岩土力学 ›› 2025, Vol. 46 ›› Issue (11): 3473-3484.doi: 10.16285/j.rsm.2025.0086CSTR: 32223.14.j.rsm.2025.0086

• 基础理论与实验研究 • 上一篇    下一篇

裂隙介质中毛细黏聚作用影响颗粒运移-堵塞机制研究

张仁君1, 2,肖碧3,杨志兵1, 2,郑小康3,胡冉1, 2,陈益峰1, 2   

  1. 1. 武汉大学 水资源工程与调度全国重点实验室,湖北 武汉 430072;2. 武汉大学 水工岩石力学教育部重点实验室,湖北 武汉 430072; 3. 长江勘测规划设计研究有限责任公司,湖北 武汉 430010
  • 收稿日期:2025-01-25 接受日期:2025-11-04 出版日期:2025-11-14 发布日期:2025-11-11
  • 通讯作者: 杨志兵,男,1982年生,博士,教授,博士生导师,主要从事多孔和裂隙介质渗流理论与控制方面的研究工作。E-mail: zbyang@whu.edu.cn
  • 作者简介:张仁君,男,1999年生,博士,博士后,主要从事裂隙岩体多相渗流方面的研究。E-mail: rjZhang@whu.edu.cn
  • 基金资助:
    国家重点研发计划项目(No. 2024YFE0197700);国家自然科学基金资助项目(No. 52494972,No. 42377066)

Investigation on mechanisms of particle migration and clogging affected by capillary-cohesion in fractured media

ZHANG Ren-jun1, 2, XIAO Bi3, YANG Zhi-bing1, 2, ZHENG Xiao-kang3, HU Ran1, 2, CHEN Yi-feng1, 2   

  1. 1. State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, Hubei 430072, China; 2. Key Laboratory of Rock Mechanics in Hydraulic Structural Engineering of the Ministry of Education, Wuhan University, Wuhan, Hubei 430072, China; 3. Changjiang Institute of Survey, Planning, Design and Research Co., Ltd, Wuhan, Hubei 430010, China
  • Received:2025-01-25 Accepted:2025-11-04 Online:2025-11-14 Published:2025-11-11
  • Supported by:
    This work was supported by the National Key Research and Development Program of China (2024YFE0197700) and the National Natural Science Foundation of China (52494972, 42377066).

摘要: 颗粒间液桥引起的毛细黏聚作用广泛存在于自然界和工程应用中,其具有胶结作用,使颗粒聚集。研究毛细黏聚颗粒在裂隙介质中的运移-堵塞过程,对于理解颗粒传输过程具有重要意义。通过可视化试验,探讨了粗糙裂隙中毛细黏聚颗粒的运移-堵塞过程,提出了堵塞模式试验相图。结果表明,毛细黏聚作用使颗粒聚集成团,粒径增大,从而显著促进裂隙堵塞,并且运移-堵塞过程在高流速下为条纹堵塞模式,低流速下为完全堵塞模式或入口密封模式。水动力学分析显示,流速分布控制着堵塞条纹的生长及主要渗流通道的改变。此外,Smoluchowski理论能够较好地描述堵塞条纹随时间的线性增长规律。研究成果为评价和控制裂隙中颗粒运移-堵塞过程提供了理论依据和技术思路。

关键词: 毛细黏聚作用, 裂隙渗流, 颗粒迁移, 堵塞

Abstract:

The cohesion effect induced by liquid bridges between particles, which promotes particle aggregation, is widespread in both natural environments and engineering applications. Understanding the migration and clogging processes of particles in fractured media under the influence of capillary-cohesion is crucial for advancing particle transport knowledge. Through visualization experiments and seepage calculations, the processes of capillary-cohesive particle migration and clogging are studied. A phase diagram of clogging patterns in the space of capillary-cohesion and flowrate is proposed. Experimental results show that capillary- cohesion induces particle agglomeration, increasing effective particle diameter and significantly enhancing fracture clogging. Stripe-like clogging patterns occur at high flow rates, while complete clogging patterns or entrance sealing patterns occur at low flow rates. Hydrodynamic analysis reveals that fluid velocity distributions control the growth of clogging stripes and the change in residual flow channels in the complete clogging patterns. Furthermore, Smoluchowski theory effectively describes the linear growth behavior of clogging stripes over time. These findings elucidate the mechanism of capillary-cohesive particle migration and clogging in rock fractures, providing theoretical and technical guidance for evaluating and controlling particle transport in fractured media.

Key words: capillary-cohesion, fracture seepage, particle migration, clogging

中图分类号: TU 441
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