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Mathematical modelling of heat transmission in the temperature history apparatus by using inverse method to evaluate the latent heat of high temperature PCMs

机译:使用逆方法评价高温PCMS潜热的温度历史仪中热传递的数学建模

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摘要

High temperature phase change materials (PCMs) are being proposed as thermal energy storage media in concentrated solar power plants. The thermophysical properties of PCMs, such as the latent heat of fusion/solidification need to be defined to enable system design and evaluate system performance and cost analysis. Several methods have been used to measure the latent heat of fusion/solidification of PCMs including the T-history method. The original assumption of the T-history method is the Biot number should be less than 0.1 where the lumped capacitance method is applicable. However, when the Biot number is more than 0.1 then the original equations are not applicable to estimate the latent heat of PCM. This paper demonstrates how a one-dimensional heat transfer mathematical model can be used by applying an inverse method to overcome the limitation of the lumped capacitance method in the original T-history method to determine the latent heat of PCMs. The mathematical model demonstrates that variation of the temperature distributions inside the samples for the discharge curves. Furthermore, this model shows the errors in the latent heat values if the T-history method is used, it is evident from the discharge curves of low thermal conductivity PCMs that the original simplified equations used for interpreting the T-history test results are not applicable for calculating the latent heat at different ambient temperature.
机译:在集中的太阳能发电厂中提出了高温相变材料(PCM)作为热能存储介质。 PCM的热物理性质,例如融合/凝固的潜热,需要定义为能够实现系统设计和评估系统性能和成本分析。已经使用了几种方法来测量包括T历史法的PCM融合/凝固的潜热。 T-ustrouls方法的原始假设是Biot数应小于0.1,其中块状电容方法适用。然而,当Biot数量大于0.1时,原始方程不适用于估计PCM的潜热。本文演示了如何通过应用逆方法来使用一维传热数学模型来克服原始T历史方法中的集总电容方法的限制来确定PCM的潜热。数学模型表明,用于放电曲线的样品内的温度分布的变化。此外,如果使用T历史方法,则该模型示出了潜热值中的误差,从低导热率PCM的放电曲线明显,用于解释T历史测试结果的原始简化方程不适用用于在不同环境温度下计算潜热。

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