Abstract
The current greenhouse effect caused by massive CO<sub>2</sub> accumulation must be addressed urgently. Because of the ocean's enormous capacity, the high density of CO<sub>2</sub> hydrate, and the high stability of CO<sub>2</sub> sequestration in hydrate form, the process of hydrate generation can trap CO<sub>2</sub> molecules into the lattice of water molecules and is considered for the sequestration of CO<sub>2</sub> in hydrate form in the ocean. In this paper, molecular dynamics (MD) simulations are used to investigate the kinetic behavior of CO<sub>2</sub> hydrate growth in ion-containing electrolyte solutions. The mechanism of salt ion effect on hydrate growth during pressure changes is investigated. The simulations show that in the presence of salt ions, the hydrate growth rate fluctuates significantly, despite the fact that a greater driving force can facilitate the hydrate growth process. Higher pressures increase guest molecule occupancy in the hydrate cage, while the saline environment causes competition for water molecules between the hydrate cage and salt ions, increasing the proportion of empty cages. Lower pressures and the presence of salt ions reduce CO<sub>2</sub> molecules' selectivity for the smaller 5<sup>12</sup> cages, creating a barrier to hydrate growth. The findings of the study look at the microscopic mechanism of CO<sub>2</sub> hydrate generation in seawater and serve as a guide for future implementation of hydrate method CO<sub>2</sub> sequestration technology in the marine environment.
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