Numerical simulation of the vibration response of the permafrost subgrade under harmonic irregularity in the Qinghai-Tibet Railway

被引:0
|
作者
Tang, Chen-Xuan [1 ,2 ]
Zhu, Zhan-Yuan [2 ,3 ]
Ma, Yong [1 ]
Zheng, Si-Cheng [2 ]
Yao, Zhi [1 ]
Xie, Guang-Ci [1 ]
Yang, Wen-Zha [1 ]
Xu, Jiao [2 ]
机构
[1] Sun Yat Sen Univ, Sch Ocean Engn & Technol, Zhuhai 519082, Peoples R China
[2] Sichuan Agr Univ, Coll Civil Engn, Dujiangyan 611830, Peoples R China
[3] Xichang Univ, Sch Civil & Hydraul Engn, Xichang 615000, Peoples R China
来源
ENGINEERING RESEARCH EXPRESS | 2024年 / 6卷 / 04期
基金
中国国家自然科学基金;
关键词
harmonic excitation; ice-rich permafrost; train-track-subgrade coupled dynamics model; Qinghai-Tibet Railway; DYNAMIC STRESS; TRACK; TRAIN; BEHAVIOR; FOUNDATION; EMBANKMENT; PLATEAU; SURFACE;
D O I
10.1088/2631-8695/ad82a3
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Harmonic excitation can significantly increase the dynamic response of wheel-rail interactions when a train passes. In this study, based on the train-track vertical coupled dynamics model (ZL-TNTLM) and ABAQUS, a unified train-track-subgrade coupled dynamics model is established. Field measurement data corroborated its accuracy and reliability. The analysis focused on the dynamic response of the permafrost subgrade of the Qinghai-Tibet Railway (QTR) to harmonic excitation, including the track-sleeper force and vertical dynamic stress. This study examined the influences of the wavelength, wave depth, and railhead depression on the dynamic response of a subgrade. The results indicated that single-harmonic excitation amplifies the track-sleeper forces and the vertical dynamic stress in the subgrade, particularly near the harmonic centre. Additionally, axle load variations and seasonal thawing broaden the dynamic stress range on the subgrade, with harmonic excitation exacerbating this impact, thereby increasing the risk to the stability of the ice-rich permafrost layer. A decrease in wavelength and increase in wave depth result in a greater number of affected sleepers, intensifying the vertical vibrations of the subgrade, especially in the medium- and high-frequency ranges of vertical dynamic stress. Notably, wavelengths between 1 and 2 m significantly exacerbate the adverse effects on the ice-rich permafrost layer. Shorter wavelengths also induce higher-frequency vibrations. These findings offer valuable insights for the design, operation, and maintenance of permafrost subgrade systems under irregular excitation.
引用
收藏
页数:20
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