中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mechanism of evolution on winter-time natural convection cooling effect of fractured-rock embankment in permafrost regions

文献类型:期刊论文

作者Sun, BX; Xu, XZ; Lai, YM; Wang, SJ; Zhang, JZ
刊名CHINESE SCIENCE BULLETIN
出版日期2005-12-01
卷号50期号:23页码:2744-2754
ISSN号1001-6538
关键词permafrost Qinghai-Tibet Plateau climate warming fractured-rock embankment natural convection
DOI10.1360/982004-639
通讯作者Sun, BX(sbinxiang@263.net)
英文摘要Mechanism and evolution of the pore-air natural convection cooling effect in fractured-rock embankments in permafrost regions are studied using a numerical representation of the non-dimensional governing equations in variable permeability porous media. The analyses show that winter-time natural convection in fractured-rock embankments begins to occur in the side slope portions and gradually develops from the left and right side slope portions to the middle portion of embankment. The more significant distortion of isotherms from their initial orientations due to heat conduction alone is that the cooling effect of winter-time natural convection on the fractured-rock embankment is stronger. The minimum critical Rayleigh numbers triggering natural convection of the pore-air in the side slope portions and the middle portion of embankment were obtained. The factors of influence on triggering winter-time convection cooling effect in fractured-rock embankments were analyzed. Finally, the assertion that the techniques of the fractured-rock revetment and berm are the effective measures to maintain the heat stability of the roadbed in permafrost regions is theoretically demonstrated.
收录类别SCI
WOS关键词THERMAL REGIME ; POROUS-MEDIA ; ACTIVE LAYER ; TEMPERATURE ; RAILWAY ; PLATEAU ; BALLAST ; MODEL
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000235457300014
URI标识http://www.irgrid.ac.cn/handle/1471x/2555700
专题寒区旱区环境与工程研究所
通讯作者Sun, BX
作者单位1.Shaoxing Coll Arts & Sci, Dept Civil Engn, Shaoxing 312000, Peoples R China
2.Chinese Acad Sci, State Key Lab Frozen Soil Engn Cold & Arid Reg, Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
3.Minist Commun, Highway Survey & Design Inst 1, Xian 710068, Peoples R China
推荐引用方式
GB/T 7714
Sun, BX,Xu, XZ,Lai, YM,et al. Mechanism of evolution on winter-time natural convection cooling effect of fractured-rock embankment in permafrost regions[J]. CHINESE SCIENCE BULLETIN,2005,50(23):2744-2754.
APA Sun, BX,Xu, XZ,Lai, YM,Wang, SJ,&Zhang, JZ.(2005).Mechanism of evolution on winter-time natural convection cooling effect of fractured-rock embankment in permafrost regions.CHINESE SCIENCE BULLETIN,50(23),2744-2754.
MLA Sun, BX,et al."Mechanism of evolution on winter-time natural convection cooling effect of fractured-rock embankment in permafrost regions".CHINESE SCIENCE BULLETIN 50.23(2005):2744-2754.

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来源:寒区旱区环境与工程研究所

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