摘要
采用稳态对比法,对2种厚度、孔隙竖直的空心砖做了竖向传热对比试验.结果表明:当零温端位于试样顶部时(模式Ⅰ),试样底部(暖端)温度的初始下降速率要比零温端位于试样底部时(模式Ⅱ)其顶部(暖端)温度的初始下降速率快;当试样的内部温度场稳定以后,模式Ⅰ下的试样竖向温差要比模式Ⅱ下的温差小,并且在试样的整个降温过程中,模式Ⅰ下暖端的降温幅度要比模式Ⅱ下的大.通过近似分析表明,模式Ⅰ的空心砖传热系数是模式Ⅱ的3倍多.在多年冻土地区搞工程建设,合理利用空心砖的这种竖向传热差异性,将有利于增强下部地基的稳定性.
The heat transfer performance of hollow bricks with two kinds of thickness under the condition of vertical aperture was studied by steady comparison method. The results show: (1) for the system with the cold end being 0 ℃ 0 it is cooled more quickly when the cold end is located on the top (mode Ⅰ ) than on the bottom (mode Ⅱ ) ; (2) when the temperature region of system come to stabilization, the temperature fall of the warm end is higher for the mode I than the mode Ⅱ. At the same time, the temperature difference of the warm end for mode Ⅱ is less than mode Ⅰ. Finally, it is indicated by the approximate calculation that thermal transfer coefficient for the mode Ⅰ is 2 times higher than mode Ⅱ. If the heat transfer difference of hollow bricks can be applied, stability of the groundwork will be enhanced.
出处
《建筑材料学报》
EI
CAS
CSCD
2006年第1期72-76,共5页
Journal of Building Materials
基金
中国科学院知识创新工程重大项目(KZCX1-SW-04)
关键词
空心砖
传热系数
传热系数比
多年冻土
hollow brick
heat transfer coefficient
ratio of heat transfer coefficient
permafrost