Our present understanding
of surface dissolution of nuclear fuels
such as uranium dioxide (UO2) is limited by the use of
nonlocal characterization techniques. Here we discuss the use of state-of-the-art
scanning transmission electron microscopy (STEM) to reveal atomic-scale
changes occurring to a UO2 thin film subjected to anoxic
dissolution in deionized water. No amorphization of the UO2 film surface during dissolution is observed, and dissolution occurs
preferentially at surface reactive sites that present as surface pits
which increase in size as the dissolution proceeds. Using a combination
of STEM imaging modes, energy-dispersive X-ray spectroscopy (STEM-EDS),
and electron energy loss spectroscopy (STEM-EELS), we investigate
structural defects and oxygen passivation of the surface that originates
from the filling of the octahedral interstitial site in the center
of the unit cells and its associated lattice contraction. Taken together,
our results reveal complex pathways for both the dissolution and infiltration
of solutions into UO2 surfaces.