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高温-高含冰量冻结黏土强度试验研究
引用本文:马小杰,张建明,常小晓,郑波,张明义. 高温-高含冰量冻结黏土强度试验研究[J]. 岩土力学, 2008, 29(9): 2498-2502
作者姓名:马小杰  张建明  常小晓  郑波  张明义
作者单位:1. 中国科学院寒区旱区环境与工程研究所冻土工程国家重点实验室,兰州 730000;2. 浙江建设职业技术学院,杭州 311231
基金项目:中国科学院寒区旱区环境与T程研究所创新工程项目,中国科学院知识创新工程项目,中国科学院国际合作项目,中国科学院基金 
摘    要:为研究高温-高含冰量冻土的强度特性,分别开展了不同温度、不同含水率的冻结黏土单轴无侧限抗压强度试验。分析了高温-高含冰量冻结黏土在单轴压缩试验过程中的破坏类型、应力-应变关系;单轴抗压强度与温度、含水率之间的关系以及饱和冻结黏土单轴抗压强度对温度的敏感性-含水率关系。研究结果表明:当温度低于-0.9 ℃时,高温-高含冰量冻结黏土存在最不利含水率,在相同的温度条件下,该含水率状态下冻土抗压强度最小;当温度高于-0.6 ℃时,高含冰量冻土随含水率的增加,单轴抗压强度增大。

关 键 词:高温-高含冰量冻土  应力-应变关系  破坏类型  抗压强度  
收稿时间:2006-12-12

Experimental research on strength of warm and ice-rich frozen clays
MA Xiao-jie,ZHANG Jian-ming,CHANG Xiao-xiao,ZHENG Bo,ZHANG Ming-yi. Experimental research on strength of warm and ice-rich frozen clays[J]. Rock and Soil Mechanics, 2008, 29(9): 2498-2502
Authors:MA Xiao-jie  ZHANG Jian-ming  CHANG Xiao-xiao  ZHENG Bo  ZHANG Ming-yi
Affiliation:1.State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China; 2. Zhejiang College of Construction, Hangzhou 311231, China
Abstract:In order to study the strength character of warm and ice-rich frozen soil, a series of uniaxial compressive strength tests of frozen clays with water contents of 20 %, 40 %, 60 %, 90 %, 120 % at temperatures of –0.3 ℃, –0.6 ℃, –0.9 ℃, –1.5 ℃, –5.0 ℃ were conducted respectively. The test results indicate that: 1) the type of stress-strain curves for the warm and ice-rich frozen clays(temperature: –0.3 ℃ to -1.5 ℃, water content: 60 %-120 % ) is strain-hardening, and the form of sample failure is plastic; 2) The compressive strength of warm frozen clay with water contents of 40 % to 90 % increases linearly with the decrease of temperature, the sensitivity of the strength of lower water content saturation frozen clay to temperature is higher than that of higher water content saturation frozen clay; at the water content of 120 %, the amplitude of the increase in compressive strength decreases with decreasing temperature; 3) when the temperature of the warm frozen clay is lower than -0.9 ℃, there is a most disadvantageous water content (at the same temperature, the compressive strength of the frozen soil at this water content is the lowest); when the temperature of the warm frozen clay is higher than -0.6 ℃, the strength increases with water content increasing.
Keywords:warm and ice-rich frozen soil  stress-strain relation  failure type  compressive strength  
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