岩土力学 ›› 2023, Vol. 44 ›› Issue (12): 3349-3359.doi: 10.16285/j.rsm.2022.2005

• 基础理论与实验研究 • 上一篇    下一篇

宽广吸力范围非饱和土剪切强度试验研究及其预测

牛庚1, 2,朱晓凤1,李俊星1,吕梦缘1,安荔琪1,陈子晗1   

  1. 1. 青岛理工大学 理学院,山东 青岛 266520;2. 中国科学院武汉岩土力学研究所 岩土力学与工程国家重点实验室,湖北 武汉 430071
  • 收稿日期:2022-12-28 接受日期:2023-03-31 出版日期:2023-12-20 发布日期:2023-12-21
  • 作者简介:牛庚,男,1991年生,博士,讲师,主要从事非饱和土力学方面的研究工作。
  • 基金资助:
    国家自然科学基金(No.42307236,No.12172187);山东省自然科学基金(No.ZR2023QE001);岩土力学与工程国家重点实验室开放基金课题(No.SKLGME021019)

Experimental study on shear strength of unsaturated soil over a wide suction range and its prediction

NIU Geng1, 2, ZHU Xiao-feng1, LI Jun-xing1, LÜ Meng-yuan1, AN Li-qi1, CHEN Zi-han1   

  1. 1. School of Science, Qingdao University of Technology, Qingdao, Shandong 266520, China; 2. State Key Laboratory of Geomechanics and Geotechnical Engineering, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China
  • Received:2022-12-28 Accepted:2023-03-31 Online:2023-12-20 Published:2023-12-21
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (42307236, 12172187), the Natural Science Foundation of Shandong Province (ZR2023QE001) and the Open Research Fund of State Key Laboratory of Geomechanics and Geotechnical Engineering (SKLGME021019).

摘要: 以弱膨胀土为试验材料,开展了宽广吸力范围内非饱和土的持水和强度特性试验研究,并提出适用于宽广吸力范围的非饱和土强度模型。结果表明,在广吸力范围内,应力−应变曲线随吸力增加而增高,在低吸力范围呈现应变硬化,在高吸力范围呈现应变软化。低吸力范围,试样呈现剪缩变形;高吸力范围,试样在轴向应变2%处开始呈现剪胀趋势。此外,提出一种区分吸附水和毛细水的土−水特征曲线模型,并假设吸力引起的强度增强部分主要由毛细水决定。将有效应力系数用毛细水饱和度替代,并代入Bishop非饱和土强度公式,利用不同类型土剪切强度的实测数据和文献中剪切强度模型对比,表明该强度模型可以很好地描述宽广吸力范围内的非饱和土强度。

关键词: 非饱和土, 剪切强度, 土-水特征曲线, 有效应力系数, 宽广吸力范围

Abstract: In this paper, the experimental studies on the water retention and strength properties of unsaturated weakly expansive soil in a wide suction range were carried out, and a strength model of unsaturated soil over a wide suction range was proposed. The results show that in the wide suction range, the stress-strain curve increases with the increase of suction. The strain hardening occurs in the low suction range, while the strain softening appears in the high suction range. In the low suction range, the sample presents shear deformation, while in the high suction range, the sample begins to show a shear dilation trend at the axial strain of 2%. In addition, a soil-water retention curve model was proposed to distinguish adsorbed water from capillary water, assuming that the strength increment caused by suction is mainly determined by capillary water. The degree of saturation of capillary water was used to replace the effective stress coefficient and then it was substituted into the Bishop’s unsaturated soil strength formula. The proposed model was verified by test data of various soil types and compared with the models in the literature. The results show that the proposed model can well describe the strength of unsaturated soil in a wide suction range.

Key words: unsaturated soil, shear strength, soil-water retention curve, effective stress coefficient, wide suction range

中图分类号: TU443
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