岩土力学 ›› 2025, Vol. 46 ›› Issue (1): 199-212.doi: 10.16285/j.rsm.2024.0380

• 基础理论与实验研究 • 上一篇    下一篇

循环荷载作用下含倾斜单裂隙砂岩力学响应特征及渗流演化规律

唐劲舟1, 2,唐文豪1, 2,杨科1, 2, 3,赵延林4,刘钦节1, 2, 3,段敏克1, 2,谭哲4   

  1. 1.安徽理工大学 矿业工程学院 安徽 淮南,232001;2.安徽理工大学 安徽省关闭废弃矿井资源开发利用工程研究中心,安徽 淮南,232001; 3.合肥综合性国家科学中心能源研究院,安徽 合肥,230031;4.湖南科技大学 资源环境与安全工程学院,湖南 湘潭,411201
  • 收稿日期:2024-03-29 接受日期:2024-08-08 出版日期:2025-01-10 发布日期:2025-01-04
  • 通讯作者: 杨科,男,1979年生,博士,教授,主要从事废弃矿井资源开发与利用等方面的研究工作。E-mail: keyang2003@163.com
  • 作者简介:唐劲舟,男,1990年生,博士,讲师,主要从事深部岩石力学方面的研究。E-mail: tangjinzhou@outlook.com
  • 基金资助:
    安徽高校自然科学研究项目(No.2022AH050811);安徽理工大学引进人才基金(No.2021yjrc30);安徽理工大学校级重点项目(No.QNZD2021-06)。

Mechanical response characteristics and seepage evolution patbern of sandstone with an inclined single fracture under cyclic loading

TANG Jin-zhou1, 2, TANG Wen-hao1, 2, YANG Ke1, 2, 3, ZHAO Yan-lin4, LIU Qin-jie1, 2, 3, DUAN Min-ke1, 2, TAN Zhe4   

  1. 1.School of Mining Engineering, Anhui University of Science and Technology, Huainan, Anhui 232001, China; 2. Anhui Engineering Research Center of Exploitation and Utilization of Closed/Abandoned Mine Resources, Anhui University of Science and Technology, Huainan, Anhui 232001, China; 3. Institute of Energy, Hefei Comprehensive National Science Center, Hefei, Anhui 230031, China; 4. School of Resource Environment and Safety Engineering, Hunan University of Science and Technology, Xiangtan, Hunan 411201, China
  • Received:2024-03-29 Accepted:2024-08-08 Online:2025-01-10 Published:2025-01-04
  • Supported by:
    This work was supported by the Natural Science Research Project of Anhui Educational Committee (2022AH050811), the Scientific Research Foundation for High-level Talents of Anhui University of Science and Technology (2021yjrc30) and University-level Key Projects of Anhui University of Science and Technology (QNZD2021-06).

摘要:

为了研究循环荷载对裂隙岩体力学破坏特征和渗流演化规律的影响,开展轴压和孔压低频多次循环加卸载条件下含倾斜粗糙单裂隙砂岩的应力-渗流耦合试验。结果表明:在应力的作用下,岩样沿预制裂隙面发生相对滑移,裂隙表面凸起在滑移过程中发生磨损、剪断,凸起的剪断和磨损会导致加载过程中应力的小幅跌落,也是导致流量在压缩过程中发生波动的主要原因;对于含倾斜单裂隙的试样,其强度主要取决岩块是否沿预制裂隙面产生滑移和孔压的大小;在轴压循环加卸载过程中,裂隙岩体随着循环次数的增加产生损伤劣化,试样抵抗变形的能力变弱,表现为弹性模量非线性下降,泊松比非线性上升;孔压循环加卸载会减短衰减蠕变段的时间,在稳定蠕变阶段会减小蠕变的应变率;循环加卸载过程中流量是一个动态演化的过程,在加载初期,因为裂隙在应力的作用下发生闭合,流量呈下降趋势,随后流量随着轴压的循环加载―卸载而减小―增大;基于灰度阈值分割方法可以将裂隙的连通域和接触域较好的分离开,连通域与整个裂隙面面积相比得到的裂隙连通率Ф,最终流量随分形维数 与裂隙连通率 Ф 的增大呈指数级增大。

关键词: 裂隙岩体, 循环加卸载, 力学特性, 渗流, 形貌表征

Abstract:

To investigate the impact of cyclic loading on the mechanical damage characteristics and seepage evolution of fractured rock mass, the stress-seepage coupling tests were conducted on sandstone samples containing an inclined rough single fracture under conditions of axial and pore pressures low frequency repeatedly loading and unloading. The results indicate that under stress, rock samples exhibit relative slip along pre-existing fractures, with surface protrusions undergoing wear and shear. These protrusions cause a slight stress drop during loading, leading to flow rate fluctuations during compression. For samples with inclined fractures, strength is mainly determined by slip along pre-existing fractures and pore pressure magnitude. During cyclic loading and unloading under axial compression, fractured rock mass undergoes progressive damage and deterioration with increasing cycles. This reduces the samples’ ability to resist deformation. Additionally, samples exhibit a nonlinear decrease in elastic modulus and a nonlinear increase in Poisson’s ratio with increasing cycles. Pore pressure cycling shortens the decay creep stage and reduces strain rates in the stable creep stage. The flow rate dynamically evolves during cyclic loading and unloading. Initially, the flow rate decreases due to fracture closure under stress. Subsequently, it decreases and then increases with cyclic axial stress. The grayscale threshold segmentation method effectively separates connected and contact zones of fractures. It shows that final flow increases exponentially with increases in fractal dimension D and connection ratio Φ.

Key words: fractured rock mass, cyclic loading and unloading, mechanical properties, seepage, morphological characterization

中图分类号: TD 435
[1] 刘佳奇, 张碧川, 冯增朝, 李学成, 郭纪哲. 实时高温循环加卸载下花岗岩双轴力学特性[J]. 岩土力学, 2026, 47(5): 1553-1566.
[2] 蔡天佐, 宋勇军, 张森, 龚泊友, 田汝栋, 刘贯飞. 温度-渗流-应力耦合作用下冻融砂岩蠕变特性试验研究[J]. 岩土力学, 2026, 47(5): 1583-1596.
[3] 黄娟, 章驰, 余俊. 任意埋深下体外排水隧道渗流场解析解[J]. 岩土力学, 2026, 47(5): 1621-1631.
[4] 潘泓, 黄才穆, 骆冠勇, 彭斯格, 刘荣照, 曹洪. 富水复合砂层突涌破坏行为及孔压响应特征试验研究[J]. 岩土力学, 2026, 47(4): 1171-1182.
[5] 姜景山, 左永振, 程展林, 潘家军, 黄鑫, 占飞杰. 粗粒料力学特性的应力路径大型真三轴试验研究[J]. 岩土力学, 2026, 47(3): 755-766.
[6] 王志良, 肖智桓, 申林方, 李邵军. 基于物理信息神经网络岩石裂隙渗流传热耦合作用机制研究[J]. 岩土力学, 2026, 47(2): 703-716.
[7] 杨云钦, 韩立军. 开采扰动影响下巷道围岩损伤与渗透特性演化规律研究[J]. 岩土力学, 2026, 47(1): 101-114.
[8] 贾宝新, 袁庆雷. 注浆影响下隧道渗流场及最小覆土厚度修正研究[J]. 岩土力学, 2026, 47(1): 255-266.
[9] 张胜, 柏巍, 徐鼎平, 郑虹, 江权, 李志伟, 向天兵, . 循环荷载作用下砂岩损伤演化的声发射与电阻率监测及理论研究[J]. 岩土力学, 2025, 46(S1): 53-66.
[10] 苗日成, 唐贝, 祁飞, 江志安, 崔溦, . 随机裂隙岩体滚刀破岩过程离散元模拟研究[J]. 岩土力学, 2025, 46(S1): 541-552.
[11] 吴俊, 闵一凡, 征西遥, 韩晨, 牛富俊, 朱宝林, . 地质聚合物固化淤泥法制备再生细骨料的压缩变形特性研究[J]. 岩土力学, 2025, 46(S1): 159-170.
[12] 江文豪, 王浩, 廖光志, 陈滨华, . 时变降雨场景下双层非饱和土中水分一维瞬态渗流解析解[J]. 岩土力学, 2025, 46(9): 2721-2737.
[13] 王昕琪, 冯子军, 陈正男, 高祺, 阴伟涛, 靳佩桦, 李玉彬, . 超临界水作用下花岗岩裂隙渗流特性演化规律研究[J]. 岩土力学, 2025, 46(9): 2847-2858.
[14] 屈俊童, 时启壮, 郭颖杰, 张 翔, 刘 熠, 蒋德阳. 冻融循环作用下冰碛土力学特性及损伤机制研究[J]. 岩土力学, 2025, 46(9): 2859-2872.
[15] 侯小强, 杨芮, 李瑞冬, 樊小鹏, 郑佳乐, 侯宝胜, . 卵石土混合体随机生成方法与宏细观力学演化特性研究[J]. 岩土力学, 2025, 46(9): 2967-2979.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!