中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Typical embankment settlement/heave patterns of the Qinghai-Tibet highway in permafrost regions: Formation and evolution

文献类型:期刊论文

作者Yu, Fan1; Qi, Jilin2; Lai, Yuanming1,3; Sivasithamparam, Nallathamby4; Yao, Xiaoliang1; Zhang, Mingyi1; Liu, Yongzhi1,5; Wu, Guilong1,5
刊名ENGINEERING GEOLOGY
出版日期2016-11-30
卷号214页码:147-156
关键词Qinghai-Tibet Highway Permafrost Settlement Frost heave Typical pattern Formation and evolution
ISSN号0013-7952
DOI10.1016/j.enggeo.2016.10.013
通讯作者Qi, Jilin(jilinqi@bucea.edu.cn)
英文摘要The Qinghai-Tibet Highway (QTH) in China has been experiencing a serious embankment settlement/heave for more than half a century. The settlement/heave is resulted from several mechanical processes taking place in different soil layers. In this paper, four typical settlement/heave patterns of road embankments in permafrost regions, namely "steady-low rate", "fluctuate", "down step" and "steady-high rate" are proposed based on 3-year monitored data of embankment settlement/heave and ground temperature at four road sections as well as previous published data of the QTH. Their formation mechanisms and evolution trend in the process of permafrost degradation are discussed from the viewpoints of engineering geology and mechanical process, based on the clarification of the deformation characteristics of different soil layers of a typical road embankment The results show that the four patterns are caused by the negligible settlement/heave, freeze-thaw cycling in an open condition, consolidation of the thawed permafrost layers, and creep of warm permafrost layers respectively. The pattern will change from one to another during the process of permafrost degradation, which will become very' complex with the occurrence of frost heave. The results can help revealing the deformation mechanism of road embankments in permafrost regions, and can benefit road construction and maintenance in the future. (C) 2016 Elsevier B.V. All rights reserved.
收录类别SCI
WOS关键词ROAD EMBANKMENT ; FREEZE-THAW ; FROST HEAVE ; DEGRADATION ; PLATEAU ; CHINA ; SOILS ; BENEATH ; CANADA
WOS研究方向Engineering ; Geology
WOS类目Engineering, Geological ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000389096000015
出版者ELSEVIER SCIENCE BV
URI标识http://www.irgrid.ac.cn/handle/1471x/2557520
专题寒区旱区环境与工程研究所
通讯作者Qi, Jilin
作者单位1.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China
2.Beijing Univ Civil Engn & Architecture, Beijing High Inst Res Ctr Engn Structures & New M, Beijing 100044, Peoples R China
3.Lanzhou Jiaotong univ, Sch Civil Engn, Lanzhou 730070, Peoples R China
4.Norwegian Geotech Inst, Computat Geomech Div, N-0806 Oslo, Norway
5.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Beiluhe Observat Stn Frozen Soil Environm & Engn, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Yu, Fan,Qi, Jilin,Lai, Yuanming,et al. Typical embankment settlement/heave patterns of the Qinghai-Tibet highway in permafrost regions: Formation and evolution[J]. ENGINEERING GEOLOGY,2016,214:147-156.
APA Yu, Fan.,Qi, Jilin.,Lai, Yuanming.,Sivasithamparam, Nallathamby.,Yao, Xiaoliang.,...&Wu, Guilong.(2016).Typical embankment settlement/heave patterns of the Qinghai-Tibet highway in permafrost regions: Formation and evolution.ENGINEERING GEOLOGY,214,147-156.
MLA Yu, Fan,et al."Typical embankment settlement/heave patterns of the Qinghai-Tibet highway in permafrost regions: Formation and evolution".ENGINEERING GEOLOGY 214(2016):147-156.

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