The Kinetic Monte Carlo (KMC) method is widely used to study the growth of
islands on surfaces. The growth behaviour is characterized by the scaling p
roperties of the island size distribution and its time evolution. Two stage
s of growth are considered: the diffusion and aggregation regime (at less t
han about 30% coverage), and a coalescence model relevant to higher coverag
e. It is shown how details of the growth processes revealed by the KMC simu
lations can be coupled with scaling ideas to provide a proper understanding
of the island size statistics and their time dependence fur both regimes.
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