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In-plane shear (Mode Ⅱ) crack sub-critical propagation of rock at high temperature

机译:面内剪切(模式Ⅱ)在高温下岩石的裂纹亚临界传播

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In-plane shear crack sub-critical propagation of rock at high temperature was studied by finite element method and shear-box (I.e. Compression-shear) test with newly designed electrically conductive adhesive method. Numerical and experimental results show that the normalized shear (Mode Ⅱ) stress intensity factors, KTⅡ/KⅡ0 is decreased as the temperature increases because high temperature can improve stress distribution at crack tip and reduce the Mode Ⅱ stress intensity factor. Microscopic features of fractured surface are of little pits and secondary micro-cracks in the vicinity (1.5-4.0 mm) of the crack tip. The chevron-shape secondary cracks gradually merge in the length of about 4-5 mm and disappear along the direction of crack propagation. Stable shear crack propagation time is increased with the increasing temperature while the stable shear crack propagation rate is decreased with the increasing temperature, since high temperature can increase the shear (Mode Ⅱ) fracture toughness and prevent the crack growth. It is necessary to ensure the ligament of specimen long enough to measure the maximum unstable crack propagation rate of rock.
机译:面内,在高温下岩石剪裂缝亚临界传播通过有限元法和剪切框(即压缩 - 剪切)试验新设计的导电性粘接剂的方法的研究。数值模拟和实验结果表明,该归一化剪切(Ⅱ)应力强度因子,KTⅡ/KⅡ0降低随着温度的升高,因为高温可以提高在裂纹尖端的应力分布,降低了Ⅱ型应力强度因子。断裂面的微观特征是在裂纹尖端的附近(1.5-4.0毫米)的小凹坑和二次微裂纹。人字形形状二次裂纹在约4-5毫米的长度逐渐合并和沿裂纹传播的方向消失。稳定剪切裂纹传播时间与增加的温度增加,而稳定的剪切裂纹扩展速率随温度的升高减少,因为高温可以增加剪切(Ⅱ)的断裂韧性和防止裂纹扩展。这是必要的,以确保试样足够长的时间来测量岩石的最大不稳定裂纹扩展速率的韧带。

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