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首页> 外文期刊>Rock Mechanics and Rock Engineering >Numerical Assessment of the Progressive Rock Fracture Mechanism of Cracked Chevron Notched Brazilian Disc Specimens
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Numerical Assessment of the Progressive Rock Fracture Mechanism of Cracked Chevron Notched Brazilian Disc Specimens

机译:人字形缺口巴西盘形试样渐进岩石断裂机理的数值评估

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摘要

The International Society of Rock Mechanics (ISRM) suggested cracked chevron notched Brazilian disc method falls into a major testing category of rock fracture toughness measurement by virtue of chevron notched rock samples. A straight through crack front during the whole fracturing process is assumed in the testing principle but is never assessed. In this study, the progressive rock fracture mechanism of cracked chevron notched Brazilian disc rock specimens is numerically simulated for the first time. Two representative sample types with distinct geometry of notch ligaments are modelled. The assumption of a straight through crack front for chevron notched fracture samples is critically assessed. The results show that not only the notch tip but also the saw-cut chevron notch cracks during the experiments. The straight through crack front assumption is never satisfied in the realistic rock fracture progress of chevron notched disc samples. In addition, the crack features prominent curved front, far from being straight. In contrast to the sample type with narrow notch ligament, the acoustic emission (AE) of the simulation on the sample with wide notch ligament depicts obvious biased fracturing of the prescript fracturing route of the notch. The numerically observed progressive fracture mechanism calls for more attention on how to accurately calibrate the critical dimensionless stress intensity factor for a better measurement of Mode I fracture toughness via chevron notched samples.
机译:国际岩石力学学会(ISRM)建议,开裂的V形缺口巴西圆盘法因V形缺口岩石样品而成为岩石断裂韧性测量的主要测试类别。测试原理假定整个压裂过程中出现直通裂纹,但从未对其进行评估。在这项研究中,首次数值模拟了开裂的V形缺口巴西盘状岩石标本的渐进岩石断裂机理。对具有代表性的刻槽韧带几何形状的两种代表性样品类型进行了建模。对人字形缺口样品的直裂纹前缘的假设进行了严格评估。结果表明,不仅在实验过程中出现了缺口尖端,而且出现了锯齿状V形缺口。在人字形缺口盘样品的实际岩石破裂过程中,无法满足直通裂纹前沿的假设。另外,裂纹的特征在于突出的弯曲前部,而不是直的。与具有窄刻痕韧带的样品类型相反,具有宽刻痕韧带的样品的模拟声发射(AE)反映出刻痕的开裂断裂路线有明显的偏斜断裂。在数值上观察到的渐进断裂机制需要更多地关注如何准确校准关键的无量纲应力强度因子,以便通过人字形缺口样品更好地测量I型断裂韧性。

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