青藏高原铁路多年冻土路堤的碎石层高度  

BALLAST LAYER HEIGHT OF RAILWAY EMBANKMENT IN QINGHAI-TIBET PLATEAU PERMAFROST REGION

作　　者：孙斌祥[1] 徐学祖[1] 赖远明[2] 汪双杰[3] 章金钊[3] 

机构地区：[1]绍兴文理学院土木工程系,绍兴312000 [2]中科院寒区旱区环境与工程研究所冻土工程国家重点实验室,兰州730000 [3]中交第一公路勘察设计研究院,西安710068

出　　处：《工程力学》2006年第6期127-134,共8页Engineering Mechanics

基　　金：国家杰出青年科学基金资助项目(40225001);国家西部交通建设科技项目(200231800004);绍兴文理学重点学科建设(2003016)联合资助

摘　　要：分析表明路堤尺寸、形状和边界形式对碎石路堤自然对流效应的发生有显著影响,需要根据具体工程要求来确定路堤的压力边界条件。对4种压力边界情况的碎石路堤自然对流进行了数值计算,显示透气边界的碎石路堤自然对流降温效应为最强。最后,通过引入自然对流指数,提出了实际冻土路堤碎石层填筑高度的确定方法,具体给出了粒径为2cm^4cm、4cm^6cm、6cm^8cm和8cm^10cm的碎石层填筑高度,并对粒径为6cm^8cm的碎石层填筑高度进行了实验验证,结果表明,通过自然对流指数所确定的碎石层高度对实际冻土路堤工程的设计具有参考价值。The analysis shows that the sizes, shapes and boundary conditions of embankment impact substantially on triggering the natural convective effect in ballast embankments. Pressure boundary conditions of ballast embankment are dependent on engineering conditions. The numerical results on ballast embankments with four pressure boundary conditions show that the natural convection cooling effect in ballast embankment with air-permeable boundaries is the strongest. A natural convection index for representing the cooling effectiveness of winter-time natural convection in ballast embankments is introduced. The approach to evaluate ballast layer heights in railway embankments in cold regions is developed. Evaluating ballast layer heights of embankment with the grain sizes of 2cm-4cm, 4cm-6cm, 6cm-8cm and 8cm-10cm is performed. Validity of ballast layer heights with the grain size of 6cm-8cm was demonstrated experimentally. The test results show that the ballast layer heights in railway embankments evaluated by the natural convection index are available for design of ballast embankment.

关 键 词：碎石路堤 自然对流 碎石层高度 青藏铁路 多年冻土 

分 类 号：TU445[建筑科学—岩土工程] U213.1[建筑科学—土工工程]