加热和冷却工艺对黄锈花岗岩力学性能影响的研究

Luming Zhou , Zhende Zhu , Erkan Oterkus , Selda Oterkus , Huicong Xu
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摘要

高温岩石遇水冷却造成的地质灾害与地下开采和隧道工程密切相关。为充分了解温度变化对岩石力学性能的影响,对黄锈花岗岩试样进行加热-自然冷却和加热-水冷却循环,实验研究了这些过程对试样力学性能的影响。讨论了加热-冷却过程对岩石宏观力学性能的影响机理。基于Drucker-Prager准则和Weibull分布函数,引入损伤变量修正因子来反映峰值后应变软化特性,建立了花岗岩的热-力耦合损伤本构模型。结果表明:在自然冷却模式下,当温度超过600℃时,力学性能明显恶化,破坏模式由脆性破坏转变为延性破坏;在水冷却模式下,当温度低于400℃时,峰值强度和变形模量随着循环次数的增加而增加,而在600℃时,峰值强度和弹性模量明显下降。在所有温度下,峰值应变随循环次数和温度的增加而增加,花岗岩的破坏模式有由拉伸破坏模式向剪切破坏模式转变的趋势。实验结果验证了损伤本构模型的正确性。采用模型威布尔分布函数中的形状参数r和尺度参数S作为反映脆性程度和峰值强度的指标。该研究有助于了解高温环境下岩石的行为,以预防和减轻潜在的地质灾害。
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Research on the effects of heating and cooling processes on the mechanical properties of yellow rust granite

Geological hazards caused by high-temperature rocks cooling down after encountering water are closely related to underground mining and tunneling projects. To fully understand the impact of temperature changes on the mechanical properties of rocks, yellow rust granite samples were subjected to heating-natural cooling and heating-water cooling cycles to experimentally study the effects of these processes on the mechanical properties of the samples. The mechanism of the heating-cooling process on the macromechanical properties of the rock was discussed. Based on the Drucker-Prager criterion and Weibull distribution function, a damage variable correction factor was introduced to reflect the post-peak strain softening characteristics, and a thermo-mechanical coupled damage constitutive model of the granite was established. The results showed that in the natural cooling mode, the mechanical properties deteriorate significantly when the temperature exceeded 600 ​°C, and the failure mode changed from brittle failure to ductile failure. In the water cooling mode, the peak strength and deformation modulus increased at temperatures below 400 ​°C with an increase in the cycle number, while at 600 ​°C, the peak strength and elastic modulus notably decreased. The peak strain increased with the increase of the cycle number and temperature at all temperatures, and the failure mode of the granite tended to change from tensile failure mode to shear failure mode. The experimental results were used to validate the damage constitutive model. The shape parameter r and scale parameter S in the Weibull distribution function of the model were used as indicators to reflect the brittleness degree and peak strength. This study helps to understand the behavior of rocks in high-temperature environments, in order to prevent and mitigate potential geological hazards.

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