Engineering geological characteristics and processes of permafrost along the Qinghai-Xizang (Tibet) Highway

被引:55
作者
Wu, QB [1 ]
Shi, B
Fang, HY
机构
[1] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res, State Key Lab Frozen Soil Engn, Lanzhou 730000, Gansu, Peoples R China
[2] Nanjing Univ, ACEI, Dept Earth Sci, Nanjing 210093, Peoples R China
[3] Univ N Carolina, GIEES, Charlotte, NC 28223 USA
基金
中国国家自然科学基金;
关键词
asphalt pavement; freeze-thaw cycles; ground temperature; permafrost; roadbed stability; thaw-settlement;
D O I
10.1016/S0013-7952(02)00242-9
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Engineering geological problems of thaw-settlement and frost-heave occur frequently along the Qinghai-Xizang (Tibet) Highway (QXH) line and produce an adverse impact on roadbed stability. Eight monitoring sites were established along the QXH to investigate the engineering geological characteristics and environmental process of permafrost, including the upper and lower boundary of the active layer under the natural surface, the seasonal freeze-thaw depth under the asphalt pavement, the permafrost table temperature and roadbed stability. The investigation results show that the active layer thickness and permafrost table temperature under an asphalt pavement are higher than under a natural surface due to the absorption heat and reduced evaporation capability of the asphalt pavement. The implication for highway design and construction in permafrost areas are discussed. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:387 / 396
页数:10
相关论文
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