岩土力学 ›› 2025, Vol. 46 ›› Issue (7): 2071-2084.doi: 10.16285/j.rsm.2024.1265CSTR: 32223.14.j.rsm.2024.1265

• 基础理论与实验研究 • 上一篇    下一篇

冻结钙质黏土复杂应力路径下的力学响应及本构模型研究

曹祎1, 2, 3,荣传新2, 3,王衍森1,常磊2, 3,王彬2, 3   

  1. 1.中国矿业大学 深地工程智能建造与健康运维全国重点实验室,江苏 徐州 221116; 2.安徽理工大学 矿山地下工程教育部工程研究中心,安徽 淮南 221116;3.安徽理工大学 土木建筑学院,安徽 淮南 232001
  • 收稿日期:2024-10-14 接受日期:2025-03-03 出版日期:2025-07-10 发布日期:2025-07-08
  • 通讯作者: 荣传新,男,1968年生,博士,教授,主要从事冻土力学及岩土与地下结构工程研究。E-mail: chxrong@aust.edu.cn
  • 作者简介:曹祎,男,1998年生,博士研究生,主要从事冻土力学及人工地层冻结理论与应用研究。E-mail: cyaust@163.com
  • 基金资助:
    国家自然科学基金项目(No.51878005,No.52074264);矿山地下工程教育部工程研究中心开放基金(No.JYBGCZX2024103);江苏省研究生科研与实践创新计划项目(No.KYCX24_2818);中国矿业大学研究生创新计划项目(No.2024WLKXJ197);安徽省自然科学基金面上项目(No.2408085ME147)。

Mechanical response and constitutive modeling of frozen calcareous clay under complex multi-axial stress paths

CAO Yi1, 2, 3, RONG Chuan-xin2, 3, WANG Yan-sen1, CHANG Lei2, 3, WANG Bin2, 3   

  1. 1. State Key Laboratory of Intelligent Construction and Healthy Operation & Maintenance of Deep Underground Engineering, China University of Mining & Technology, Xuzhou, Jiangsu 221116, China; 2. Engineering Research Center of Underground Mine Construction, Ministry of Education, Anhui University of Science and Technology, Huainan, Anhui 221116, China; 3. School of Civil Engineering and Architecture, Anhui University of Science and Technology, Huainan, Anhui 232001, China
  • Received:2024-10-14 Accepted:2025-03-03 Online:2025-07-10 Published:2025-07-08
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51878005, 52074264), the Open Fund for Engineering Research Center of Underground Mine Construction, Ministry of Education (JYBGCZX2024103), the Postgraduate Research Practice Innovation Program of Jiangsu Province (KYCX24_2818), the Graduate Innovation Program of China University of Mining and Technology (2024WLKXJ197) and Anhui Provincial Natural Science Foundation (2408085ME147).

摘要: 两淮矿区广泛分布着钙质黏土层,其具有冰点低、冻胀性强、遇水易崩解、强度低等特点,对冻结法施工提出了严峻挑战。为探究冻结钙质黏土在复杂应力路径下的力学响应,通过ZSZ-2000冻土真三轴试验平台,开展了不同围压、温度、含水率和中主应力系数条件下的真三轴压缩试验,分析了冻结钙质黏土在其影响下的强度和变形特性。试验结果表明:冻结钙质黏土强度与中主应力系数和围压呈现出良好的二次函数关系,与温度呈负相关,与含水率呈正相关。随着含水率的增加,其破坏强度的增长速率逐渐降低。破坏强度受中主应力效应和围压效应的共同控制,均表现出明显的强化-弱化双重作用,并存在临界中主应力系数bc=0.75,临界围压σ3c =3 MPa。随着围压的增大,体应变由先剪缩后剪胀逐渐转变为纯剪缩的特性,且随着值的增大,试样峰值体应变逐渐变大。基于试验结果,建立了考虑温度、含水率和中主应力系数影响的改进邓肯-张模型,并验证模型的可靠性。研究结果可为冻结壁设计优化和深部冻结法凿井提供理论依据。

关键词: 冻结黏土, 中主应力系数, 强度演化规律, 真三轴应力路径, 邓肯-张模型

Abstract: Calcium clay layers are widely distributed in the Huainan-Huaibei mining area, with the characteristics of low freezing point, strong frost heave, easy disintegration upon contact with water, and low strength, posing a severe challenge to construction using freezing methods. To investigate the mechanical response of frozen calcareous clay under complex stress paths, true triaxial compression tests were performed on the ZSZ-2000 frozen soil true triaxial test platform, varying confining pressures, temperatures, moisture contents, and intermediate principal stress ratios. The strength and deformation characteristics of frozen calcareous clay under these varying conditions were analyzed. The test results indicate that the strength of frozen calcareous clay has a good quadratic relationship with the intermediate principal stress coefficient b and confining pressure, is negatively correlated with temperature, and positively correlated with moisture content. Furthermore, the rate of increase in the failure strength of frozen calcareous clay decreases as the moisture content rises. The failure strength is significantly influenced by the intermediate principal stress and confining pressure, showing both strengthening and weakening effects. A critical intermediate principal stress coefficient of bc =0.75 and a critical confining pressure of σ3c=3 MPa were identified. As the confining pressure rises, the volumetric strain gradually shifts from initial shear contraction followed by shear dilation to pure shear contraction. Moreover, as the b value increases, the peak volumetric strain of the samples also increases. Based on the experimental results, an improved Duncan-Chang model was developed, taking into account the effects of temperature, moisture content, and intermediate principal stress coefficient, and its reliability was verified. The research findings provide a theoretical foundation for optimizing frozen wall design and deep shaft excavation using freezing methods.

Key words: frozen clay, intermediate principal stress coefficient, strength evolution law, true triaxial stress path, Duncan-Chang model

中图分类号: TU 411
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