Stress relaxation of warm frozen soil under drained or undrained conditions

被引:0
|
作者
Wang, SongHe [1 ]
Qi, JiLin [1 ]
机构
[1] Chinese Acad Sci, Cold & Arid Reg Environm Engn Res Inst, State Key Lab Frozen Soil Engn, Lanzhou 730000, Gansu, Peoples R China
来源
SCIENCES IN COLD AND ARID REGIONS | 2011年 / 3卷 / 06期
基金
中国国家自然科学基金;
关键词
warm frozen soil; stress relaxation; confining pressure; drained and undrained conditions; volumetric change;
D O I
10.3724/SP.J.1226.2011.00468
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
To investigate the influence of drainage conditions on stress relaxation characteristics of warm frozen soil, a series of laboratory tests were carried out under drained and undrained conditions. The results indicate that confining pressure obviously influences the relaxation process of warm frozen soil. Under undrained condition, with increase in confining pressure, the critical relaxation duration tends to grow as well as instantaneous relaxation. But the relaxation rate is sensitive to confining pressure in the initial stage, and with further development, the effect tends to diminish. Under drained condition, the relaxation rate is greater than that under undrained condition in the initial stage but with the development of relaxation, the difference decreases. The volumetric deformation of warm frozen clay under drained condition is much larger than that under undrained condition.
引用
收藏
页码:468 / 472
页数:5
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