层状千枚岩的断裂特性

蔺海晓 钱立振 程龙 郭腾飞

蔺海晓, 钱立振, 程龙, 郭腾飞. 层状千枚岩的断裂特性[J]. 高压物理学报, 2021, 35(5): 054206. doi: 10.11858/gywlxb.20210707
引用本文: 蔺海晓, 钱立振, 程龙, 郭腾飞. 层状千枚岩的断裂特性[J]. 高压物理学报, 2021, 35(5): 054206. doi: 10.11858/gywlxb.20210707
LIN Haixiao, QIAN Lizhen, CHENG Long, GUO Tengfei. Fracture Characteristics of Layered Phyllite[J]. Chinese Journal of High Pressure Physics, 2021, 35(5): 054206. doi: 10.11858/gywlxb.20210707
Citation: LIN Haixiao, QIAN Lizhen, CHENG Long, GUO Tengfei. Fracture Characteristics of Layered Phyllite[J]. Chinese Journal of High Pressure Physics, 2021, 35(5): 054206. doi: 10.11858/gywlxb.20210707

层状千枚岩的断裂特性

doi: 10.11858/gywlxb.20210707
基金项目: 国家自然科学基金(41772163,51674100)
详细信息
    作者简介:

    钱立振(1993-),男,硕士研究生,主要从事煤岩体损伤力学研究. E-mail:1668624368@qq.com

    通讯作者:

    蔺海晓(1978-),男,副教授,主要从事煤岩体损伤力学研究. E-mail:hpulhx@hpu.edu.cn

  • 中图分类号: O347.3;TU45

Fracture Characteristics of Layered Phyllite

  • 摘要: 采用中心直切槽半圆盘层状岩样测试了层状千枚岩的断裂性能,并基于黏结单元建立了层状岩石的有限元数值计算模型,系统研究了层理倾角、层理强度、层理间距及切缝倾角等参数对层状千枚岩断裂特性的影响。结果表明:当层理倾角在0°~90°范围内时,Ⅰ型断裂韧度逐渐增大,峰值载荷和峰值位移也呈增大趋势;层理倾角为零时,发生张拉破坏。层理倾角在15°~45°时,剪切破坏占主导;层理倾角在60°~90°时,张拉破坏占主导。层理倾角为零时,破坏模式受层理强度影响较小;层理倾角分别为15°和30°时,随着层理强度增大,试样由剪切破坏向拉-剪耦合破坏演化;层理倾角在45°~90°时,试样均呈现拉-剪耦合破坏,且随着层理强度增大,试样有向拉伸破坏为主演化的趋势。层理间距较小时,裂纹呈沿层–穿层阶梯状扩展趋势明显;切缝倾角较大时,裂纹穿层扩展趋势明显。

     

  • 图  不同层理倾角的岩样

    Figure  1.  Rock specimens with different bedding dip angles

    图  试样的几何尺寸和加载方向

    Figure  2.  Geometrical dimensions and loading direction of the specimens

    图  应力强度因子计算模型

    Figure  3.  Calculation model of stress intensity factor

    图  不同层理倾角试样的断裂韧度

    Figure  4.  Fracture toughness of specimens withdifferent beddings dip angles

    图  不同层理倾角试样的载荷-位移曲线

    Figure  5.  Load-displacement curves of specimens with different beddings dip angles

    图  黏结单元模型

    Figure  6.  Model of bonding element

    图  黏结单元线性牵引分离定律

    Figure  7.  Linear traction separation law of bonding element

    图  试样的数值模型

    Figure  8.  Numerical model of specimens

    图  不同层理倾角页岩的断裂破坏[29]

    Figure  9.  Fracture failure of shale with different bedding dip angles[29]

    表  1  中心直切槽半圆盘无量纲应力强度因子结果比较[27]

    Table  1.   Comparison of dimensionless stress intensity factor for a half disk with a central straight slotted[27]

    a/RS/RYError/%
    This paperRef.[27]
    0.10.52.7522.7241.03
    0.30.52.4932.538−1.77
    0.80.512.850 12.665 1.46
    下载: 导出CSV

    表  2  模型中的单元力学细观参数

    Table  2.   Microscopic parameters of element mechanics in the model

    Element typeLocationElastic modulus/GPaPoisson’s ratioDensity/(kg·mm−3)
    Entity elementRock material37.760.232.623 × 103
    下载: 导出CSV
    Element typeLocationTensile strength/MPaShear strength/MPaNormal stiffness/(MPa·mm−1)Tangential stiffness/(MPa·mm−1)Failure displacement/mm
    Cohensive element
    Bedding3.39944238380.05
    Stroma6.61937768153530.10
    下载: 导出CSV

    表  3  不同层理倾角试样的试验与数值模拟结果对比

    Table  3.   Comparison between experimental and numerical simulationresults of specimens with different bedding dip angles

    Bedding dip angle/(°)Load-displacement curvesTest failure result Simulated failure result
    0
    15
    30
    45
    60
    75
    90
    下载: 导出CSV

    表  4  各层理倾角试样在不同层理强度下的数值模拟破坏结果

    Table  4.   Numerical failures of each bedding dip angles' specimen under different bedding strength

    Bedding dip angle/(°)
    Simulated result
    0.50.81.11.5
    0
    15
    30
    45
    60
    75
    90
    下载: 导出CSV

    表  5  各层理倾角试样在不同层理间距下的数值模拟破坏结果

    Table  5.   Numerical simulation failure results of each bedding dip angles' specimen under different bedding distance

    Bedding dip angle/(°)
    Simulated result
    d=3 mmd=5 mmd=8 mmd=12 mm
    0
    15
    30
    45
    60
    75
    90
    下载: 导出CSV

    表  6  各层理倾角试样在不同切缝倾角下的数值模拟破坏结果

    Table  6.   Numerical failures of each bedding dip angles' specimen under different cutting seam dip angles

    Bedding dip angle/(°)
    Simulated result
    β=0°β=30°β=45°β=60°
    0
    15
    30
    45
    60
    75
    90
    下载: 导出CSV
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  • 收稿日期:  2021-01-11
  • 修回日期:  2021-01-28

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