张晗, 张晓平, 张旗, 等. 2023. 含双裂隙试样裂纹贯通细观机理研究[J]. 工程地质学报, 31(3): 968-980. doi: 10.13544/j.cnki.jeg.2021-0071.
    引用本文: 张晗, 张晓平, 张旗, 等. 2023. 含双裂隙试样裂纹贯通细观机理研究[J]. 工程地质学报, 31(3): 968-980. doi: 10.13544/j.cnki.jeg.2021-0071.
    Zhang Han, Zhang Xiaoping, Zhang Qi, et al. 2023. Study on meso-mechanism of crack coalescence in specimens containing double pre-existing flaws[J]. Journal of Engineering Geology, 31(3): 968-980. doi: 10.13544/j.cnki.jeg.2021-0071.
    Citation: Zhang Han, Zhang Xiaoping, Zhang Qi, et al. 2023. Study on meso-mechanism of crack coalescence in specimens containing double pre-existing flaws[J]. Journal of Engineering Geology, 31(3): 968-980. doi: 10.13544/j.cnki.jeg.2021-0071.

    含双裂隙试样裂纹贯通细观机理研究

    STUDY ON MESO-MECHANISM OF CRACK COALESCENCE IN SPECIMENS CONTAINING DOUBLE PRE-EXISTING FLAWS

    • 摘要: 为了揭示不同裂纹贯通模式的细观演化机理,采用颗粒流程序(PFC)模拟含平行双裂隙石膏试样的单轴压缩试验。对双预制裂隙在不同相对位置时试样内出现的裂纹贯通模式进行分类,并对不同贯通模式形成过程中预制裂隙周围的力链和颗粒位移场进行分析。研究发现预制裂隙的相对位置会改变压缩过程中其周围的接触力分布以及颗粒位移趋势,进而影响预制裂隙端部以及岩桥区域裂纹的扩展路径。当两预制裂隙几乎共面时,在岩桥区域存在接触力集中情况,岩桥区域首先出现微张拉裂纹,随着加载,这些微张拉裂纹逐渐演化为宏观剪切带并连接两个预制裂隙端点,形成Ⅰ型贯通。当岩桥倾角较大且两个预制裂隙不重叠时,岩桥区域的接触力集中程度增大,岩桥区域首先出现竖向的微张拉裂纹并演化为竖向的宏观裂纹连接两个预制裂隙端点,导致Ⅱ或Ⅶb型贯通。当两个预制裂隙的端部部分重叠时,由于应力屏蔽效应,重叠端部的压缩接触力集中程度小于未重叠端部,导致翼裂纹成为主导贯通的裂纹。当两个预制裂隙在竖直方向完全重叠时,两预制裂隙同侧端点之间的接触力集中导致出现由压致拉的张拉裂纹连接预制裂隙同侧端点,形成Ⅴ型贯通。出现Ⅱ、Ⅴ和Ⅶb型贯通试样的微裂纹数量曲线呈现阶梯状增长的趋势,表明这3类贯通中宏观裂纹的扩展是由应变能的突然释放导致的。

       

      Abstract: To reveal the meso-mechanism of crack coalescence, this paper uses particle flow code(PFC) to simulate uniaxial compression test of gypsum specimens containing double parallel pre-existing flaws. The paper classifies the crack coalescence types in the specimens with different geometry of double pre-existing flaws, and analyzes the force chain and particle displacement field around the pre-existing flaws. It is found that the relative position of pre-existing flaws can affect the contact force distribution and particle displacement filed around the pre-existing flaws, and then affect the crack propagation path. When the two pre-existing flaws are nearly coplanar, there is a concentration of contact force in the rock bridge area. Micro-tensile cracks first appear in the rock bridge area and gradually evolve into macro-shear band with the loading. These micro-tensile cracks lead to type Ⅰ coalescence. When the rock bridge inclination angle is large and the two pre-existing flaws do not overlap, the contact force concentration in the rock bridge area increases. Vertical micro-tensile cracks first appear in the rock bridge area. Macro-cracks evolving from micro-tensile cracks connect pre-existing flaw tips, resulting in the type Ⅱ or Ⅶb coalescence. When the tips of two pre-existing flaws are partially overlapped, the compressive contact force concentration at the overlapped tips is smaller than that at the non overlapped tips due to the stress shielding effect, which leads to the wing cracks becoming the main cracks leading to coalescence. When the two pre-existing flaws overlap in the vertical direction, the contact force between the two pre-existing flaws on the same side tips is concentrated, resulting in tensile cracks caused by compression. Tensile cracks induced by compression connect the tips of the pre-existing flaws on the same side, forming type Ⅴ coalescence. The results show that the number of micro-cracks in the samples with type Ⅱ, Ⅴ and Ⅶb coalescence increases step by step, which indicates that the propagation of macro-cracks in these three coalescence types are caused by the sudden release of strain energy.

       

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