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季节性冻土区铁路路基含水率变化特征研究
引用本文:王兴,赵相卿,贾海峰,李舟,梁恒祥. 季节性冻土区铁路路基含水率变化特征研究[J]. 铁道勘察, 2021, 0(1): 32-36
作者姓名:王兴  赵相卿  贾海峰  李舟  梁恒祥
作者单位:中铁西北科学研究院有限公司;青海省冻土与环境工程重点实验室
基金项目:中国国家铁路集团有限公司科技研究开发计划重点课题(2017G002-R)。
摘    要:季节性冻土区路基冻害一直是困扰铁路工程建设和运营的核心问题.针对兰新铁路西段路基冻害严重的问题,探讨不同工程措施对路基冻融循环过程中含水率变化的影响,以及含水率对路基冻结深度及冻胀变形的影响规律.研究结果表明,季节性冻结对兰新铁路西段路基含水率影响的范围在0.4~0.8m,影响深度有限;"隔一挖一"、"隔三挖一"等工程...

关 键 词:铁路路基  冻结深度  试验研究  季节性冻土区  水分迁移

Study on the Variation Characteristics of Moisture Content of Railway Subgrade in Seasonally Frozen Soil Area
Wang Xing,Zhao Xiangqin,Jia Haifeng,Li Zhou,Liang Hengxiang. Study on the Variation Characteristics of Moisture Content of Railway Subgrade in Seasonally Frozen Soil Area[J]. Railway Investigation and Surveying, 2021, 0(1): 32-36
Authors:Wang Xing  Zhao Xiangqin  Jia Haifeng  Li Zhou  Liang Hengxiang
Affiliation:(Northwest Research Insititute Co.,Ltd.of CREC,Lanzhou 730070,China;Qinghai Province Key Laboratory of Frozen Soiland Environment Engineering,Geermu 816000,China)
Abstract:The frost damage of railway subgrade is consistently the core problem that puzzles road engineering construction and operation in seasonally frozen soil area.In view of the serious problem of subgrade frost damage of Lanzhou Xinjiang Railway,this study mainly focused on the influences of different engineering measures on the variation of water content in the process of freeze-thaw cycle of subgrade.The influence law of moisture content on subgrade freezing depth and frost heave deformation were discussed.The results show that the influence of seasonal freezing on the water content of roadbed in the west section of Lanzhou-Xinjiang Railway is limited,and the maximum depth is about 0.8m and the maximum range is 0.4~0.6 m.Measures including“one excavation after another”and“one excavation after three”can effectively reduce the moisture content and frost heave of subgrade.As the water content decreases by 2%~5%,the frost heave and deformation are reduced by 50%~70%.
Keywords:railway subgrade  frozen depth  experimental research  seasonally frozen soil area  migration of moisture
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