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Measurement and Modelling of Water ContentEffects on Thermal Properties of Compressed SoilBuilding Blocks

机译:含水量的测量和建模对压缩土砌块热性能的影响

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Aims: The aim of this paper was to determine the thermal conductivity and the thermal effusivity of the compressed soil building blocks as a function of their water content.Study Design: Samples with dimensions 53x40x20 mm~(3) were produced for experiment. Eight containers and an oven were used to determine the equilibrium moisture content. The thermal properties of samples were obtained using a symmetrical hot strip method device.Place and Duration of Study: University of Yaounde I and National Advanced School of Engineering, Laboratory of Energizing, Water and Environment, between March 2014 and October 2014.Methodology: Thereafter, sorption isotherm of this building material was determined using the gravimetric static method of saturated salt solutions at 30°C (ambient average temperature), and GAB equation was applied to discuss the results. Then, a symmetrical hot strip method device was used to measure the thermal conductivity and the thermal effusivity of these samples, with their water content varying from 0 to a maximum value of 0.139 kg_(w.)kg_(db)~(-1).An adapted device was developed to prevent water evaporation on the lateral faces of the samples.Results:Both thermal conductivity and thermal effusivity were modelled and the experimental results were processed to evaluate these thermal properties of compressed soil building blocks.A new simplified model, based on a physical approach with assumption of an ideal shrinkage of the material during the evaporation of water, was built.Conclusion: Calculated and experimental values of thermal properties were in good agreement, with a maximum standard error of 1.671 Wm~(-)~(2)K~(?-1)s~(1/2 )for thermal effusivity and of 0.024 Wm~(-1)K~(-1) for thermal conductivity. The suitability of this model for other buildings material will be further studied.
机译:目的:本文的目的是确定压缩的土壤构件的热导率和热发射率随其含水量的变化。研究设计:制备尺寸为53x40x20 mm〜(3)的样品进行实验。使用八个容器和一个烤箱确定平衡水分含量。研究的样品的热性质使用对称的热剥法设备进行研究。研究地点和持续时间:雅温得第一大学和国家工程学院,能源,水与环境实验室,2014年3月至2014年10月。 ,使用饱和盐溶液的重量静态方法在30°C(环境平均温度)下确定该建筑材料的吸附等温线,并使用GAB方程式讨论结果。然后,使用对称的热剥法装置测量这些样品的热导率和热发射率,其水含量从0到最大值0.139 kg_(w。)kg_(db)〜(-1)不等。结果,对热导率和热效率进行了建模,并对实验结果进行了处理以评估压缩土构件的这些热性能。一个新的简化模型基于物理方法,假设材料在水蒸发过程中具有理想的收缩率。结论:热性能的计算值和实验值吻合良好,最大标准误差为1.671 Wm〜(-)〜 (2)K〜(?-1)s〜(1/2)表示热导率,0.024 Wm〜(-1)K〜(-1)表示热导率。该模型对其他建筑材料的适用性将进一步研究。

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