LIN Man-qing, ZHANG Lan, LIU Xi-qi, et al. Microscopic analysis of rockburst failure on specimens under gradient stress[J]. 2020, 41(9): 2984-2992.
DOI:
LIN Man-qing, ZHANG Lan, LIU Xi-qi, et al. Microscopic analysis of rockburst failure on specimens under gradient stress[J]. 2020, 41(9): 2984-2992.DOI: 10.16285/j.rsm.2019.2136.
Microscopic analysis of rockburst failure on specimens under gradient stress
Rockburst has become an urgent safety problem in deep mining
and stress gradient plays a significant role in controlling rockburst. To explore the influence of stress gradients on the microscopic failure of surrounding rock
a pneumatic-hydraulic coupled rockburst simulation testing device was used to achieve six-sides loading in three-directions and the gradient loading in the top direction. When the gradient loading was applied at the top
the confining pressure was kept unchanged. Loading-unloading tests were carried out on rock similar material specimens by using rockburst physical models under different stress gradients. The analysis of microscopic morphology of failure surface was conducted using the scanning electron microscope (SEM). The results showed that failure phenomena and characteristics of rockburst were significantly different under varied paths of stress gradient. The greater the stress gradient is
the smaller the pores among the crystals is and the higher the density of the crystals is. The ratio of shear failure to splitting failure is different under different stress gradient paths. The higher the stress gradient is
the greater the ratio of shear failure is. The fractal dimension of detrital crystal contour increases with the increase of stress gradient.
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Related Author
XIAO Xiao-chun
FAN Yu-feng
WU Di
DING Xin
WANG Lei
ZHAO Bao-you
HE Na
CHEN Ning-sheng
Related Institution
School of Civil Engineering, Shaoxing University
Key Laboratory of Rock Mechanics and Geohazards of Zhejiang Province, Shaoxing University
School of Mechanics and Engineering, Liaoning Technical University
Key Laboratory of Mountain Hazards and Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Resources