›› 2016, Vol. 37 ›› Issue (10): 2761-2768.doi: 10.16285/j.rsm.2016.10.004

• Fundamental Theroy and Experimental Research • Previous Articles     Next Articles

Permeability evolution of brittle rock in progressive failure process under triaxial compression

WANG Wei1, 2, LI Xue-hao1, 2, HU Da-wei3, CAO Ya-jun1, 2   

  1. 1. Geotechnical Research Institute, Hohai University, Nanjing, Jiangsu 210098, China; 2. Key Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing, Jiangsu 210098, China; 3.State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China
  • Received:2015-02-04 Online:2016-10-11 Published:2018-06-09
  • Supported by:

    This work was supported by the National Program on Key Basic Research Project of China (973 Program) (2011CB013504), the National Natural Science Foundation of China (11672343, 51479193) and the Fundamental Research Funds for the Central Universities (2016B20214, 2016B08014).

Abstract: Rock progressive failure is usually accompanied by development of cracks. The propagation behaviour of rock cracks is closely related to the evolution of rock permeability. In order to investigate the permeability properties of rock during progressive failure, a series of hydro-mechanical triaxial coupling tests is carried out on tuff specimens under different confining pressures and seepage pressures using triaxial servo-controlled seepage equipment. Based on the experimental results, the following conclusions are drawn. At the stable crack growth stage, the permeability keeps low and stable and the permeability corresponding to crack initiation strength can be used to determine the minimum value of permeability. At the crack unsteady growth stage, the permeability increases significantly and the increase of permeability can be divided into two stages, which can be reflected by crack circumferential strain. The inflection point of crack circumferential strain curve is used to identify the initial permeability. At the softening stage after failure, the permeability decreases and enters into a residual stable stage, which can be reflected by crack circumferential strain rate. The circumferential strain rate can be used to determine the position of the peak of permeability.

Key words: progressive failure of rocks, crack propagation, crack initiation strength, damage strength, permeability evolution

CLC Number: 

  • TU 458

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