4.6 Article

Calorimetric study of carbon dioxide (CO2) hydrate formation and dissociation processes in porous media

Journal

CHEMICAL ENGINEERING SCIENCE
Volume 264, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ces.2022.118108

Keywords

CO2 hydrate; Cold storage; Differential thermal analysis; Particle and pore size; Porous media; Water saturation

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Understanding the mechanisms of gas hydrate formation and dissociation in porous media is crucial for the development of new energy-efficient and environmentally friendly technologies related to cold storage. This study investigates CO2 hydrate formation and dissociation in two different porous materials, sand and silica gel. The results show that factors such as water saturation, particle size, and morphology of the porous media can affect the process, with silica gel showing a higher amount of hydrate formed compared to sand.
Understanding the formation and dissociation mechanisms of gas hydrate in porous media is important for the development of new energy-efficient and environmentally friendly technologies related to cold storage as they provide significant latent heat and energy density at suitable phase change temperature. The challenge is to understand the interactions between gas hydrates and the chosen storage media in order to assess the operating conditions likely to optimize time and energy consumption in cold produc-tion and storage systems. In this work, CO2 hydrates formation and dissociation are investigated in two morphologically different porous materials: sand and silica gels. A calorimetric approach is applied to study both the CO2 hydrate formation kinetics, particularly the induction time, and the amount of hydrate formed for each of the two porous materials. The experiments are performed using a differential thermal analysis device with two identical measuring cells. The present work is focused on assessing the effect of key factors like water saturation, particle size and the morphology of porous media on CO2 hydrate formation and dissociation processes. Overall, the results do not show a statistically significant correlation between these factors and the induction time. Interestingly, the results obtained with dual porous silica gel showed a higher amount of hydrate formed compared to those with sand for similar ini-tial pressure, temperature and water content conditions. This result may be due to the fact that silica gels provide higher surface area due to their smaller particle size (20-45 lm vs 80-450 lm for sand), and the presence of internal pore volume in silica gel particles.(c) 2022 Elsevier Ltd. All rights reserved.

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