循环荷载下花岗岩的动力变形参数试验研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
利用MTS 815Flex Test GT岩石力学试验系统,对花岗岩进行了不同加载频率单轴压缩下的5级正弦波加卸载试验。正弦波加载频率依次为1、2、3、4Hz,循环应力幅值由岩石平均抗压强度的20%~60%等间距确定,每级应力幅值为400个振动循环。试验结果表明,花岗岩塑性变形随加载次数的增加而逐渐增大,且动应力动应变滞回环为月牙形;同一加载频率下,花岗岩的动弹性模量、动泊松比和单位体积耗散能随动应力水平的升高而升高,且随着加载频率的升高,动弹性模量逐渐降低,而动泊松比和单位体积耗散能逐渐升高,表明动荷载频率越高,对岩石劣化作用的能力越强;同一级动荷载下花岗岩动弹性模量和动泊松比随循环周次增加而变化不明显,单位体积耗散能随循环周次增加逐渐减小。
The uniaxial five stress levels cyclic loading and unloading tests under different loading frequencies for granite are carried out on the MTS 815 Flex Test GT rock mechanics test system in sine wave.Sine wave loading frequencies were 1Hz,followed by 2Hz,3 Hz and 4 Hz,cyclic stress amplitude depended on 20% to 60% average of rock compressive strength on same space,and the cyclic number of every level cyclic stress was 400 cycles.The research results are shown as follows: with the increase of loading times,the plastic deformation of granite increases gradually;the hysteresis loop of dynamic stress and strain is the crescent;meanwhile,under the same loading frequency,granite's dynamic elastic modulus,dynamic Poisson's ratio and the energy dissipation of unit volume increase progressively with the increment of dynamic stress amplitude;along with loading frequency increasing,the dynamic elastic modulus gradually reduce,and dynamic Poisson's ratio gradually rises as well as the energy dissipation of unit volume;the results suggest that the higher frequency of the dynamic loading,the stronger ability the dynamic loading has to weaken rock;under the same level of dynamic loading,granite's dynamic elastic modulus and dynamic Poisson's ratio change little with the increment of loading times,but the energy dissipation of unit volume gradually decreases.
引文
[1]钱七虎.深部地下工程空间开发中的关键科学问题[A].钱七虎院士论文选集[C].北京:科学出版社,2007:549-568.
    [2]张运良,马艳晶.基于两类典型动力人工边界的水电站地下洞室群地震反应分析[J].水电能源科学,2010,28(3):70-73,145.
    [3]刘建锋,徐进,裴建良,等.盐岩损伤测试中卸载模量研究[J].四川大学学报(工程科学版),2011,43(4):57-62.
    [4]刘建锋,谢和平,徐进,等.循环荷载作用下岩石阻尼特性的试验研究[J].岩石力学与工程学报,2008,27(4):712-717.
    [5]刘建锋,徐进,李青松,等.循环荷载下岩石阻尼参数测试的试验研究[J].岩石力学与工程学报,2010,29(5):1 036-1 041.
    [6]朱明礼,朱珍德,李刚,等.循环荷载作用下花岗岩动力特性试验研究[J].岩石力学与工程学报,2009,28(12):2 520-2 526.
    [7]肖建清,冯夏庭,丁德馨,等.常幅循环荷载作用下岩石的滞后及阻尼效应研究[J].岩石力学与工程学报,2010,29(8):1 677-1 683.
    [8]聂明,徐进,任浩楠,等.大理岩阻尼参数与动弹性参数的动三轴试验研究[J].岩石力学与工程学报,2011,30(S2):3 989-3 994.
    [9]长江水利委员会长江科学院,成都勘测设计研究院,黄河水利委员会勘测规划设计研究院,等.水利水电工程岩石试验规程(SL264-2001)[S].北京:中国水利水电出版社,2001.
    [10]杨春和,马洪岭,刘建锋.循环加、卸载下盐岩变形特性试验研究[J].岩土力学,2009,30(12):3562-3 568.
    [11]黎立云,谢和平,鞠杨,等.岩石可释放应变能及耗散能的实验研究[J].工程力学.2011,28(3):35-40
    [12]徐志英.岩石力学(第三版)[M].北京:中国水利水电出版社,1993.
    [13]蔡美峰,何满潮,刘东燕.岩石力学与工程[M].北京:科学出版社,2002.
    [14]尤明庆,华安增.岩石试样破坏过程的能量分析[J].岩石力学与工程学报,2002,21(6):778-781.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心