Effect of loading rates on mechanical behavior and strain localization characteristics of sandstone

IF 2.8 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES Environmental Earth Sciences Pub Date : 2024-11-26 DOI:10.1007/s12665-024-11963-x
Lunan Wang, Xiangru Hu, Nan Wu, Yingying Zhao, Yibo Pang, Hongyu Bai
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Abstract

Determining the effect of loading rates on rock mechanical properties and deformation behavior is of vital importance for underground engineering with high-intensity excavation. In this study, uniaxial compression experiments with the digital image correlation technique were conducted to investigate the mechanical properties, failure modes, and apparent strain fields of the sandstone samples under different quasi-static loading rates. The loading rate effect on the characteristics of strain localization and energy was subsequently analyzed. Results show that with increasing loading rates, both the elastic modulus and uniaxial compressive strength increase logarithmically, and the failure mode changes from shear failure to tensile failure. Meanwhile, there are relationships between the initiation and development of strain localization and the loading rates. As the loading rate increases, the stress and stress level of strain localization initiation and the expansion rate of strain localization at most time increase gradually, while the duration from strain localization initiation to macro-failure decreases. The expansion area of strain localization has no obvious change pattern. In addition, the increase of loading rates enhances the energy absorption, storage, and dissipation properties of the samples, resulting in a higher energy state. It is the essential reason for the differences in mechanical behavior and strain localization of sandstone under different loading rates.

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确定加载速率对岩石力学性能和变形行为的影响对于高强度开挖的地下工程至关重要。本研究利用数字图像相关技术进行了单轴压缩实验,研究了不同准静态加载速率下砂岩样品的力学性能、破坏模式和表观应变场。随后分析了加载速率对应变定位和能量特征的影响。结果表明,随着加载速率的增加,弹性模量和单轴抗压强度均呈对数增长,破坏模式从剪切破坏转变为拉伸破坏。同时,应变局部化的产生和发展与加载速率也有关系。随着加载速率的增加,应变局部开始时的应力和应力水平以及大部分时间应变局部的扩展速率逐渐增加,而从应变局部开始到宏观破坏的持续时间则逐渐缩短。应变局部的扩展面积没有明显的变化规律。此外,加载速率的增加会增强样品的能量吸收、储存和耗散特性,从而形成更高的能量状态。这是不同加载速率下砂岩力学行为和应变局部化差异的根本原因。
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来源期刊
Environmental Earth Sciences
Environmental Earth Sciences 环境科学-地球科学综合
CiteScore
5.10
自引率
3.60%
发文量
494
审稿时长
8.3 months
期刊介绍: Environmental Earth Sciences is an international multidisciplinary journal concerned with all aspects of interaction between humans, natural resources, ecosystems, special climates or unique geographic zones, and the earth: Water and soil contamination caused by waste management and disposal practices Environmental problems associated with transportation by land, air, or water Geological processes that may impact biosystems or humans Man-made or naturally occurring geological or hydrological hazards Environmental problems associated with the recovery of materials from the earth Environmental problems caused by extraction of minerals, coal, and ores, as well as oil and gas, water and alternative energy sources Environmental impacts of exploration and recultivation – Environmental impacts of hazardous materials Management of environmental data and information in data banks and information systems Dissemination of knowledge on techniques, methods, approaches and experiences to improve and remediate the environment In pursuit of these topics, the geoscientific disciplines are invited to contribute their knowledge and experience. Major disciplines include: hydrogeology, hydrochemistry, geochemistry, geophysics, engineering geology, remediation science, natural resources management, environmental climatology and biota, environmental geography, soil science and geomicrobiology.
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