. Sandstone loading failure was a process of the mutations of releasable elastic strain energy, dissipative energy, and releasable elastic strain energy. The mutation of dissipative energy was used as the starting mark of the sandstone warning state, and the second mutation of releasable elastic strain energy was used as the end mark of the sandstone warning state. Besides, the warning range corresponded to the loading time of 178 to 208 s. Finally, the sandstone instability warning interval was re-determined from deformation field evolution characteristics in the sandstone damage process, with a loading time of 180-204 s. This was consistent with the warning interval specified using the cusp catastrophe theory. The combination of AE, DIC, and cusp catastrophe theory revealed the mutation characteristics and early warning interval of sandstone failure. Hence, the results provide significant importance to predicting rock failure.
引用
收藏
页码:1865 / 1877
页数:13
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