岩土力学 ›› 2026, Vol. 47 ›› Issue (10): 3633-3650.doi: 10.16285/j.rsm.2025.1171CSTR: 32223.14.j.rsm.2025.1171

• 数值分析 • 上一篇    下一篇

天然裂缝影响下干热岩水/超临界CO2压裂机制数值研究

禹海涛1, 2,张改2,闫晓3,姜文河2,王海波4,李栓5   

  1. 1.同济大学 土木工程防灾减灾国家重点实验室,上海 200092;2.同济大学 土木工程学院 地下建筑与工程系,上海 200092; 3.同济大学 航空航天与力学学院,上海 200092;4.中石化石油勘探开发研究院,北京 100089;5.青海大学 土木水利学院,青海 西宁 810016
  • 收稿日期:2025-11-01 接受日期:2026-03-25 出版日期:2026-10-10 发布日期:2026-10-09
  • 通讯作者: 闫晓,女,1994年生,博士,助理教授,主要从事多相多场耦合计算与深地能源工程研究。E-mail: xiao_yan@tongji.edu.cn
  • 作者简介:禹海涛,男,1983年生,博士,教授,主要从事岩土与深地工程防灾减灾研究。E-mail: yuhaitao@tongji.edu.cn
  • 基金资助:
    国家自然科学基金青年基金(No. 42307209);青海省科技计划(No. 2024-ZJ-717)。

Numerical investigation of water/supercritical CO₂ fracturing mechanisms in hot dry rock with pre-existing fractures

YU Hai-tao1, 2, ZHANG Gai2, YAN Xiao3, JIANG Wen-he2, WANG Hai-bo4, LI Shuan5   

  1. 1. State Key Laboratory of Disaster Reduction in Civil Engineering, Tongji University, Shanghai 200092, China; 2. Department of Geotechnical Engineering, College of Civil Engineering, Tongji University, Shanghai 200092, China; 3. School of Aerospace Engineering and Applied Mechanics, Tongji University, Shanghai 200092, China; 4. Petroleum Exploration and Production Research Institute of SINOPEC, Beijing 100089, China; 5. School of Civil Engineering and Water Resources, Qinghai University, Xining, Qinghai 810016, China
  • Received:2025-11-01 Accepted:2026-03-25 Online:2026-10-10 Published:2026-10-09
  • Supported by:
    This work was supported by the National Natural Science Foundation for Young Scientists of China (42307209) and the Natural Science Foundation of Qinghai Province (2024-ZJ-717).

摘要:

目前干热岩(hot dry rock,简称HDR)地热储层开发主要采用水-增强型地热系统(enhanced geothermal system,简称EGS)和CO2-EGS两种技术手段。高温干热岩储层中天然裂缝的存在显著影响压裂裂缝扩展,并且裂缝之间的相互作用与压裂液的性质密切相关。然而,与传统水力压裂相比,干热岩储层超临界CO2(supercritical CO2,简称ScCO2)压裂裂缝与天然裂缝相互作用模式及其机制尚不明晰,且缺乏对水和ScCO2压裂裂缝与天然裂缝相交模式的差异性研究。为此,建立了分别考虑水和ScCO2作用下的岩体热-流-固-损伤耦合模型,通过物理试验验证了数值模型模拟压裂裂缝扩展及相交模式的正确性,并开展了不同原地环境(水平应力差、天然裂缝倾角、胶结强度)和施工条件(注入温度、注入速率)下的压裂模拟。结果表明,裂缝相交模式可分为沿天然裂缝转向、偏移交叉与穿透天然裂缝3种类型。与注入低温水相比,低温ScCO2诱导热应力使得注入温度每降低10 ℃,裂缝的平均起裂压力和平均扩展压力分别降低了17.86%和0.9%。高温环境下ScCO2远比水更能有效渗透至微孔隙并连通天然裂缝,使得不同储层水平地应力差、天然裂缝逼近角及注入速率变化条件下,更易激活天然裂缝并形成交叉裂缝。此外,ScCO2压裂适用于深部高温、天然裂缝发育且胶结强度中低的干热岩储层;而水力压裂则更适合于需产生定向裂缝扩展路径的高胶结或高应力差井段。该研究成果对合理选择干热岩压裂液并改善裂缝网络形态具有理论指导意义。

关键词: 天然裂缝, 干热岩, 多场耦合, 水力压裂, 超临界CO2压裂

Abstract:

Water-enhanced geothermal system (EGS) and CO2-EGS are currently the primary technologies for geothermal resource extraction in hot dry rock (HDR) reservoirs. The presence of natural fractures in high-temperature HDR reservoirs significantly affects the fracture propagation path, and the interactions between fracturing fractures and natural fractures are closely related to the fracturing fluid. However, compared to conventional hydraulic fracturing, the interaction patterns and mechanisms between fractures during supercritical CO2 (ScCO2) fracturing in HDR reservoirs remain unclear in existing studies. Moreover, there is a lack of comparative analysis on the fracture interaction patterns and mechanisms between hydraulic fracturing and ScCO2 fracturing in the presence of natural fractures. A thermo-hydro-mechanical-damage coupled model is developed to simulate the interaction between fractures during water/ScCO2 fracturing in a HDR reservoir, which is validated by experimental results. Numerical simulations are then conducted under different in-situ conditions (horizontal stress difference, natural fracture inclination angle, cementation strength) and operational parameters (injection temperature and injection rate). The results show that the interaction patterns can be categorized into three types: turning along natural fractures, offsetting and crossing, and penetration through natural fractures. Compared to low-temperature water injection, the thermal stress induced by low-temperature ScCO2 reduces the initiation pressure and extension pressure by 17.86% and 0.9%, respectively, for every 10 °C decrease in injection temperature. Under high-temperature environments, ScCO2 has significantly higher permeability than water, allowing it to more effectively diffuse into micro-pores and connect natural fractures. This leads to intersecting fractures under varying reservoir horizontal stress differences, natural fracture inclination angles and injection rate conditions during ScCO2 fracturing. Additionally, the study further reveals that ScCO2 fracturing is suitable for deep, high-temperature, naturally fractured geothermal reservoirs with moderate to low cementation strength, facilitating the development of complex fracture networks. In contrast, hydraulic fracturing is more appropriate for intervals characterized by high cementation strength or elevated stress differences, where strict control over fracture propagation paths is required. These findings provide theoretical guidance for the rational selection of fracturing fluids and optimization of fracture network morphology in geothermal reservoir stimulation.

Key words: natural fracture, hot dry rock, multi-field coupling, hydraulic fracturing, supercritical CO2 fracturing

中图分类号: TU 456
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