Thermodynamic and kinetic characterization of methane hydrate 'nucleation, growth and dissociation processes, according to the labile Cluster theory

Methane hydrates were formed and then dissociated in presence of fresh water and a pure quartz porous medium, by using a small-scale experimental apparatus, appositely designed for those experiments. The most significant phases describing the process, or nucleation, massive growth and dissociation, were characterized both thermodynamically and kinetically. Methane hydrate equilibrium was defined in presence of such porous medium and the hydrate formation rate was calculated for kinetic considerations. To do this, the Labile Clusters Theory was considered and, according to it, hydrate formation was considered a first-order chemical kinetic equation for the time dependence. Finally, pressure variation over time was discussed. The comparison between trend assumed by those parameters revealed consistent and visible similarities, which allowed to a very deepened characterization about all three phases making up the whole process.

Automated summary

In this study, methane hydrates were analyzed for their thermodynamic and kinetic properties in the presence of fresh water and a pure quartz porous medium. The Labile Clusters Theory was used to calculate the hydrate formation rate as a first-order chemical kinetic equation, providing insights into the time dependence of the process. Pressure variations were also discussed, revealing consistent similarities with other parameters and allowing for a detailed characterization of the entire process.