Dissolution and Hydrate-Formation Processes behind the Shock Wave in a Gas–Liquid Mixture

摘要

One of the important factors of Earth’s climate change is an increase in the carbon-dioxide concentration in the Earth atmosphere. A promising way of gas recycling is its conversion into a gas–hydrate state and storage at the ocean bottom at a low temperature and high static pressure [1]. One of the main parameters providing the economic feasibility of this way is the formation rate of carbonic-acid hydrate. There are various methods of intensification of the hydratization process for gases: the fine dispersion of the gas-saturated jet in gaseous atmosphere [2], the intense hashing of water saturated with dissolved gas [3], the vibration action on the liquid saturated with gas [4], the ultrasonic action on the medium [5], etc. The basic disadvantage of the proposed methods is their low rate of gas-hydrate formation.