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Study on Crack Propagation Process of Granite Samples Based on AE and its Location Technique

机译:基于AE的花岗岩样品裂纹扩展过程及其定位技术研究

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Acoustic emission (AE), which is produced by the micro-cracks occurrence or growth, is an ubiguitous phenomenon associated with brittle fracture in many materials. AE technique can monitor the microfractures development in the rock sample continuously and in-real-time, which is better than other methods. In this paper, acoustic emission (AE) and location technique was employed to study rock failure process. It was investigated using different precut crack granite samples (70 mm×70 mm×150 mm),and AE sensors were surface mounted. A Geiger location algorithm allows AE event location from first arrival times to be determined by AE sensors, which was applied to study the crack initiation and propagation process, also to analyze the crack spatial evolution mode with stress changing during the total loading process. The experimental results showed AE activity represents different characters with stress-strain changing during the total loading process ; the quantity of AE events was very little in the initial loading up to crack initiation ; when initial crack generated AE events apparently increased ; AE events was in quiet period after crack initiation up to before crack propagation ; AE activity sharply increased from crack stable propagation up to crack unstable propagation; especially in crack unstable propagation step AE events reach the most quantity in the division strain. There is "void space" of AE events during the AE location results; the "void space" of AE events is the position of macroscopic crack breakthrough, which can be used to predict the crack breakthrough position of rock samples. Meanwhile, AE location results are also direct reflection of interior stress field propagation process. AE location result also reflect directly the spatial position, direction and spatial curved face of crack propagation in the rock sample, which is very significant to study the mechanism of rock failure.
机译:由微裂纹的发生或增长产生的声发射(AE)是与许多材料中的脆性断裂相关的普遍现象。声发射技术可以连续,实时地监测岩石样品中的微裂缝发育情况,优于其他方法。本文采用声发射和定位技术研究岩石破坏过程。使用不同的预切割裂纹花岗岩样品(70 mm×70 mm×150 mm)进行了研究,并在表面安装了AE传感器。 Geiger定位算法允许AE传感器确定从首次到达时间起的AE事件位置,该算法被用于研究裂纹的萌生和扩展过程,还分析了在整个加载过程中应力变化的裂纹空间演化模式。实验结果表明,在整个加载过程中,AE活性表现出不同的特征,随应力-应变的变化。从初始加载到裂纹萌生的AE事件数量很少;当初始裂纹产生的AE事件明显增加时; AE事件处于裂纹萌发后直至裂纹扩展之前的平静期;从裂纹稳定扩展到裂纹不稳定扩展,AE活动急剧增加。特别是在裂纹不稳定扩展步骤中,AE事件在分割应变中达到最大。 AE定位结果期间,AE事件存在“空白”。声发射事件的“空隙空间”是宏观裂纹突破的位置,可以用来预测岩石样品的裂纹突破的位置。同时,声发射的定位结果也直接反映了内部应力场的传播过程。声发射定位结果也直接反映了岩石样品中裂纹扩展的空间位置,方向和空间弯曲面,对研究岩石破坏机理具有十分重要的意义。

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