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压剪作用下椭圆孔洞砂岩的裂纹扩展规律研究

邓逸 李壮 何运 刘帅 刘广川

邓逸, 李壮, 何运, 刘帅, 刘广川. 压剪作用下椭圆孔洞砂岩的裂纹扩展规律研究[J]. 岩土工程技术, 2026, 40(4): 608-615. doi: 10.20265/j.cnki.issn.1007-2993.2025-0210
引用本文: 邓逸, 李壮, 何运, 刘帅, 刘广川. 压剪作用下椭圆孔洞砂岩的裂纹扩展规律研究[J]. 岩土工程技术, 2026, 40(4): 608-615. doi: 10.20265/j.cnki.issn.1007-2993.2025-0210
DENG Yi, LI Zhuang, HE Yun, LIU Shuai, LIU Guangchuan. Crack propagation laws in sandstone containing elliptical holes under compression-shear loading[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(4): 608-615. doi: 10.20265/j.cnki.issn.1007-2993.2025-0210
Citation: DENG Yi, LI Zhuang, HE Yun, LIU Shuai, LIU Guangchuan. Crack propagation laws in sandstone containing elliptical holes under compression-shear loading[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(4): 608-615. doi: 10.20265/j.cnki.issn.1007-2993.2025-0210

压剪作用下椭圆孔洞砂岩的裂纹扩展规律研究

doi: 10.20265/j.cnki.issn.1007-2993.2025-0210
基金项目: 国家自然科学基金(51804058);重庆市教委科学技术研究项目(KJQN201800729)
详细信息
    作者简介:

    邓 逸,男,1978年生,大学本科,高级工程师,主要从事岩土工程、地下工程等领域的研究工作。E-mail:3560115641@qq.com

    通讯作者:

    刘 帅,男,2001年生,在读硕士研究生,主要从事地下工程等领域的研究工作。E-mail:1505695343@qq.com

  • 中图分类号: TU45

Crack propagation laws in sandstone containing elliptical holes under compression-shear loading

  • 摘要: 为揭示压剪作用下椭圆孔洞砂岩的裂纹扩展规律及其主控因素作用机制,依据室内试验结果,标定砂岩的数值模拟细观力学参数,开展不同孔洞倾角和长短轴比下的压剪数值试验,并对裂纹扩展规律及影响因素作用机制进行分析。研究结果表明:(1)峰值剪切应力、起裂应力及二者差值均随孔洞倾角增大呈先减后增趋势;当孔洞倾角为60°时,三者均达到最小值,试件最易达到破坏状态。(2)平均起裂角随孔洞倾角的增加表现为先增大、后减小、再增大的趋势,并在孔洞倾角为30°,120°时分别取得最大、最小值;起裂角与长短轴比之间未表现出明显相关性。(3)孔洞倾角和长短轴比显著影响裂纹扩展行为,但其作用机制不同。其中,孔洞倾角通过改变应力分布主导裂纹起裂位置和扩展路径,长短轴比通过改变孔洞几何形状影响局部应力状态,进而控制裂纹扩展行为。研究结论可为含孔洞岩体工程稳定性控制与评估提供理论依据。

     

  • 图  1  平行黏结模型示意图

    Figure  1.  Schematic diagram of parallel bonding model

    图  2  数值模拟模型

    Figure  2.  Numerical simulator

    图  3  应力−应变曲线

    Figure  3.  Stress−strain curve

    图  4  破坏形态

    Figure  4.  Destruction form

    图  5  起裂应力随法向压应力变化图(α=30°,k=3)

    Figure  5.  Crack initiation stress vs. normal compressive stress variation diagram (α=30°, k=3)

    图  6  起裂应力随孔洞倾角变化图(k=3,σc=3 MPa)

    Figure  6.  The variation diagram of crack initiation stress with hole inclination angle (k=3, σc=3 MPa)

    图  7  起裂角监测

    Figure  7.  Cracking angle monitoring

    图  8  平均起裂角

    Figure  8.  Average crack initiation angle

    图  9  裂纹扩展破坏情况(α=30°,k=3,σc=3 MPa)

    Figure  9.  Crack propagation failure (α=30°, k=3, σc=3 MPa)

    表  1  平行黏结模型宏观参数

    Table  1.   Macroscopic parameters of parallel bond model

    场景抗压强度/MPa抗拉强度/MPa弹性模量/GPa泊松比
    室内试验71.237.0812.040.185
    数值模拟73.247.8311.970.185
    下载: 导出CSV

    表  2  平行黏结模型细观参数

    Table  2.   Mesoscopic parameters of parallel bond model

    颗粒参数 取值 黏结参数 取值
    颗粒最小半径/mm 0.45 平行黏结弹性模量/GPa 5.5
    颗粒最大半径/mm 0.75 平行黏结刚度比 1.6
    颗粒密度/(kg∙m−3 2574 平行黏结法向强度/MPa 15
    颗粒摩擦系数 0.5 平行黏结黏聚力/MPa 28
    颗粒接触刚度比 1.6 平行黏结内摩擦角/(°) 35
    颗粒接触模量/GPa 5.5 平行黏结半径系数 1
    下载: 导出CSV

    表  3  不同倾角α下裂纹扩展模式(k=3)

    Table  3.   Crack propagation modes under different inclination angles α (k=3)

    椭圆孔洞倾角
    α=0° α=30° α=60° α=90° α=120° α=150°
    压应力 压应力集中区 拉应力集中区
    下载: 导出CSV

    表  4  不同长短轴比k下裂纹扩展模式(α=30°)

    Table  4.   Crack propagation mode under different long-short axis ratio k (α=30°)

    椭圆孔洞长短轴比
    k=1 k=2 k=3 k=4 k=5 k=6
    压应力 压应力集中区 拉应力集中区
    下载: 导出CSV
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出版历程
  • 收稿日期:  2025-05-09
  • 修回日期:  2025-08-28
  • 录用日期:  2025-09-01
  • 刊出日期:  2026-08-08

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