Exploring the influence of fabric anisotropy on the active failure of shield tunnel through DEM

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL Bulletin of Engineering Geology and the Environment Pub Date : 2024-09-16 DOI:10.1007/s10064-024-03878-5
Qixiang Yan, Chunyi Wei, Junnan Ren, Yaozhong Cui, Wencheng He, Runfang Sun
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Abstract

Fabric anisotropy significantly influences the mechanical behavior of sandy soils, potentially resulting in diverse failure patterns during shield tunneling owing to insufficient support pressure. In this paper, a set of specimens with bedding angles (\(\alpha\)) and an isotropic specimen are well generated to simulate active failure at the tunnel face using DEM. The evolving failure of the soil in distinct \(\alpha\) are scrutinized, and ground settlement is further explored. Furthermore, microscopic information is juxtaposed to systematically elucidate the influence of \(\alpha\) on failure patterns at a microscopic level. Macroscopic findings reveal that, aside from specimens with \(\alpha\) = 0° and 90°, particle displacement experiences deflection as it extends toward the ground surface in other specimens. However, this deflection behavior is only noticeable under conditions of large deformation. Additionally, across all specimens, the maximum displacement of the ground surface is observed in those with \(\alpha\) = 90°, while the minimum value is noted in specimens with \(\alpha\) = 45°. Notably, considerable particle rotation occurs within the shear face. However, the deflection behavior has not been found in specimens with \(\alpha\) = 0° and 90°. Similarly, in specimens with these two specimens, there is no noteworthy deflection observed in the principal direction of contact normal.

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通过 DEM 探索织物各向异性对盾构隧道主动破坏的影响
敷层各向异性对砂土的力学行为有很大影响,可能导致盾构掘进过程中因支撑压力不足而出现不同的破坏模式。本文利用 DEM 生成了一组具有垫层角(\(\alpha\))的试样和一个各向同性试样,以模拟隧道面的主动破坏。仔细观察了土壤在不同角度(\(α\))下的演变破坏过程,并进一步探讨了地面沉降问题。此外,还并列了微观信息,以便在微观层面系统地阐明()对破坏模式的影响。宏观研究结果表明,除了 \(\alpha\) = 0° 和 90° 的试样外,其他试样中的颗粒位移在向地表延伸时会出现偏转。然而,这种变形行为只有在大变形条件下才明显。此外,在所有试样中,地表的最大位移出现在 \(\α\) = 90°的试样中,而最小值出现在 \(\α\) = 45°的试样中。值得注意的是,相当大的颗粒旋转发生在剪切面内。然而,在 \(\alpha\) = 0° 和 90° 的试样中没有发现挠曲行为。同样,在这两种试样中,在接触法线的主要方向上也没有观察到值得注意的挠曲。
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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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