Abstract
During methane dissolution in water in a closed space, the pressure varies exponentially with time until the formation of methane hydrate. A model of this process is proposed that fits experimental data well. The methane concentration at the onset of hydrate formation is calculated as a function of temperature and pressure.
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Martynets, V.G., Afanas'ev, I.S., Bezverkhii, P.P. et al. Equilibrium and Kinetic Properties of Methane Hydrate. Theoretical Foundations of Chemical Engineering 36, 495–499 (2002). https://doi.org/10.1023/A:1020686031117
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DOI: https://doi.org/10.1023/A:1020686031117