Influence of initial water content on unsaturated shear strength of compacted GaoMiaoZi (GMZ) bentonite

被引:3
|
作者
Zhao, N. F. [1 ]
Ye, W. M. [1 ,2 ]
Wang, Q. [1 ]
Chen, B. [1 ]
Cui, Y-J [1 ,3 ]
机构
[1] Tongji Univ, Key Lab Geotech & Underground Engn, Minist Educ, Shanghai 200092, Peoples R China
[2] Minist Educ China, United Res Ctr Urban Environm & Sustainable Dev, Shanghai 200092, Peoples R China
[3] UR Navier CERMES, Ecole Ponts ParisTech, Paris, France
基金
中国国家自然科学基金;
关键词
critical state line; Hvorslev surface; compacted bentonite; initial water content; CRITICAL-STATE; BEHAVIOR; FRAMEWORK;
D O I
10.1139/cgj-2019-0431
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
This paper presents an experimental study on the influence of initial water content on unsaturated shear strength of compacted bentonite. Isotropic loading and triaxial shear tests were conducted on compacted GaoMiaoZi (GMZ) bentonite specimens with different initial water contents. Isotropic loading test and triaxial shear test results show that the compression index increases and yield stress decreases with increasing water content, while the swelling index stays constant. For normally consolidated and lightly overconsolidated bentonite, unsaturated shear strength can be described by the critical state line. For highly overconsolidated bentonite, unsaturated shear strength can be described by the Hvorslev surface. The critical state line and Hvorslev surface are found to be linear for the specimens with different water contents. The critical state stress ratio and the Hvorslev surface parameters are found to decrease with an increase in water content of the bentonite studied.
引用
收藏
页码:142 / 146
页数:5
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