瞬态热带法测定硅钙石型硅酸钙的导热系数

Gaosheng Wei , Xinxin Zhang , Fan Yu
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引用次数: 8

摘要

给出了硅钙石型硅酸钙保温材料在不同温度和压力下的热导率实验结果。为瞬态热带法(THS)设计了两种专用环境,即室温至1450 K的高温环境和大气压至10−3 Pa的真空环境。测定了四种密度的硅钙石型硅酸钙在环境温度至1000 K、0.045 Pa范围内对大气压的热导率。结果表明:硅钙石型硅酸钙的导热系数随密度的降低而明显降低,随压力的降低而明显降低,在100 Pa左右达到最小值;硅钙石型硅酸钙的导热系数随着T3的增加几乎呈线性增加,并且在低密度下比在高密度下增加得更多。热导率测量的不确定度估计在环境温度下约为3%,在800 K时约为6%。
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Thermal conductivity measurements on xonotlite-type calcium silicate by the transient hot-strip method

The experimental results of the thermal conductivities of xonotlite-type calcium silicate insulation materials were presented at different temperatures and pressures. Two appropriative surroundings, i.e. an elevated temperature surrounding from ambient temperature to 1450 K and a vacuum surrounding from atmosphere pressure to 10−3 Pa, were designed for the transient hot-strip (THS) method. The thermal conductivities of xonotlite-type calcium silicate with four densities from ambient temperature to 1000 K and 0.045 Pa to atmospheric pressure were measured. The results show that the thermal conductivity of xonotlite-type calcium silicate decreases apparently with the fall of density, and decreases apparently with the drop of pressure, and reaches the least value at about 100 Pa. The thermal conductivity of xonotlite-type calcium silicate increases almost linearly with T3, and increases more abundantly with low density than with high density. The thermal conductivity measurement uncertainty is estimated to be approximately 3% at ambient temperature, and 6% at 800 K.

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