岩土力学 ›› 2025, Vol. 46 ›› Issue (8): 2434-2448.doi: 10.16285/j.rsm.2024.1174CSTR: 32223.14.j.rsm.2024.1174

• 基础理论与实验研究 • 上一篇    下一篇

气压-应力耦合作用下盐岩应力松弛特性研究

刘雯1, 2,范金洋1, 2,刘文浩1, 2,陈结1, 2,刘伟1, 2,吴斐1, 2   

  1. 1. 重庆大学 煤矿灾害动力学与控制国家重点试验室,重庆 400044;2. 重庆大学 资源与安全学院,重庆 400044
  • 收稿日期:2024-09-23 接受日期:2024-12-17 出版日期:2025-08-11 发布日期:2025-08-14
  • 通讯作者: 范金洋,男,1989年生,博士,教授,主要从事岩土力学、采矿工程、安全工程方面的研究。E-mail:Jinyang.f@cqu.edu.cn
  • 作者简介:刘雯,女,2002年生,硕士研究生,主要从事盐穴储氢稳定性方面的研究。E-mail:cqlw3708@163.com
  • 基金资助:
    科技部国家重点研发计划(课题)(No. 2024YFB4007103)

Stress relaxation characteristics of salt rock under the action of air barometric stress coupling

LIU Wen1, 2, FAN Jin-yang1, 2, LIU Wen-hao1, 2, CHEN Jie1, 2, LIU Wei1, 2, WU Fei1, 2   

  1. 1. State Key Laboratory for the Coal Mine Disaster Dynamics and Controls, Chongqing University, Chongqing 400044 China; 2. School of Resources and Safety, Chongqing University, Chongqing 400044 China
  • Received:2024-09-23 Accepted:2024-12-17 Online:2025-08-11 Published:2025-08-14
  • Supported by:
    This work was supported by the National Key Research and Development Program of the Ministry of Science and Technology (Project) (2024YFB4007103).

摘要: 为保障国家能源安全,近年来国家加大了对压缩空气储能技术的研发投入,这类工程较以往常规工程情况更为复杂,岩石的应力松弛特性也会受更多因素影响。针对压缩空气储能工程特点,从新研究角度出发,进行了气压-应力耦合作用下盐岩应力松弛试验,探究不同气压、轴向启动应力条件下盐岩的应力松弛特性。结果表明:(1)盐岩的应力松弛宏观规律不受气压影响,气压-应力耦合作用下盐岩的应力松弛仍可划分为快速、减速、稳定松弛3个阶段。其中,快速松弛阶段的松弛量占整体松弛量50%左右,而稳定松弛阶段在整个松弛过程中占比最大;(2)盐岩应力松弛受轴向启动应力和气压影响,轴向启动应力和气压越高,应力松弛初速度越大,稳定松弛阶段的松弛速率越大,应力松弛度越大;(3)循环气压下盐岩的应力松弛为循环性松弛,松弛曲线受控于其循环上下限对应的恒定气压时盐岩的应力松弛曲线;(4)松弛后盐岩的环境扫描电镜(environmental scanning electron microscopy,ESEM)图像表明,微裂纹产生和发展是造成盐岩内部损伤的主要机制。松弛后盐岩的细观结构损伤主要有晶粒碎屑、晶内裂纹、沿晶裂纹和穿晶裂纹;(5)改进的非线性二单元广义Maxwell松弛模型可以较好地描述不同的启动应力、气压条件下盐岩的应力松弛行为,为盐穴压缩空气储能库的稳定性评估提供一定参考。

关键词: 盐岩, 气压-应力耦合, 应力松弛, 非线性应力松弛模型

Abstract: To enhance national energy security, recent years have witnessed an increase in state investment directed towards the research and development of compressed air energy storage (CAES) technology. These initiatives are inherently more complex than traditional projects, as the stress relaxation characteristics of geological formations, particularly rocks, are influenced by a multitude of factors. According to the characteristics of CAES engineering, stress relaxation experiments of salt rock under barometric stress coupling were carried out from a new perspective to explore the stress relaxation characteristics of salt rock under different air pressures and axial starting stress conditions. The results show that: (1) The macroscopic behavior of stress relaxation in salt rock is independent of air pressure, and the process can be categorized into three distinct stages: rapid relaxation, decelerated relaxation, and stable relaxation. Notably, the rapid relaxation phase accounts for approximately 50% of the total relaxation, while the stable relaxation phase represents the predominant portion of the entire relaxation process. (2) The stress relaxation behavior of salt rock is significantly influenced by both axial starting stress and air pressure. Specifically, increased axial starting stress and air pressure correlate with heightened initial stress relaxation rates, greater relaxation rates, and an enhanced degree of stress relaxation during the stable relaxation phase. (3) Under cyclic pressure conditions, the stress relaxation of salt rock exhibits a cyclic relaxation pattern, with the relaxation curve being governed by the stress relaxation curve of salt rock at constant pressure, corresponding to its cyclic upper and lower limits. (4) Environmental scanning electron microscopy (ESEM) images of the relaxed salt rock reveal that the formation and propagation of micro-cracks constitute the primary mechanism of internal damage within the salt rock. Post-relaxation, the meso-structural damage observed in the salt rock includes grain debris, intragranular cracks, intergranular cracks, and trans-granular cracks. (5) The improved nonlinear two-element generalized Maxwell relaxation model can better describe the stress relaxation behavior of salt rock under different starting stresses and pressure conditions, and provide a certain reference for the stability assessment of salt cavern compressed air energy storage.

Key words: salt rock, barometric stress coupling, stress relaxation, nonlinear stress relaxation model

中图分类号: TU 452
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