We
investigate the effects of high solvated-methane concentration
on methane-hydrate nucleation at 250 K and 500 atm. We consider solutions
at four levels of methane molar fraction in the initial H2O–CH4 solution, χCH4
= 0.038, 0.044, 0.052, and 0.058, which are higher than (metastable)
bulk supersaturation. χCH4
is controlled
independently of the temperature and pressure thanks to the use of
special simulation techniques [Phys. Chem. Chem. Phys.
2011, 13, 13177]. These conditions
mimic a possible increase of local methane concentration beyond supersaturation
induced, for example, by freeze concentration or thermal fluctuations.
The nucleation mechanism and kinetics are investigated using the dynamical
approach to nonequilibrium molecular dynamics. We demonstrate a hydrate-forming/-ordering
process of solvated methane and water molecules in a manner consistent
with both the “blob” hypothesis and “cage adsorption
hypothesis”: the system initially forms an amorphous nucleus
at high methane concentration, which then gets ordered, forming the
clathrate crystallite. We evaluate nucleation rates using both the
methods of the mean first-passage time, i.e., the curve of the average
time the system takes to reach a crystalline nucleus of given size,
and survival probability, i.e., probability that up to a given time
the system has not nucleated yet. We found a dependence of the nucleation
rate on initial methane concentration of a form consistent with the
dependence of classical nucleation theory rate on supersaturation
and determined the relevant parameters of this relation. We found
a very rapid increase of nucleation rate with solvated-methane concentration,
proving that methane molar fraction, even beyond bulk supersaturation,
is key at triggering the homogeneous nucleation of clathrate. We derive
a kinetic equation that allows for estimation of the nucleation rate
over a wide range of concentration conditions.