Multicomponent
crystals, for which natural gas hydrates are important
examples, have drawn considerable attention because of their scientific
and industrial importance. By performing large-scale molecular dynamics
simulations on hydrate nucleation of several common natural gases
(CH4, C2H6, C3H8, and H2S) and their mixtures, we aim to elucidate the
roles of gas molecules and their compositions on mixed hydrate nucleation.
We find that at a fixed temperature and solution composition, the
induction time (τ) sequence for pure guest hydrate nucleation
is τ(C2H6) < τ(C3H8) < τ(CH4) < τ(H2S).
A relatively small number of guest molecules with a shorter induction
time for pure guest hydrate nucleation can promote the formation of
initial nuclei of a mixed hydrate. Detailed cage analysis shows that
small guests such as CH4 can induce the formation of more
standard cages for mixture systems with either C2H6 or C3H8 systems, thereby reducing the
formation of nonstandard cages and impacting the nucleation kinetics.
Enrichment of CH4 in the nucleated cluster of C2H6/CH4 and C3H8/CH4 mixed hydrates was also observed. Four cage type subsets,
i.e., 5126
a
, 415106
b
, 42586
c
, and 43566
d
(with a ranging from 0, 2,
3, 4; b from 2 to 6; c from 0 to
6; and d from 0 to 6) are identified as dominating
the complete-cage populations for the hydrates formed in this study.
Moreover, four-membered water rings appear to play an increasingly
larger role in nucleated clusters as the size of guest molecules becomes
larger.