岩土力学 ›› 2025, Vol. 46 ›› Issue (11): 3421-3430.doi: 10.16285/j.rsm.2024.1578CSTR: 32223.14.j.rsm.2024.1578

• 基础理论与实验研究 • 上一篇    下一篇

单向冻融作用下砂岩力学各向异性演化与损伤模型

吕志涛1,赵志远1,蔡毅1,夏才初2,段君义1   

  1. 1. 南昌大学 工程建设学院,江西 南昌 330031;2. 宁波大学 岩石力学研究所,浙江 宁波 315211
  • 收稿日期:2024-12-22 接受日期:2025-06-06 出版日期:2025-11-14 发布日期:2025-11-11
  • 通讯作者: 段君义,男,1991年生,博士,讲师,主要从事特殊土力学与岩土工程方面的研究。E-mail:junyidjy@163.com
  • 作者简介:吕志涛,男,1990年生,博士,副教授,主要从事岩石力学与地下工程方面的教学和科研工作。E-mail: lvzhitao90@126.com
  • 基金资助:
    国家自然科学基金项目(No. 52108370);江西省自然科学基金项目(No. 20212BAB214062,No. 20224BAB204061,No. 20243BCE51121)。

Evolution of anisotropic mechanical properties and damage model of sandstone under unidirectional freeze-thaw action

LYU Zhi-tao1, ZHAO Zhi-yuan1, CAI Yi1, XIA Cai-chu2, DUAN Jun-yi1   

  1. 1. School of Infrastructure Engineering, Nanchang University, Nanchang, Jiangxi 330031, China; 2. Institute of Rock Mechanics, Ningbo University, Ningbo, Zhejiang 315211, China
  • Received:2024-12-22 Accepted:2025-06-06 Online:2025-11-14 Published:2025-11-11
  • Supported by:
    This work was supported by National Natural Science Foundation of China (52108370) and Jiangxi Provincial Natural Science Foundation (20212BAB214062, 20224BAB204061, 20243BCE51121).

摘要: 目前研究岩石冻融损伤主要基于各向均匀冻融试验,但寒区工程中单向冻融作用的情况广泛存在。目前,对单向冻融作用下岩石力学特性演化及其损伤模型认识不足。因此,选取砂岩为研究对象,进行单向冻融循环试验及单轴压缩试验,对比分析冻融后砂岩平行和垂直冻融方向的弹性模量、抗压强度、应力-应变曲线、压缩破坏模式,以研究单向冻融作用下岩石力学特性演化。试验发现,单向冻融作用后,砂岩平行冻融方向抗压强度大于垂直冻融方向,平行冻融方向弹性模量小于垂直冻融方向,平行冻融方向的峰值应力和峰值应变均大于垂直冻融方向;砂岩平行冻融方向的单轴压缩破坏模式与未冻融时相同,表现为“X”型压剪破坏,而垂直冻融方向的破坏模式为破坏面沿加载方向的劈裂破坏模式。单向冻融作用下,砂岩力学性质从初始状态的各向同性向各向异性演化。基于上述试验现象,引入单向冻融各向异性系数,建立单向冻融作用下砂岩损伤模型并利用试验数据对模型进行了验证。

关键词: 砂岩, 单向冻融, 力学特性演化, 各向异性, 损伤模型

Abstract: Current research on rock freeze-thaw damage mainly focuses on uniform freeze-thaw tests. However, the situation of unidirectional freeze-thaw action is widely present in cold region engineering, and there is a lack of sufficient understanding of the evolution of mechanical properties and damage models under unidirectional freeze-thaw conditions. Therefore, this study selected sandstone as the research object and conducted unidirectional freeze-thaw cycle tests and uniaxial compression tests. The elastic modulus, uniaxial compressive strength, stress-strain curves, and failure modes under uniaxial compression were analyzed for sandstone samples parallel and perpendicular to the freeze-thaw direction after undergoing freeze-thaw cycles. The results indicate that, following unidirectional freeze-thaw action, the compressive strength of sandstone parallel to the freeze-thaw direction is greater than that perpendicular to it, while the elastic modulus parallel to the freeze-thaw direction is smaller than that in the perpendicular direction. Both the peak stress and strain in the parallel direction are higher than those in the perpendicular direction. In uniaxial compression tests, the failure mode of sandstone parallel to the freeze-thaw direction remains consistent with that of samples that have not undergone freeze-thaw action, exhibiting X-shaped shear failure, whereas the failure mode perpendicular to the freeze-thaw direction manifests as splitting along the loading direction. Under unidirectional freeze-thaw action, the mechanical properties of sandstone transition from isotropy to anisotropy. Based on the aforementioned experimental observations, an anisotropic coefficient for unidirectional freeze-thaw was introduced, and a damage model for sandstone under unidirectional freeze-thaw conditions was established. The model was subsequently validated using experimental data.

Key words: sandstone, unidirectional freeze-thaw, mechanical characteristics evolution, anisotropy, damage model

中图分类号: TU 451
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