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王帅, 许莹, 张艳博, 姚旭龙, 刘祥鑫, 梁鹏. 基于CT扫描的砂岩主次裂纹扩展特征及影响因素研究[J]. 岩土工程学报, 2022, 44(4): 702-711. DOI: 10.11779/CJGE202204013
引用本文: 王帅, 许莹, 张艳博, 姚旭龙, 刘祥鑫, 梁鹏. 基于CT扫描的砂岩主次裂纹扩展特征及影响因素研究[J]. 岩土工程学报, 2022, 44(4): 702-711. DOI: 10.11779/CJGE202204013
WANG Shuai, XU Ying, ZAHNG Yan-bo, YAO Xu-long, LIU Xiang-xin, LIANG Peng. Characteristics and influencing factors for propagation of primary and secondary cracks in sandstone based on CT scan[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(4): 702-711. DOI: 10.11779/CJGE202204013
Citation: WANG Shuai, XU Ying, ZAHNG Yan-bo, YAO Xu-long, LIU Xiang-xin, LIANG Peng. Characteristics and influencing factors for propagation of primary and secondary cracks in sandstone based on CT scan[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(4): 702-711. DOI: 10.11779/CJGE202204013

基于CT扫描的砂岩主次裂纹扩展特征及影响因素研究

Characteristics and influencing factors for propagation of primary and secondary cracks in sandstone based on CT scan

  • 摘要: 为了研究岩石在压应力条件下主次裂纹的萌生及扩展规律,对砂岩在单轴压缩条件下的破裂过程进行CT扫描试验,分析了砂岩中主次裂纹的形貌特征;同时,定量探讨了砂岩在不同变形阶段主裂纹的表面积和体积以及次生裂纹的分形维数,并运用Image pro plus 6.0和Image J软件计算了砂岩在不同高度位置主次裂纹的长度和数量,研究了主次裂纹的扩展及其影响因素。研究结果表明,主导砂岩破裂的是萌生于砂岩表面两种不同方向的主裂纹,主裂纹表面积和体积的增长速率随着荷载水平的增加而不同。在主裂纹的周围产生了许多次生裂纹,次生裂纹的分形维数随着荷载水平的增加而非线性增加。不同荷载水平下,砂岩在不同高度位置的主次裂纹长度和数量变化各不相同。在砂岩破坏前,影响砂岩主次裂纹扩展的主要因素是主裂纹的长度,在砂岩破坏后,影响砂岩主次裂纹扩展的主要因素是次生裂纹的长度。该结论对未来岩石破坏失稳的预测分析奠定了理论基础。

     

    Abstract: In order to study the initiation and propagation of the primary and secondary cracks under compressive stress conditions, the CT tests are conducted on the fracture process of sandstone under uniaxial compression, and the morphological characteristics of the primary and secondary cracks in sandstone are analyzed. Meanwhile, the surface area and volume of the primary cracks and the fractal dimension of the secondary cracks are quantitatively discussed at different deformation stages of sandstone. The length and number of the primary and secondary cracks are calculated at different heights of sandstone using the software Image pro plus 6.0 and Image J to study the propagation and influencing factors of the primary and secondary cracks. The results show that the primary cracks initiate on the sandstone surface in two different directions, and the growth rates of the surface area and the volume of the primary cracks vary with the increase of the load level. Many secondary cracks are produced around the primary cracks. The fractal dimension of the secondary cracks increases nonlinearly with the increase of the load level. Under different load levels, the length and number of the primary and secondary cracks at different heights of sandstone vary. Before the failure of sandstone, the main factor affecting the propagation of the primary and secondary cracks is the length of the primary cracks. After the failure of sandstone, the main factor affecting the propagation of the primary and secondary cracks is the length of the secondary cracks. The conclusion lays a theoretical foundation for the prediction and analysis of rock failure and instability in the future.

     

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