Numerical investigation on the deformation of railway embankment under normal faulting

被引:0
作者
Chen H. [1 ]
Liu J. [1 ,2 ,3 ]
Li Z. [1 ]
Liu X. [4 ]
Nan J. [1 ]
Liu J. [1 ,2 ,3 ]
机构
[1] School of Civil Engineering, Sun Yat-Sen University, Guangzhou
[2] State Key Laboratory for Tunnel Engineering, Sun Yat-Sen University, Zhuhai
[3] Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai
[4] School of Civil and Engineering Management, Guangzhou Maritime University, Guangzhou
[5] State Key Laboratory for Track Technology of High-speed Railway, China Academy of Railway Sciences, Beijing
来源
Journal of Infrastructure Preservation and Resilience | 2024年 / 5卷 / 01期
基金
中国国家自然科学基金;
关键词
Affected zone; Deformation pattern; Fault rupture outcropping; Finite element modelling; Normal fault; Railway embankment;
D O I
10.1186/s43065-024-00100-4
中图分类号
学科分类号
摘要
Active faults in the earthquake region are consistently regarded as a potential geological hazard to the construction and operation of railway engineering. However, the effects of normal faulting on railway embankments have not been investigated thoroughly. For bridging this knowledge gap, three-dimensional finite element analysis considering the influence of faulting offset, the soil layer’s thickness, the fault dip angle and the embankment cross-fault angle are conducted to clarify the normal faulting effects on the railway embankment. Emphasis is given to the stress and strain characteristic in the fault rupture outcropping regions on the embankment, the deformation of the embankment centerline for design purposes, and the determination of the affected zones for railway embankment preservation. The analysis shows that the normal fault rupture outcropping regions on railway embankment are tensile yield in most cases. The existence of the soil layer and its thickening would widen the affected zones and the regions where the fault ruptures outcrops. The fault dip angle and the cross-fault angle of the embankment have a complex effect on the behaviors of the crossing embankment. The depth of the subsidence zone of the embankment would increase with the decrease of the fault dip angle and the large fault dip angle would change the primary fault rupture to be a compressive one directly above the fault line. If the embankment crosses the fault line obliquely, the curvature radius of the centerline would hardly meet the design code. © The Author(s) 2024.
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