天然岩石的热物理特性及其热物理特性变化对蓄热性能的影响分析

Energy Storage Pub Date : 2024-05-08 DOI:10.1002/est2.631
Luckywell Seyitini, Basim Belgasim, Christopher C. Enweremadu
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引用次数: 0

摘要

本研究对津巴布韦用于低温工业热能储存(TES)的天然岩石样本进行了热特性分析。确定了热稳定性、比热容、热扩散率、热导率和密度。对这些参数的变化进行了评估,并分析了它们对热储存性能的影响。发现不同地点的玄武岩和辉绿岩样本在室温下的平均比热容分别为 826 焦耳/千克 K 和 853 焦耳/千克 K。玄武岩和辉绿岩样本的比热容差异不大,分别为 3.4% 和 1.7%。此外,对于同类型但不同产地的岩石,玄武岩和辉绿岩样本的密度分别相差 0.3% 和 0.7%,可以忽略不计。不过,所有火成岩和变质岩样本的热扩散率都有很大差异,其中石英岩的热扩散率最高,为 2.1 × 10-6 m2/s,而其他样本的热扩散率在 0.9 × 10-6 至 1.6 × 10-6 m2/s之间。这意味着,使用不同地点的不同或相同岩石类型的显热式热沉系统的热效率可能很高,容易被忽视。热重分析结果表明,所研究的岩石样本具有良好的热稳定性,适合低温蓄热应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Thermo-physical characterisation of natural rocks and impact analysis of variations in their thermo-physical properties on thermal storage performance

In this study, the thermal characterisation of natural rock samples from Zimbabwe for low-temperature industrial thermal energy storage (TES) applications was carried out. Thermal stability, specific heat capacity, thermal diffusivity, thermal conductivity and density were determined. Variations in these parameters were evaluated and their impact on thermal storage performance was analysed. Basalt and dolerite samples from different locations were found to have average specific heat capacities of 826 and 853 J/kg K, respectively, at room temperature. Insignificant variations were observed with differences of 3.4% for basalt and 1.7% for dolerite samples. Also, negligible differences of 0.3% and 0.7% in densities for rocks of the same type but of different origins were obtained for basalt and dolerite samples, respectively. However, significant variations in thermal diffusivity of all the igneous and metamorphic samples were observed with quartzite rock exhibiting the highest value of 2.1 × 10−6 m2/s, while the values for the other samples range from 0.9 × 10−6 to 1.6 × 10−6 m2/s. This implies that the thermal efficiency of sensible TES systems that use different or the same rock types from different locations can be significantly high to be overlooked. Thermo-gravimetric analysis results revealed that the rock samples studied have good thermal stability for low-temperature heat storage applications.

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