“…Similar to ice formation and melting, gas hydrate may undergo phase transitions of three stages, i.e., nucleation, , growth, , and dissociation. , Accumulated research efforts via experimental studies ,− and modeling/simulation work ,− have been made in attempt to gain more understanding of hydrate formation and dissociation phenomena for decades. It is relatively easy to monitor and study hydrate growth and dissociation on a macroscopic scale. ,,− During nucleation, the water–gas clustering process is an energy battle between the volume excess free energy (favorable, reduced enthalpy) and surface excess free energy (unfavorable, reduced entropy) in the metastable region. Nucleation is stochastic and intractable because initial embryos of hydrate clusters of different sizes would not obtain the critical size to form stable nuclei until the free energy barrier of pushing away the old phases is overcome. , Only a nucleus surpassing such energy barrier would reach critical size for sustainable nucleation and trigger macroscopic growth.…”