Measurement of the thermal properties of unsaturated compacted soil by the transfer function estimation method. (25th February 2020)

• Record Type: Journal Article
• Authors: Lahoori, M.; Jannot, Y.; Rosin-Paumier, S.; Boukelia, A.; Masrouri, F.
• Is Part Of: Applied thermal engineering. Volume 167(2019)
• Publication Date: 2020-02-25
• Subjects: Soil thermal properties -- Transfer function -- Unsaturated compacted soil -- Inverse analytical model; Heat engineering -- Periodicals; Heating -- Equipment and supplies -- Periodicals; Periodicals; 621.40205
• DOI: 10.1016/j.applthermaleng.2019.114795
• Languages: English
• ISSNs: 1359-4311

Abstract

Highlights: The thermal properties of unsaturated compacted soil are investigated. A thermo-regulated metric scale container is used to compact the tested soil. An inverse analytical model is developed to estimate the soil thermal properties. The estimated thermal conductivity is compared to two other classical methods. Abstract: Thermal energy storage in embankments can be considered a new economically efficient and environmentally friendly technology in geotechnical engineering. In these structures, horizontal heat exchanger loops can be installed inside different layers of compacted soil to store heat in the medium during the summer to be extracted during the winter. Compacted soils are usually unsaturated; therefore, reliable estimates and measurements of unsaturated compacted soil thermal properties, such as the volumetric heat capacity, thermal conductivity, and thermal diffusivity, are important in the efficiency analysis of these structures. However, there is no available method to characterize the evolution of these parameters over time in compacted soil. In this study, several temperature sensors were placed inside different layers of unsaturated compacted soil in a cylindrical container (height of 0.8 m and diameter of 0.6 m ) to monitor imposed temperature cycle variations. An inverse analytical model based on the one-dimensional radial heat conduction equation is proposed to estimate the thermal diffusivity using the temperature variation between two temperature sensors. The volumetric heat capacity was measured with a calorimeter in the laboratory, enabling estimation of the thermal conductivity of the compacted soil. Then, this estimated thermal conductivity was compared with the thermal conductivity values measured with two different methods (one steady-state and one transient-state method). The estimated thermal conductivity was close to the value measured with the transient-state method. It was demonstrated that steady-state methods are not suitable for the measurement of thermal conductivities as high as 2.5 W . m - 1 . K - 1 since thermal contact resistances are no longer negligible.