posted on 2017-10-12, 00:00authored byJosé P. B. Mota, Daniel Martins, Diogo Lopes, Isabel Catarino, Grégoire Bonfait
The
energetics and phase behavior of the MIL-53(Al) metal–organic
framework upon low-temperature (15–260 K), subatmospheric H2 adsorption are studied experimentally using a volumetric
technique and theoretically by grand canonical Monte Carlo simulation.
The adsorption equilibrium data are recorded for a fixed amount of
H2 in the system at stable increasing temperature steps
starting from 15 K while recording the equilibrium pressure attained
at each step. The adsorption isotherms are generated by repeating
the experiments for different fixed amounts of adsorbate in the system
and connecting the equilibrium points obtained at the same temperature.
The solid–fluid interactions are modeled using the TraPPE-UA
force field and the fluid–fluid interactions using a parametrization
consistent with the same force field; quantum effects on H2 adsorption are taken into account via a quartic approximation of
the Feynman–Hibbs variational approach. The use of a consistent
force field with proven transferability of its parameters provides
an accurate description of the experimental adsorption equilibria
and isosteric heats of adsorption. Because of the weak solid–fluid
interaction, the Henry constant for H2 adsorption in the
large-pore (LP) form of MIL-53(Al) surpasses that for H2 adsorption in the narrow-pore (NP) form at a temperature lower than
that at which the dehydrated structure of the material collapses.
However, the saturation capacity of the LP form is always higher than
that of the NP phase. The phase behavior of MIL-53(Al) upon temperature-induced
H2 desorption is interpreted in terms of the osmotic thermodynamic
theory. For the conditions spanned in the experiments MIL-53(Al) exhibits
at most a single structural transition and its phase behavior depends
not only on pressure and temperature but also on the thermal history
of the bare material.