Oil & Gas Geology ›› 2024, Vol. 45 ›› Issue (5): 1447-1455.doi: 10.11743/ogg20240517

• Methods and Technologies • Previous Articles     Next Articles

Mechanical properties of the Silurian Longmaxi Formation shale, southern Sichuan Basin and its microfracturing mechanisms

Xun GONG1,2(), Zhijun JIN1,2(), Xinhua MA1,3,4, Yuyang LIU3,4, Guanfang LI5, Huan MIU6   

  1. 1.Institute of Energy,Peking University,Beijing 100871,China
    2.School of Earth and Space Sciences,Peking University,Beijing 100871,China
    3.Research Institute of Petroleum Exploration & Development,PetroChina,Beijing 100083,China
    4.National Energy Shale Gas R&D (Experiment) Center,Langfang,Hebei 065007,China
    5.Key Laboratory of Shale Gas and Geoengineering,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China
    6.Unconventional Petroleum Research Institute,China University of Petroleum (Beijing),Beijing 102249,China
  • Received:2024-04-08 Revised:2024-09-06 Online:2024-10-30 Published:2024-11-06
  • Contact: Zhijun JIN E-mail:2201110675@stu.pku.edu.cn;jinzj1957@pku.edu.cn

Abstract:

To reveal the mechanical properties and microfracturing mechanisms of shales, we investigate shales in the Silurian Longmaxi Formation in the southern Sichuan Basin using X-ray diffraction (XRD) analysis, together with triaxial compression, micro-computed tomography (micro-CT) and scanning electron microscopy (SEM) tests. The results indicate that the mechanical properties and reservoir physical properties of shale are significantly influenced by its mineral composition and confining pressure. Specifically, an increase in the brittle mineral content enhances its elastic modulus and peak stress, indicating positive correlations between these mechanical properties and the brittle mineral content. In contrast, higher clay mineral content increases the shale plasticity while reducing its rock strength. As confining pressure increases, fractures in the shale gradually close, and the pores deform and contract, leading to reduced porosity. A higher confining pressure results in greater compression. Two dominant types of fractures form during shale damage: boundary fractures occurring at interfaces between mineral grains and internal fractures occurring within grains. For shales with similar mechanical properties, increasing confining pressure shifts their dominant fracture type from boundary to internal fractures. Additionally, higher confining pressure causes the boundary and internal fractures to evolve into fracture zones, leading to an increased fracture density in the shale.

Key words: microfracturing mechanism, fracture, rock mechanics, shale, Longmaxi Formation, Silurian, southern Sichuan Basin

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