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原状黄土冻融过程抗剪强度劣化机理试验分析
引用本文:许健,李诚钰,王掌权,任建威,袁俊. 原状黄土冻融过程抗剪强度劣化机理试验分析[J]. 土木建筑与环境工程, 2016, 38(5): 90-98. DOI: 10.11835/j.issn.1674-4764.2016.05.012
作者姓名:许健  李诚钰  王掌权  任建威  袁俊
作者单位:1. 西安建筑科技大学 土木工程学院,西安,710055;2. 西安市地下铁道有限责任公司,西安,710018;3. 中国电力工程顾问集团 西北电力设计院有限公司,西安 710075; 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
基金项目:国家自然科学基金(51478385、51208409);陕西省教育厅专项科研计划(12JK0914);冻土工程国家重点实验室开放基金(SKLFSE201312);西北电力设计院技术创新科研项目(XB1-TM04-2013)@@@@Natural Science Foundation of China (No.51478385,No.51208409);Special Research Program of Shaanxi Province Education Department (No.12JK0914);Open Foundation of state key Laboratory of Permafrost Engineering(No.SKLFSE201312);Technology Innovation Research Project of North West Electric Power Design Institute(XB1-TM04-2013)
摘    要:通过对西安Q_3原状黄土在封闭系统冻融作用下的电镜扫描和直剪试验,研究了冻融作用对原状黄土微观结构和强度的影响。试验表明:冻融过程中原状黄土微观结构发生显著变化,大颗粒集粒数量明显减少,小粒径土颗粒所占比重增加,孔隙面积比增加。进一步基于损伤力学理论,得到微观结构冻融损伤度随冻融次数增加呈指数增加趋势,反映出冻融作用一定程度上破坏黄土体的结构强度,但多次冻融后黄土体结构强度趋于稳定的残余强度。冻融过程土样表面结构发生破坏,且含水率越高,土体表面特征破坏越严重。粘聚力随冻融次数增加呈指数衰减趋势,且含水率越高,粘聚力衰减幅值和速率越小;粘聚力随含水率增加表现出线性衰减特征,且冻融后粘聚力与含水率的变化规律近似重合;内摩擦角无明显规律性变化。粘聚强度冻融损伤系数随冻融次数增加呈指数增加趋势,随含水率升高有增大趋势。基于试验数据规律性,进一步提出了原状黄土粘聚强度劣化模型,该模型经试验验证可较好描述原状黄土粘聚强度劣化规律。

关 键 词:原状黄土  冻融作用  电镜扫描  微观结构  抗剪强度
收稿时间:2016-03-09

Experimental analysis on the mechanism of shear strength deterioration of undisturbed loess during the freeze-thaw process
Xu Jian,Li Chengyu,Wang Zhangquan,Ren Jianwei and Yuan Jun. Experimental analysis on the mechanism of shear strength deterioration of undisturbed loess during the freeze-thaw process[J]. Journal of Civil,Architectrual & Environment Engineering, 2016, 38(5): 90-98. DOI: 10.11835/j.issn.1674-4764.2016.05.012
Authors:Xu Jian  Li Chengyu  Wang Zhangquan  Ren Jianwei  Yuan Jun
Affiliation:School of Civil Engineering, Xi''an University of Architecture and Technology, Xi''an, 710055, P. R. China,Xi''an Metro Ltd., Xi''an, 710018, P. R. China,School of Civil Engineering, Xi''an University of Architecture and Technology, Xi''an, 710055, P. R. China,School of Civil Engineering, Xi''an University of Architecture and Technology, Xi''an, 710055, P. R. China and Northwest Electric Power Design Institute of Co. Ltd. of China Power Engineering Consulting Group, Xi''an, 710075, P. R. China;Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730000, P. R. China
Abstract:SEM and direct shear tests were conducted to study the influence of freeze-thaw action on the microstructure and strength of xi ’an Q3 undisturbed loess under the closed system.The experimental results showed that the microstructure of loess changes significantly during the freeze-thaw process,withthe number of large particles aggregate decreasing,the proportion of small particle size increasing,and theratio of pore increasing.Based on the damage mechanics theory,the freezing-thawing damage degree versusfreezing-thawing times was established. Analysis indicated that the freezing-thawing damage degreeexponentially increased with the increase of freezing-thawing times, representing that the structuralstrength of loess can be destroyed by freezing-thawing. However,the structural strength eventuallyreached a residual strength value after repeated freezing and thawing.Freezing-thawing made the surfacestructure of soil destroyed,and had a bigger influence with the increace of water content.The cohesionexponentially decreased with freezing and thawing times increasing, and had a smaller attenuationamplitude and rate with the increase of water content.With the increase of water content,the cohesionlinearly decreased,and had an approximately same variation after freezing and thawing.The internalfriction angle had no obvious variation during the whole freezing-thawing process.The freezing-thawingdamage coefficient of cohesion exponentially increased with the increase of freezing-thawing times,and alsoincreased with water content increasing.A cohesion strength deterioration model was developed based onthe laboratory test results,and the model can be used to well describe the strength deterioration regularityby the test verification.
Keywords:undisturbed loess  freeze-thaw action  SEM  microstructure  shear strength
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