理论与试验研究

基于细观孔隙的高温冻土蠕变变形试验研究

  • 郭焕明 ,
  • 张虎 ,
  • 刘枫 ,
  • 丑亚玲 ,
  • 郑波
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  • 1.兰州理工大学 土木工程学院,兰州 730050;
    2.东北林业大学 土木与交通学院,哈尔滨 150040;
    3.中国科学院西北生态环境资源研究院 冻土工程国家重点实验室,兰州 730000;
    4.中国水电建设集团十五工程局有限公司,西安 710399;
    5.中铁西南科学研究院有限公司,成都 611731
郭焕明(2001—),男,甘肃会宁人,硕士生,主要从事软土与冻土地基处理、数值模拟及计算等研究。E-mail: 2199827118@qq.com
张虎(1986—),男,山东济宁人,博士,教授,主要从事寒区工程与环境、冻土地基处理、数值模拟等教学和研究。E-mail:zhanghu@nefu.edu.cn

收稿日期: 2025-02-25

  网络出版日期: 2025-10-17

基金资助

国家自然科学基金(41971085);四川省科技计划(2024NSFSC0158)

Experimental Study on Creep Deformation of High-Temperature Frozen Soil Based on Microscopic Pores

  • Guo Huanming ,
  • Zhang Hu ,
  • Liu Feng ,
  • Chou Yaling ,
  • Zheng Bo
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  • 1. School of Civil Engineering, Lanzhou University of Technology, Lanzhou 730050, P.R. China;
    2. College of Civil Engineering and Transportation, Northeast Forestry University, Harbin 150040, P.R. China;
    3. State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, P.R. China;
    4. Sino hydro 15th Engineering Bureau Co., Ltd., Xi 'an 710399, P.R. China;
    5. China Railway Southwest Research Institute Co., Ltd., Chengdu 611731, P.R. China

Received date: 2025-02-25

  Online published: 2025-10-17

摘要

高温冻土在长期荷载作用下易发生蠕变变形,为探究其内部孔隙结构对高温冻土蠕变变形的影响,对高温冻土开展了不同温度、干密度和轴向应力下的静三轴蠕变试验,同时也对蠕变试验结束后的风干三轴试样进行了CT扫描及孔隙提取处理。结果表明:通过Avizo对CT扫描图片进行3D建模和孔隙提取,采用3种不同方法对提取孔隙进行孔隙等效分析后发现,球体等效误差最小,因此选择球体等效进行细观孔隙分析,并将孔隙分为0~200 μm、200~500 μm、500~1 000 μm、>1 000 μm共4类;在所给试验条件下,试样孔径主要分布在200~500 μm区间内,而蠕变变形量与孔径>500 μm孔隙数目呈正相关关系;蠕变变形随着温度的升高、干密度的减小和轴向应力的增大而增大,且温度、干密度和轴向应力都会对高温冻土蠕变变形和孔径>500 μm的孔隙数目产生显著的影响;试样内部孔径>500 μm的孔隙数量随着温度的升高、干密度的减小和轴向应力的增大而增加。

本文引用格式

郭焕明 , 张虎 , 刘枫 , 丑亚玲 , 郑波 . 基于细观孔隙的高温冻土蠕变变形试验研究[J]. 地下空间与工程学报, 2025 , 21(5) : 1613 -1620 . DOI: 10.20174/j.JUSE.2025.05.15

Abstract

The high-temperature frozen soil is prone to creep deformation under long-term load. In order to explore the influence of its internal pore structure on the creep deformation of high-temperature frozen soil, static triaxial creep tests under different temperatures, dry densities and axial stresses were carried out on the high-temperature frozen soil. At the same time, CT scanning and pore extraction were carried out on the air-dried triaxial samples after the creep test. The results show that: Avizo was used to conduct 3D modeling and pore extraction on CT scan images. After conducting pore equivalence analysis on the extracted pores using three different methods, it was found that sphere equivalent error was the smallest. Therefore, sphere equivalent was selected for microscopic pore analysis, and the pores were divided into four categories: 0~200 μm, 200~500 μm, 500~1 000 μm and >1 000 μm. Under the given test conditions, the pore size of the sample is mainly distributed in the range of 200~500 μm, and the creep deformation is positively correlated with the number of pores with the pore size >500 μm. The creep deformation increases with the increase of temperature, the decrease of dry density and the increase of axial stress, and the temperature, dry density and axial stress all have significant effects on the creep deformation and the number of pores with pore size >500 μm. The number of pores with pore size >500μm increases with increasing temperature, decreasing dry density and increasing axial stress.

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