吉林大学学报(地球科学版) ›› 2025, Vol. 55 ›› Issue (6): 1923-1944.doi: 10.13278/j.cnki.jjuese.20250261

• 地质工程与环境工程 • 上一篇    下一篇

冻土-结构界面剪切性能研究进展综述

王伯昕,王天略,王清,陈慧娥   

  1. 吉林大学建设工程学院,长春130026

  • 出版日期:2025-11-26 发布日期:2025-12-30
  • 通讯作者: 王清(1959— ),女,教授,博士生导师,主要从事土体工程地质方面的研究,E-mail:wangqing@jlu.edu.cn
  • 作者简介:王伯昕(1980— ),男,教授,博士生导师,主要从事土-混凝土界面力学性能方面的研究,E-mail:boxinwang@jlu.edu.cn
  • 基金资助:
    国家自然科学基金项目(42072296,42572353)

A Review of Research Progress on Shear Behaviour of Frozen Soil-Structure Interfaces

Wang Boxin,Wang Tianlüe,Wang Qing,Chen Huie   

  1. College of Construction Engineering,Jilin University,Changchun 130026,China
  • Online:2025-11-26 Published:2025-12-30
  • Supported by:
    Supported by the National Natural Science Foundation of China (42072296,42572353)

摘要: 在寒区工程中,冻土-结构界面的剪切性能是影响设施长期服役稳定性的关键因素,而现有研究对多物理场作用下的界面损伤机制缺乏系统表征。为揭示热力学条件扰动下,各影响因素通过调整冰水相变过程,进而重塑冻土-结构界面的力学行为,本文从试验方法、影响因素及本构模型三个方面,对冻土-结构界面剪切性能的研究进展进行了系统梳理与评述。首先通过总结直剪试验、现场原位试验及模型桩试验等方法,明确了热-水-盐-力多场耦合条件下各因素对界面力学行为的影响路径;进而分析了温度、水分、冻融循环和盐分等因素通过调控冰水相变过程对界面剪切性能的作用机制;最后,评估了现有冻土-结构界面本构模型的适用性与局限性。结果表明:温度梯度与水分迁移通过调控冰水相变过程的冰胶结强度与未冻水膜厚度改变界面剪切性能;冻融循环引发的孔隙重构与冰晶分异,导致界面强度劣化;盐分则通过改变相变温度阈值和盐结晶膨胀效应,影响界面空间构成。现有模型在冰水相变、长期冻融及多场耦合表征上存在明显不足。建议未来从“试验-观测-模型”多角度出发,结合跨尺度观测技术构建界面热-水-盐-力耦合模型,为寒区工程抗冻胀设计和灾害防控提供设计依据与研究方向。


关键词: 界面体系, 剪切性能, 冻土, 结构界面, 冰水相变, 冻融循环, 本构模型

Abstract:  In cold region engineering, the shear performance of frozen soil-structure interface is a key factor influencing the long-term service stability of facilities. However, the existing studies lack systematic characterization of the interface damage mechanism under the action of multi-physical field interactions. In order to reveal the mechanical behavior of frozen soil-structure interface by adjusting the ice-water phase transition process under the disturbance of thermodynamic conditions, this study systematically reviews the research progress of shear properties of frozen soil-structure interface from three aspects such as experimental methods, influencing factors and constitutive models. Firstly, by summarizing the methods of direct shear test, in-situ test and model pile test, the influence pathways of various factors on the mechanical behavior of the interface under the multi-field coupling condition of heat-water-salt-force are clarified. Furthermore, the mechanism of temperature, moisture, freeze-thaw cycle and salt on the interfacial shear performance by regulating the ice-water phase transition process was analyzed. Finally, the applicability and limitations of the existing constitutive model of frozen soil-structure interface are evaluated. The results show that the temperature gradient and water migration change the interfacial shear performance by regulating the ice cementation strength and the thickness of the unfrozen water film during the ice-water phase transition process. The pore reconstruction and ice crystal differentiation caused by freeze-thaw cycles lead to the deterioration of interface strength. Salt affects the interface space composition by changing the phase transition temperature threshold and salt crystallization expansion effect. The existing models have obvious deficiencies in ice-water phase transition, long-term freeze-thaw and multi-field coupling characterization. It is suggested that future work focus on developing a thermo-hyforr-salt-mechanical coupled interface model based on a “test-observation-model” framework integrated  with cross-scale observation technology, thereby providing a design basis and research direction for frost-heave prevention and disaster mitigation in cold regions.


Key words:  , interface system, shear performance, frozen soil, structural interface, ice-water phase transition, freeze-thaw cycle, constitutive model

中图分类号: 

  • P642.14
[1] 王伯昕, 高银龙, 王清, 刘佳奇. 冻融循环对季冻土区粉质黏土-混凝土界面剪切性能的影响[J]. 吉林大学学报(地球科学版), 2024, 54(5): 1592-1603.
[2] 韩长玉, 赵浩汀.

路基填筑短期内热棒高导热性影响 [J]. 吉林大学学报(地球科学版), 2024, 54(2): 570-580.

[3] 赵越, 司运航, 张译丹, 赵京禹. 水化-冻融耦合条件下大理岩蠕变损伤本构模型[J]. 吉林大学学报(地球科学版), 2024, 54(1): 231-241.
[4] 苑晓青, 吴泽炬, 王清, 陈慧娥, 林森, 牛岑岑, 徐鑫. 冻融循环对钙剂改良土体分散性效果的影响[J]. 吉林大学学报(地球科学版), 2023, 53(6): 1812-1825.
[5] 赵越, 李磊, 闫晗, 肖万山, 苏艳军. 水化-冻融耦合作用下大理岩单轴蠕变力学特性[J]. 吉林大学学报(地球科学版), 2023, 53(4): 1195-1203.
[6] 张 军, 张 泽, 郭 磊, 谢春磊, 金豆豆, 翟金榜. 不同施工季节对多年冻土区锥柱式基础地温回冻影响[J]. 吉林大学学报(地球科学版), 2023, 53(2): 502-.
[7] 吕建航, 杨忠年, 时伟, 李国玉, 凌贤长, 张莹莹. 冻融循环下加筋膨胀土边坡稳定性模型试验[J]. 吉林大学学报(地球科学版), 2021, 51(5): 1587-1596.
[8] 张琦, 杨忠年, 时伟, 凌贤长, 涂志斌. 冻融循环下初始含水率对非饱和膨胀土剪切特性试验[J]. 吉林大学学报(地球科学版), 2021, 51(5): 1544-1550.
[9] 崔赢, 沈宇鹏, 张中琼. 环境因素对兴-贝型多年冻土分布与发育的影响[J]. 吉林大学学报(地球科学版), 2021, 51(5): 1427-1440.
[10] 石梁宏, 李双洋. 寒区渠基黏土热参数最优概率分布[J]. 吉林大学学报(地球科学版), 2021, 51(2): 473-482.
[11] 徐新木, 张耀平, 付玉华, 雷大星, 邹雄刚. 冻融循环下含节理类岩石试样剪切破坏特性[J]. 吉林大学学报(地球科学版), 2021, 51(2): 483-494.
[12] 孙洪伟, 傅汝进. 季冻土区临水轻台结构冻拔特征分析及防治[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1405-1414.
[13] 张泽, 周泓, 秦琦, 邴慧, 武俊杰, 周攀峰. 冻融循环作用下黄土的孔隙特征试验[J]. 吉林大学学报(地球科学版), 2017, 47(3): 839-847.
[14] 孙忠军,杨志斌,秦爱华,张富贵,周亚龙. 中纬度带天然气水合物地球化学勘查技术[J]. 吉林大学学报(地球科学版), 2014, 44(4): 1063-1070.
[15] 宿晓萍,王清,王文华,孙昊月. 季节冻土区盐渍土环境下混凝土抗冻耐久性机理[J]. 吉林大学学报(地球科学版), 2014, 44(4): 1244-1253.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!