Abstract

The effect of island coalescence on island density during epitaxial growth is studied by kinetic Monte Carlo simulations. We find that the ratio N/N c between the island density N at time t and the number N c of islands per unit area that have coalesced up to the time t is a function of the coverage, but is independent of the specific material or the growth conditions. We analyze the results of our simulations by using several mean-field kinetic models of increasing complexity. They show that the simulation results are reproduced accurately only by a kinetic model which includes the spatial correlation between the location of the islands. The existence of a denuded zone around each island is particularly important, as it pushes the onset of coalescence towards higher coverages and increases the coalescence rate when the process starts.

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