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昆仑山隧道浅埋段地温特征分析
引用本文:王建,汤国璋,王星华.昆仑山隧道浅埋段地温特征分析[J].岩土力学,2007,28(11):2396-2400.
作者姓名:王建  汤国璋  王星华
作者单位:1.中南大学 土建学院,长沙 410075;2.铁道第一勘察设计院,兰州 730000
摘    要:多年冻土区昆仑山隧道浅埋段出现渗漏水后,浅埋段的地温特征成为治理病害的重要依据之一。根据2004年3~5月份的地质观测资料,分析浅埋段的地温特征,并采用数值模拟技术,追溯隧道工程施工前的地温状态,从而得出该隧道浅埋段2#冲沟存在一个未被冻结的通道;隧道工程对周边地温产生较大影响;最大冻结深度约10 m,最大融化深度不超过4 m。

关 键 词:多年冻土  地温  数值模拟  
文章编号:1000-7598-(2007)11-2396-05
收稿时间:2005-04-14
修稿时间:2005-04-14

Analysis of ground temperature at a valley of Kunlun Mountain tunnel
WANG Jian,TANG Guo-zhang,WANG Xing-hua.Analysis of ground temperature at a valley of Kunlun Mountain tunnel[J].Rock and Soil Mechanics,2007,28(11):2396-2400.
Authors:WANG Jian  TANG Guo-zhang  WANG Xing-hua
Institution:1.School of Civil and Architectural Engineering, Central South University, Changsha 410075, China; 2.The First Survey and Design Institute of China Railway, Lanzhou 730000, China
Abstract:Since water seepage comes out of Kunlun Mountain tunnel at a valley,understanding the ground temperature at the valley is one of the most important things to treat the disease.The ground temperature is studied;it is traced back before tunneling by numerical simulation on the basis of geological observation information from March to May,2004.So it is educed as follows:(1) there is an unfrozen channel underground the valley;(2) the ground temperature around the tunnel is affected by tunneling;(3) the maximum frozen depth is about 10 m;and the maximum thawing depth is not over 4 m.
Keywords:permafrost  ground temperature  numerical simulation
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