Effect of stress difference and microfabric on the strength of deep granite

IF 4.2 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL Bulletin of Engineering Geology and the Environment Pub Date : 2025-02-13 DOI:10.1007/s10064-025-04148-8
Liangjie Gu, Jun Zhao, Yangyi Zhou, Yan Zhang, Zhaofeng Wang
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Abstract

A multitude of subterranean engineering projects are established within granite bodies, where the mechanical properties of granite are predominantly influenced by the existing stress environment and inherent microfabric. As the depth of engineering projects increases, the characteristic stress differential becomes more pronounced, indicating a discernible distinction from the stress conditions encountered in shallow engineering applications. To elucidate the influence mechanism of microfabric and stress disparity on granite strength, a quantitative analysis is conducted on the microfabric of five types of granites. The results show that the strength of granite is primarily determined by initial damage, structural coefficient, biotite content, and quartz content. With an increase in stress differential, the impact of initial damage and biotite content on granite strength diminishes, while the influence of quartz content and structural coefficient on granite strength begins to intensify. A subjective and objective comprehensive evaluation model is established to quantify the weight ratio of microfabric on granite strength. The coupling mechanism of stress difference and microfabric on the granite strength is revealed from the rock fracture directional development induced by the increase of stress difference. The results can be used as a guide to understand the granite strength characteristics according to the lithofacies and true three-dimensional stress environment, and provide an effective theoretical basis for the safe construction of deep granite engineering.

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应力差和微织物对深花岗岩强度的影响
大量地下工程都建立在花岗岩体内部,花岗岩的力学性能主要受现有应力环境和固有微组构的影响。随着工程项目深度的增加,特征应力差变得更加明显,表明与浅层工程应用中遇到的应力条件有明显的区别。为阐明微组构和应力差对花岗岩强度的影响机理,对5种花岗岩的微组构进行了定量分析。结果表明,花岗岩的强度主要由初始损伤、结构系数、黑云母含量和石英含量决定。随着应力差的增大,初始损伤和黑云母含量对花岗岩强度的影响减弱,石英含量和结构系数对花岗岩强度的影响开始增强。建立主客观综合评价模型,量化微织物对花岗岩强度的权重比。从应力差增大引起岩石裂缝定向发育的角度,揭示了应力差与微组构对花岗岩强度的耦合机制。研究结果可为根据岩相和真实三维应力环境了解花岗岩强度特征提供指导,为深部花岗岩工程的安全施工提供有效的理论依据。
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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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