Numerical investigation of seismic behaviour of railway embankments in cold regions

To investigate more fully seismic behaviour of the Qinghai-Tibet railway embankment, a comprehensive discussion and a781nalysis is conducted in this paper by applying a numerical technique. Specifically, the one dimensional equivalent linear ground response analysis was conducted in permafrost regio...

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Bibliographic Details
Published in:Journal of the Croatian Association of Civil Engineers
Main Authors: Chen Tuo, Mu Yanhu, Wang Jianzhou, Zhang Junwei
Format: Article in Journal/Newspaper
Language:English
Croatian
Published: Croatian Association of Civil Engineers 2021
Subjects:
Online Access:https://doi.org/10.14256/JCE.2814.2019
https://doaj.org/article/6344e95fd9c0485ea566fdd0e971e0d3
Description
Summary:To investigate more fully seismic behaviour of the Qinghai-Tibet railway embankment, a comprehensive discussion and a781nalysis is conducted in this paper by applying a numerical technique. Specifically, the one dimensional equivalent linear ground response analysis was conducted in permafrost regions. On this basis, the seismic response of a typical railway embankment was further studied by applying the nonlinear dynamic finite element analysis method. As a result, nonlinear behaviour of permafrost sites was determined, and the dynamic acceleration, velocity and displacement of the embankment was discussed and the quantitative assessment was approximately estimated. The results indicate that the dynamic response of the embankment has distinct nonlinear characteristics. The peak ground acceleration coefficient at the embankment shoulder is larger than the natural ground surface, marking a 73% increase compared to the coefficient on the natural ground surface. When the seismic intensity reaches a certain value, a plastic zone gradually appears in the embankment, and a continuous extension of the plastic zone can be noted with an increase in peak acceleration of the input seismic wave. The findings of this research may provide an additional insight and have significant implications for further research of cold regions.