岩土力学 ›› 2025, Vol. 46 ›› Issue (3): 905-915.doi: 10.16285/j.rsm.2024.0670

• 基础理论与实验研究 • 上一篇    下一篇

径向冻融过程中软黏土水热力试验研究

郭焕明1,张虎2, 3,丑亚玲1,郑波4,胡金涛2,韩善博1   

  1. 1. 兰州理工大学 土木工程学院,甘肃 兰州 730050;2. 东北林业大学 土木与交通学院,黑龙江 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,甘肃 兰州 730000;4. 中铁西南科学研究院有限公司,四川 成都 611731
  • 收稿日期:2024-05-30 接受日期:2024-08-29 出版日期:2025-03-10 发布日期:2025-03-10
  • 通讯作者: 张虎,男,1986年生,博士,教授,主要从事寒区工程与环境、软土与冻土地基处理、数值模拟及计算等教学和研究。E-mail: zhanghu@nefu.edu.cn
  • 作者简介:郭焕明,男,2001年生,硕士研究生,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
  • 基金资助:
    黑龙江省优秀青年基金(No.YQ2022D001);国家自然基金(No.41971085);四川省科技计划(No.2024NSFSC0158)

Hydro-thermal-mechanical experiment of soft clay during radial freeze-thaw process

GUO Huan-ming1, ZHANG Hu2, 3, CHOU Ya-ling1, ZHENG Bo4, HU Jin-tao2, HAN Shan-bo1   

  1. 1. School of Civil Engineering, Lanzhou University of Technology, Lanzhou, Gansu 730050, China; 2. College of Civil Engineering and Transportation, Northeast Forestry University, Harbin, Heilongjiang 150040, China; 3. State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China; 4. Southwest Research Institute of China Railway, Chengdu, Sichuan 611731, China
  • Received:2024-05-30 Accepted:2024-08-29 Online:2025-03-10 Published:2025-03-10
  • Supported by:
    This work was supported by the Outstanding Youth Fund of Heilongjiang Province (YQ2022D001) the National Natural Science Foundation (41971085) and Sichuan Science and Technology Project (2024NSFSC0158).

摘要: 为了探究径向冻融条件下软黏土水热力过程,开展了不同温度下软黏土冻融试验,对比分析了各冻融过程中土样温度、含水率、土压力、排水量和耗电量的变化规律。试验结果表明:冻融过程中土样实际温度下降速率均与冻结锋面的移动速率呈正相关关系,温度的传递效率主要与传热距离、传热介质和能量损失率有关;在土样冻结过程中,水分的迁移与冷端对水分的吸力作用和冻胀过程中冻胀对水分的相对作用密切相关;冻结过程中产生的环向和径向冷生构造会加速软黏土中水分的排出,冻胀力会对未冻区土体产生固结作用;通过对试验过程中冻结范围、排水量和耗电量的对比,发现试验温度为−15 ℃时在冻结过程中产生的融沉圈直径最大,此时的能耗比也最大,因此,将−15 ℃作为本系列试验的最佳冻结温度。

关键词: 软土地基, 人工冻结, 水热力过程, 最佳温度

Abstract: In order to investigate the hydro-thermal-mechanical process of soft clay under radial freeze-thaw conditions, freeze-thaw tests of soft clay at different temperatures were carried out, and the changes in temperature, water content, soil pressure, water discharge, and power consumption of soil samples were analyzed and compared. The results show that the actual temperature drop rate is positively correlated with the moving rate of the frozen front, and the temperature transfer efficiency is mainly related to the heat transfer distance, heat transfer medium, and energy loss rate. During the freezing of soil samples, the migration of water is closely related to the suction effect of the cold end on water and the relative effect of frost heave on water. The circumferential and radial cryogenic structures produced during the freezing process will accelerate the discharge of water from the soft clay, and the frost heave force will produce a consolidation effect on the soil in the unfrozen area. By comparing the freezing range, water discharge, and power consumption during the test process, it is found that the diameter of the thawing circle generated during the freezing process is the largest when the test temperature is −15 ℃, and the energy consumption ratio is also at its highest at this point. Therefore, −15 ℃ is taken as the optimal freezing temperature for this series of tests.

Key words: soft foundation, artificial freezing, hydro-thermal-mechanical process, optimal temperature

中图分类号: TU441
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