冻土地基温度场数值模拟研究
Numerical simulation research on frozen earth temperature field
高温冻土指温度随季节变化较为敏感的多年冻土,其表层一定深度的土层处于冬冻夏融状态。在气候变暖背景下,多年冻土退化加剧,高温冻土将会在更大范围出现。因此多年冻土地区的工程建设面对越来越多高温冻土地基。在大量现有研究资料的基础上,采用数值模拟,考虑气温随时间的变化这一显著的影响因素作为边界条件进行计算分析。得出地基温度场及其稳定性与外部边界条件之间的关系和变化规律。
High-temperature frozen earth is perennial frozen earth which temperature changes with seasons .The soil in certain depth of earth surface frozen in winter and thaw in summer.In a background of climate warming, perennial frozen earth degradation intensifies.High-temperature frozen earth will appear in winder range.Therefore engineering in perennial frozen earth area will encounter more and more High-temperature frozen earth. Based on the existing research, use numerical simulation calculaton and analysis which considering the significant influence factors that temperature changes over time as boundary conditions. Draw the relationship and variation between external boundary conditions with ground temperature field and its stability.
李波、李元
工程基础科学地球物理学地质学
冻土温度场数值模拟
frozen earthtemperature fieldnumerical simulation
李波,李元.冻土地基温度场数值模拟研究[EB/OL].(2011-01-07)[2025-08-02].http://www.paper.edu.cn/releasepaper/content/201101-333.点此复制
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