Experimental Study of Direct Shear Properties of Anisotropic Reservoir Shale

Author:

Zheng Bowen123,Qi Shengwen123ORCID,Guo Songfeng123ORCID,Liang Ning123ORCID,Luo Guangming123,Zhang Xiaohui123,Lu Wei123,Jin Chao45,Li Yongchao123,Yu Xin123ORCID,Zhu Zifang123,Cong Jianing123

Affiliation:

1. Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

2. Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China

3. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China

4. School of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, China

5. Collaborative Innovation Center of Resource Exploration and Exploitation, Hebei University of Engineering, Handan 056038, China

Abstract

Understanding the shear mechanical properties of shale reservoirs is of great significance in the study of the formation stability around horizontal shale wells and the propagation and evolution of fractures for shale fracturing. However, the existing direct shear test results are limited due to small sample sizes and low shear rates. Based on previous experimental research results, the mechanical properties of anisotropic reservoir shale in direct shear tests with different experimental conditions were explored in this study. It was found that the shear mode, shear strain rate, and normal stress have a significant impact on the deformation and failure characteristics of shale. The peak shear displacement, peak shear strength, and shear stiffness of shale present an increasing trend of fluctuation, with an increase in the bedding angle. The peak shear strength of shale decreases with an increase in the shear strain rate, and this decrease trend descends with an increase in the shear strain rate. The shape of the shear fracture zone and the shear fracture mode of shale exhibit bedding effect characteristics. The fractal dimension of the shale shear fracture surface morphology shows a trend of fluctuation with the variation in the bedding angle. Further, the shear strain rate was found to play a dominant role in the fractal dimension of the shear fracture surface. The larger shear strain rate strengthens the bedding effect of the roughness for the shear fracture surface morphology. The results of this study provide a theoretical reference for determining the engineering geomechanics characteristics of shale reservoirs.

Funder

National Natural Science Foundation of China

Key Research Program of the Institute of Geology and Geophysics, CAS

Youth Innovation Promotion Association Foundation of the Chinese Academy of Sciences

Second Tibetan Plateau Scientific Expedition and Research Program

Publisher

MDPI AG

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