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雁列裂纹破裂过程的数值模型

Numerical Model for Fracture Process of Echelon Crack

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【作者】 宋惠珍袁岩光

【Author】 Song Huizhen Yuan Yanguang (Inatitute Of Geology,State Seismological Bureau)

【机构】 国家地震局地质研究所

【摘要】 本文介绍了用裂纹扩展模型计算的雁列裂纹应力场及势剪破裂区,裂纹模型可以反映出由于裂纹离面的摩擦滑动和尖端张破裂扩张导致变形局部化,计算采用平面应力有限单元模型,岩石的弹性模量E=1011Pa,泊松比v=0。25,裂纹离面的摩擦系数μ=0.6,裂纹面与第一坐标变量轴重合,在远场边界上施加分布荷载,σ2=5σ1,随着荷载逐步增加,雁列裂纹的两相向尖端首先发生张破裂,然后两反向外尖端也发生张破裂,计算输出了破裂过程的各阶段结果。计算表明:对左旋左阶梯的雁列裂纹,当裂纹面开始滑动但相向两尖端发生张破裂之前,由于相向内尖端的张破裂扩张,加速了反向外尖端的张破裂扩张,而与此同时,相应的势剪破裂区在外尖端张破裂扩张的反方向上形成,并占据优势。

【Abstract】 The finite element technique of fracture mechanics is used for computing the echelon crack stress field and zones of potential shear fracturing.The localization of deformation caused by the frictional slip of crack and extensions of tensile fracturing near crack tips can be revealed by the crack model.The computational method used is the finite element technique of plane-stress.Far-field stresses are chosen so thatσ2=5σ1,and the maximum compressionσ2 is 30°from the X direction.The elastic constant E and v are 1011 Pa and 0.25,respectively. There are three contact states on the crack surfaces during deformation of slot,namely〔1〕They stick each other when the normal and shear component of displacement are equal to zero.〔2〕They open each other when the normal component of traction Fn and the shear component Ft are positive constant.〔3〕They are specified to follow a linear friction law,in which the coefficient of frictionμ=0.6 when the normal component of displacements is equal to zero and the shear component of traction Ft satisfies the inequality Ft>0.We treat triangular quarter-point elements as elastic crack tip with anomaly of stress field near the crack tip. The computation shows: For left-lateral shear,left step echelon crack,before extensions of tensile fracture at inner tips of echelon crack modeⅡstress intensity is 1.331 at inner tip and 1.266 at outward tip of right half-length of crack.For left-length of crack, modeⅡstress intensity is 1.330 at inner tip and 1.256 at outward tip of left half-length of crack.Therefore,at first extensions of tensile fracturing occur at inner tips of echelon crack,then left half-length crack is connected with right half-length one.After that,modeⅡstress intensity increases to 1,477 at outward tip of right half-length and 1.468 at outward tip of left half-length.The results indicate that extensions of tensile fracturing at inner tips will facilitate tensile fracture at outward tips of echelon crack.At the same time,there appears to have two zones of potential shear fracturing,one of them is in the direction to opposite to that of the previous tensile fracture.Another is consistent with the X direction.After extension of tensile fracture at outward tip of crack zones of potential shear fracturing are dominant.

  • 【会议录名称】 第一届全国岩石力学数值计算及模型试验讨论会论文集
  • 【会议名称】第一届全国岩石力学数值计算及模型试验讨论会
  • 【会议时间】1986-06-20
  • 【会议地点】中国江西吉安
  • 【分类号】O346.1
  • 【主办单位】中国岩石力学与工程学会
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