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层理方向对含预制裂纹页岩Ⅰ型断裂特性的影响

Effect of bedding direction on mode Ⅰ fracture characteristics of precrack shale

  • 摘要: 层状页岩受内部层理方位分布特征的影响, 其力学性质常表现出明显的各向异性特征。为了探究层理方向对层状页岩Ⅰ型断裂特性的影响, 针对不同层理倾角β、预制裂纹角度为0°的半圆盘试件开展三点弯曲静态压缩试验和数值模拟试验。试验结果表明, 试件的Ⅰ型标准化应力强度因子Y会随着层理倾角的变化呈现出明显的差异性, 并与层理倾角呈现出良好的三次函数关系, 且仅在层理倾角β为0°和90°时, 试件表现为纯Ⅰ型断裂模式, 即层理倾角的变化会改变试件的断裂模式。同时, 试件的Ⅰ型断裂韧度随着层理倾角的增大而逐渐减小, 并与层理倾角呈二次函数关系; 当层理倾角与预制裂纹角度垂直时, 试件的Ⅰ型断裂韧度最大; 而当层理倾角和预制裂纹角度平行时, 试件的Ⅰ型断裂韧度最小。另外, 基于扩展有限元法(XFEM), 对半圆盘层状页岩试件的破断机制进行研究, 验证了试验和计算结果的准确性。

     

    Abstract: The mechanical properties of layered shales are usually anisotropic due to the influence of internal bedding azimuths. In order to explore the influence of bedding direction mode Ⅰ fracture characteristics, three point bending static compression tests and numerical simulation tests were carried out on half-disc specimens with precrack angles of 0° and different bedding dip angle β. The test results show that the mode Ⅰ standardized stress intensity factor of the specimen Y varies significantly with the change of bedding angle, and presents a good cubic function relationship with bedding angle; only when the bedding angle β is 0° or 90°, the specimen shows a pure mode Ⅰ fracture mode, that is, the change of bedding angle will change the fracture mode of the specimen. At the same time, the mode Ⅰ fracture toughness of specimens decreases gradually with the increase of bedding angle, and presents a quadratic function relationship with bedding angle. When the bedding angle is perpendicular to the precrack angle, the mode Ⅰ fracture toughness of the specimen is the largest. When the bedding angle is parallel to the precrack angle, the mode Ⅰ fracture toughness of the specimen is the smallest. In addition, based on the extended finite element method(XFEM), the fracture mechanism of the half-disc layered shale specimen is studied, and the accuracy of the test and calculation results is verified.

     

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