Experimental and GBM3D study on the failure mechanical behavior of granite with different grain sizes under conventional triaxial compression

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Bo-Wen Sun, Sheng-Qi Yang, Jin-Peng Dong, Zhi-Jin Dong, Wen-Ling Tian
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Abstract

Granite, as a ty pical crystalline rock in the earth's crust, is one of the ideal media in protection works for radioactive waste disposal. Grain size significantly influences the conventional triaxial compression mechanical properties of granite, thus also on the safety and stability of nuclear waste repositories. Thus, triaxial compression tests were performed by combining experiments with GBM3D based on PFC3D to study granite's conventional triaxial mechanical properties in grain size. Furthermore, the flexible boundaries were constructed in the numerical model using wall-zone coupling to apply lateral constraints in the model. The experiment outcomes demonstrate that coarse-grain granite contains more defects than the fine-grain granite. Concerning mechanical properties, fine-grained granite has much better mechanical properties than coarse-grained granite. However, the compressive of the initial defects at high confining pressures narrow this gap. The numerical simulation results show that the GBM3D model based on the flexible boundaries applied to the confining pressure can reasonably simulate the macroscopic mechanical behavior and non-uniform deformation of granite. This method better reflects the inhomogeneous deformation of granite specimens. The larger the grain size, the greater the spatial variation between mineral crystals, the more significant the effect on compressive stress atrophy and the tendency to produce macroscopic shear failure zones. As the confining pressure increases, the damage to the specimen is dominated by PCT/PIC leading to PCS/PTC transformation.

Abstract Image

不同晶粒大小的花岗岩在常规三轴压缩条件下的破坏力学行为的实验和 GBM3D 研究
花岗岩是地壳中的典型结晶岩,是放射性废物处置保护工程的理想介质之一。晶粒尺寸对花岗岩的常规三轴压缩力学性能有很大影响,从而也影响到核废料处置库的安全性和稳定性。因此,在 PFC3D 的基础上结合 GBM3D 试验进行了三轴压缩试验,以研究花岗岩在晶粒尺寸方面的常规三轴力学性能。此外,还在数值模型中利用壁区耦合构建了柔性边界,以在模型中应用横向约束。实验结果表明,粗晶粒花岗岩比细晶粒花岗岩含有更多的缺陷。在力学性能方面,细粒花岗岩的力学性能远远优于粗粒花岗岩。然而,在高约束压力下,初始缺陷的压缩会缩小这一差距。数值模拟结果表明,基于约束压力柔性边界的 GBM3D 模型可以合理模拟花岗岩的宏观力学行为和非均匀变形。这种方法能更好地反映花岗岩试样的不均匀变形。晶粒尺寸越大,矿物晶体之间的空间变化越大,对压应力萎缩的影响就越明显,并容易产生宏观剪切破坏区。随着约束压力的增加,试样的破坏主要由 PCT/PIC 导致 PCS/PTC 转变。
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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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