Investigation on dynamic anisotropy of bedded shale under SHPB impact compression

• Clarify five failure patterns of shales under impact compression. • Reveal the mechanical mechanisms underlying dynamic anisotropy of bedded shale. • Elucidate fundamental laws affecting micro-cracks propagation and fracture morphology. • Summarize the influence of bedding inclination and strain rate effect. Revealing the fracture characteristics of shales under impact is significant for the exploitation and utilization of geological energy. In this study, the progressive failure process of bedded shale was tested by the dynamic Split Hopkinson Pressure Bar system and measured by the high-speed camera. Furthermore, their dynamic mechanical properties and fracture features under impact compression were comprehensively investigated. The results show that according to the triggering mechanisms of micro-cracks and mechanical factors governing fracture morphology, the failure patterns of shales can be categorized into five types: splitting failure along bedding plane, slip failure along bedding plane, mixed shear cracks between layers, tensile-shear mixed cracks, and tensile crack along bedding plane. Meanwhile, when the bedding angle θ = 0°, the sample experiences splitting failure, with acoustic emissions concentrated predominantly at horizontal bedding planes. When θ = 30° and 60°, the sample experiences shear failure characterized by shear cracks, mixed shear cracks and multiple composite tensile-shear cracks. When θ = 90°, the sample exhibits tensile and splitting cracks. With increasing strain rate, the fracture pattern of the 60° sample becomes dominated by slip and tensile-shear mixed cracks. With increasing peak stress intensity, the fracture modes of the 30° and 60° samples gradually transition from center-oriented failure towards shear failure along bedding planes. Additionally, for the 90° specimen, as the shock wave intensifies, secondary splitting cracks emerge in matrix, indicative of a fracture pattern across bedding planes.

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Publication Details

Journal
Engineering Fracture Mechanics
Published
2025-03-24
DOI
https://doi.org/10.1016/j.engfracmech.2025.111075
Citations
9
Primary Topic
Rock Mechanics and Modeling
Type
article
Field-Weighted Citation Impact
7.77

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article

Investigation on dynamic anisotropy of bedded shale under SHPB impact compression

Xianhui Feng, Xu Chen, Bin Gong, Xiaofeng Cheng et al.
9 citations
Engineering Fracture Mechanics
Rock Mechanics and Modeling
7.77
article

Investigation on dynamic anisotropy of bedded shale under SHPB impact compression

Xianhui Feng, Xu Chen, Bin Gong, Xiaofeng Cheng, Xun Xi, Kaikai Wang
article en
9 citations

Abstract

• Clarify five failure patterns of shales under impact compression. • Reveal the mechanical mechanisms underlying dynamic anisotropy of bedded shale. • Elucidate fundamental laws affecting micro-cracks propagation and fracture morphology. • Summarize the influence of bedding inclination and strain rate effect. Revealing the fracture characteristics of shales under impact is significant for the exploitation and utilization of geological energy. In this study, the progressive failure process of bedded shale was tested by the dynamic Split Hopkinson Pressure Bar system and measured by the high-speed camera. Furthermore, their dynamic mechanical properties and fracture features under impact compression were comprehensively investigated. The results show that according to the triggering mechanisms of micro-cracks and mechanical factors governing fracture morphology, the failure patterns of shales can be categorized into five types: splitting failure along bedding plane, slip failure along bedding plane, mixed shear cracks between layers, tensile-shear mixed cracks, and tensile crack along bedding plane. Meanwhile, when the bedding angle θ = 0°, the sample experiences splitting failure, with acoustic emissions concentrated predominantly at horizontal bedding planes. When θ = 30° and 60°, the sample experiences shear failure characterized by shear cracks, mixed shear cracks and multiple composite tensile-shear cracks. When θ = 90°, the sample exhibits tensile and splitting cracks. With increasing strain rate, the fracture pattern of the 60° sample becomes dominated by slip and tensile-shear mixed cracks. With increasing peak stress intensity, the fracture modes of the 30° and 60° samples gradually transition from center-oriented failure towards shear failure along bedding planes. Additionally, for the 90° specimen, as the shock wave intensifies, secondary splitting cracks emerge in matrix, indicative of a fracture pattern across bedding planes.

Engineering Fracture MechanicsVol. 320
Dalian University of Technology (CN), Chengdu University of Technology (CN), Brunel University of London (GB), Northwest A&F University (CN), University of Science and Technology Beijing (CN)
UK Research and Innovation, National Natural Science Foundation of China, China Postdoctoral Science Foundation, Natural Science Foundation of Beijing Municipality
Climate action
Openalex Percentile: Top 2%
Rock Mechanics and Modeling
7.77
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