A thermal conductivity model for insulation materials considering the effect of moisture in cold regions

热导率 材料科学 保温 曲折 复合材料 多孔性 热传导 含水量 水分 热的 热扩散率 相变材料 相对湿度 岩土工程 热力学 地质学 物理 图层(电子)
作者
Wansheng Pei,Feng Ming,Mingyi Zhang,Xusheng Wan
出处
期刊:Cold Regions Science and Technology [Elsevier]
卷期号:207: 103770-103770 被引量:13
标识
DOI:10.1016/j.coldregions.2022.103770
摘要

Insulation is an important material for energy conservation and frost heave reduction in cold regions. The thermal conductivity of the insulation materials is usually considered as a constant. However, their thermal performance degenerates due to the absorption of water. To describe the variations of thermal conductivities with water content, a thermal conductivity model for three-phase insulation material was proposed by considering the insulation material's porous and moisture absorption characteristics. A tortuosity correction was introduced to reflect the heat conduction path. Then, the measured results and the existed models were used to evaluate availability of the proposed model. Finally, the quantitative influence of the porosity, water content, and thermal conductivity of solid phase on the thermal conductivity of wet insulation materials was analyzed. The results show that there is close agreement between the predicted results of the new model and the measured ones, with the maximum relative error <15%. The model with tortuosity correction can effectively calculate the thermal conductivities of the insulation materials in a full range of porosity (from 0 to 1). The thermal conductivity decreases with the increase of porosity, but increases with the increase of water content. The solid phase's thermal conductivity has little influence on the thermal conductivity of the insulation materials. The study can provide an effective method to predict the thermal performance variation of the insulation material due to the effect of moisture content in cold regions.
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