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水力劈裂裂隙扩展与软弱面作用机理离散元研究
引用本文:刘帅奇,马凤山,郭捷,孙琪皓. 水力劈裂裂隙扩展与软弱面作用机理离散元研究[J]. 东北大学学报(自然科学版), 2021, 42(3): 444-456. DOI: 10.12068/j.issn.1005-3026.2021.03.021
作者姓名:刘帅奇  马凤山  郭捷  孙琪皓
作者单位:(1. 中国科学院 地质与地球物理研究所 页岩气与地质工程重点实验室, 北京100029; 2. 中国科学院 地球科学研究院, 北京100029; 3. 中国科学院大学 地球与行星科学学院, 北京100049)
基金项目:国家自然科学基金资助项目
摘    要:针对高承压水引发水力劈裂导致巷道的突水渗水问题,对离散元流固耦合算法进行改进,更新了流体通道长度和水压力对颗粒的作用模式.进行水力劈裂裂隙(HFs)与天然软弱面(WPs)相互作用的数值模拟,得到5种作用模式,并获取不同模式之间的临界水压力值,进一步分析了试件的位移、接触力以及特征点的应力变化.结果表明:1)定压力注水试...

关 键 词:颗粒离散元  流固耦合  水力劈裂  位移响应  最大主应力
收稿时间:2020-07-02
修稿时间:2020-07-02

Discrete Element Investigation on the Interaction of Hydraulic Fracturing and Weak Plane in Deep Tunnels
LIU Shuai-qi,MA Feng-shan,GUO Jie,SUN Qi-hao. Discrete Element Investigation on the Interaction of Hydraulic Fracturing and Weak Plane in Deep Tunnels[J]. Journal of Northeastern University(Natural Science), 2021, 42(3): 444-456. DOI: 10.12068/j.issn.1005-3026.2021.03.021
Authors:LIU Shuai-qi  MA Feng-shan  GUO Jie  SUN Qi-hao
Affiliation:1. Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. Innovation Academy for Earth Science, Chinese Academy of Sciences,Beijing 100029, China; 3. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China.
Abstract:Hydraulic fracturing caused by high confined water is the root cause of water inrush in roadway. The discrete element fluid-solid coupling algorithm was improved, and the action mode of fluid channel length and water pressure on particles was updated. The interaction between the hydro-splitting fractures (HFs) and the weak planes (WPs) was simulated. Five different modes were obtained and the critical pressure values were calculated. The displacement, contact force of the specimen and the various of the stress at a specific point were analyzed. The research shows that: 1) with a constant injection pressure, the pressure value is the largest at the initial crack, then gradually decreases along the crack. 2) the displacement response are different under five interaction modes. The normal contact force has obvious vertical dominant surface in its contact direction, and the shear contact force generates four vertical dominant distribution directions. 3) the stress at Mc1 changes dramatically during the initiation stage, and the maxmium principal is always compressive. Stress response in Mc2 is relatively hysteretic. The diversity of principal stress is fundamentally determined by the interaction mode between HFs and WPs.
Keywords:particle flow code(PFC)   fluid-solid coupling   hydraulic fracturing   displacement response   maximum principal stress,
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