Coarsening of Ag films on Ag(100) at room temperature occurs primarily
via diffusion-mediated coalescence of two-dimensional adatom clusters
, rather than by Ostwald ripening, up to a coverage of 0.65 monolayer.
Above 0.8 monolayer, vacancy clusters coarsen primarily via Ostwald r
ipening, due to their much lower diffusivity. An asymmetric transition
region separates these two regimes, characterized by a near-percolati
ng structure which undergoes self-similar coarsening.