4.7 Article

Experimental and numerical investigation on thermal-moisture-mechanical behaviors on a new anti-frost cutting bed of high-speed railway in deep seasonally frozen ground regions under extreme climate

期刊

COMPUTERS AND GEOTECHNICS
卷 136, 期 -, 页码 -

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.compgeo.2021.104251

关键词

Thermal-moisture-mechanical behavior; Anti-frost cutting bed; Frost depth; Frost heave; Deep seasonally frozen ground

资金

  1. Foundation for Excellent Youth Scholars of Northwest Institute of EcoEnvironment and Resources, CAS [FEYS2019002]
  2. Research Project of State Key Laboratory of Frozen Soil Engineering [SKLFSEZQ52]
  3. Open Project of State Key Laboratory of Mechanical Behavior and System Safety of Traffic Engineering Structures, Shijiazhuang Tiedao University [KF2020-02]
  4. National Natural Science Foundation of China [41801055]

向作者/读者索取更多资源

This study examines the effectiveness of a new High-speed Railway (HSR) anti-frost cutting bed in a deep seasonally frozen ground region using monitoring data and numerical models, while discussing the impact of snow cover on soil water-heat state and causes of slope instability in cold regions.
Cutting damages caused by frost action seriously threaten the safe operation of railways in cold regions. This paper uses worth of monitoring data to examine the temperature, unfrozen water, and deformation behaviors of a new High-speed Railway (HSR) anti-frost cutting bed in a deep seasonally frozen ground region. A frost numerical model is established to study the effectiveness of the anti-frost cutting bed under extreme weather conditions. The influence of snow cover on the soil water-heat state and the causes of slope instability in cold regions are also discussed. Results demonstrate that the frost depth of the cutting top is less than that of the cutting center and that the sensitivity of different soil layers' unfrozen water content to ground temperature changes are delayed in turn. Frost heave mainly occurs in the initial freezing and freeze-thaw alternating periods at the ground surface. Greater infiltration of rainwater or snow melt will lead to a greater peak frost value. Slopes in frozen soil regions are thus prone to instability and collapse at the freeze-thaw interface. These findings will help to improve understandings of thermal-moisture-mechanical behaviors for cutting beds with spatiotemporally in deep seasonally frozen ground regions, thereby potentially improving HSR operation quality.

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