不同低温与加载速率下冻结饱和砂岩Ⅱ型动态断裂特性

赵涛, 崔朝, 贾海梁, 杨光宇

赵涛,崔朝,贾海梁,等. 不同低温与加载速率下冻结饱和砂岩Ⅱ型动态断裂特性[J]. 煤田地质与勘探,2025,53(4):191−202. DOI: 10.12363/issn.1001-1986.25.02.0106
引用本文: 赵涛,崔朝,贾海梁,等. 不同低温与加载速率下冻结饱和砂岩Ⅱ型动态断裂特性[J]. 煤田地质与勘探,2025,53(4):191−202. DOI: 10.12363/issn.1001-1986.25.02.0106
ZHAO Tao,CUI Zhao,JIA Hailiang,et al. Characteristics of dynamic mode Ⅱ fracture of frozen saturated sandstones under varying low temperatures and loading rates[J]. Coal Geology & Exploration,2025,53(4):191−202. DOI: 10.12363/issn.1001-1986.25.02.0106
Citation: ZHAO Tao,CUI Zhao,JIA Hailiang,et al. Characteristics of dynamic mode Ⅱ fracture of frozen saturated sandstones under varying low temperatures and loading rates[J]. Coal Geology & Exploration,2025,53(4):191−202. DOI: 10.12363/issn.1001-1986.25.02.0106

 

不同低温与加载速率下冻结饱和砂岩Ⅱ型动态断裂特性

基金项目: 国家自然科学基金面上项目(42271148)
详细信息
    作者简介:

    赵涛,1981年生,男,陕西西安人,副教授,硕士生导师。 E-mail:zhaotao@xust.edu.cn

    通讯作者:

    贾海梁,1987年生,男,山东东营人,教授,博士生导师。 E-mail:hailiang.jia@xust.edu.cn

  • 中图分类号: TD313

Characteristics of dynamic mode Ⅱ fracture of frozen saturated sandstones under varying low temperatures and loading rates

  • 摘要:
    背景 

    研究动力扰动下冻结饱和砂岩Ⅱ型断裂,包括临界应力强度因子(断裂韧度)变化特征以及能量耗散机制,对煤矿冻结井筒安全钻爆掘砌至关重要。

    方法 

    利用分离式霍普金森压杆装置,在不同温度和不同加载速率下进行一系列动态SCC试验,分析了冻结饱和砂岩应力强度因子−时间曲线、断裂韧度和能量耗散机制随温度和加载速率的演化规律。总结宏观与微观层面上砂岩剪切断裂面特征,并利用核磁手段揭示了冻结效应的微观影响机制。此外,基于有限元模拟,进一步分析了断裂特性的加载速率效应。

    结果和结论 

    结果表明:(1)随温度下降,冻结饱和砂岩断裂过程中岩石断裂韧度增大,相应地砂岩吸收的能量增加,能量利用率呈现一定的增长趋势。随加载速率增加,砂岩断裂韧度呈线性增加,岩石断裂吸收的能量也呈现增加趋势,而能量利用率呈现减小的趋势。(2)试件剪切面存在2种不同的断裂模式:“阶梯状”剪切滑移和“断口状”剪切滑移。(3)依据核磁数据总结了孔隙水冻结的3个阶段:过冷阶段,此阶段未冻水含量不变;快速冻结阶段,此阶段自由水与毛细水基本相变,大部分结合水冻结,断裂韧度迅速增加;缓慢冻结阶段,此阶段少部分结合水冻结,断裂韧度缓慢提升。(4)模拟应变−时间曲线与试验应变−时间较为吻合,表明模拟结果合理可靠,经模拟发现岩桥上出现明显的应力集中现象,并且随加载速率的增加剪应力呈现增加趋势,砂岩的断裂韧度与断裂吸收能均存在加载速率强化机制。研究成果对西部富水软岩地层冻结井筒的钻爆掘砌具有指导作用。

    Abstract:
    Background 

    Investigating the mode Ⅱ fracture of frozen saturated sandstones under dynamic disturbances, including changes in their critical stress intensity factor (SIF; i.e., fracture toughness) and energy dissipation mechanisms, is crucial for the safe excavation of frozen wellbores through drilling and blasting in coal mines.

    Methods 

    Using a split Hopkinson pressure bar (SHPB), this study conducted experiments on the dynamic mode Ⅱ fracture of a sandstone specimen using the short core in compression (SCC) method (also referred to as dynamic SCC experiments) under varying temperatures and loading rates. Accordingly, this study analyzed the SIF versus time curves of the frozen saturated sandstones, as well as the evolutionary patterns of their fracture toughness and energy dissipation mechanisms varying with the temperature and loading rate. Furthermore, it summarized the characteristics of the shear fracture planes of the sandstone specimen at macroscopic and microscopic scales and revealed the microscopic mechanisms behind the low-temperature strengthening effect using nuclear magnetic resonance (NMR). Additionally, this study further analyzed the effects of the loading rate on fracture characteristics using finite element simulation.

    Results and Conclusions 

    The results indicate that with a decrease in temperature, the frozen saturated sandstones exhibited intensifying fracture toughness. Accordingly, energy absorbed during sandstone fracture increased, and the energy utilization ratio showed an increasing trend. With an increase in the loading rate, the fracture toughness increased linearly, energy absorbed during sandstone fracture also showed an increasing trend, but the energy utilization ratio exhibited a decreasing trend. Two different fracture modes were observed on the shear planes of the SCC specimen: stepped and fracture-shaped shear slips. The NMR data revealed that the pore water freezing of the sandstones can be divided into three stages: supercooling, rapid freezing, and slow freezing sequentially. In the first stage, the unfrozen water content remained unchanged. In the rapid freezing stage, the free and capillary water roughly experienced phase transition, and most of the bound water froze, leading to rapidly enhanced fracture toughness. In the slow freezing stage, a small amount of bound water froze, with fracture toughness increasing slowly. The strain versus time curves derived from numerical simulation agreed well with those obtained using experiments, suggesting reasonable and reliable simulation results. The simulation results revealed significant stress concentration on the rock bridge of the SCC specimen and that the shear stress showed an increasing trend with the loading rate. Moreover, both the fracture toughness of the sandstones and energy absorbed during sandstone fracture increased with an increase in the loading rate. The results of this study can serve as a guide for the excavation of frozen wellbores through drilling and blasting in water-rich soft rock formations in West China.

  • 图  1   试样尺寸

    Fig.  1   Specimen size

    图  2   动态SCC试验系统

    Fig.  2   Experimental setup for dynamic SCC experiments

    图  3   动态应力平衡曲线

    Fig.  3   Dynamic stress balance curves

    图  4   CSRF恒定应变率和计算原理

    Fig.  4   Constant strain rate factor (CSRF) and its calculating principle

    图  5   应力强度因子与时间曲线

    Fig.  5   SIF vs. time curve

    图  6   冻结饱和砂岩Ⅱ型动态断裂应力强度因子−时间曲线

    Fig.  6   Curves showing mode Ⅱ dynamic fracture SIF vs. time for frozen saturated sandstones

    图  7   不同温度下冻结砂岩Ⅱ型动态断裂韧度−加载速率曲线

    Fig.  7   Fracture toughness vs. loading rate for the dynamic mode Ⅱ fracture of frozen saturated sandstones under varying temperatures

    图  8   不同加载速率下冻结饱和砂岩Ⅱ型动态断裂韧度−温度曲线

    Fig.  8   Curves showing the temperature-varying fracture toughness of the dynamic mode Ⅱ dynamic fracture of frozen saturated sandstones under varying loading rates

    图  9   吸收能与能量利用率随加载速率变化

    Fig.  9   Curves showing the absorbed energy and energy utilization ratio varying with the loading rate

    图  10   吸收能与能量利用率随温度变化

    Fig.  10   Curves showing the temperature-varying absorbed energy and energy utilization ratio

    图  11   SCC试件断裂模式以及剪切面破坏特征

    Fig.  11   Overall fracture mode and shear plane failure characteristics of the SCC specimen

    图  12   SCC试件断裂面微观形貌

    Fig.  12   Microscopic morphologies of the fracture planes of the SCC specimen

    图  13   冻结饱和砂岩未冻水含量随温度变化

    Fig.  13   Temperature-varying unfrozen water content in frozen saturated sandstones

    图  14   微观机理

    Fig.  14   Enhancing micromechanisms of saturated sandstones under low temperatures

    图  15   模拟验证

    Fig.  15   Simulation-based verification

    图  16   不同加载速率下试件模型动态剪应力分布

    Fig.  16   Distribution of dynamic shear stress of the specimen model under varying loading rates

    表  1   砂岩基本物理参数

    Table  1   Fundamental physical parameters of sandstones

    饱和密度/(g·cm−3) 孔隙率/% 抗压强度/MPa 弹性模量/GPa
    2.56 4.65 82 7.2
    下载: 导出CSV

    表  2   拟合曲线相关参数

    Table  2   Related parameters of the fitted curves of fracture toughness vs. loading rate

    温度/℃ a b R2
    25 0.98 0.014 0.97
    −0.2 1.15 0.018 0.97
    −5 1.59 0.023 0.99
    −10 2.43 0.021 0.97
    −15 2.03 0.025 0.96
    −20 3.49 0.018 0.94
    下载: 导出CSV

    表  3   模拟参数设定

    Table  3   Simulation parameter setting

    类别 弹性模量/GPa 密度/(g·cm−3) 黏聚力/MPa 泊松比
    入射杆 210 7.8 0.3
    反射杆 210 7.8 0.3
    透射杆 210 7.8 0.3
    试件 8.43 2.5 20 0.15
    紫铜片 115 8.93 0.34
      注:“—”表示该类别没有设置参数。
    下载: 导出CSV
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出版历程
  • 收稿日期:  2025-02-14
  • 修回日期:  2025-03-20
  • 刊出日期:  2025-04-24

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