Island-size distribution and capture numbers in three-dimensional nucleation: Dependence on island morphology

John Royston and Jacques G. Amar
Phys. Rev. E 80, 041602 – Published 13 October 2009

Abstract

The scaling of the monomer and island densities, island-size distribution (ISD), and capture-number distribution (CND) as a function of the fraction of occupied sites (coverage) and ratio Dh/F of the monomer hopping rate Dh to the (per site) monomer creation rate F are studied for the case of irreversible nucleation and growth of fractal islands in three dimensions (d=3). We note that our model is a three-dimensional analog of submonolayer growth in the absence of island relaxation and may also be viewed as a simplified model of the early stages of vacancy cluster nucleation and growth under irradiation. In contrast to results previously obtained for point-islands in d=3, for which mean-field behavior corresponding to a CND which is independent of island size was observed, our results indicate that for fractal islands the scaled CND increases approximately linearly with island size in the asymptotic limit of large Dh/F. In addition, while the peak height of the scaled ISD for fractal islands appears to diverge with increasing Dh/F, the dependence on Dh/F is much weaker than for point-islands in d=3. The results of a self-consistent rate-equation calculation for the coverage and Dh/F dependence of the average island and monomer densities are also presented and good agreement with simulation results is obtained. For the case of point-islands, the value of the exponent χ describing the Dh/F dependence of the island density at fixed coverage, e.g., Nsat(Dh/F)χ, is in good agreement with the value (χ=1/3) expected for irreversible growth. However, for both compact and fractal islands in d=3, our results indicate that the value of χ (χ0.42) is significantly larger. In order to explain this behavior, an analytical expression [e.g., χ=df/(3df2)] for the dependence of χ on island fractal dimension df in d=3 is derived and found to give reasonable agreement with our simulation and rate-equation results for the case of point-islands (df=), compact islands (df=3), and fractal islands (df2.5). A general expression for the exponent χ, valid for d2, as a function of the critical island size i and df is also derived.

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  • Received 17 February 2009
  • Publisher error corrected 25 June 2010

DOI:https://doi.org/10.1103/PhysRevE.80.041602

©2009 American Physical Society

Corrections

25 June 2010

Erratum

Authors & Affiliations

John Royston* and Jacques G. Amar

  • Department of Physics & Astronomy, University of Toledo, Toledo, Ohio 43606, USA

  • *jroysto@utnet.utoledo.edu
  • jamar@physics.utoledo.edu

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Issue

Vol. 80, Iss. 4 — October 2009

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