岩土力学 ›› 2026, Vol. 47 ›› Issue (9): 3009-3024.doi: 10.16285/j.rsm.2025.1222CSTR: 32223.14.j.rsm.2025.1222

• 基础理论与实验研究 • 上一篇    下一篇

围压作用下岩石非线性断裂特性及断裂过程区长度表征

罗森林1, 2,张广清1, 2,乔佳1, 2,孙斌1, 2,周大伟1, 2   

  1. 1. 中国石油大学(北京) 石油工程学院,北京 102249;2. 中国石油大学(北京) 油气资源与工程全国重点实验室,北京 102249
  • 收稿日期:2025-11-12 接受日期:2026-04-21 出版日期:2026-09-11 发布日期:2026-09-01
  • 通讯作者: 张广清,男,1975年生,博士,教授,博士生导师,主要从事石油工程岩石力学方面的研究。E-mail: zhangguangqing@cup.edu.cn
  • 作者简介:罗森林,男,1998年生,博士研究生,主要从事岩石非线性断裂方面的研究。E-mail: yysenlin_luo@163.com
  • 基金资助:
    国家自然科学基金重点项目(No.52434001)。

Nonlinear fracture characteristics of rock under confining pressure and characterization length of fracture process zone

LUO Sen-lin1, 2, ZHANG Guang-qing1, 2, QIAO Jia1, 2, SUN Bin1, 2, ZHOU Da-wei1, 2   

  1. 1. College of Petroleum Engineering, China University of Petroleum (Beijing), Beijing 102249, China; 2. State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum (Beijing), Beijing 102249, China
  • Received:2025-11-12 Accepted:2026-04-21 Online:2026-09-11 Published:2026-09-01
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (52434001).

摘要:

深层油气资源开发潜力巨大,但储层压裂改造受到高围压影响,裂缝尖端呈现显著非线性力学行为,导致水力裂缝扩展困难。为明确围压作用下岩石的非线性断裂特性,采用黄砂岩标准单边缺口梁试件开展了围压条件下的三点弯曲断裂试验,并利用声发射采集系统监测了断裂过程区(fracture process zone,简称FPZ)发育过程。结果表明:岩石在围压作用下具有显著的非线性断裂特征,并且高围压水平延长了峰前FPZ发育和演化的整个过程。高围压水平下岩石内部的微观断裂机制由沿着矿物颗粒断裂向穿透矿物颗粒断裂转变,这种微观断裂模式的转变是导致宏观断裂面光滑化和断裂能升高的根本原因。基于内聚区模型(cohesive zone model,简称CZM),建立了围压作用下FPZ长度的解析模型。随着围压增加,FPZ长度减小,而断裂能增大,表明围压不仅约束了FPZ的发育空间,更显著提高了单位面积FPZ的能量耗散强度。宏观上表现为更高应力水平才能驱动FPZ进一步发育和裂缝扩展。这一现象反映了围压对岩石非线性断裂行为的强化效应。研究结果可为深层压裂改造提供理论支撑。

关键词: 围压, 断裂力学, 三点弯曲试验, 非线性断裂, 断裂过程区

Abstract:

Deep oil and gas resources have considerable development potential. However, reservoir fracturing is affected by high confining pressure. The fracture tip exhibits pronounced nonlinear mechanical behavior, which hinders hydraulic fracture propagation. To clarify the nonlinear fracture characteristics of rocks under confining pressure, three-point bending fracture experiments were conducted on standard single-edge notched beam specimens of yellow sandstone. The evolution of the fracture process zone (FPZ) was monitored using an acoustic emission system. The results show that rock exhibits significant nonlinear fracture characteristics under confining pressure, and that higher confining pressure prolongs the entire pre-peak evolution of the FPZ. At high confining pressures, the microscopic fracture mechanism in rock shifts from intergranular to transgranular fracture. This transition in the microscopic fracture mode is the primary reason for the smoother fracture surface and the increase in fracture energy. Based on the cohesive zone model (CZM), an analytical model was established to predict the FPZ length. As confining pressure increases, the FPZ length decreases, whereas the fracture energy increases. This indicates that confining pressure not only limits the extent of FPZ development but also significantly enhances the energy dissipation intensity per unit area within the zone. Macroscopically, this manifests as a requirement for a higher stress level to drive further FPZ development and fracture propagation. This phenomenon reflects the strengthening effect of confining pressure on the nonlinear fracturing behavior of rock. The research results provide theoretical support for stimulation and modification of deep reservoirs.

Key words: confining pressure, fracture mechanics, three-point bending experiment, nonlinear fracture, fracture process zone

中图分类号: TE349
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