吉林大学学报(地球科学版)

• 地质工程与环境工程 • 上一篇    下一篇

广西红土击实特性的影响因素及机理分析

王清1, 张奇1,马玉飞1,高郢2,鲍硕超1   

  1. 1.吉林大学建设工程学院,长春130026;
    2.南京瑞迪建设科技有限公司,南京210000
  • 收稿日期:2014-04-17 出版日期:2014-11-26 发布日期:2014-11-26
  • 作者简介:王清(1959-),女,教授,博士生导师,主要从事红土、黄土及软土等土体的工程地质及岩土工程研究工作,E-mail:wangqing@jlu.edu.cn
  • 基金资助:

    国家自然科学基金国际合作项目(40911120044);青海省电力设计院自立课题项目(63-K2012-02)

The Influence Factors of Compaction Characteristics and Mechanism Analysis of Laterite in Guangxi

Wang Qing1, Zhang Qi1, Ma Yufei1, Gao Ying2, Bao Shuochao1   

  1. 1.College of Construction Engineering, Jilin University, Changchun130026, China;
    2.Nanjing R&D Tech Group Co.,Ltd.,Nanjing210000, China
  • Received:2014-04-17 Online:2014-11-26 Published:2014-11-26

摘要:

红土是由原岩在湿热气候条件下经过红土化作用形成的具有高含水率、大孔隙比、较高强度和较低压缩性的一种特殊土。由于其特殊的工程地质性质形成了红土具有较大工后沉降的特性。目前,工程中普遍采用强夯的地基处理方法对其进行处理,对于夯后红土地基变形则通过现场监测结合室内试验的方法进行研究。笔者通过室内击实试验和击实后红土的高压固结试验,深入探讨影响红土击实效果和击实后压实性的主要因素,并对各影响因素进行影响机理分析。试验结果表明:红土的击实效果与击实功成正比,与黏粒质量分数、塑性指数、游离氧化铁质量分数成反比;击实后红土的压缩模量受含水率、干密度及饱和度等因素的综合影响,并且各因素的影响程度不尽相同;当含水率大于18%时,土体处于近饱和状态,含水率与干密度已经不能反映饱和红土的压实性了,即在实际的强夯工程上这种土的含水率不宜大于18%,否则会产生较大的工后沉降。

关键词: 红土, 压实性, 强夯, 饱和度, 广西

Abstract:

Laterite is a kind of special soil which was formed by the laterization in the condition of hot and humid climate with the characteristics of high moisture content, large void ratio, higher strength and lower compressibility. As its special engineering geological properties there will be a larger settlement after construction on the foundation of red soil. Nowadays, the dynamic compaction as a method of ground treatment is widely applied and the deformation of laterite foundation after construction is always studied by field monitoring combined with laboratory test. The main factors which affect the compaction effect and the compaction characteristics of the laterite after compaction are deeply discussed on the base of the compaction test and consolidation test in the laboratory. And the mechanism analysis of factors are made. The experimental results show that the compaction effect has related with the content of clay, the plastic index, the free iron oxide and the compaction effort. The more content of clay, the higher plastic index and the more content of the free iron oxide would lead the worse compaction effect. The compaction effect is also in proportion to the compaction effort. The compression modulus of laterite after compaction is affected differently by the factors such as moisture content, dry density and degree of saturation. When the moisture content of the laterite is greater than 18% and the degree of saturation is close to 100%. The moisture content and dry density can’t reflect the compaction characteristics. Hence, in practical engineering the moisture content of the laterite shuold not be greater than 18% to avoid the larger settlement.

Key words: laterite, compaction characteristics, dynamic compaction, degree of saturation, Guangxi Province

中图分类号: 

  • TU446
[1] 吴健, 胡向阳, 梁玉楠, 汤翟, 郑香伟. 珠江口盆地低阻油层饱和度评价方法[J]. 吉林大学学报(地球科学版), 2015, 45(1): 312-319.
[2] 康志强, 何师意, 罗允义. 表层岩溶系统水化学成因及植被恢复条件下变化趋势——以广西马山弄拉兰电堂泉为例[J]. 吉林大学学报(地球科学版), 2015, 45(1): 232-239.
[3] 宋延杰,姜艳娇,宋杨,张依妮. 古龙南地区低阻油层胶结指数和饱和度指数影响因素实验[J]. 吉林大学学报(地球科学版), 2014, 44(2): 704-714.
[4] 莫修文, 陆敬安, 沙志彬, 马龙. 确定天然气水合物饱和度的测井解释新方法[J]. J4, 2012, 42(4): 921-927.
[5] 辛治国, 侯加根, 冯伟光. 密闭取心饱和度校正数学模型[J]. J4, 2012, 42(3): 698-704.
[6] 于红岩, 李洪奇, 郭兵, 孙海涛, 张海霞. 基于成因机理的低阻油层精细评价方法[J]. J4, 2012, 42(2): 335-343.
[7] 闫伟林, 覃豪, 李洪娟. 基于导电孔隙的中基性火山岩储层含气饱和度解释模型[J]. J4, 2011, 41(3): 915-920.
[8] 苏俊磊, 王艳, 孙建孟. 应用可变T2截止值确定束缚水饱和度[J]. J4, 2010, 40(6): 1491-1495.
[9] 李雄炎, 李洪奇, 阴平, 陈亦寒, 周金煜. 柴达木盆地三湖地区第四系低饱和度气层的成因机理[J]. J4, 2010, 40(6): 1241-1247.
[10] 范森葵, 王登红, 梁婷, 吴德成, 韦可利, 周鸿军, 黄惠明, 屈文俊. 广西大厂96号矿体的成矿元素地球化学特征与成因[J]. J4, 2010, 40(4): 781-790.
[11] 赖富强, 孙建孟, 王敏. 应用随裂缝倾角变化的孔隙模型改进储层饱和度计算[J]. J4, 2010, 40(3): 713-720.
[12] 黄布宙,付有升,李舟波,李庆峰,许淑梅,张莹. 拉尔盆地碎屑岩储层束缚水饱和度的确定海[J]. J4, 2008, 38(4): 713-0718.
[13] 吴鸿梅,童海奎,刘沣,任文恺,许国武,王维. 北祁连红土沟-川刺沟金矿与韧性剪切带的成矿关系[J]. J4, 2008, 38(4): 581-0586.
[14] 邢玉东,王常明,张立新,匡少华. 阜新-朝阳高速公路段湿陷性黄土路基处理方法及效果[J]. J4, 2008, 38(1): 98-0104.
[15] 韦 复 才. 桂林红土的工程地质性质及其主要工程地质问题[J]. J4, 2005, 35(06): 775-0781.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!