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中低应变率范围内花岗岩单轴压缩特性的尺寸效应研究
引用本文:梁昌玉,李 晓,张 辉,李守定,赫建明,马超锋.中低应变率范围内花岗岩单轴压缩特性的尺寸效应研究[J].岩石力学与工程学报,2013,32(3):528-536.
作者姓名:梁昌玉  李 晓  张 辉  李守定  赫建明  马超锋
作者单位:(1. 中国科学院地质与地球物理研究所 工程地质力学重点实验室,北京 100029;2. 中交路桥技术有限公司,北京 100011; 3. 清华大学 水利水电工程系,北京 100084;4. 中航勘察设计研究院有限公司,北京 100098)
基金项目:国家重点基础研究发展计划(973)项目(2009CB724605,2010CB731501);国家自然科学基金资助项目(41027001)
摘    要: 利用变频动态加载岩石力学试验系统对直径为50 mm,长度分别为50,75,100,125 mm的花岗岩试样进行中低应变率范围内的加载试验。研究结果表明:(1) 试样强度具有显著的应变率依赖性,随着应变率增大,压缩强度近似以乘幂关系增大。(2) 静载和准动态加载条件下,岩石强度基本上随试样长度的增加而减小。(3) 不同应变率加载条件下,直径为50 mm的试样,长径比不小于2时,方能取得基本稳定的试验结果。(4) 峰值应变随试样尺寸的增大逐渐减小。(5) 割线模量E50和线性段弹性模量Et随试样尺寸的增大而增大,且Et>E50。(6) 破裂形式具有显著的应变率效应,随着应变率的增高,破碎程度加大;其尺寸效应则表现为:应变率 <10-3 s-1时,随着尺寸的增大,破裂形式表现为劈裂–锥形破裂–剪切破裂的过程;应变率 >10-2 s-1时,破裂形式则直接由锥形破裂变为剪切破裂。

关 键 词:岩石力学尺寸效应岩石动态力学性质破裂形式准动态试验
收稿时间:2012-10-04;

RESEARCH ON SIZE EFFECT OF UNIAXIAL COMPRESSION PROPERTIES OF GRANITE UNDER MEDIUM AND LOW STRAIN RATES
LIANG Changyu,LI Xiao,ZHANG Hui,LI Shouding,HE Jianming,MA Chaofeng,.RESEARCH ON SIZE EFFECT OF UNIAXIAL COMPRESSION PROPERTIES OF GRANITE UNDER MEDIUM AND LOW STRAIN RATES[J].Chinese Journal of Rock Mechanics and Engineering,2013,32(3):528-536.
Authors:LIANG Changyu  LI Xiao  ZHANG Hui  LI Shouding  HE Jianming  MA Chaofeng  
Affiliation:(1. Key Laboratory of Engineering Geomechanics,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2. CCCC Road and Bridge Consultants Co.,Ltd.,Beijing 100011,China;3. Department of Hydraulic and Hydropower Engineering,Tsinghua University,Beijing 100084,China;4. AVIC Geotechnical Engineering Institute Co.,Ltd.,Beijing 100098,China)
Abstract:The static and quasi-dynamic tests on granite specimens under various strain rates are conducted by using rock dynamic loading system. The specimens are 50 mm in diameter,with the length of 50,75,100,125 mm,respectively. The research results are drawn as follows:(1) Specimen strength is significantly dependent on strain rates and increases with the growth of strain rates with a power relationship. (2) Under static and quasi-dynamic loading conditions,rock strength generally decreases with the increase in specimen length. (3) When the diameter of specimen is 50 mm,the aspect ratio should be not smaller than 2;then steady test results can be obtained under different strain rates. (4) Peak strain under each strain rate decreases with increasing specimen size. (5) Both of secant modulus E50 and elastic modulus Et increase with increasing specimen size;and Et is larger than E50. (6) Failure mode is significantly dependent on strain rates and failure is serious when the strain rate increases. When strain rate  <10-3 s-1,failure mode has a process of split failure-taper failure-shear failure;when strain rate  >10-2 s-1,the failure mode changes from taper failure to shear failure directly.
Keywords:rock mechanics  size effect  rock dynamic mechanical properties  failure mode  quasi-dynamic test
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