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In case of hemispherical islands Vincent’s equation for the, kinetics reads (formula presented) where (formula presented) and (formula presented), being the film thickness. Moreover, the (formula presented) ratio is found to scale as (formula presented) (Ref
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In case of hemispherical islands Vincent’s equation for the S kinetics reads (formula presented) where (formula presented) and (formula presented) h being the film thickness. Moreover, the (formula presented) ratio is found to scale as (formula presented) (Ref. 2).
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17
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0003010354
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85038917794
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In film growth driven by coalescence the island density, as a function of film thickness, reads (formula presented), being a constant. This equation holds for simultaneous nucleation. Nevertheless, the conclusion reached in Ref., applies also to this case provided (formula presented) is the whole number of nucleation events, (formula presented)
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In film growth driven by coalescence the island density, as a function of film thickness, reads (formula presented) A being a constant. This equation holds for simultaneous nucleation. Nevertheless, the conclusion reached in Ref. 3 applies also to this case provided (formula presented) is the whole number of nucleation events, (formula presented)
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