Abstract
A study of the formation of a crystal hydrate film CH4 · 6H2O on the surface of an immobile solution of methane in water have shown that, at early stages of film formation, hydrate crystals and their agglomerates are in motion at a velocity of 2–5 mm/s caused by crystal growth. Collisions of agglomerates are accompanied by their rotations at a Ω ∼ 0.2–2 rad/s rate. The motion of crystals and agglomerates is explained using the hydrodynamic model that takes into account the surface tension and the difference in the pressure exerted by the medium on the growing and nongrowing faces of crystals, which sets them in chemoreactive motion.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
