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边坡渗流对冻土地区路基稳定性的影响分析
引用本文:李东庆,魏春玲,吴紫汪.边坡渗流对冻土地区路基稳定性的影响分析[J].兰州大学学报(自然科学版),2000,36(3):175-179.
作者姓名:李东庆  魏春玲  吴紫汪
作者单位: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,甘肃,兰州,730000
2. 兰州大学,出版社,甘肃,兰州,730000
基金项目:国家自然科学基金!(4 970 10 0 4 ),中国科学院知识创新经费资助项目
摘    要:利用数值模拟方法,分析了在多年冻土地区修筑路堤后,夏季路式边坡积水通过路堤及在其下土壤的渗流过程中,由于对流换热所引起的路堤基底的不稳定现象。通过计算机数值模拟进一步证实,夏季路基边坡积水可导致路基基底之下的多年冻土上限下降,并使路基下形成凹型融化核或扩大已有融化核的深度和范围,从而加大路堤的融化下沉量和冬季的冻胀量,造成路基稳定性程度明显下降。

关 键 词:边坡渗流  路基  融化核  稳定性  冻土地区
修稿时间:

Analysis of the Influence of the Slope Seepage on Embankment Stability
Li Dongqing,Wei Chunling,Wu Ziwang.Analysis of the Influence of the Slope Seepage on Embankment Stability[J].Journal of Lanzhou University(Natural Science),2000,36(3):175-179.
Authors:Li Dongqing  Wei Chunling  Wu Ziwang
Abstract:The unstable phenomen a of embankment on frozen soil were analyzed in summer by using the numerical mode ling, which was caused by the convection heat transfer of water from the slope a fter the construction of the embankment. The conclusions were that the permafros t table under the roadbed would fall and the concave thawed core was formed or f urther enlarged, thereby the thawing settlement in summer and frost heave in wi nter would be increased, so that the stabilities of embankment would obviously b e decreased.
Keywords:slope seepage  embankm ent on frozen soil  thawed core  stability
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