Semi-analytical solution for mechanical analysis of tunnels crossing strike-slip fault zone considering nonuniform fault displacement and uncertain fault plane position

IF 3.7 2区 材料科学 Q1 METALLURGY & METALLURGICAL ENGINEERING
Heng-hong Yang, Ming-nian Wang, Li Yu, Xiao Zhang
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Abstract

The tunnel subjected to strike-slip fault dislocation exhibits severe and catastrophic damage. The existing analysis models frequently assume uniform fault displacement and fixed fault plane position. In contrast, post-earthquake observations indicate that the displacement near the fault zone is typically nonuniform, and the fault plane position is uncertain. In this study, we first established a series of improved governing equations to analyze the mechanical response of tunnels under strike-slip fault dislocation. The proposed methodology incorporated key factors such as nonuniform fault displacement and uncertain fault plane position into the governing equations, thereby significantly enhancing the applicability range and accuracy of the model. In contrast to previous analytical models, the maximum computational error has decreased from 57.1% to 1.1%. Subsequently, we conducted a rigorous validation of the proposed methodology by undertaking a comparative analysis with a 3D finite element numerical model, and the results from both approaches exhibited a high degree of qualitative and quantitative agreement with a maximum error of 9.9%. Finally, the proposed methodology was utilized to perform a parametric analysis to explore the effects of various parameters, such as fault displacement, fault zone width, fault zone strength, the ratio of maximum fault displacement of the hanging wall to the footwall, and fault plane position, on the response of tunnels subjected to strike-slip fault dislocation. The findings indicate a progressive increase in the peak internal forces of the tunnel with the rise in fault displacement and fault zone strength. Conversely, an augmentation in fault zone width is found to contribute to a decrease in the peak internal forces. For example, for a fault zone width of 10 m, the peak values of bending moment, shear force, and axial force are approximately 46.9%, 102.4%, and 28.7% higher, respectively, compared to those observed for a fault zone width of 50 m. Furthermore, the position of the peak internal forces is influenced by variations in the ratio of maximum fault displacement of the hanging wall to footwall and the fault plane location, while the peak values of shear force and axial force always align with the fault plane. The maximum peak internal forces are observed when the footwall exclusively bears the entirety of the fault displacement, corresponding to a ratio of 0: 1. The peak values of bending moment, shear force, and axial force for the ratio of 0:1 amount to approximately 123.8%, 148.6%, and 111.1% of those for the ratio of 0.5:0.5, respectively.

考虑非均匀断层位移和不确定断层面位置的穿越走向滑动断层带隧道力学分析的半解析解法
受到走向滑动断层变位影响的隧道会出现严重的灾难性破坏。现有的分析模型通常假设断层位移均匀且断层面位置固定。而震后观测表明,断层带附近的位移通常是不均匀的,断层面位置也是不确定的。在本研究中,我们首先建立了一系列改进的控制方程来分析隧道在走向滑动断层错动下的力学响应。所提出的方法将断层位移不均匀和断层面位置不确定等关键因素纳入了控制方程,从而大大提高了模型的适用范围和精度。与以往的分析模型相比,最大计算误差从 57.1% 降至 1.1%。随后,我们通过与三维有限元数值模型进行对比分析,对所提出的方法进行了严格验证,两种方法的结果在定性和定量方面都表现出高度一致,最大误差为 9.9%。最后,利用所提出的方法进行了参数分析,以探讨各种参数(如断层位移、断层带宽度、断层带强度、悬壁与底壁最大断层位移比以及断层面位置)对遭受走向滑动断层错动的隧道响应的影响。研究结果表明,隧道的峰值内力会随着断层位移和断层带强度的增加而逐渐增大。相反,断层带宽度的增加会导致峰值内力的减小。例如,断层带宽度为 10 米时,弯矩、剪力和轴力的峰值分别比断层带宽度为 50 米时高出约 46.9%、102.4% 和 28.7%。此外,内力峰值的位置受悬壁与底壁最大断层位移比和断层面位置变化的影响,而剪力和轴力的峰值始终与断层面一致。当脚墙完全承受全部断层位移时,内力峰值最大,对应于 0:1 的比率。比值为 0:1 时的弯矩、剪力和轴力峰值分别约为比值为 0.5:0.5 时的 123.8%、148.6% 和 111.1%。
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
Journal of Central South University
Journal of Central South University METALLURGY & METALLURGICAL ENGINEERING-
CiteScore
6.10
自引率
6.80%
发文量
242
审稿时长
2-4 weeks
期刊介绍: Focuses on the latest research achievements in mining and metallurgy Coverage spans across materials science and engineering, metallurgical science and engineering, mineral processing, geology and mining, chemical engineering, and mechanical, electronic and information engineering
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