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盾构出洞水平冻结解冻温度场三维有限元分析
引用本文:王效宾,杨平,张婷,王海波.盾构出洞水平冻结解冻温度场三维有限元分析[J].解放军理工大学学报,2009,10(6):586-590.
作者姓名:王效宾  杨平  张婷  王海波
作者单位:南京林业大学,土木工程学院,江苏,南京,210037 
基金项目:江苏省"六大人才高峰"培养计划资助项目,苏州市科技局苏州轨道交通专项基金资助项目 
摘    要:为揭示人工冻土解冻规律,对某地铁区间隧道盾构出洞水平冻结工程融化温度场进行了三维数值模拟分析,并研究了土体导热系数、比热容、含水率和环境温度等因素变化对人工冻土融化温度场的影响.计算结果表明:冻结帷幕解冻所需热量主要来自于与隧道管片和混凝土槽壁接触的大气;解冻过程可为负温阶段、相变阶段和正温阶段,土体温度在负温阶段上升较快,相变阶段上升速度明显变缓,进入正温区后土体温度回升速度再次增大;负温阶段受比热容的影响比较显著,含水率增大引起相变阶段明显延长,导热系数和环境温度变化对三个阶段都有显著影响.为跟踪注浆控制融沉提供了理论依据.

关 键 词:盾构出洞  人工水平冻结法  解冻温度场  三维有限元  影响因素

3-D finite element analysis of melting temperature field in hield tunneling horizontal freezing reinforcing engineering
WANG Xiao-bin,YANG Ping,ZHANG Ting and WANG Hai-bo.3-D finite element analysis of melting temperature field in hield tunneling horizontal freezing reinforcing engineering[J].Journal of PLA University of Science and Technology(Natural Science Edition),2009,10(6):586-590.
Authors:WANG Xiao-bin  YANG Ping  ZHANG Ting and WANG Hai-bo
Institution:College of Civil Engineering,Nanjing Forestry University,Nanjing 210037,China;College of Civil Engineering,Nanjing Forestry University,Nanjing 210037,China;College of Civil Engineering,Nanjing Forestry University,Nanjing 210037,China;College of Civil Engineering,Nanjing Forestry University,Nanjing 210037,China
Abstract:To reveal the thaw ing law o f art ificially f rozen soil, the melt ing temper ature f ield of horizo ntal fr eezing eng ineer ing project in the const ruct ion of subw ay hield tunneling w as studied w ith the 3-D numerical simulation analysis. T he ef fect of the thermal conduct ivity , the specific heat capacity and the w ater co ntent of so il and the environmental temperature on the melting temper ature field of art ificially fr ozen soil w er e studied. The r esul ts show that mo st of the heat fo r thaw ing f reezing curtain is fr om air co ntact ing w ith tunnel segment and concrete groo ve wall , the thaw ing process includes the negat ive-temperature stage, the phase t ransit io n stage and the posit ive-temperature stage, and that the so il temperature increases fast in the neg ativ e-temperature stage, slow s dow n in the phase t ransit ion stag e and increases fast ag ain in the posit ive-temperature stag e. The result s also show that the ef fect o f specif ic heat capacity on the soil temperature in negat ive-temper ature stage is significant . T he increase of w ater content in so il causes the extension of the phase t ransit io n stage, and that the inf luence o f thermal conductivity and env ironment temperature on all the three stag es is significant . The f inding s provide theoret ical support to gro ut ing t racking and thaw sett lement cont rolling .
Keywords:hield tunneling  art ificial hor izontal freezing metho d  melting temperature f ield  3-D finite element  inf luencing factor s
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