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

机译:高温下岩石的面内剪切(Ⅱ型)裂纹亚临界扩展

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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:通过有限元方法和新设计的导电胶方法进行的剪切盒试验(即压缩剪切),研究了岩石在高温下的面内剪切裂纹亚临界扩展。数值和实验结果表明,归一化剪切(Ⅱ型)应力强度因子KTⅡ/KⅡ0随着温度的升高而降低,因为高温可以改善裂纹尖端的应力分布并降低Ⅱ型应力强度因子。断裂表面的微观特征是裂纹尖端附近(1.5-4.0 mm)的小凹坑和次级微裂纹。人字形次级裂纹在约4-5 mm的长度内逐渐融合,并沿着裂纹扩展的方向消失。高温可增加剪切(Ⅱ型)断裂韧性,阻止裂纹扩展,稳定的剪切裂纹扩展时间随温度的升高而增加,而稳定的裂纹扩展速率则随温度的升高而降低。必须确保试样的韧带足够长,以测量岩石的最大不稳定裂纹扩展速率。

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