Along with available
adsorption isotherms and uptake kinetic data,
microscopic knowledge of the guest self-diffusion and intracrystalline
movement of the simple air binary mixture of nitrogen (N2) and oxygen (O2) within Li–LSX zeolite is needed
to optimize the design and to reach a breakthrough high-efficiency
of air separation process based on the selective adsorption in this
zeolite. In the current work for the first time, an all-atom molecular
dynamics (MD) simulation is used to study the average single-particle
dynamics, self-diffusion, and microscopic structure of the atmospheric
binary gaseous mixtures of N2 and O2 in Li–LSX
zeolite at temperatures between (260 and 700) K. The common order
of magnitude of the computed guest self-diffusion coefficients at
different temperatures is in the range of 10–9 -
10–8 m2·s–1 and
corresponding activation energies obtained using the Arrhenius equation
varied in the range of ∼0.6 for O2 to 1.6–3.3
kcal·mol–1 for N2 in simulations
with mobile and with fixed extra-framework Li+ on SIII
sites (Li–III), respectively. Present results provide some
new molecular-level insights into the link between the behaviors of
the pendulum-like motion of Li–III with the guest molecules.
Results show that O2 guest molecules freely move into the
supercages and channels of the zeolite without any attachment to the
key sorption cationic sites and the behavior of O2 is independent
of the fixed or mobile Li–III situation during of simulations.
In contrast, the oscillatory motion or immobility of the Li–III
cation is found to have a surprisingly large influence on the intracrystalline
N2 self-diffusion, the local (N2–Li–III)
structural correlation, and the mean time of attachment of N2 to Li–III. The different observed adsorption behavior of
two guest components was previously connected to the difference in
their relative values of permanent quadrupole moments which causes
different guest–Li–III affinities. These are well explained
by a microscopic structural and dynamical analysis in current study.
O2 component diffuses faster than N2 within
the nanoporous Li–LSX zeolite, especially with a greater relative
diffusivity difference for simulations with fixed Li–III at
relatively low temperatures which correspond to favorable selective
adsorption conditions. The computed O2/N2 diffusion
selectivity ratio increases with decreasing temperature.