Monazite is a rare earth element (REE)-containing mineral
that
consists of (REE)PO4 formal units and is one of the most
important sources of these critical materials. The concentration of
REEs from mined monazite ore often involves froth flotation, which
is a beneficiation process that enhances the efficiency of downstream
processing. The effectiveness of froth flotation is largely governed
by the ability of collector agents to selectively bind to monazite
particles. Thus, a molecular-level understanding of monazite interfacial
chemistry is integral to the design of effective collector agents.
To address this need, we performed density functional theory (DFT)
calculations and a variety of experimental techniques to characterize
La-monazite and elucidate its crystal morphology. Interestingly, we
find minimal differences in the predicted morphologies of La-monazite
for hydrous and anhydrous environments, which are largely dominated
by low-index facets (e.g., {110}, {100}, and {010}). Indexing of synthesized
La-monazite crystals via X-ray diffraction also uncovers {110} and
{100} as the predominant facets. The average surface energies of 0%
and 100% water coverage La-monazite crystals were predicted to be
0.87 and 0.76 J/m2, respectively, while calorimetry suggests
values of 1.30 and 1.15 J/m2, respectively. The apparent
discrepancies between the theoretical and experimental values are
expected and attributed to defects present in physical crystals, in
contrast to the perfect mineral surfaces in simulations. The difference
in surface energy between the 0% and 100% water coverage morphologies
predicted by theory is consistent with the value measured via calorimetry.
DFT reveals a wide range of adsorption energies for water across the
studied facets, but in all cases, water is predicted to strongly bind
to monazite surfaces with an average adsorption energy of −92.7
kJ/mol for a La-monazite single crystal. This study provides the groundwork
necessary for the rational design of froth flotation collector agents
by granting molecular-level insight into the predominant facets of
monazite.