The molecular sieving
of H2 and its isotopes produced
by nuclear plants is a long-standing research where some adsorption
processes are well identified. However, some mechanisms governing
the diffusion of the proton and its isotopes within a faujasite NaX
at low temperatures (40–100 K) are still troublesome to characterize.
Notwithstanding, an understanding of the processes governing adsorption
diffusion within narrow pores is essential for the development of
recycling procedures of gases produced by nuclear plants. At cryogenic
temperatures, it is well known that quantum effects are revealed and
the heterogeneity of the guest structure plays an important role in
the adsorption process. Here, we focus on the consequences of these
two factors on molecular sieving and transport coefficients based
on molecular dynamics including the Feynman–Hibbs quantum approximation.
Our results show at temperatures below 77 K that H2 has
a lower adsorption capacity and a lower diffusion coefficient than
those of D2 and T2. Here, we give an original
explanation of this diffusion inversion in terms of the activation
energies. We show that this energy is greater for H2 by
30 and 50% than that for D2 and T2, respectively.
Moreover, experimentally, it has been shown that the pore heterogeneity
of the faujasite NaX leads to an increase of the self-diffusion coefficient
with loading. For explaining this unexpected behavior, several authors
have proposed a scenario based on either privileged adsorption sites
or the residence time of molecules near the guest pore walls, followed
by isotropic jumps. Here, we report an original analysis based on
the mean square displacements, revealing the presence of slow and
fast molecular mobility regimes. The ensemble of our results provide
useful physical information about the development of recycling procedures
of gases produced by nuclear plants.