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| MESOSCOPIC DEFORMATION AND FRACTURE OF MARBLE AT UNDERGROUND POWERHOUSE OF JINPING I HYDROPOWER STATION |
| DING Xiuli1,LU Quangang1,2,HUANG Shuling1,DUAN Haibo1,3,CHENG Peng1 |
| 岩石力学;三维颗粒流理论;细观结构模型;参数敏感性分析;应力路径;细观破裂演化 |
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Abstract Deformation and fracture of brittle marble is closely related to the extension of internal microcracks,and the macroscopic mechanical response of marble depends on its mesoscopic structures. Because the micro cracks are sealed in rock bodies,it is very difficult to grasp the development mechanism of the internal microcracks. With the help of the three-dimensional theory of particle flow and introducing the BPM model and the technology of super unit clump,a mesoscopic structure model of marble in terms of the mineral configurations was established on the basis of the testing result of SEM on the mineral contents of marble from the underground powerhouse of Jinping I hydropower station. The mesoscopic mechanical parameters of marble based on the sensitivity analysis was determined according to the indoor testing results of the uniaxial and triaxial compression and the mesoscopic numerical model of marble was also constructed. The deformation and fracture and the expansion process of marble under different stress states and stress paths were analyzed through numerical simulations. The numerical results of the macroscopic mechanical response of marble were found to agree well with the laboratory testing results. The numbers of microcracks grew slowly initially and soon exponentially under the condition of uniaxial and low confining pressures,however,the growth curve was approximately an “S” shape under the condition of high confining pressure. As the increasing of the confining pressure,the proportion of the tensile cracks reduced gradually,and the shear cracks increased. Under the identical initial confining pressure,the axial strain at the peak strength of rock was smaller and the proportion of tensile cracks was higher in the unloading stress path than the ones in the loading stress path. The tensile cracks played the leading role in the unloading process and eventually caused the tensile macro fracture surface to be formed,indicated that the volume expansion effect of marble under unloading was more significant and the brittle characteristics was more obvious. Under the different stress states and stress paths,the control mechanism of tensile crack propagation interacted with the one of shear crack friction,one grew slowly,the other grew fast.
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Received: 26 June 2014
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| [1] POTYONDY D O,CUNDALL P A. A bonded-particle model for rock[J]. International Journal of Rock Mechanics and Mining Sciences,2004,41(8):1 329–1 364.
[2] 丁秀丽,卢 波,黄书岭,等. 雅砻江锦屏I级水电站技施阶段——高应力低强度应力比条件大型地下洞室群围岩开裂变形机制及稳定性研究[R]. 武汉:长江科学院,2010.(DING Xiuli,LU Bo,HUANG Shuling,et al. Technical construction stage of Jinping I hydropower station on Yalong River—research on stability and fracturing mechanism of surrounding rock mass for large underground powerhouse under conditions of high in-situ stress and low strength stress ratio[R]. Wuhan:Yangtze River Scientific Research Institute,2010.(in Chinese))
[3] HOEK E,BIENIAWSKI Z T. Brittle fracture propagation in rock under compression[J]. International Journal of Fracture Mechanics,1965,1(3):137–155.
[4] DEY T N,WANG C Y. Some mechanisms of microcrack growth and interaction in compressive rock failure[J]. International Journal of Rock Mechanics and Mining Sciences and Geomechanics Abstracts,1981,18(3):199–209.
[5] YAMADA I,MASUDA K,MIZUTANI H. Electromagnetic and acoustic emission associated with rock fracture[J]. Physics of the Earth and Planetary Interiors,1989,57(1):157–168.
[6] TANG C N. Numerical simulation of progressive rock failure and associated seismicity[J]. International Journal of Rock Mechanics and Mining,1997,34(2):249–261.
[7] 赵兴东,李元辉,刘建坡,等. 基于声发射及其定位技术的岩石破裂过程研究[J]. 岩石力学与工程学报,2008,27(5):990–995. (ZHAO Xingdong,LI Yuanhui,LIU Jianpo,et al. Study on rock failure process based on acoustic emission and its location technique[J]. Chinese Journal of Rock Mechanics and Engineering,2008,27(5):990–995.(in Chinese))
[8] 葛修润. 岩石疲劳破坏的变形控制律、岩土力学试验的实时X射线CT扫描和边坡坝基抗滑稳定分析的新方法[J]. 岩土工程学报,2008,30(1):1–20.(GE Xiurun. Deformation control law of rock fatigue failure,real-time X-ray CT scan of geotechnical testing,and new method of stability analysis of slopes and dam foundations[J]. Chinese Journal of Geotechnical Engineering,2008,30(1):1–20.(in Chinese))
[9] 谢和平,鞠 杨,黎立云,等. 岩体变形破坏过程的能量机制[J]. 岩石力学与工程学报,2008,27(9):1 729–1 740.(XIE Heping,JU Yang,LI Liyun,et al. The energy mechanism of the process of the rock mass deformation and failure[J]. Chinese Journal of Rock Mechanics and Engineering,2008,27(9):1 729–1 740.(in Chinese))
[10] MARTIN C D. The strength of massive Lac du Bonnet granite around underground opening[Ph. D. Thesis][D]. Winnipeg:University of Manitoba,1993.
[11] LAU J S O,CHANDLER N A. Innovative laboratory testing[J]. International Journal of Rock Mechanics and Mining Sciences,2004,41(8):1 427–1 445.
[12] BIENIAWSKIZT. Mechanism of brittle fracture of rock,parts I,II and III[J]. International Journal of Rock Mechanics and Mining Sciences and Geomechanics Abstracts,1967,4(4):395–430.
[13] BRACE W F,PAULDING B W,SCHOLZ C. Dilatancy in the fracture of crystalline rocks[J]. Journal of Geophysical Research,1966,71(16):3 939–3 953.
[14] LAJTAI E Z,CARTER B J,AYARI M L. Criteria for brittle fracture in compression[J]. Engineering Fracture Mechanics,1990,37(1):59–74.
[15] FAIRHURST C,COOK N G W. The phenomenon of rock splitting parallel to the direction of maximum compression in the neighborhood of a surface[C]// Proceedings of the 1st Congress of International Society on Rock Mechanics. Lisbon:[s.n.],1966:687–692.
[16] 黄书岭. 高应力下脆性岩石的力学模型与工程应用研究[博士学位论文][D]. 北京:中国科学院研究生院,2008.(HUANG Shuling. Study of mechanical model of brittle rock under high stress condition and its engineering applications[Ph. D. Thesis][D]. Beijing:Graduate University,Chinese Academy of Sciences,2008.(in Chinese))
[17] Itasca Consulting Group,Inc.. PFC3D(particle flow code),version 4.0[M]. Minneapolis,Minnesota:Itasca Consulting Group,Inc.,2008:11–19.
[18] CUNDALL P A,STRACK O D L. A discrete numerical model for granular assemblies[J]. Géotechnique,1979,29(1):47–65.
[19] CHO N,MARTIN C D,SEGO D C. A clumped particle model for rock[J]. International Journal of Rock Mechanics and Mining Sciences,2007,44(6):997–1 010.
[20] WANG Y N,TONON F. Modeling Lac du Bonnet granite using a discrete element model[J]. International Journal of Rock Mechanics and Mining Sciences,2009,46(5):1 124–1 135.
[21] HAZZARD J F,YOUNG R P. Simulating acoustic emissions in bonded-particle models of rock[J]. International Journal of Rock Mechanics and Mining Sciences,2000,37(5):867–872.
[22] 夏才初,宋英龙,唐志成,等. 粗糙节理剪切性质的颗粒流数值模拟[J]. 岩石力学与工程学报,2012,31(8):1 545–1 552.(XIA Caichu,SONG Yinglong,TANG Zhicheng,et al. Partical flow code numerical simulation of rough joint in shear[J]. Chinese Journal of Rock Mechanics and Engineering,2012,31(8):1 545–1 552.(in Chinese)) |
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