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Experimental study on time-dependent stress and strain of in-plane shear (Mode Ⅱ) fracture process of rock

机译:岩石面内剪切(Ⅱ型)断裂过程的时变应力和应变试验研究

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Shear-box test with strain measurement was used to study time-dependent stress and strain of in-plane shear (Mode Ⅱ)fracture process of rock and to reveal the mechanism of Mode Ⅱ fracture. Numerical results show that the maximum shear stress τmax at the crack tip is much larger than the maximum tensile stress σ1 and the ratio of τmax/σ1 is about 5, which favors Mode Ⅱ fracture of rock. Test results indicate that the strain-time curve comprises three stages: the linear deformation stage, the micro-cracking stage and the macroscopic crack propagation. The strain in the direction of the original notch plane is negative, due to restraining effect of compressive loading applied to the original notch plane. Both σ1 and τmax are increased as the load increases, but the slope of τmax is larger than that of σ1 and the value of τmax is always larger than that of σ1. Therefore, τmax reaches its limited value at peak load before σ1 and results in Mode Ⅱ fracture of rock. Shear-box (i.e. compression-shear) test becomes a potential standard method for achieving the true Mode Ⅱ fracture and determining Mode Ⅱ fracture toughness of rock.
机译:利用剪切应变试验和应变测量方法研究了岩石面内剪切(Ⅱ型)断裂过程的时变应力和应变,揭示了Ⅱ型断裂的机理。数值结果表明,裂纹尖端的最大切应力τmax远大于最大拉应力σ1,τmax/σ1之比约为5,有利于岩石的Ⅱ型断裂。测试结果表明,应变-时间曲线包括三个阶段:线性变形阶段,微裂纹阶段和宏观裂纹扩展。由于施加到原始缺口平面的压缩载荷的抑制作用,原始缺口平面方向上的应变为负。 σ1和τmax都随负载的增加而增加,但是τmax的斜率大于σ1的斜率,并且τmax的值始终大于σ1的斜率。因此,τmax在σ1之前的峰值载荷处达到其极限值,并导致岩石的Ⅱ型断裂。剪切箱试验(即压缩剪切)成为实现岩石真实Ⅱ型断裂并确定岩石Ⅱ型断裂韧性的潜在标准方法。

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