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Crack initiation stress and strain of jointed rock containing multi-cracks under uniaxial compressive loading:A particle flow code approach
引用本文:范祥,陈新,曹平,CAO Ping.Crack initiation stress and strain of jointed rock containing multi-cracks under uniaxial compressive loading:A particle flow code approach[J].中南工业大学学报(英文版),2015(2):638-645.
作者姓名:范祥  陈新  曹平  CAO Ping
作者单位:School of Resources and Safety Engineering, Central South University;Rock Mass Modeling and Computational Rock Mechanics Laboratories,University of Arizona;School of Mechanics and Civil Engineering, China University of Mining and Technology (Beijing)
基金项目:Project(11102224)supported by the National Natural Science Foundation of China;Project(201206370124)supported by the China Scholarship Council,China
摘    要:The ratio of crack initiation stress to the uniaxial compressive strength(SCI,B/SUC,B) and the ratio of axial strain at the crack initiation stress to the axial strain at the uniaxial compressive strength(B,UCB,CI,A,A/SSSS) were studied by performing numerical stress analysis on blocks having multi flaws at close spacing’s under uniaxial loading using PFC3 D. The following findings are obtained: SCI,B/SUC,B has an average value of about 0.5 with a variability of ± 0.1. This range agrees quite well with the values obtained by former research. For joint inclination angle, β=90°,B,UCB,CI,A,A/SSSS is found to be around 0.48 irrespective of the value of joint continuity factor, k. No particular relation is found betweenB,UCB,CI,A,A/SSSS and β; however, the average B,UCB,CI,A,A/SSSS seems to slightly decrease with increasing k. The variability ofB,UCB,CI,A,A/SSSS is found to increase with k.Based on the cases studied in this work,B,UCB,CI,A,A/SSSS ranges between 0.3 and 0.5. This range is quite close to the range of 0.4to 0.6 obtained for SCI,B/SUC,B. The highest variability of ± 0.12 forB,UCB,CI,A,A/SSSS is obtained for k=0.8. For the remaining k values the variability ofB,UCB,CI,A,A/SSSS can be expressed within ± 0.05. This finding is very similar to the finding obtained for the variability of SCI,B/SUC,B.

关 键 词:jointed  rock  multi  flaws  uniaxial  loading  PFC3D  model  crack  initiation  stress(SCI  B)  axial  strain  at  crack  initiation
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