王效宾, 胡俊, 居俊. 水泥改良土杯型冻土壁融化温度场三维数值模拟[J]. 煤田地质与勘探, 2017, 45(4): 102-106,111. DOI: 10.3969/j.issn.1001-1986.2017.04.018
引用本文: 王效宾, 胡俊, 居俊. 水泥改良土杯型冻土壁融化温度场三维数值模拟[J]. 煤田地质与勘探, 2017, 45(4): 102-106,111. DOI: 10.3969/j.issn.1001-1986.2017.04.018
WANG Xiaobin, HU Jun, JU Jun. 3D numerical simulation of melting temperature field of cement-improved soil cup-shaped frozen soil wall[J]. COAL GEOLOGY & EXPLORATION, 2017, 45(4): 102-106,111. DOI: 10.3969/j.issn.1001-1986.2017.04.018
Citation: WANG Xiaobin, HU Jun, JU Jun. 3D numerical simulation of melting temperature field of cement-improved soil cup-shaped frozen soil wall[J]. COAL GEOLOGY & EXPLORATION, 2017, 45(4): 102-106,111. DOI: 10.3969/j.issn.1001-1986.2017.04.018

水泥改良土杯型冻土壁融化温度场三维数值模拟

3D numerical simulation of melting temperature field of cement-improved soil cup-shaped frozen soil wall

  • 摘要: 为掌握水泥改良土杯型冻土壁的解冻规律,以南京地铁10号线过江隧道盾构出洞水平冻结加固工程为例,对水泥改良土杯型冻土壁融化温度场进行了三维数值模拟,并研究了导热系数、比热容、相变潜热等因素变化对融化温度场的影响规律。结果表明:冻结水泥土解冻速度受初始温度影响较小,受冻土位置影响较大;解冻过程中,冻土壁外侧1 m处的非冻结土温度先降后升,冻土壁外侧3~7 m处土体温度始终呈下降趋势;随着导热系数减小、相变潜热增大、比热容增大,解冻时间延长;比热容对冻结水泥土解冻过程的影响主要体现在升温阶段,相变潜热主要影响冻土相变阶段,导热系数既影响升温阶段又影响相变阶段。

     

    Abstract: To investigate the thawing law of cement-improved cup-shaped frozen soil wall, this paper performs 3D numerical simulation on the melting temperature field of cement-improved cup-shaped frozen soil wall and presents a comprehensive study of various influential factors, namely, thermal conductivity, specific heat and latent heat of the temperature field. This study was based on the horizontal freezing reinforcement project of shield tunnel of Nanjing Metro Line 10. It was found that initial temperature has little effect on the thawing rate of freezing cement soil while the location of frozen soil had larger influence on it. During the thawing process, the temperature of non-frozen soil at the outer wall of 1 m frozen soil decreased in the beginning stage and then increased, but there was an constant decrease in the soil temperature at the outer wall of 3~7 m frozen soil. The thawing time prolonged with the decrease of thermal conductivity, the increase of latent heat and the specific heat capacity. The effect of specific heat capacity was mainly reflected in the heating stage and the latent heat had main impact on the phase change of frozen soil. Thermal conductivity affects not only the heating stage but also the phase change.

     

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