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首页> 外文期刊>E3S Web of Conferences >Thermal energy storage in embankments: Investigation of the thermal properties of an unsaturated compacted soil
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Thermal energy storage in embankments: Investigation of the thermal properties of an unsaturated compacted soil

机译:堤防热能储存:对不饱和压实土的热性能的研究

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摘要

Thermal energy storage in compacted soils can be considered as a new economically efficient and environmentally friendly technology in geotechnical engineering. Compacted soils are usually unsaturated; therefore, reliable estimates and measurements of their thermal properties are important in the efficiency analysis of these structures. In this study, a method is used to estimate the thermal properties of an unsaturated compacted soil. Several temperature sensors were placed in a thermo-regulated metric scale container to monitor the imposed temperature variation in the range of the 20 to 50 °C. This imposed temperature variation reproduced the temperature variation in the thermal energy storages. An inverse analytical model based on a one-dimensional radial heat conduction equation is used to estimate the thermal diffusivity using the temperature variation between two temperature sensors. The volumetric heat capacity was measured using a calorimeter in the laboratory, enabling the estimation of the thermal conductivity of the compacted soil. Then, this estimated thermal conductivity was compared with the thermal conductivity values measured with two other methods (steady-state and transient-state method). The difference between them are discussed in terms of the sample heterogeneity, sample size, and measurement method.
机译:压实土壤中的热能储存可被认为是岩土工程中的一种新的经济上有效和环保的技术。压实的土壤通常是不饱和的;因此,在这些结构的效率分析中,其热性能的可靠估计和测量非常重要。在该研究中,使用一种方法来估计不饱和压实土的热性质。将几个温度传感器置于热调节的公制刻度容器中,以监测20至50℃的范围内的施加温度变化。这种施加的温度变化再现了热能存储器中的温度变化。基于一维径向导热方程的反向分析模型用于使用两个温度传感器之间的温度变化来估计热漫射率。在实验室中使用量热计测量体积热容量,从而能够估计压实土的导热率。然后,将该估计的导热性与用另外两种方法(稳态和瞬态 - 状态方法)测量的导热率值进行比较。它们之间的差异在样品异质性,样品大小和测量方法方面讨论。

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