单轴压缩下粉砂岩热图像特征粗糙度演化特性研究

Study on the evolution of thermal image characteristics of the thermal image of the powder sandstone under uniaxial compression

  • 摘要: 为探寻粉砂岩破裂失稳过程中红外异常,引入分形理论,通过盒维数法计算出粉砂岩红外热图像特征粗糙度,结合方差及AIRT对单轴压缩下粉砂岩特征粗糙度演化特征进行分析。结果表明:热图像的特征粗糙度演化过程与方差相似,具体可分为三个阶段:在压密阶段,特征粗糙度和方差迅速增大且方差在这个阶段刻画较好;弹性阶段,特征粗糙度开始变小,二者刻画能力相当;塑性-峰后阶段,特征粗糙度值波动性增强,跳动幅度和频率都明显增加,且在应力峰值点转为变大, 此现象即为岩石破裂红外前兆信息,阶段刻画能力较方差更理想。

     

    Abstract: In order to explore the infrared anomaly in the process of fracture instability, The fractal theory is introduced to calculate the characteristic roughness of the infrared thermal image of siltstone by the box dimension method.Combining variance and AIRT to analyze the characteristics of the evolution of the characteristics of the sandstone under uniaxial compression.The results show that the evolution of the characteristic roughness of the thermal image is similar to the variance, and it can be divided into three stages.In the compaction stage, The characteristic roughness and the variance increase rapidly, and the variance is well characterized at this stage.In the elastic stage, the characteristic roughness starts to become smaller, and the ability to portray the same as the two.In the post peak stage, the characteristic roughness value is enhanced, and the amplitude and frequency are increased obviously., and in the peak stress, characteristic roughness began to become big, which is infrared precursor information.In this stage, the ability to describe the characteristic is more ideal than variance.

     

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