基于连续介质热力学的冻土中未冻水含量与温度的关系

许多关于未冻水含量与温度之间关系的经验公式缺乏连续介质热力学理论的证明,且在温度接近0℃时出现奇异,因此不能很好地拟合冻土中未冻水含量与温度之间的关系曲线。从引入未冻水含量作为内变量和与内变量功共轭的相变潜热出发,利用连续介质热力学理论推导出冻土中未冻水含量与负温绝对值关系的理论公式。实验证明,所求得的公式可以很好地拟合冻土中未冻水含量与负温绝对值的关系曲线。

现浇混凝土-冻土接触面传热特性影响因素研究

现浇混凝土-冻土接触面传热特性直接影响灌注桩表面冻结强度,研究现浇混凝土-冻土接触面传热特性影响因素对冻土区桩基础设计和施工具有重要意义。基于小型模型桩试验条件建立数值模型,开展混凝土浇筑过程中混凝土-冻土接触面传热特性研究,分析了混凝土浇筑温度、水胶比、冻土温度、冻土含水量引起的接触面热流和温度变化。结果表明:浇筑温度由5℃升高至30℃,0.5 h混凝土与冻土接触面热流增大381.2%.水胶比由0.4增大至0.6,0.5 h接触面热流减少23.7%.接触面温度随冻土含水量的增大呈先增大后减小趋势,峰值在冻土液限附近。导热系数和相变热作用的转变起到了决定作用。冻土温度在-1^-3℃之间降低时,接触面温度随冻土温度降低而升高。浇筑后0~1 h(尤其是0~0.5 h)是混凝土对冻土释放热量的主要时间。

Variation characteristics of temperature and moisture content of seasonal frozen soil during freezing process in Changchun,China

In China, seasonal frozen soil is widely distributed. The freezing damage of subgrade soil in Jilin Province has been one of major engineering geological problems troubling the safety of road, in which some common damage phenomena, such as frost heave, subsidence deformation and frost boiling, are all caused by water translocation. Aiming at the phenomenon, the changes of moisture content of seasonal frozen soil in Changchun City are mainly studied by long-term field observation and indoor testing of physical properties under different conditions, and then the variation characteristics of moisture content in soil under different compactness and temperature conditions are realized. The results show that the increasing section of moisture content and negative temperature section all lie in O. 0 - 1.0 m of subgrade. Both lowest air and earth temperature occur in January to February, and the most negative temperature ranges from -7℃ to -10℃.