Significance: Understanding the clathrate formation mechanism has important implications on natural gas exploitation, storage, and transportation. A key toward clathrate formation is the hydrate nucleation, which involves complex interplay between water and guest molecules at nanoscale and multiple kinetic stages. Herein, by tracing the kinetic evolution of multiple ternary water-ring aggregations based on trajectories of large-scale molecular dynamics simulations, we identified a generic nucleation pathway to clathrate formation. This observed nucleation pathway is driven by numerous compression/shedding processes among the methane hydration layers, and it can explain the widely accepted “blob” model of clathrate nucleation. The molecular insight into the nucleation pathway allows us to quantitatively assess the nucleation timescales as well as the critical nucleus sizes in the clathrate formation.

Adsorption and non-binding-hydrate sites produce synergistic effects that lead to unstable adsorption and inhibition effects (recurring destruction of hydrate).

Over the last two decades, the swelling properties of montmorillonite (MMT) have been studied in many experimental and simulation works, but less attention has been given to MMT containing a mixture of monovalent/monovalent and monovalent/bivalent cations in the interlayer spaces. We carried out a molecular dynamics simulation of the swelling patterns of Na-, Mg-, Na/Cs-, Na/Mg-MMT in an isobaric isothermal ensemble (NPT) at T = 300 K and p = 1 atm. The simulation reproduced a swelling pattern of Na-, Mg-, Na/Cs-, Na/Mg-MMT and the swelling curves obtained showed the difference between the hydration mechanisms of the type of MMT used in this study. We also found out that the differences in size and hydration energy of Na, Cs and Na, Mg ions have strong implications on the structure of interlayer water. This has led to the difference in the swelling curves of the simulated Na-, Mg-, Na/Cs- and Na/Mg-MMT. For Na/Cs-MMT, the hydration energy of Na cations increased compared to that in Na-MMT, the hydration energy of Cs cations decreased in Na/Cs-MMT compared to that in Cs-MMT and also for Na/Mg-MMT, the hydration energy of Na cations increased compared to that in Na-MMT and that of Mg cations decreased in comparison with that in Mg-MMT. The diffusion coefficient of Cs cations obtained in this simulation was higher than that of Mg and Na cations in Cs-, Mg- and Na-MMT, respectively. Cesium cations have been seen to have a low hydration energy compared to Na and Mg cations and can be used as a good inhibitor of Na-MMT swelling process.

Density functional theory calculations and molecular dynamics simulations were performed to investigate the hydrogen storage capacity in the sII hydrate. Calculation results show that the optimum hydrogen storage capacity is ~5.6 wt%, with the double occupancy in the small cage and quintuple occupancy in the large cage. Molecular dynamics simulations indicate that these multiple occupied hydrogen hydrates can occur at mild conditions, and their stability will be further enhanced by increasing the pressure or decreasing the temperature. Our work highlights that the hydrate is a promising material for storing hydrogen.