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首页> 外文期刊>Bulletin of engineering geology and the environment >A new quantitative method to identify the crack damage stress of rock using AE detection parameters
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A new quantitative method to identify the crack damage stress of rock using AE detection parameters

机译:使用AE检测参数识别岩石裂纹损伤应力的新定量方法

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摘要

The quantitative determination of crack damage stress is of significant importance for investigating rock deformation and failure. In this study, a new quantitative method for determining the crack damage stress of rock materials was proposed based on acoustic emission (AE) signal detection. Ten rock materials were subjected to uniaxial compression testing, during which real-time AE signals and axial, lateral, and volumetric strain values were recorded. The AE cumulative count curves of the different rock materials were calculated based on the AE counts. These curves were divided into three stages as the axial stress increased: the slowly increasing stage, the steady stage, and the sharply increasing stage. The point where the sharply increasing stage began was defined as the P(R)point and could be accurately determined based on a fitting optimization method. Then, the damage stress was calculated by using the crack volumetric strain model. Finally, the relationship between the R stress (axial stress corresponding to the P(R)point) and the crack damage stress was investigated for the ten rock materials. The results showed that there was a good correspondence between the R stress and the crack damage stress. Hence, the R stress can be used to determine the crack damage stress and the starting point of the unstable crack growth stage in rock materials.
机译:定量测定裂纹损伤应激对于调查岩石变形和失败具有重要意义。在该研究中,基于声发射(AE)信号检测,提出了一种用于确定岩材料裂纹损伤应力的新定量方法。对单轴压缩测试进行十个岩石材料,在此期间记录实时AE信号和轴向,横向和体积应变值。基于AE计数计算不同岩材料的AE累积计数曲线。随着轴向应力增加,这些曲线分为三个阶段:缓慢增加阶段,稳定阶段和急剧增加的阶段。急剧增加阶段开始的点被定义为P(R)点,并且可以基于拟合优化方法精确地确定。然后,通过使用裂缝体积应变模型计算损伤应力。最后,对十个岩石材料研究了R应力(对应于P(R)点的轴应力)和裂纹损伤应力的关系。结果表明,R应力与裂纹损伤应力之间存在良好的对应关系。因此,R应力可用于确定岩石材料中不稳定裂纹生长阶段的裂纹损伤应力和起始点。

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