酸基压裂液作用下沁水煤断裂韧度与应变局部化各向异性演化特征

Anisotropic evolution characteristics of fracture toughness and strain localization of Qinshui coal under action of acid-based fracturing fluid

  • 摘要: 煤层气开发对缓解我国天然气短缺至关重要,煤层酸化体积压裂时构建大体积裂缝网络是实现高效开采的关键。开展酸基压裂液作用下无烟煤断裂韧度与应变局部化各向异性试验研究,对于深入理解煤储层压裂裂缝的起裂和扩展规律极为重要。基于此,研究对经加压水基压裂液和酸基压裂液作用后含5种不同层理角度(0°、22.5°、45.0°、67.5°、90.0°)直切槽半圆弯曲(NSCB)沁水无烟煤样开展了三点弯曲加载试验,探究了不同压裂液作用下煤样断裂韧度各向异性特征。结合数字图像相关法(DICM)探讨了不同加载阶段煤样应变局部化区(SLZ)和高应变区(HSZ)的各向异性演化规律,并建立了两者间的幂函数关系。同时,通过对不同加载阶段裂纹张开位移(COD)的监测,定量表征了裂纹张开位移随载荷演化的动态响应规律。运用Geomagic三维检测计量软件及Surfer三维立体绘图软件对煤样断面结构进行精细网格化处理及三维云图绘制,探究煤岩破断面粗糙度各向异性特征。结果表明:与水基压裂液组相比,酸基压裂液组煤样随层理角度的增大,其断裂韧度呈现出更为显著的减韧特征,表明抵抗裂纹扩展能力下降。5种层理角度组中,酸基压裂液作用煤样应变局部化区长度较水基压裂液组均呈现增长趋势,而当层理角度为45.0°时差异最为显著,酸基压裂液组应变局部化区长度较水基压裂液组增长了36.184%;当层理角度为90.0°时差异最小,仅增长了1.913%。2种压裂液作用下,应变局部化区与高应变区长度之间遵循不同幂函数关系;此外,还建立了裂纹张开位移随煤样表面不同测线高度变化的数学模型。相关研究成果为酸化压裂无烟煤裂纹起裂与扩展机制研究提供了试验基础,为煤层酸化压裂设计、复杂缝网形成机制及其调控方法提供了理论参考。

     

    Abstract: Coalbed methane (CBM) development is of critical importance for alleviating the shortage of natural gas in China. The construction of a large-scale fracture network during acid-based volumetric fracturing is key to achieving efficient CBM extraction. An experimental investigation of the anisotropy of fracture toughness and strain localization in anthracite subjected to acid-based fracturing fluid is essential for a deeper understanding of crack initiation and propagation during reservoir fracturing. To this end, three-point bending tests were conducted on straight-notched semi-circular bending (NSCB) specimens of Qinshui anthracite with five different bedding plane angles (0°, 22.5°, 45.0°, 67.5°, and 90.0°) after treatment with pressurized water-based and acid-based fracturing fluids. The anisotropic characteristics of fracture toughness of coal specimens treated with acid-based fracturing fluid were examined. Using digital image correlation method (DICM), the anisotropic evolution of the strain localization zone (SLZ) and the high-strain zone (HSZ) was explored at different loading stages, and a power-law relationship between them was established. Meanwhile, through monitoring of the crack opening displacement (COD) at various loading stages, the dynamic response of crack opening displacement as a function of load evolution was quantitatively characterized. The three-dimensional structural reconstruction of coal specimen fracture surfaces was carried out using Geomagic three-dimensional inspection software and Surfer three-dimensional mapping software, enabling fine meshing and three-dimensional contour mapping to explore the anisotropic characteristics of fracture surface roughness. The results indicate that, compared with the water-based fracturing fluid group, the acid-based fracturing fluid group exhibits a more pronounced reduction in fracture toughness with increasing bedding angle, suggesting a decreased resistance to crack propagation. Among the five bedding angle groups, the length of the strain localization zone in coal specimens treated with acid-based fracturing fluid showed an increasing trend relative to that in the water-based group, with the most significant difference observed at a bedding angle of 45.0°, where the length increased by 36.184%. The smallest difference was observed at 90.0°, with an increase of only 1.913%. Under the action of the two types of fracturing fluids, different power-law relationships were followed between the lengths of the strain localization zone and the high-strain zone. In addition, a mathematical model describing the variation of crack opening displacement with different measurement line heights on the coal specimen surface was established. The relevant findings provide an experimental basis for the study of crack initiation and propagation mechanisms in acid-fractured anthracite and offer theoretical references for the design of acid-based coal reservoir fracturing, the formation mechanism of complex fracture networks, and their control methods.

     

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