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Nonlinear Damage and Failure Behavior of Brittle Rock Subjected to Impact Loading

机译:冲击载荷作用下脆性岩石的非线性破坏与破坏行为

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摘要

The damage and fragmentation of rock induced by impact loading is one of typical nonlinear problems in underground engineering. Rock specimen such as rock plate was found to become invalid under impact loading. This paper presents brittle fragmentation for dynamic damage of rock plate based on the edge-on impact (EOI) test with varying impact velocities (10 ms~(-1) to 40 ms~(-1)) and impact angles. High-speed camera was used to study the relation among crack initiation and propagation, impact velocity and impact angle. The patterns of fracture of the crack under impact are observed and the influence of impact angle on the growth of the crack is analyzed. The results demonstrate that only when the impact velocity is less than a critical value does a damaged zone, whose size increases with the impact velocity, appear on the edge of the sample. When the velocity exceeds the critical value, some radial cracks occur around the damaged zone and extend outward from the boundaries of damaged zone. The radial crack length and damaged zone increase with impact velocity and are influenced by the impact angle. However, at a certain velocity, the damage zone decreases and the crack length increase. It shows that there was an obvious incubation period of crack forming. According to test results, the study found that the impact velocity of this jump is about 25 ms~(-1)-3 m s~(-1) and scope of the impact resistance optimized angle is about 15°-30°.
机译:冲击载荷引起的岩石破坏和破碎是地下工程中典型的非线性问题之一。发现诸如岩石板的岩石样本在冲击载荷下变得无效。本文基于冲击速度(10 ms〜(-1)至40 ms〜(-1))和冲击角度的边碰冲击(EOI)试验,提出了岩壁动力损伤的脆性破碎方法。用高速相机研究了裂纹萌生与扩展,冲击速度和冲击角度之间的关系。观察了裂纹在冲击下的断裂形态,并分析了冲击角对裂纹扩展的影响。结果表明,只有当冲击速度小于临界值时,尺寸随冲击速度而增加的损坏区域才会出现在样品边缘。当速度超过临界值时,在损坏区域周围会出现一些径向裂纹,并从损坏区域的边界向外延伸。径向裂纹长度和损坏区域随冲击速度而增加,并受冲击角度的影响。但是,在一定速度下,损伤区域减小并且裂纹长度增加。结果表明,裂纹形成有一个明显的潜伏期。根据测试结果,研究发现该跳跃的冲击速度约为25 ms〜(-1)-3 m s〜(-1),耐冲击性最佳角度范围约为15°-30°。

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