›› 2016, Vol. 37 ›› Issue (5): 1373-1379.doi: 10.16285/j.rsm.2016.05.020

• 基础理论与实验研究 • 上一篇    下一篇

应变率与含水率对冻土单轴压缩特性影响研究

杜海民,马 巍,张淑娟,周志伟   

  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,甘肃 兰州 730000
  • 收稿日期:2014-07-28 出版日期:2016-05-10 发布日期:2018-06-09
  • 通讯作者: 马巍,男,1963年生,博士,博士生导师,研究员,主要从事冻土力学方面的科研工作。E-mail: mawei@lzb.ac.cn E-mail: duhaimin@lzb.ac.cn
  • 作者简介:杜海民,男,1987年生,博士研究生,主要从事冻土力学方面的研究与学习。
  • 基金资助:

    国家重点基础研究发展计划项目 (973计划) (No. 2012CB026106);优秀国家重点实验室专项基金(No. 41023003);冻土工程国家重点实验室自主课题(No. SKLFSE-ZT-07)。

Effects of strain rate and water content on uniaxial compressive characteristics of frozen soil

DU Hai-min, MA Wei, ZHANG Shu-juan, ZHOU Zhi-wei   

  1. State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, Gansu730000, China
  • Received:2014-07-28 Online:2016-05-10 Published:2018-06-09
  • Supported by:

    This work was supported by the National Program on Key Basic Research Project of China (973 Program) (2012CB026106), the Special Found of Excellent State Key Laboratory(41023003) and the Independent Program for State Key Laboratory of Frozen Soil Engineering (SKLFSE-ZT-07).

摘要: 通过对泥浆制样法制备的冻结粉质砂土的单轴压缩试验,系统地研究了冻结砂土在一个宽泛应变率以及含水率范围内的单轴压缩破坏应变特性和线弹模量特性。结果表明:随着应变率的增加,当含水率为12.0%,破坏应变逐渐增大;当含水率在16.7%~24.0%范围内时,破坏应变先增大后减小;当含水率大于等于30.6%时,破坏应变逐渐减小,3种情况下破坏应变最终都逐渐趋于稳定。破坏应变随含水率增加而先急剧增大到一个最大值,然后急剧减小,当含水率超过41.5%时,基本趋于冰的破坏应变。线弹模量先随着应变率的增大而非线性增大到一个最大值,然后应变率的继续增大使线弹模量逐渐减小,线弹模量与应变率的关系满足二次抛物函数规律。在温度为 2.0 ℃,应变率小于4.67×10-3 s-1的条件下,线弹模量随着含水率的增大而非线性增大,直至最后趋于冰的线弹模量;而在大于等于该应变率的条件下,随着含水率的增大,线弹模量先增大到一个最大值,然后减小趋于冰的线弹模量。当温度为 5.0 ℃时,类似的应变率临界值为1.00×10-2 s-1。

关键词: 冻结砂土, 单轴压缩, 破坏应变, 线弹模量, 应变率, 含水率

Abstract: Based on a mud method of preparation sample, some uniaxial compressive tests are conducted on the frozen silty sand samples prepared with the mud sample preparation method. The failure strain and linear elastic modulus characteristics of frozen silty sand under uniaxial compression are investigated systemically in a wide range of strain rate and water content. The experimental results show that with rise of strain rate, failure strain increases gradually when water content is 12.0%; failure strain firstly increases and then decreases with growth of stain rate when water content is between 16.7% and 24.0%; when water content is greater than or equal to 30.6%, with increasing strain rate, failure strain decreases gradually; for the above three cases, the failure strain always tends gradually to be stable in the end. With increasing water content, failure strain firstly increases to a maximum sharply and then decreases dramatically. The failure strain tends to the failure strain of ice after water content is beyond 41.5%. Linear elastic modulus increases nonlinearly to a peak with increasing water content and then further rise of water content makes it lower, which can be described by a quadratic polynomial model. At 2.0 ℃, when strain rate less than 4.67×10-3 s-1, with increase of water content, linear elastic modulus increases nonlinearly and then tends to the linear elastic modulus of ice; when strain rate greater than or equal to 4.67×10-3 s-1, linear elastic modulus firstly increases to a maximum and then decreases to the linear elastic modulus of ice with increase of water content. When temperature is at 5.0 ℃, the similar critical value of strain rate to 4.67×10-3 s-1 is 1.00×10-2 s-1.

Key words: frozen silty sand, uniaxial compression, failure strain, linear elastic modulus, strain rate, water content

中图分类号: 

  • TU 411

[1] 张艳博, 吴文瑞, 姚旭龙, 梁鹏, 田宝柱, 黄艳利, 梁精龙, . 单轴压缩下花岗岩声发射、红外特征及 损伤演化试验研究[J]. 岩土力学, 2020, 41(S1): 139-146.
[2] 黄巍, 肖维民, 田梦婷, 张林浩, . 不规则柱状节理岩体力学特性模型试验研究[J]. 岩土力学, 2020, 41(7): 2349-2359.
[3] 杨凯旋, 侯天顺. 击实试验类型对EPS颗粒轻量土击实特性的 影响规律[J]. 岩土力学, 2020, 41(6): 1971-1982.
[4] 刘新宇, 张先伟, 岳好真, 孔令伟, 徐超, . 花岗岩残积土动态冲击性能的SHPB试验研究[J]. 岩土力学, 2020, 41(6): 2001-2008.
[5] 杜宇翔, 盛谦, 王帅, 付晓东, 罗红星, 田明, 王立纬, 梅鸿儒. 昔格达组半成岩微观结构与力学性质研究[J]. 岩土力学, 2020, 41(4): 1247-1258.
[6] 史振宁, 戚双星, 付宏渊, 曾铃, 何忠明, 方睿敏, . 降雨入渗条件下土质边坡含水率分 布与浅层稳定性研究[J]. 岩土力学, 2020, 41(3): 980-988.
[7] 刘希灵, 刘周, 李夕兵, 韩梦思. 单轴压缩与劈裂荷载下灰岩声发射b值特性研究[J]. 岩土力学, 2019, 40(S1): 267-274.
[8] 刘红岩. 宏细观缺陷对岩体力学特性及边坡稳定影响研究[J]. 岩土力学, 2019, 40(S1): 431-439.
[9] 郑耀林, 章荣军, 郑俊杰, 董超强, 陆展, . 絮凝-固化联合处理超高含水率 吹填淤泥浆的试验研究[J]. 岩土力学, 2019, 40(8): 3107-3114.
[10] 闫亚景, 闫永帅, 赵贵章, 张泰丽, 孙强, . 基于高密度电法的天然边坡水分运移规律研究[J]. 岩土力学, 2019, 40(7): 2807-2814.
[11] 田军, 卢高明, 冯夏庭, 李元辉, 张希巍. 主要造岩矿物微波敏感性试验研究[J]. 岩土力学, 2019, 40(6): 2066-2074.
[12] 王鹏飞, 谭文辉, 马学文, 李子建, 刘景军, 武洋帆, . 不同胶结度断层泥强度参数与含水率关系[J]. 岩土力学, 2019, 40(5): 1657-1662.
[13] 王娟娟, 郝延周, 王铁行. 非饱和压实黄土结构特性试验研究[J]. 岩土力学, 2019, 40(4): 1351-1357.
[14] 王 腾, 吴 瑞. 黏土中海底管线竖向贯入阻力研究[J]. 岩土力学, 2019, 40(3): 871-878.
[15] 高 峰, 熊 信, 周科平, 李杰林, 史文超, . 冻融循环作用下饱水砂岩的强度劣化模型[J]. 岩土力学, 2019, 40(3): 926-932.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!