Effect of thermocapillary convection on the melting of phase change materials in microgravity: Experiments and simulations

• Published in: International journal of heat and mass transfer Vol. 154; p. 119717
• Main Authors: Salgado Sánchez, P., Ezquerro, J.M., Porter, J., Fernández, J., Tinao, I.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01-06-2020; Elsevier BV
• Subjects: Aspect ratio; Computational fluid dynamics; Computer simulation; Containers; Enthalpy; Free surfaces; Marangoni convection; Mathematical models; Melting; Microgravity; Parabolic flight; Phase change materials; Porosity; Thermal conductivity; Thermal diffusion; Thermal energy; Thermocapillary convection; Thermocapillary effect; Phase change materials; Thermocapillary effect; Microgravity; Marangoni convection
• ISSN: 0017-9310; 1879-2189
• DOI: 10.1016/j.ijheatmasstransfer.2020.119717

•First microgravity experiments investigating enhancement of PCM melting due to thermocapillary convection.•Heat transport measured by observing the cross-sectional liquid area over time.•Phase change modelled numerically using an enthalpy-porosity based formulation.•Thermocapillary convection enhances heat transport by approximately a factor of two, depending on geometry.
Experiments on the melting of n-octadecane in the presence of a free surface were performed under the reduced gravity conditions of a parabolic flight, where natural gravitational convection is negligible. The results constitute the first systematic experimental investigation of the capacity of thermocapillary (Marangoni) convection to enhance heat transfer during the melting of organic Phase Change Materials (PCMs) in microgravity, where their low thermal conductivity leads to significant lag (long response times) that, in some applications, constrains their utility as passive thermal control devices. Rectangular containers of three different aspect ratios holding n-octadecane and a layer of air were heated from one side in order to observe the melting process. During the relatively short microgravity periods, which lasted approximately 20 s, the effect of thermocapillary convection remained concentrated in a layer near the free surface that is thinner than the PCM height H for the aspect ratios considered. The weak dependence of this layer on the lower region, where heat transport is dominated by thermal diffusion, means that the relative contribution of thermocapillary convection decreases with H. The experimental results are supported and complemented by a series of numerical simulations modelling the phase change and liquid dynamics with an enthalpy-porosity-based formulation of the Navier-Stokes equations. Very good agreement with the experimental observations is found.