湿化泥岩路基上拱变形计算方法及数值模拟研究
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1.长沙理工大学 交通学院;2.长沙理工大学 土木与环境工程学院

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U416.1

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国家自然科学基金面上项目(52278439,52078066);湖南省科技创新计划资助(2025AQ2015);交通运输行业重点科技项目(2022-MS1-032);湖南省科技创新计划项目(2023RC3138);湖南省自然科学基金面上项目(2023JJ30035);中央引导地方科技发展资金项目(桂科ZY24212051);湖南省自然科学基金委青年项目(2024JJ6282)


Calculation Method and Numerical Simulation Study of Wetting Mudstone Subgrade
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    摘要:

    【目的】为研究泥岩路堑路基因湿化变形而构成的长期潜在威胁,以湿化泥岩路基为研究对象,旨在提供一种有效的湿化泥岩路基变形预测方法。【方法】本研究利用计算方法与数值模拟相结合的手段,探究了湿化条件下路基上拱的变形特征,揭示了不同泥岩密度、表层含水率以及施工扰动条件下泥岩路基上拱变形的影响规律。【结果】结果显示:路基表层泥岩相同湿化情况下,各时间段下的路基上拱变形,均呈现出路基两侧变形急剧增大,路基中心区域变形逐渐放缓;路基表层湿化程度越大,路基整体变形也越显著,水份沿深度方向的扩散逐渐平稳,在路基深度5m处,路基湿化程度相差<5%;路基表层泥岩受扰动后,路基变形随着受扰动程度的增大而增加,且路基变形逐渐呈现出“M”型的趋势,路基两侧变形增幅相较于路基中心区域更加明显。【结论】本研究表明,在不同因素下路基的竖向变形情况,主要取决于不同路基深度下泥岩的湿化程度,本研究可为后续泥岩路基湿化上拱变形的治理提供一定的参考。

    Abstract:

    [Purposes] In order to investigate the long-term potential risks posed by the moisture-induced deformation of mudstone road embankments, this study focuses on moisture-sensitive mudstone roadbeds, aiming to provide an effective method for predicting their deformation. [Methods] This study employs a combination of computational methods and numerical simulations to investigate the deformation characteristics of roadbed heaving under wetting conditions, revealing the influence patterns of different mudstone densities, surface water contents, and construction disturbance conditions on the heaving deformation of mudstone roadbeds. [Findings] The results indicate that under the same wetting conditions of the subgrade surface mudstone, the arching deformation of the subgrade at different time periods shows a sharp increase in deformation on both sides of the subgrade, while the deformation in the central area of the subgrade gradually slows down. The greater the wetting degree of the subgrade surface, the more significant the overall deformation of the subgrade. Moisture diffusion along the depth gradually stabilizes, and at a subgrade depth of 5 meters, the difference in wetting degree is less than 5%. After disturbance of the subgrade surface mudstone, subgrade deformation increases with the level of disturbance, and the deformation gradually exhibits an "M"-shaped trend, with the increase in deformation on both sides of the subgrade being more pronounced than in the central area. [Conclusions] This study indicates that the vertical deformation of the subgrade under various factors primarily depends on the degree of moisture in the mudstone at different subgrade depths. The findings of this research can provide a reference for the management of hoisting deformation in mudstone subgrades due to wetting in subsequent works.

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  • 收稿日期:2025-09-29
  • 最后修改日期:2025-11-25
  • 录用日期:2025-11-26
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