Abstract:
A theoretical model of the methane bubble migration under conditions of the hydrate development in an upward flow of water in a vertical pipe is proposed and constructed. We consider
two limiting mechanisms that determine the hydrate development kinetics in the process of gas
bubble floating-up. If the hydrate development intensity is determined by the heat removal from
the bubble surface by a liquid, the height at which the hydrate formation process terminates
amounts to fractions of meters; in the case where the process is limited by gas diffusion through
the hydrated peel, tens of meters.
The critical mass flow rates of gas and water needed to complete the process of hydrate formation have been obtained. It is found that the migration of gas bubbles in the reactor is accompanied by two possible modes of the hydrate development depending on the initial mass flow rate
of water: gas bubbles go over into the hydrated state either completely as separate inclusions or
partially with the formation of bubbles with a hydrate shell. The influence of the initial mass flow
of water on the dynamics of the hydrate formation process is analyzed at different values of hydrostatic pressure (or gas source operation depths).