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Tensile Behaviors of Granite: Grain Scale Cracking and Fracture Process Zone

机译:花岗岩的拉伸行为:晶粒裂纹和骨折过程区

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This work presents results on grain scale cracking behaviors, inhomogeneous deformation and fracture process zone of Australian Harcourt granite under tensile conditions. Brazilian test was performed with cracking initiation and propagation being monitored by a high speed camera (2 × 10~5 frames/s). Digital image correlation (DIC) was utilized to obtain full-field kinetics and, the development of fracture process zone was characterized using an extended DIC algorithm. The obtained real-time information was further cooperated with the distribution of mineral grains obtained by the synchrotron micro CT and the digital photograph of crack surfaces. The initiative location and the interaction between the micro-cracking process and mineral grains were identified and analyzed. It is found that the first crack initiates on a quartz grain near a biotite particle with some deviation away from the disc geometrical center. Besides, biotite grains trend to deviate or arrest micro cracks resulting from the cleavage structure and higher ductility. The fracture process zone presents as a narrow band whereas it occurs and develops prior to visible cracks.
机译:这项工作提出了谷物裂解行为的结果,在拉伸条件下澳大利亚Harcourt花岗岩的不均匀变形和断裂过程区域。通过高速相机(2×10〜5帧/秒)监测裂化启动和传播进行巴西试验。利用数字图像相关(DIC)来获得全场动力学,并使用扩展DIC算法表征裂缝处理区的开发。获得的实时信息进一步配合通过同步rotron Micro CT和裂缝表面的数字照片获得的矿物质的分布。鉴定并分析了微裂解工艺和矿物质之间的主动位置和相互作用。发现第一裂纹在黑云母颗粒附近的石英粒上引发,偏离圆盘几何中心。此外,Biotite谷物趋势偏离或捕获由切割结构和更高的延展性引起的微裂缝。裂缝过程区域作为窄带呈现,而在可见裂缝之前发生并发发。

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