岩土力学 ›› 2026, Vol. 47 ›› Issue (5): 1777-1787.doi: 10.16285/j.rsm.2025.0577CSTR: 32223.14.j.rsm.2025.0577

• 数值分析 • 上一篇    下一篇

循环注采作用下盐穴储氢库温度和压力演化建模与分析

陈祥胜1, 2,施锡林3,李银平3,丁海滨1, 2,罗如平1, 2   

  1. 1. 华东交通大学 土木建筑学院,江西 南昌 330013;2. 华东交通大学 山区土木工程安全与韧性全国重点实验室,江西 南昌 330013; 3. 中国科学院武汉土力学研究所 岩土力学与工程安全全国重点实验室,湖北 武汉 430071
  • 收稿日期:2025-06-03 接受日期:2025-12-09 出版日期:2026-05-11 发布日期:2026-05-12
  • 作者简介:陈祥胜,男,1994年生,博士,副教授,主要从事盐岩能源地下储备、岩石力学等方面的研究。E-mail:chenxs15@163.com
  • 基金资助:
    国家自然科学基金项目(No. 52208372);江西省自然科学基金项目(No. 20242BAB23037,No. 20232BAB204072);江西省赣鄱俊才支持计划·青年科技人才托举项目(No. 2025QT11)。

Modeling and analyzing the evolution of temperature and pressure in a salt cavern hydrogen storage under cyclic injection and production

CHEN Xiang-sheng1, 2, SHI Xi-lin3, LI Yin-ping3, DING Hai-bin1, 2, LUO Ru-ping1, 2   

  1. 1. School of Civil Engineering and Architecture, East China Jiaotong University, Nanchang, Jiangxi 330013, China; 2. State Key Laboratory of Safety and Resilience of Civil Engineering in Mountain Area, East China Jiaotong University, Nanchang, Jiangxi 330013, China; 3. State Key Laboratory of Geomechanics and Geotechnical Engineering Safety, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China
  • Received:2025-06-03 Accepted:2025-12-09 Online:2026-05-11 Published:2026-05-12
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (52208342), the Jiangxi Provincial Natural Science Foundation (20242BAB23037, 20232BAB204072) and Jiangxi Province Ganpo Outstanding Talents Support Program-Young Scientific and Technological Talent Development Project (2025QT11).

摘要: 准确揭示盐腔压力和温度演化规律是分析盐穴储氢库稳定性和密闭性安全的必要条件。基于循环注采作用下腔内热- 流-固耦合效应,建立了腔内温度和压力演化模型,提出了围岩温度影响区范围和热应力计算方法。模型的有效性和准确性得到了加拿大Melville盐穴储库现场温度和压力监测数据的验证,吻合度高达90%以上。研究结果表明:循环注采作用下盐穴储氢库腔内温度随时间呈浪花形周期性变化,函数关系为分段的双指数函数;腔内压力随时间呈异形锯齿波周期性变化,函数关系为分段的线性函数与双指数函数。二者首先经历同步上升(注氢)或下降(采氢)阶段,注采停止后转向同步稳定阶段,各阶段持续时间主要由注采压力、流量以及围岩对流换热效应控制。日注采模式下,同步稳定阶段的压力在短期内变化极其缓慢,压力将演变为梯形波周期性变化。循环注采期间围岩因腔内温度变化将派生出热应力和附加位移,8~16 MPa的单一注采工况下,盐腔温度波动影响范围主要集中在腔壁围岩5 m范围之内。由于氢气的热传递和对流换热效率最高,注采氢在围岩中的温度影响区大于其他能源存储气体。

关键词: 盐穴储氢库, 循环注采, 热-流-固耦合, 温度和压力演化

Abstract: Accurately revealing the evolution patterns of pressure and temperature in salt caverns is essential for analyzing the stability and safety of hydrogen storage facilities. A model was developed to describe the evolution of temperature and pressure in the cavern, based on the thermo-hydro-mechanical coupling effects during cyclic injection and production. Additionally, methods for calculating the temperature influence zone and thermal stress in the surrounding rock were proposed. The model’s validity and accuracy were verified using on-site temperature and pressure monitoring data from the Melville salt cavern storage facility in Canada, achieving over 90% consistency. The research results indicate that, under cyclic injection and production, the temperature in the salt cavern hydrogen storage facility exhibits a wave-like periodic variation over time, described by a piecewise bi-exponential function. In contrast, the pressure varies periodically in the form of an irregular sawtooth wave, represented by a piecewise combination of linear and bi-exponential functions. Both temperature and pressure initially experience synchronous increases (during injection) or decreases (during production), followed by a synchronous stabilization phase after injection and production cease. The duration of each phase is primarily influenced by the injection and production pressures, flow rate, and the convective heat transfer effects in the surrounding rock. Under daily injection and production modes, the pressure during the stabilization phase changes very slowly in the short term, evolving into a periodic trapezoidal wave pattern. During cyclic injection and production, the surrounding rock experiences thermal stress and additional displacement due to temperature changes in the cavern. The temperature fluctuations in the salt cavern primarily affect the surrounding rock within 5 m of the cavern wall under single injection and production conditions ranging from 8 MPa to 16 MPa. Due to hydrogen’s superior heat transfer and convective efficiency, the temperature influence zone in the surrounding rock during hydrogen injection and production is significantly larger than that of other energy storage gases.

Key words: salt cavern hydrogen storage, cyclic injection and production, thermo-hydro-mechanical coupling, temperature and pressure evolution

中图分类号: TU 452
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