1995
DOI: 10.1103/physrevlett.75.2148
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Diffusion of Monolayer Adatom and Vacancy Clusters: Langevin Analysis and Monte Carlo Simulations of their Brownian Motion

Abstract: In recent observations of Brownian motion of islands of adsorbed atoms and of vacancies with mean radius R, the cluster diffusion constant varies as R 21 and R 22. From an analytical Langevin description of the cluster's steplike boundary, we find three cases, R 21 , R 22 , and R 23 , corresponding to the three microscopic surface mass-transport mechanisms of straight steps. We thereby provide a unified treatment of the dynamics of steps and of clusters. For corroboration, we perform Monte Carlo simulations of… Show more

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Cited by 174 publications
(170 citation statements)
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“…From simulations performed at T = 300 K, 500 K, and 700 K, the effective diffusion barriers are found to increase almost monotonically with size, while the diffusion coefficient takes the form shown in is mildly temperature dependent [28]. This is consistent with the theoretical value of 3/2 for large island motion dominated by atom diffusion along island perimeter [17]. …”
Section: Diffusion Coefficientssupporting
confidence: 76%
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“…From simulations performed at T = 300 K, 500 K, and 700 K, the effective diffusion barriers are found to increase almost monotonically with size, while the diffusion coefficient takes the form shown in is mildly temperature dependent [28]. This is consistent with the theoretical value of 3/2 for large island motion dominated by atom diffusion along island perimeter [17]. …”
Section: Diffusion Coefficientssupporting
confidence: 76%
“…One of the most important questions that still remains open is the role of island diffusion, since for mobile islands the aggregation rates in the RE approach depend explicitly on the diffusion coefficients D s of islands of different sizes s. Island diffusion on surfaces has been studied both theoretically [7,8,9] and experimentally [10,11,12,13,14,15,16]. While in the large island limit the size dependence of the island diffusion coefficients can be classified based on simple basic processes [17], for smaller islands D s depends on the geometric and energetic details of the underlying surface, and can be a complicated, non-monotonic function of s [18,19].…”
Section: Introductionmentioning
confidence: 99%
“…Traditional simplistic mean-field-type analyses of the dependence of cluster diffusion coefficient D on size N ͑for large N͒ suggest different behavior for the TD and PD classes. 8,11 However, it is clear that the actual behavior will depend strongly on the magnitude of the rate controlling bulk vacancy transport ͑relative to other rates͒ and on the size of the cluster. In our current studies, the clusters are sufficiently small that bulk vacancies cannot form, so cluster diffusion is unambiguously associated with the PD class.…”
Section: Lattice-gas Models For Cluster Diffusionmentioning
confidence: 99%
“…[8][9][10][11] If they do, we are implicitly regarding the four atoms adjacent to the interior vacancy as ''perimeter'' atoms and the kinetic rules would allow one of them to exchange with the vacancy, thus facilitating its diffusion. Such models are traditionally placed in the so-called terrace diffusion ͑TD͒ class.…”
Section: Lattice-gas Models For Cluster Diffusionmentioning
confidence: 99%
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