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孔隙水压力作用下热处理北山花岗岩变形特性试验研究

胡少华, 章光, 赵顺利, 姜秀玲, 陈益峰, 周创兵

胡少华, 章光, 赵顺利, 姜秀玲, 陈益峰, 周创兵. 孔隙水压力作用下热处理北山花岗岩变形特性试验研究[J]. 岩土工程学报, 2016, 38(z2): 330-335. DOI: 10.11779/CJGE2016S2054
引用本文: 胡少华, 章光, 赵顺利, 姜秀玲, 陈益峰, 周创兵. 孔隙水压力作用下热处理北山花岗岩变形特性试验研究[J]. 岩土工程学报, 2016, 38(z2): 330-335. DOI: 10.11779/CJGE2016S2054
HU Shao-hua, ZHANG Guang, ZHAO Shun-li, JIANG Xiu-ling, CHEN Yi-feng, ZHOU Chuang-bing. Laboratory tests on deformation characteristics of thermally treated Beishan granite under high pore water pressure[J]. Chinese Journal of Geotechnical Engineering, 2016, 38(z2): 330-335. DOI: 10.11779/CJGE2016S2054
Citation: HU Shao-hua, ZHANG Guang, ZHAO Shun-li, JIANG Xiu-ling, CHEN Yi-feng, ZHOU Chuang-bing. Laboratory tests on deformation characteristics of thermally treated Beishan granite under high pore water pressure[J]. Chinese Journal of Geotechnical Engineering, 2016, 38(z2): 330-335. DOI: 10.11779/CJGE2016S2054

孔隙水压力作用下热处理北山花岗岩变形特性试验研究  English Version

基金项目: 国家自然科学基金项目(51579188); 中国博士后科学基金项目(2015M580672); 水资源与电工程科学国家重点实验室开放基金项目(2015SGG02)
详细信息
    作者简介:

    胡少华(1986- ),男,讲师、博士,主要从事裂隙岩体水-力耦合试验与数值模拟方面的的教学和科研。E-mail: sh_kxin@whu.edu.cn。

Laboratory tests on deformation characteristics of thermally treated Beishan granite under high pore water pressure

  • 摘要:

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    Abstract: This study aims to examine the influence of coupled thermo-hydro-mechanical processes on the stress-strain curves, mechanical properties, failure mode and damage evolution process. Using THM coupling system, triaxial compression tests were performed on the thermally-treated Beishan granite under high pore water pressure. The σ1-ε1 curves are basically in coincidence with each other under different pore water pressure in the preexisting micro-crack closure region and the linear elastic region, which gradually start to move towards the ε1 axis as the cracks were initiated and propagated. Moreover, with the increase of pore water pressure, the peak strength and the corresponding axial strain decrease, while the inclination of the shear failure surface increases and the damage process evolves more quickly. It was demonstrated that the influence of pore water pressure on the rock damage and failure is mainly manifested in accelerating the process from crack growth to macro instability.
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出版历程
  • 收稿日期:  2016-05-18
  • 发布日期:  2016-10-19

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