Uniaxial compressive mechanical properties of rock at low temperature
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摘要: 以非線性熱彈性理論為基礎,建立了考慮巖石冰脹效應的變物性本構方程,給出了干燥低溫和飽和凍結狀態下單軸壓縮強度和力學特性參數隨溫度的變化關系.借助花崗巖在兩種狀態下的壓縮試驗結果,探討了低溫花崗巖的單軸壓縮力學特性.飽和凍結狀態下的抗壓強度大于干燥低溫狀態的抗壓強度,其相差量隨著溫度降低有增加趨勢;在同種狀態下抗壓強度隨溫度降低呈增長趨勢,增長率逐漸減小.低溫附加強度主要由巖石基質熱力效應所貢獻,而由巖石孔隙冰脹效應引起的附加強度相對較小.花崗巖在干燥低溫和飽和凍結狀態下,變形模量均隨溫度的降低呈增大趨勢,而泊松比變化相對較小.Abstract: Based on the nonlinear thermo-elastic theory,a constitutive equation with variable properties was established in consideration of the expansion force of pore ice,and the relationships of the uniaxial compressive strength and the mechanical parameters with temperature were proposed in the drying and low-temperature condition and the saturated freezing condition.Mechanical properties of granite under uniaxial compression were discussed according to compression experimental results of granite in both the conditions.It is shown that the compressive strength under the saturated freezing condition is greater than that under the condition of drying and low temperature,and their difference increases with decreasing temperature.The compressive strength in the same state increases with decreasing temperature,and the growth rate gradually decreases.The additional strength is mainly caused by thermal effects of the rock matrix,and the expansion force of pore ice has relatively little effect.The elastic modulus of granite increases with decreasing temperature in both the conditions,but the change of Poisson's ratio is little.
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Key words:
- rock /
- low temperature testing /
- compression testing /
- mechanical properties /
- granite
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