岩土力学 ›› 2026, Vol. 47 ›› Issue (5): 1492-1500.doi: 10.16285/j.rsm.2025.0425CSTR: 32223.14.j.rsm.2025.0425

• 基础理论与实验研究 • 上一篇    下一篇

考虑体变的横观各向同性黄土持水特性研究

郭楠1,王飞龙1,杨校辉1,浦金升1,陈正汉2   

  1. 1. 兰州理工大学 土木与水利工程学院,甘肃 兰州 730050;2. 联勤保障部队工程大学,重庆 400041
  • 收稿日期:2025-04-22 接受日期:2025-08-08 出版日期:2026-05-11 发布日期:2026-05-08
  • 作者简介:郭楠,女,1987年生,博士,副教授,主要从事非饱和土与特殊土及地基处理等方面的教学和科研工作。E-mail: 355094754@qq.com
  • 基金资助:
    国家自然科学基金项目(No. 42462028,No. 52168051,No. 52368049);甘肃省杰出青年基金(No. 25JRRA057);兰州市青年科技人才创新项目(No. 2023-QN-52,No. 2023-QN-27)

Water retention characteristics of transversely isotropic loess with consideration of volume change

GUO Nan1, WANG Fei-long1, YANG Xiao-hui1, PU Jin-sheng1, CHEN Zheng-han2   

  1. 1. School of Civil and Hydraulic Engineering, Lanzhou University of Technology, Lanzhou, Gansu 730050, China; 2. PLA Joint Logistics Support Force University of Engineering, Chongqing 400041, China
  • Received:2025-04-22 Accepted:2025-08-08 Online:2026-05-11 Published:2026-05-08
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (42462028, 52168051, 52368049), Gansu Provincial Foundation for Distinguished Young Scholars (25JRRA057) and the Lanzhou Youth Science and Technology Talent Innovation Project (2023-QN-52, 2023-QN-27).

摘要:

横观各向同性黄土在竖向应力作用下会发生脱湿收缩现象,导致其持水特性和力学行为改变,若处理不当将会给工程带来巨大损失,但研究竖向应力作用下脱湿收缩对其持水特性影响的理论模型未见报道。为此,采用压力板仪,对不同初始干密度的横观各向同性黄土进行土-水特征曲线(soil-water characteristic curve,简称SWCC)试验,测得每级吸力s稳定后的含水率和体积变化。结果表明:初始干密度较低土样,在较大竖向应力、较小吸力下θ-sθ 为体积含水率)关系曲线呈现略有上扬趋势,其余土样含水率均随吸力增大而减小;在吸力增大的过程中,除初始干密度较小土样外,不同竖向应力下,相同初始干密度土样的SWCC均发生交叉;当吸力增大到一定数值时,竖向应力越大,土样wθ 和饱和度S数值越大;初始干密度越大,土样SWCC受竖向应力变化影响越小;土样体应变随竖向应力和吸力增大而增大。结合广义胡克定律及Fredlund-Xing模型,建立了在竖向应力-吸力耦合作用下的横观各向同性黄土体应变模型及考虑体应变的土-水特征曲线模型。两模型均能较好地反映不同竖向应力下横观各向同性黄土脱湿收缩过程中体应变和饱和度的变化规律。研究成果不仅能丰富和发展非饱和土的SWCC模型,而且对天然成层地基和填土地基工程安全性具有重要理论价值与应用意义。

关键词: 横观各向同性, 非饱和黄土, 体积变化, 持水特性, 竖向应力

Abstract:

Transversely isotropic loess undergoes dehumidification and shrinkage when subjected to vertical stress, resulting in changes to its water-retention characteristics and mechanical behavior. Improper management of this phenomenon can lead to substantial engineering losses. However, no theoretical models have been reported that investigate the impact of dehumidification and shrinkage on water-retention characteristics under vertical stress. This study utilized a pressure plate apparatus to perform soil-water characteristic curve (SWCC) tests on transversely isotropic loess with different initial dry densities. Water content w and volumetric changes were measured after stabilization at each suction level. The results indicate that, except for soil samples with lower initial dry density, the θ-s (θ is volumetric water content) curve displayed a slight upward trend under high vertical stress and low suction, while the water content of other samples generally decreased with increasing suction. During the suction increase, except for soil samples with very low initial dry density, the SWCCs of samples with the same initial dry density but different vertical stresses intersected. As suction increases to a certain value, higher vertical stress results in larger values of w, θ, and saturation Sr for the soil sample. Soil samples with higher initial dry densities exhibited reduced sensitivity to variations in vertical stress within their SWCCs. The volumetric strain of the soil sample increases with both increasing vertical stress and suction. By integrating generalized Hooke’s law with the Fredlund-Xing model, we established a volumetric strain model that accounts for coupled vertical stress-suction effects and a modified SWCC model for volume changes. Both models effectively captured the evolution of volumetric strain and saturation in transversely isotropic loess during dehumidification and shrinkage under varying vertical stresses. This research not only advances the theoretical framework of unsaturated soil SWCC models, but also offers critical insights for ensuring the safety of natural stratified foundations and compacted fill engineering projects.

Key words: transverse isotropy, unsaturated loess, volume change, water-holding characteristics, vertical stress

中图分类号: TU 444
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