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Experimental study on crack coalescence behavior of double unparallel fissure-contained sandstone specimens subjected to freeze-thaw cycles under uniaxial compression

机译:单轴压缩下双不平行裂隙含砂岩样品冻融循环裂纹聚结特性的试验研究

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摘要

To study the rock fracturing characteristics in cold-region engineering, uniaxial compression tests are conducted on double unparallel fissure-contained sandstone specimens subjected to freeze-thaw (FT) cycles. First, the effects of FT cycles on the water absorption, peak strength, initiation stress and deformation behavior of flawed sandstone specimens are investigated. The water absorption, uniaxial compressive strength, initiation stress, elastic modulus and deformation modulus of flawed sandstone specimens decrease with an increase in the number of FT cycles. However, the peak strain of flawed sandstone specimens increases with an increase in the number of FT cycles. Second, the cracking processes of flawed sandstone specimens are investigated in detail via images captured by a high-speed digital video camera system. The relationship between the real-time crack coalescence and the axial stress-strain curve of flawed specimens, which evaluates the macroscopic deformation characteristics of precracked rock subjected to FT cycles well, is considered. Third, the interaction mechanism of fissures in rock specimens is discussed. Fourth, the influence of water and temperature on the rock-weakening process is discussed. In this study, during the rock FT cycle weakening process, the effect of water, including the dissolution effect and the stress effect, is analyzed, whereas temperature damages the rock by means of different temperature gradients and the phase transition of water. Finally, the local strong fatigue-damaged zones around the fissure tips of sandstone specimens are also analyzed. These experimental results are helpful to improve the understanding of fracture mechanisms of a rock mass in cold-region engineering.
机译:为了研究寒区工程中的岩石破裂特性,对经受冻融(FT)循环的双重不平行裂隙含砂岩标本进行了单轴压缩试验。首先,研究了FT循环对有缺陷的砂岩样品的吸水率,峰值强度,初始应力和变形行为的影响。缺陷砂岩样品的吸水率,单轴抗压强度,初始应力,弹性模量和变形模量随FT循环次数的增加而降低。但是,随着FT循环次数的增加,有缺陷的砂岩样品的峰值应变会增加。其次,通过高速数字摄像机系统捕获的图像,详细研究了有缺陷的砂岩标本的开裂过程。考虑了实时裂纹的聚结与有缺陷试样的轴向应力-应变曲线之间的关系,从而很好地评估了经受FT循环的预裂岩石的宏观变形特性。第三,探讨了裂缝在岩石标本中的相互作用机理。第四,讨论了水和温度对岩石弱化过程的影响。在这项研究中,在岩石FT循环弱化过程中,分析了水的作用,包括溶解作用和应力作用,而温度则通过不同的温度梯度和水的相变来破坏岩石。最后,还分析了砂岩标本裂缝尖端周围的局部强疲劳破坏区域。这些实验结果有助于增进对寒冷地区工程中岩体破裂机理的理解。

著录项

  • 来源
    《Cold regions science and technology》 |2019年第2期|166-181|共16页
  • 作者单位

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400045, Peoples R China|Chongqing Univ, Sch Civil Engn, Chongqing 400045, Peoples R China;

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400045, Peoples R China|Chongqing Univ, Sch Civil Engn, Chongqing 400045, Peoples R China;

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400045, Peoples R China|Chongqing Univ, Sch Civil Engn, Chongqing 400045, Peoples R China;

    Chongqing Univ, Sch Civil Engn, Chongqing 400045, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sandstone; Freeze-thaw (FT) cycle; Crack coalescence; Fracture mechanism; Uniaxial compression;

    机译:砂岩冻融循环裂缝合并断裂机制单轴压缩;

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