热损伤砂岩力学特性与声发射试验研究

    Experimental Study on Mechanical Properties and AE of Thermally Damaged Sandstone

    • 摘要: 为探讨不同温度作用下砂岩热损伤力学特性与声发射演化规律,借助MTS815岩石力学伺服试验机配套声发射仪对砂岩开展不同温度下的试验(25、100、200、400、600、800、1 000 ℃)。结果表明:砂岩表观形态与体积发生变化的临界温度为400 ℃;脆延性转化的临界温度为600 ℃;弹性模量呈现出先增加后降低的变化趋势,相反,孔隙度的演化规律为先降低后增加;初始加载至屈服阶段,声发射计数呈零星状态分布;屈服阶段至加载结束,声发射计数密度急剧增加;基于声发射累积计数定义的损伤变量能够较好地表征整个损伤演化过程,并结合有效介质理论和裂纹闭合模型得到了理论的应力-应变曲线。

       

      Abstract: To investigate the mechanical properties and acoustic emission of thermally damaged sandstone under different temperatures, using MTS815 rock mechanics servo testing machine and acoustic emission to carry out various tests of sandstone at different temperatures(25 °C, 100 °C, 200 °C, 400 °C, 600 °C, 800 °C and 1 000 °C). The results show that the critical temperature of the surface morphology and volume change of sandstone is 400 °C. The temperature of brittle ductile transition of sandstone is 600 °C. The elastic modulus of sandstone increased first and then decreased. On the contrary, the porosity of sandstone decreased first and then increased gradually. From the initial to yield loading stage, the acoustic emission events distributed in a sporadic state. However, the event density of acoustic emission increased sharply from the yielding to the final loading stage. The damage variable defined by the cumulative acoustic emission counts which can better characterize the entire process of damage evolution. Based on the effective medium theory and crack closure model, the theoretical stress-strain curve of sandstone is obtained.

       

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