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

冻融循环作用下土体结构演化规律及其工程性质改变机理

张泽,马巍,齐吉琳   

  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
  • 收稿日期:2013-03-05 出版日期:2013-11-26 发布日期:2013-11-26
  • 作者简介:张泽(1981-),男,助理研究员,博士,主要从事冻土土质学、寒区工程地质与环境的研究,E-mail:zhangze@lzb.ac.cn
  • 基金资助:

    国家自然科学基金项目(41301070);中国科学院西部之光博士项目(2013-03);教育部留学回国人员科研启动基金项目(第46批);中国科学院寒区旱区环境与工程研究所青年人才基金项目(2013-03);冻土工程国家重点实验室自主研究项目(SKLFSE-ZQ-13)

Structure Evolution and Mechanism of Engineering Properties Change of Soils Under Effect of Freeze-Thaw Cycle

Zhang Ze, Ma Wei, Qi Jilin   

  1. State Key Laboratory of Frozen Soil Engineering / Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou730000, China
  • Received:2013-03-05 Online:2013-11-26 Published:2013-11-26

摘要:

寒区工程被破坏的最主要原因之一就是冻融循环作用,冻融循环过程可导致土的工程性质发生较大的变化,进而导致寒区工程设施产生变形,甚至失稳。对冻融循环作用下土的结构、基本物理性质以及力学性质进行了分析和总结。研究发现:冻融循环作用后土颗粒之间的原有结构被破坏,从而形成新的结构,土中团粒会发生分裂和团聚作用,团粒粒径向均一性趋势发展,并且在不同的内部及外部条件下,土会产生不同的构造;冻融循环后,土的渗透性增大,塑性指数减小。松散土和密实土的密度以及孔隙比具有不同的变化趋势,并且可使无湿陷性的黄土状土中大孔隙增加并产生湿陷性。土的力学性质变化趋势不一,一方面这与土的构造变化直接相关,另一方面冻融循环试验方法的不同也是引起研究结果差异性较大的重要原因。因此,需要建立冻融循环作用下土工程性质变异性的判定方法、评价及预测体系,而这些也可能成为未来研究工作的方向。

关键词: 冻融循环, 工程性质, 土体结构, 物理性质, 力学性质

Abstract:

Freeze-thaw cycle effect is one of the most important reasons that cause engineering problems in cold zone. Freeze-thaw cycles may lead to great changes of soil engineering properties, and subsequently cause unacceptable deformation or failure of engineering facilities. The research achievements of the soil engineering change caused by freeze-thaw cycles were analyzed and summarized from structure, basic physical properties and mechanical properties of soil. After freeze-thaw cycles, initial soil fabric was destroyed and reformed, in which clayey aggregates experienced fragmentation and recombination and formed a more uniform structure. Under different internal and external conditions, soil may form different structure. After the action of freezethaw cycle, the permeability of soil increases, plastic index decreases, porosity and density of loose and dense soils have different change trend. Soil mechanics properties show different trends in various test results. On one hand it is relate to the changes of soil structure, and on another hand different method of freeze-thaw cycle test can lead to different research results. Therefore, we need to establish the method of judgments, evaluation and prediction system for variation of soil engineering properties under the freezethaw cycle effect, which can be become the direction of future research work.

Key words: freeze-thaw cycle, engineering property, soil structure, physical property, mechanical property

中图分类号: 

  • P642.14
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[2] 宿晓萍,王清,王文华,孙昊月. 季节冻土区盐渍土环境下混凝土抗冻耐久性机理[J]. 吉林大学学报(地球科学版), 2014, 44(4): 1244-1253.
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[6] 卢全中,彭建兵. 黄土体工程地质的研究体系及若干问题探讨[J]. J4, 2006, 36(03): 404-409.
[7] 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.
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