Chen-xuan Tang , Zhan-yuan Zhu , Yong Ma , Fei Luo , Si-cheng Zheng , Zhi Yao , Yuan-yao Zhu , Zu-yin Zou , Zi-hong Guo
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First, the vibration load significantly impacts the subgrade 6 m below the sleeper, producing distinct vertical dynamic stress waves due to the wheels and bogies. Dynamic compression stress dominates the subgrade and is influenced by the train structure, speed, and sleeper spacing. While the 2D model tends to underestimate the dynamic stress in shallower layers, it concurs with the 3D model in deeper subgrade dynamics within a 10% margin of error. Then, the principal stress axis of the subgrade soil rotates synchronously with train movements, exhibiting regular stress paths in the YZ plane (longitudinal section) with depth-dependent variations in the stress cycles and deviatoric stress. Finally, predominantly originating from sleeper-induced vibrations, the subgrade vibration acceleration varies with the train speed, sleeper spacing, and season and is most pronounced in the vertical direction. 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Then, the principal stress axis of the subgrade soil rotates synchronously with train movements, exhibiting regular stress paths in the YZ plane (longitudinal section) with depth-dependent variations in the stress cycles and deviatoric stress. Finally, predominantly originating from sleeper-induced vibrations, the subgrade vibration acceleration varies with the train speed, sleeper spacing, and season and is most pronounced in the vertical direction. 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引用次数: 0
摘要
研究列车诱发的响应特性对于安全运行冻土铁路路基至关重要。本文建立了列车-轨道-路基-地面关系的三维热力-机械耦合非线性动态模型,用于分析列车诱发的冻土铁路路基动态应力、加速度和应力路径特征,并利用现场监测数据验证了该模型。此外,还讨论了二维和三维模型之间的差异,以及影响冻土路基的季节变化、列车速度、轴载和列车类型。主要结果如下。首先,振动载荷对枕木下 6 米的路基产生了重大影响,车轮和转向架产生了明显的垂直动应力波。动态压缩应力在路基中占主导地位,并受到列车结构、速度和枕木间距的影响。虽然二维模型倾向于低估较浅地层的动态应力,但在较深的路基动态应力方面,二维模型与三维模型的误差范围在 10%以内。然后,路基土的主应力轴与列车运行同步旋转,在 YZ 平面(纵断面)上显示出规则的应力路径,应力周期和偏差应力的变化与深度有关。最后,路基振动加速度主要来自枕木引起的振动,随列车速度、枕木间距和季节而变化,在垂直方向上最为明显。这项研究为青藏铁路(QTR)冻土路基的振动响应提供了理论指导。
Dynamic response of a permafrost railway subgrade with 3D train-track-subgrade-ground model simulations
Studying train-induced response characteristics is essential for safely operating permafrost railway subgrades. A three-dimensional thermal-mechanical coupling nonlinear dynamic model of train-track-subgrade-ground relationships was established to analyse the train-induced dynamic stress, acceleration and stress path characteristics of a permafrost railway subgrade, and field monitoring data were used to verify this model. The differences between the 2D and 3D models are also discussed, along with the seasonal changes, train speed, axle load, and train type affecting permafrost subgrades. The main results are as follows. First, the vibration load significantly impacts the subgrade 6 m below the sleeper, producing distinct vertical dynamic stress waves due to the wheels and bogies. Dynamic compression stress dominates the subgrade and is influenced by the train structure, speed, and sleeper spacing. While the 2D model tends to underestimate the dynamic stress in shallower layers, it concurs with the 3D model in deeper subgrade dynamics within a 10% margin of error. Then, the principal stress axis of the subgrade soil rotates synchronously with train movements, exhibiting regular stress paths in the YZ plane (longitudinal section) with depth-dependent variations in the stress cycles and deviatoric stress. Finally, predominantly originating from sleeper-induced vibrations, the subgrade vibration acceleration varies with the train speed, sleeper spacing, and season and is most pronounced in the vertical direction. This study provides theoretical guidance for the vibration response of permafrost subgrades on the Qinghai-Tibet Railway (QTR).
期刊介绍:
Cold Regions Science and Technology is an international journal dealing with the science and technical problems of cold environments in both the polar regions and more temperate locations. It includes fundamental aspects of cryospheric sciences which have applications for cold regions problems as well as engineering topics which relate to the cryosphere.
Emphasis is given to applied science with broad coverage of the physical and mechanical aspects of ice (including glaciers and sea ice), snow and snow avalanches, ice-water systems, ice-bonded soils and permafrost.
Relevant aspects of Earth science, materials science, offshore and river ice engineering are also of primary interest. These include icing of ships and structures as well as trafficability in cold environments. Technological advances for cold regions in research, development, and engineering practice are relevant to the journal. Theoretical papers must include a detailed discussion of the potential application of the theory to address cold regions problems. The journal serves a wide range of specialists, providing a medium for interdisciplinary communication and a convenient source of reference.