岩土力学 ›› 2026, Vol. 47 ›› Issue (7): 2347-2359.doi: 10.16285/j.rsm.2025.0633CSTR: 32223.14.j.rsm.2025.0633

• 基础理论与实验研究 • 上一篇    下一篇

真三轴条件下非饱和盐渍黄土的临界状态特性

张少英1,邵帅1,邵生俊1, 2, 3,王泽驰1,吴昊1,朱学亮1   

  1. 1.西安理工大学 土木建筑工程学院,陕西 西安 710048;2.西安理工大学 岩土工程研究所,陕西 西安 710048; 3.西安理工大学 陕西省黄土力学与工程重点实验室,陕西 西安 710048
  • 收稿日期:2025-06-18 接受日期:2025-10-09 出版日期:2026-07-13 发布日期:2026-07-09
  • 作者简介:张少英,女,1994年生,博士研究生,主要从事非饱和盐渍黄土力学特性等方面研究。E-mail: zsy1606115755@163.com
  • 基金资助:
    国家自然科学基金项目(No.52108342);陕西省自然科学基础研究计划-引汉济渭联合基金项目(No.2019JLP-21,No.2019JLZ-13);西安理工大学博士启动金(No.107-451122001)。

Critical state characteristics of saline loess under true triaxial conditions

ZHANG Shao-ying1, SHAO Shuai1, SHAO Sheng-jun1, 2, 3, WANG Ze-chi1, WU Hao1, ZHU Xue-liang1   

  1. 1. School of Civil Engineering and Architecture, Xi’an University of Technology, Xi’an, Shaanxi 710048, China; 2. Institute of Geotechnical Engineering, Xi’an University of Technology, Xi’an, Shaanxi 710048, China; 3. Shaanxi Key Laboratory of Loess Mechanics and Engineering, Xi’an University of Technology, Xi’an, Shaanxi 710048, China
  • Received:2025-06-18 Accepted:2025-10-09 Online:2026-07-13 Published:2026-07-09
  • Supported by:
    This work was supported by the Natural Science Foundation of China (52108342), Basic Research Program of Natural Science in Shaanxi Province-Han-Wei Joint Found Project (2019JLP-21,2019JLZ-13) and the Doctoral Initial Funding of Xi’an University of Technology (107-451122001).

摘要:

为探究渗透吸力对非饱和黄土在三维应力条件下的压缩、屈服、临界状态特性的影响,针对不同孔隙水盐浓度黄土,利用非饱和真三轴仪在控制基质吸力条件下进行了等向压缩试验和等pb剪切试验(p为净平均应力,b为中主应力参数)。研究结果表明:等向压缩曲线随渗透吸力增大而逐渐下移,屈服应力呈减小趋势。剪切破坏强度随着b值增大而减小,随着渗透吸力增大而增大。不同b值条件下,p-qq为广义剪应力)平面内临界状态线可使用有效净平均应力归一为饱和土临界状态线,其斜率M随渗透吸力增大而增大。子午平面内的塑性势面呈椭圆形,随着渗透吸力增大逐渐长轴变短,短轴变长。e-lgpe为非饱和土孔隙比)平面内临界状态线均随着渗透吸力增大而上移,斜率l0l1逐渐减小。非饱和土和饱和土临界状态孔隙比(es)之比e/es与气相饱和度(1−Sr)Sr为临界状态时土的饱和度)可实现归一化描述,并进一步考虑渗透吸力π建立了三维非饱和盐渍黄土临界状态孔隙比预测模型。

关键词: 非饱和真三轴试验, 盐渍黄土, 渗透吸力, 临界状态特性

Abstract:

 To explore the influence of osmotic suction on the compression, yield, and critical state characteristics of unsaturated loess under three‑dimensional stress conditions, isotropic compression tests and constant p & constant b shear tests were conducted on loess with different pore water salinities by means of a suction‑controlled unsaturated true triaxial apparatus. The results show that the isotropic compression curve gradually moves down with the increase of osmotic suction, and the yield stress shows a decreasing trend. The shear strength decreases with the increase of b value and increases with the increase of osmotic suction. Under different b values, the critical state line in the p-q plane can be normalized to the critical state line of saturated loess by using the effective net mean stress, and the slope M increases with the increase of osmotic suction. The plastic potential surfaces in the meridian plane are elliptical. In the meridian plane, the plastic potential surfaces exhibit an elliptical shape. As the osmotic suction escalates, the major axis progressively diminishes in length, whereas the minor axis experiences an elongation. The critical state line in the e-lgp plane (e is the void ratio of unsaturated soil) exhibits an upward shift as osmotic suction increases, accompanied by a gradual reduction in the slopes denoted by l0, l1. The ratio of the critical state void ratio of unsaturated loess to that of saturated loess, denoted as e/es, exhibits a normalized relationship with the gas saturation (1−Sr, Sr is the degree of saturation of soil in the critical state). Furthermore, by incorporating the osmotic suction p, a three-dimensional predictive model is developed for determining the critical state void ratio of unsaturated saline loess.

Key words: unsaturated true triaxial test, saline loess, osmotic suction, critical state characteristics

中图分类号: TU 431
[1] 张少英, 邵帅, 邵生俊, 朱学亮, 吴昊, 王泽驰. 真三轴条件下非饱和盐渍土广义有效应力研究[J]. 岩土力学, 2025, 46(12): 3773-3783.
[2] 王立业, 周凤玺, 秦虎, . 饱和盐渍土分数阶蠕变模型及试验研究[J]. 岩土力学, 2020, 41(2): 543-551.
[3] 马田田,韦昌富,陈 盼,夏晓龙. NaCl溶液对土体持水特性影响的试验研究[J]. , 2015, 36(10): 2831-2836.
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