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SUBCRITICAL CRACK GROWTH UNDER MODE I, II, AND III LOADING FOR COCONINO SANDSTONE

机译:在I,II和III模式下对COCONINO砂岩的亚裂纹扩展

摘要

In systems subjected to long-term loading, subcritical crack growth is the principal mechanism causing the time-dependent deformation and failure of rocks. Subcritical crack growth is environmentally-assisted crack growth, which can allow cracks to grow over a long period of time at stresses far smaller than their failure strength and at tectonic strain rates. The characteristics of subcritical crack growth can be described by a relationship between the stress intensity factor and the crack velocity. This study presents the results of studies conducted to validate the constant stress-rate test for determining subcritical crack growth parameters in Coconino sandstone, compared with the conventional testing method, the double torsion test. The results of the constant stress-rate test are in good agreement with the results of double torsion test. More importantly, the stress-rate tests can determine the parameter A with a much smaller standard deviation than the double torsion test. Thus the constant stress-rate test seems to be both a valid and preferred test method for determining the subcritical crack growth parameters in rocks. We investigated statistical aspects of the constant stress-rate test. The effects of the number of tests conducted on the subcritical crack growth parameters were examined and minimum specimen numbers were determined. The mean and standard deviation of the subcritical crack growth parameters were obtained by randomly selecting subsets from the original strength data. In addition, the distribution form of the subcritical crack growth parameters and the relation between the parameter n and A were determined. We extended the constant stress-rate test technique to modes II and III subcritical crack growth in rocks. The experimental results of the modes I, II and III tests show that the values of the subcritical crack growth parameters are similar to each other. The subcritical crack growth parameter n value for Coconino sandstone has the range of 34 to 38 and the parameter A has the range of 1.02x10⁻² to 6.52x10⁻² m/s. The effect of confining stress, specimen size, and water saturation on subcritical crack growth under mode II loading has also been investigated. Finally strength parameters for Coconino sandstone were determined experimentally, including tensile strength, uniaxial compressive strength, cohesion, internal friction angle, in-plane / our-of-plane shear strength and the fracture toughness under mode I, II, and III loading.
机译:在承受长期载荷的系统中,亚临界裂纹扩展是引起岩石随时间变化的变形和破坏的主要机理。亚临界裂纹增长是环境辅助的裂纹增长,它可以使裂纹在远小于应力的破坏强度和构造应变率的情况下长时间生长。亚临界裂纹扩展的特征可以通过应力强度因子与裂纹速度之间的关系来描述。与常规测试方法双扭转测试相比,本研究提供了旨在验证用于确定Coconino砂岩中亚临界裂纹扩展参数的恒定应力速率测试的研究结果。恒定应力率测试的结果与双扭转测试的结果非常吻合。更重要的是,应力率测试可以确定参数A,其标准偏差比双扭转测试小得多。因此,恒定应力率测试似乎是确定岩石中亚临界裂纹扩展参数的有效且首选的测试方法。我们研究了恒定应力率测试的统计方面。检查了试验次数对亚临界裂纹扩展参数的影响,并确定了最小试样数。通过从原始强度数据中随机选择子集,可以获得亚临界裂纹扩展参数的平均值和标准差。另外,确定了亚临界裂纹扩展参数的分布形式以及参数n和A之间的关系。我们将恒定应力率测试技术扩展到岩石中的II型和III型亚临界裂纹扩展。 I,II和III模式的实验结果表明,亚临界裂纹扩展参数的值彼此相似。 Coconino砂岩的亚临界裂纹扩展参数n值的范围为34到38,参数A的范围为1.02x10 6到6.52x10 6 m / s。还研究了模式II载荷下限制应力,试样尺寸和水饱和度对亚临界裂纹扩展的影响。最后,通过实验确定了Coconino砂岩的强度参数,包括抗张强度,单轴抗压强度,内聚力,内摩擦角,面内/面内剪切强度以及模式I,II和III下的断裂韧性。

著录项

  • 作者

    Ko Tae Young;

  • 作者单位
  • 年度 2008
  • 总页数
  • 原文格式 PDF
  • 正文语种 EN
  • 中图分类

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