岩土力学 ›› 2023, Vol. 44 ›› Issue (4): 1217-1229.doi: 10.16285/j.rsm.2022.0658

• 数值分析 • 上一篇    下一篇

交叉裂隙岩体裂纹扩展试验及混合有限−离散元数值模拟研究

梁东旭1,张农1, 2, 3,荣浩宇4   

  1. 1. 徐州工程学院 土木工程学院,江苏 徐州 221116;2. 中国矿业大学 矿业工程学院,江苏 徐州 221116; 3. 中国矿业大学 煤炭资源与安全开采国家重点实验室,江苏 徐州 221116;4. 河海大学 土木与交通学院,江苏 南京 210098
  • 收稿日期:2022-05-05 接受日期:2022-07-11 出版日期:2023-04-18 发布日期:2023-04-29
  • 通讯作者: 张农,男,1968年生,博士,教授,主要从事巷道围岩控制、智能掘进方面的研究。E-mail: zhangnong@cumt.edu.cn E-mail:dongxuliang@cumt.edu.cn
  • 作者简介:梁东旭,男,1989年生,博士,讲师,主要从事岩石力学、巷道支护方面的研究。
  • 基金资助:
    国家自然科学基金重点项目(No.52034007);国家自然科学基金面上项目(No.52074263)

Experiment and hybrid finite-discrete element modelling of crack propagation in cross-fissured rock masses

LIANG Dong-xu1, ZHANG Nong1, 2, 3, RONG Hao-yu4   

  1. 1. School of Civil Engineering, Xuzhou University of Technology, Xuzhou, Jiangsu 221116, China; 2. School of Mines, China University of Mining and Technology, Xuzhou, Jiangsu 221116, China; 3. State Key Laboratory of Coal Resources and Safe Mining, China University of Mining and Technology, Xuzhou, Jiangsu 221116, China; 4. College of Civil and Transportation Engineering, Hohai University, Nanjing, Jiangsu 210098, China
  • Received:2022-05-05 Accepted:2022-07-11 Online:2023-04-18 Published:2023-04-29
  • Supported by:
    This work was supported by the Key Program of National Natural Science Foundation of China (52034007) and the General Program of National Natural Science Foundation of China (52074263).

摘要: 对预制交叉裂隙岩石试样进行裂纹扩展试验,研究了裂纹萌生、扩展、聚合过程,分析了主裂隙和轴向载荷夹角及主次裂隙夹角对裂纹起裂应力和聚合应力的影响,并用混合有限元−离散元程序,即图形处理器并行化的3D Y-HFDEM代码对试验进行了仿真计算,实现了岩石破坏从连续介质向非连续介质的过渡,对裂纹类及损伤破坏模式进行了识别,捕捉到了试验中难以发现的现象。研究表明:随主裂隙与轴向载荷夹角增加,裂纹聚合区的拉伸裂纹数量增加;裂纹起裂和聚合应力与主裂隙与轴向载荷夹角成正比;主次裂隙夹角增加,岩石的破坏模式由拉伸破坏转为剪切破坏,交叉裂隙加剧岩石破碎程度;主裂隙尖端萌生扩展的拉伸−剪切混合裂缝引起的破坏在岩石破坏中占主导地位,是导致岩体失去承载能力的主控裂纹;混合有限元−离散元仿真软件GPGPU并行化的3D Y-HFDEM IDE在岩石裂纹扩展研究中具有优势,可以捕捉实验室难以发现的损伤断裂类型,可以作为岩石裂纹扩展研究的有力工具。

关键词: 交叉裂隙, 裂纹扩展, 混合有限?离散元仿真, 聚合类型, 起裂应力

Abstract: Crack propagation experiments were conducted on the prefabricated cross-fissured rock specimens to study the crack initiation, propagation, and coalescence processes. The effects of the angle between the primary fissure and the axial load and the angle between the primary and minor fissures on the crack initiation stress and the coalescence stress were analyzed. The experiments were modelled and calculated with a hybrid finite-discrete element program, i.e., 3D Y-HFDEM code parallelized by a graphic processor. The transition of rock damage from continuous to the discontinuous medium was achieved. Crack categories and damage modes were identified and the phenomenon that was difficult to find in the experiments was captured. It is shown that the number of tensile cracks in the crack coalescence zone increases as the angle between the main fissure and the axial load increases. The crack initiation and coalescence stresses are proportional to the angle between the main fissure and the axial load. The damage mode of the rock changes from tensile damage to shear damage as the angle between the primary and minor fissures increases. Cross fissures increase the degree of rock fragmentation. Damage caused by mixed tensile-shear cracks initiating and propagating at the tip of the primary fissure dominates the rock damage and is the main control fissure leading to the loss of bearing capacity of the rock mass. The hybrid finite-discrete element simulation software GPGPU parallelized 3D Y-HFDEM IDE is advantageous in study of rock crack propagation to capture damage and fracture types that are difficult to detect in the laboratory, and can be a powerful tool for study of rock crack propagation.

Key words: rossed fissures, crack extension, 3D hybrid finite-discrete element modelling, coalescence category, crack initiation stress

中图分类号: TU452
[1] 刘一鸣, 李振, 冯国瑞, 杨鹏, 白锦文, 黄炳雄, 李东, . 循环加卸载下裂隙砂岩声−热响应特征及前兆规律[J]. 岩土力学, 2025, 46(9): 2773-2791.
[2] 李满, 辛昊哲, 刘先珊, 张帆, 胡大伟, 杨福见, . 基于修正相场模型的岩体混合模式破裂数值研究[J]. 岩土力学, 2025, 46(8): 2600-2612.
[3] 马鹏飞, 张艺晨, 袁超, 徐茂洲, 郭小雄, . 软弱层岩体间隔破裂现象的近场动力学方法模拟[J]. 岩土力学, 2025, 46(7): 2296-2307.
[4] 都海龙, 金爱兵, 秦文静, 商瑞豪, 王传江, 马赛, . 单轴压缩下水泥注浆煤岩力学性能及损伤特征研究[J]. 岩土力学, 2025, 46(5): 1521-1533.
[5] 周建, 廖星川, 刘福深, 尚肖楠, 沈君逸, . 应用卷积近场动力学快速模拟随机裂纹扩展[J]. 岩土力学, 2025, 46(2): 625-639.
[6] 王帅, 王豫徽, 王玲, 李佳祺, 赵梓皓, 庞凯旋, . 基于晶体模型的岩石孔隙结构与矿物组成对裂纹扩展影响机制研究[J]. 岩土力学, 2025, 46(10): 3289-3301.
[7] 韩勇, 李树忱, 袁超, 冯现大, 王修伟, . 单轴压缩下薄喷裂隙红砂岩力学性质与裂纹扩展特征分析[J]. 岩土力学, 2024, 45(9): 2583-2594.
[8] 王贵宾, 刘桓兑, 唐明豪, 杨春和, 陈世万, . 复杂应力路径下的花岗岩洞室开挖损伤区研究[J]. 岩土力学, 2024, 45(9): 2539-2553.
[9] 张朝俊, 吴顺川, 储超群, 庞瑞, . 裂隙砂岩应变场演化与超声时移衰减特征研究[J]. 岩土力学, 2024, 45(5): 1284-1296.
[10] 张宪尚, 文光才, 朱哲明, 隆清明, 刘杰, . 冲击荷载下充填节理岩体I型裂纹动态扩展特性研究[J]. 岩土力学, 2024, 45(2): 396-406.
[11] 徐浩淳, 金爱兵, 赵怡晴, 陈哲, . 热处理砂岩不同接触角巴西劈裂数值模拟研究[J]. 岩土力学, 2022, 43(S2): 588-597.
[12] 杨恩光, 杨立云, 胡桓宁, 汪自扬, 张飞. 单轴压缩荷载下闭合裂纹扩展的试验和数值研究[J]. 岩土力学, 2022, 43(S1): 613-622.
[13] 杨科, 张寨男, 池小楼, 吕鑫, 魏祯, 刘文杰, . 循环载荷下含水砂岩裂纹演化与损伤特征试验研究[J]. 岩土力学, 2022, 43(7): 1791-1802.
[14] 张黎明, 王在泉, 赵天阳, 丛宇, . 孔隙水压力作用下砂岩裂纹扩展行为的试验研究[J]. 岩土力学, 2022, 43(4): 901-908.
[15] 武东阳, 蔚立元, 苏海健, 吴疆宇, 刘日成, 周键. 单轴压缩下加锚裂隙类岩石试块裂纹扩展试验 及PFC3D模拟[J]. 岩土力学, 2021, 42(6): 1681-1692.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!