Abstract
In this research a review of the formation kinetics of TBAC-like clathrate dual hydrates is investigated. Natural gas hydrate is a solid crystalline compound formed from a combination of water and gas, and these compounds are formed at low temperatures and relatively high pressures. Hydrate is a member of the clathrite family. The guest gas molecules are trapped inside the cavities of the water network (host), which is formed by hydrogen bonding between the molecules of the water molecule, a clear example of which is smaller compounds than pentane in natural gas such as methane, ethane, propane and Carbon dioxide can be formed by pure gas or a gas mixture consisting of two or more components. Clarite is considered to be a solid solution in which guest gas molecules and hydrate gases are in contact. They are located with the host lattice (water), so gaseous hydrate is known as a non-stoichiometric solid, there is a strong hydrogen bond between the water molecules in the hydrate structure, while there is no chemical interaction between the guest and host molecules alone.
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