Reclamation
of coal fly ash, a legacy waste material,
provides
an alternative pathway for the recovery of rare earth elements (REEs)
while reducing the environmental stresses that stem from traditional
mining. The reactive transport processes underlying the recovery of
REEs from ash wastes, however, are yet to be fully elucidated owing
to the physicochemical complexity of the micro/nanoscale fly ash particles,
including the crystallinity of the particulate matrix. In this work,
we use transmission electron microscopy to characterize the material
properties of ash particles and reveal the impact of crystallinity
on the reactive transport processes governing access to and recovery
of the encapsulated REEs. Our results show, for the first time, two
distinct crystalline structures of REE-bearing aluminosilicate particles:
dense amorphous matrices that facilitate the exchange of chemical
species through their lattice interstices and porous polycrystalline
matrices characterized by connected intraparticle pores and chemical
inertness to leaching solutions. Notably, the presence of matrix crystallinity,
or the lack thereof, governs the extent of reagents consumed parasitically
by secondary reactions with the aluminosilicate matrix. Our work reveals
how the variability of crystalline structures of the ash matrices
hosting REEs defines the pathways for the recovery of REEs, providing
key insights required for the development of targeted recovery processes.