长春地区季冻土基本性质对水分迁移的影响

长春地区季冻土基本性质对水分迁移的影响

Influence of Basic Properties of Seasonally Frozen Soil on Moisture Movement in Changchun Area

摘要/Abstract

参考文献

相关文章 8

Metrics

李杨,王清,赵安平,陈慧娥

吉林大学建设工程学院，长春 130026

收稿日期:2007-06-08 修回日期:1900-01-01 出版日期:2008-03-26 发布日期:2008-03-26
通讯作者: 李杨

LI Yang, WANG Qing, ZHAO An-ping,CHEN Hui-e

College of Construction Engineering,Jilin University, Changchun 130026, China

Received:2007-06-08 Revised:1900-01-01 Online:2008-03-26 Published:2008-03-26
Contact: LI Yang

摘要： 以长春-四平线（一号样）、长春-松原线（二号样）以及长春-吉林北线（三号样）3段公路土样为研究对象，从微观结构出发，结合物理化学试验和力学试验，评价了长春地区季冻土的性质对水分迁移的影响，为长春地区季冻土的水分迁移研究、道路冻胀翻浆的防治等提供试验依据。从试验得出，长春地区季节冻土孔隙直径大部分分布在<5 μm区间，有利于水分迁移；土样矿物质含量较高，阳离子交换量比较大，粘粒含量较高，颗粒形状也较规则，水化比表面积较高，有利于水化膜形成;外载荷会对水分迁移程度产生影响,整体上三号样水分迁移量最大，一号样次之，二号样最小。

关键词: 季冻土, 水分迁移, 微观结构, 易溶盐含量, 阳离子交换

Abstract: Samples from Changchun-Siping highway, Changchun-Songyuan highway and North Changchun-Jilin highway were studied.Studied from microstructure of frozen soil, combining physicochemical tests and mechanical tests, the influence of properties of seasonally frozen soil in Changchun area on moisture movement is evaluated，which provides the experimental evidence for study of moisture movement of seasonally frozen soil and the road frost heaving and mudding in Changchun area. It is concluded from the experiments that the diameter of pore of seasonally frozen soil in Changchun area is mostly less than 5 μm, which is benefit for the migration of gravitational and capillary water. With high content of mineral substance, large cation exchange capacity, rich clay content, regular particle shape and great hydration specific surface area, it is benefit for the formation of hydration membranes. The external loads influence the moisture movement.And sample 3 has the largest quantity of moisture movement, then sample 1,and sample 2 the lest.

Key words: seasonal frozen soil, moisture movement, microstructure, content of soluble salt, exchange capacity of cation

中图分类号:

TU752

李杨,王清,赵安平,陈慧娥. 长春地区季冻土基本性质对水分迁移的影响[J]. J4, 2008, 38(2): 279-0284.

LI Yang, WANG Qing, ZHAO An-ping,CHEN Hui-e. Influence of Basic Properties of Seasonally Frozen Soil on Moisture Movement in Changchun Area[J]. J4, 2008, 38(2): 279-0284.

[1]	牛岑岑, 王清, 苑晓青, 杨静, 宋晶, 王吉亮. 渗流作用下吹填土微观结构特征定量化研究[J]. J4, 2011, 41(4): 1104-1109.
[2]	赵安平, 王清, 张中琼. 土体微观结构对冻胀影响的灰色关联及粗糙集评价[J]. J4, 2011, 41(3): 791-798.
[3]	王常明, 林容, 陈多才, 张先伟, 王科. 辽西黄土湿陷变形特性及湿陷后微观结构变化[J]. J4, 2011, 41(2): 471-477.
[4]	刘飞, 佴磊, 吕岩, 张敏. 分解度对草炭土结构特征及强度的影响试验[J]. J4, 2010, 40(6): 1395-1400.
[5]	张冲, 毛志强, 肖亮, 孙中春, 张健. 利用测井资料计算阳离子交换量Q_v的方法对比[J]. J4, 2010, 40(5): 1194-1198.
[6]	宋晶, 王清, 陈慧娥, 孙铁, 张中琼, 张鹏. 高粘性高盐量吹填土固结过程孔隙分维特征[J]. J4, 2010, 40(2): 361-367.
[7]	曲延明,舒萍,纪学雁,丁日新,白雪峰,王璞珺. 松辽盆地庆深气田火山岩储层的微观结构研究[J]. J4, 2007, 37(4): 721-0725.
[8]	马明燕，张东丽，王玉洁，胡大强，朱怀志,蒋引珊. 碱活化条件对粉煤灰合成不同类型沸石的影响[J]. J4, 2006, 36(04): 663-667.

Just accepted

Online first

Just accepted

Online first

Viewed

Full text

	From	local

	Times	21
	Rate	100%

Abstract

461

Just accepted	Online first	Issue

0	0	461

From	Others	local

Times	417	44
Rate	90%	10%

Cited

Web of Science	Crossref	ScienceDirect	Search for Citations in Google Scholar >>


This page requires you have already subscribed to WoS.

Shared

Discussed