(1. HydroChina Itasca Research and Development Center,Hangzhou,Zhejiang 310014,China;2. HydroChina Huadong Engineering Corporation,Hangzhou,Zhejiang 310014,China)
Abstract:Preferred discontinuity derived from diagenesis and tectonics reworking always results in the anisotropic characteristics of engineering rock mass. Large-scale engineering rock masses with intermittent joints set have anisotropic strength characteristic,which is influenced by the rock bridge either. So the test results of intermittent joints can not be directly used for ubiquitous joint model,while the equivalent continuum persistent joint parameters should be adopted. When the macroscopic anisotropy simulated by FLAC3D ubiquitous joint model coincides by 3DEC model,the equivalent continuum persistent joint parameters can be defined by inversion analysis. Then,indirectly equivalent continuum method has equal function with discontinuum method in describing anisotropic mechanical behavior of rock mass. In summary,numerical experiment has become a more effective way than analytical method to estimate the macroscopic parameters with random intermittent jointed rock mass. Result shows that the equivalent strength of the equivalent continuum persistent joint parameters by the combined effects of intermittent joints and the rock bridge is higher than that of the real intermittent joints. In addition,in order to keep the definition of the set of directions where the strength of the equivalent discontinuities is equal to the strength of the intermittent discontinuities containing rock bridges,the most likely apparent dip direction of the ubiquitous joint model should have ( )/2 separation angle with the real dip direction of the intermittent joints.
孟国涛1,2,方 丹2,李良权2,黄 可2,江亚丽2. 含优势断续节理组的工程岩体等效遍布节理模型强度参数研究[J]. 岩石力学与工程学报, 2013, 32(10): 2115-2121.
MENG Guotao1,2,FANG Dan2,LI Liangquan2,HUANG Ke2,JIANG Yali2. STUDY OF EQUIVALENT STRENGTH PARAMETERS OF UBIQUITOUS JOINT MODEL FOR ENGINEERING ROCK MASS WITH PREFERRED INTERMITTENT JOINTS. , 2013, 32(10): 2115-2121.
[1] SITHARAMA T G,SRIDEVIB J,SHIMIZU N. Practical equivalent continuum characterization of jointed rock masses[J]. International Journal of Rock Mechanics and Mining Sciences,2001,38(3):437–448.
[2] HOEK E,BROWN E T. Underground excavations in rock[M]. London,England:The Institution of Mining and Metallurgy,1980:125–136.
[3] GERRARD C M. Elastic models of rock masses having one,two and three sets of joints[J]. International Journal of Rock Mechanics and Mining Sciences and Geomechanics Abstracts,1982,19(4):15–23.
[4] 张玉军,刘谊平. 层状岩体的三维弹塑性有限元分析[J]. 岩石力学与工程学报,2002,21(11):1 615–1 619.(ZHANG Yujun,LIU Yiping. 3D elasto-plastic FEM analysis of layered rockmass[J]. Chinese Journal of Rock Mechanics and Engineering,2002,21(11):1 615–1 619.(in Chinese))
[5] 黄书岭,丁秀丽,邬爱清,等. 层状岩体多节理本构模型与试验验证[J]. 岩石力学与工程学报,2012,31(8):1 627–1 635.(HUANG Shuling,DING Xiuli,WU Aiqing,et al. Study of multi-joint constitutive model of layered rockmass and experimental verification[J]. Chinese Journal of Rock Mechanics and Engineering,2012,31(8):1 627–1 635. (in Chinese))
[6] 刘胜利,陈善雄,余 飞,等. 绿泥石片岩各向异性特性研究[J]. 岩土力学,2012,33(12):3 616–3 623.(LIU Shengli,CHEN Shanxiong,YU Fei,et al. Anisotropic properties study of chlorite schist[J]. Rock and Soil Mechanics,2012,33(12):3 616–3 623.(in Chinese))
[7] MIN K B,JING L R. Numerical determination of the equivalent elastic compliance tensor for fractured rock masses using the distinct element method[J]. International Journal of Rock Mechanics and Mining Sciences,2003,40(6):795–816.
[8] 孟国涛. 柱状节理岩体各向异性力学分析及其工程应用[博士学位论文][D]. 南京:河海大学,2007.(MENG Guotao. Geomechanical analysis of anisotropic columnar jointed rock mass and its application in hydropower engineering[Ph. D. Thesis][D]. Nanjing:Hohai University,2007.(in Chinese)).
[9] DIEGO I,MATTHEW P,CAROLINE D,et al. The synthetic rock mass approach for jointed rock mass modelling[J]. International Journal of Rock Mechanics and Mining Sciences,2011,48(2):219–244.
[10] 周火明,盛 谦,陈殊伟,等. 层状复合岩体变形试验尺寸效应的数值模拟[J]. 岩石力学与工程学报,2004,23(2):289–292.(ZHOU Huoming,SHENG Qian,CHEN Shuwei,et al. Numerical simulation on size-effect in deformation test of layered composite rock mass[J]. Chinese Journal of Rock Mechanics and Engineering,2004,23(2):289–292.(in Chinese)).
[11] AMADEI B,GOODMAN R E. A 3D constitutive relation for fractured rock masses[C]// Proceedings of International Symposium on Mechanical Behavior of Structured Media. Ottawa:[s. n.],1981:249–268.
[12] JAEGER C. Shear failure of anisotropic rocks[J]. Geological Magazine,1960,97(1):65–72.
[13] TIEN M,KUO C. A failure criterion for transversely isotropic rocks[J]. International Journal of Rock Mechanics and Mining Sciences,2001,38(3):399–412.
[14] 刘新荣,姜德义,鲜学福,等. 单节理岩体在真三轴压缩状态下强度特性的分析[J]. 力学与实践,2000,22(1):44–46.(LIU Xinrong, JIANG Deyi,XIAN Xuefu,et al. Stress analysis of single joint rock under real three-dimension compression[J]. Mechanics in Engineering,2000,22(1):44–46.(in Chinese))
[15] Itasca Consulting Group Inc. 3DEC(three-dimensional distinct element code) user?s manual version 5.0[R]. Minneapolis:Itasca Consulting Group Inc.,2013:26–31.