Investigation on dynamic anisotropy of bedded shale under SHPB impact compression

IF 4.7 2区 工程技术 Q1 MECHANICS
Xianhui Feng , Bin Gong , Xiaofeng Cheng , Xu Chen , Xun Xi , Kaikai Wang
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引用次数: 0

Abstract

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.
揭示页岩在冲击作用下的断裂特征对地质能源的开发利用意义重大。本研究利用动态分体式霍普金森压杆系统测试了层状页岩的渐进破坏过程,并利用高速相机对其进行了测量。此外,还全面研究了它们在冲击压缩作用下的动态力学性能和断裂特征。结果表明,根据微裂缝的触发机制和影响断裂形态的力学因素,页岩的破坏形态可分为五种类型:沿层理面劈裂破坏、沿层理面滑移破坏、层间混合剪切裂缝、拉剪混合裂缝和沿层理面拉伸裂缝。同时,当θ = 0°时,试样会出现劈裂破坏,声发射主要集中在水平基底面上。当 θ = 30° 和 60° 时,试样出现剪切破坏,其特征为剪切裂缝、混合剪切裂缝和多重拉伸-剪切复合裂缝。当 θ = 90° 时,样品出现拉伸和劈裂裂纹。随着应变速率的增加,60° 样品的断裂模式以滑移和拉剪混合裂纹为主。随着峰值应力强度的增加,30° 和 60° 样品的断裂模式逐渐从面向中心的断裂过渡到沿基底面的剪切断裂。此外,在 90° 试样中,随着冲击波的增强,基体中出现了次级劈裂裂缝,表明断裂模式是跨基底面的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
8.70
自引率
13.00%
发文量
606
审稿时长
74 days
期刊介绍: EFM covers a broad range of topics in fracture mechanics to be of interest and use to both researchers and practitioners. Contributions are welcome which address the fracture behavior of conventional engineering material systems as well as newly emerging material systems. Contributions on developments in the areas of mechanics and materials science strongly related to fracture mechanics are also welcome. Papers on fatigue are welcome if they treat the fatigue process using the methods of fracture mechanics.
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