Earth Science Frontiers ›› 2024, Vol. 31 ›› Issue (5): 117-129.DOI: 10.13745/j.esf.sf.2024.6.15

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Mechanical behavior of calcite vein-bearing shale of the Niutitang Formation in Fenggang area, northern Guizhou based on CT tests

WU Zhonghu1(), MENG Xiangrui1, LAN Baofeng2,3, LIU Jingshou4,5,6, GONG Lei7,8, YANG Yuhan1   

  1. 1. College of Civil Engineering, Guizhou University, Guiyang 550025, China
    2. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025,China
    3. Guizhou Energy Industry Research Institute Co., Ltd, Guiyang 550025, China
    4. MOE Key Laboratory of Tectonics and Petroleum Resources, China University of Geosciences (Wuhan), Wuhan 430074, China
    5. School of Earth Resources, China University of Geosciences (Wuhan), Wuhan 430074, China
    6. Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
    7. Bohai Rim Energy Research Institute, Northeast Petroleum University, Qinhuangdao 066004, China
    8. School of Earth Sciences, Northeast Petroleum University, Daqing 163318, China
  • Received:2023-11-15 Revised:2024-04-18 Online:2024-09-25 Published:2024-10-11

Abstract:

Core observations of shales from the Niutitang Formation in the northern Qianbei region show that calcite veins often act as natural fracture fillers and largely influence the shale damage patterns. The damage characteristics of calcite vein-bearing shales is important for the prediction of fracture initiation and extension behavior during hydraulic fracturing and for the engineering design. In order to reveal the influence of calcite veins on the mechanical properties and fracture characteristics of shale, uniaxial compression and acoustic emission tests are conducted at seven inclination angles of 0° to 90° in 15° increment. Combined with CT scanning technology and finite element calculations, a three-dimensional (3D) microscopic numerical model is constructed. The effects of calcite vein angle on the fine-scale shale damage process as well as shale mechanical properties are discussed, and the spatiotemporal evolution of shale microcracks are analyzed. The results show that (1) under different calcite vein angles the shale acoustic emission and stress-strain curves show similar curve shape changes, in four stages, namely compression-density, elasticity, yielding, and post-peak damage, with obvious distinctions between stages. The change curve of the characteristic intensity is “U”-shaped with a local minimum at θ of 75°. (2) Calcite veins significantly affect the damage mode: As the vein angle decreases, the damage mode changes from cleavage to cleavage-type shear, to shear-slip, and finally to cleavage-tension. (3) The reconstructed 3D model is largely consistent with physical testing data, providing insights into the process of crack expansion and penetration at shale’s interior and surface. The spatial distribution of acoustic emission reflects the compression, tension, and shear damage types at different stages, revealing the fracture mechanism of calcite-containing shale from the microscopic point of view. (4) Calcite and matrix simulatineously and anisotropically affect the macroscopic mechanical properties of shale: The higher the calcite vein angle, the stronger its slip guidance effect, and the weaker the mechanical properties of the specimens.

Key words: shale, calcite, anisotropy, three-dimensional reconstruction, northern Guizhou

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