考虑浸泡水温影响的泥质粉砂岩破坏过程声发射特征试验研究

    Experimental study on failure process characteristic of considered about the water-temperature of argillaceous siltstone

    • 摘要: 高地温水工隧洞、深部矿山工程中温度的变化对地下岩体的物理力学性质具有重要影响,目前不同水温浸泡下岩石破裂相关研究较少。本文将泥质粉砂岩置于自然干燥以及28℃(常温)、40℃、50℃、70℃、100℃共五种不同温度的水中浸泡至饱和,然后开展单轴压缩试验,研究了泥质粉砂岩的物理力学及声发射特征。研究结果表明:温度对泥质粉砂岩含水的影响存在一个临界转换点(本研究为40℃),当温度在28~40℃时,岩石含水能力被"弱化",当温度大于40℃时,泥质粉砂岩含水能力被"增强"。在28~100℃中,温度对泥质粉砂岩物理力学性质起"增强"作用,表现为弹性模量增加,刚度提升。当水温从28℃升高到40℃,声发射时域活动性增强,水温从40℃提高到100℃时,声发射时域活动性减弱。声发射能量b值和熵值曲线较好地体现了裂纹演化规律,水温越高,在形成主裂纹过程中,伴生裂纹出现的概率越低。

       

      Abstract: The change of water-temperature has an important effect on physical and mechanical properties of the rock mass underground of high temperature hydraulic tunnel and deep mining engineering.At present different water-temperature has got a less study on rock burst.This paper put research of uniaxial compression test on natural drying and five different temperatures(28℃,40℃,50℃,70℃,100℃) by argillaceous siltstone.The results show that the influence of temperature on the argillaceous siltstone water have a critical point(this study of 40℃).When the water-temperature in the range of 28℃ to 40℃,the containing-water ability of rock is "weaken".While the water-temperature is greater than 40℃,the containing-water ability of rock is "enhance".In 28~100℃,the water-temperature plays a role of "enhance" of rock physical and mechanical properties.When the water temperature rise from 28℃ to 40℃,the time-domain activity of AE increased,and the time-domain activity of AE weaken while the water temperature increased from 40℃ to 100℃.The curve of b-value and entropy can get a well reflect to the crack evolution law.In the process of formation of the main crack,the probability of accompanying-crack decreased.

       

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