Kinetic phase diagrams for island nucleation and growth using accelerated dynamics

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Kinetic phase diagrams for island nucleation and growth using accelerated dynamics

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Island sizes s 9 can hop and dissociate according to activation energies and temperature ... i 1 stable but smaller ones dissociate before they capture monomers: ... –

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Title: Kinetic phase diagrams for island nucleation and growth using accelerated dynamics


1
Kinetic phase diagrams for island nucleation and
growth using accelerated dynamics M. Basham and
P.A. Mulheran Department of Physics University of
Reading
2
Simplistic Mesoscopic simulations (DDA)
3
Scaling in the Island Size Distribution
4
Capture Zones beyond mean field
5
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6
  • Multiscale Modelling Cu/Cu(100)
  • High i is preferable because it yields narrower
    size distributions (and better spatial
    organisation), which in turn influences the
    regularity of complete films and multilayer growth

7
  • Multiscale Modelling Cu/Cu(100)
  • High i is preferable because it yields narrower
    size distributions (and better spatial
    organisation), which in turn influences the
    regularity of complete films and multilayer
    growth
  • What influence do temperature and deposition rate
    have on i?

8
  • Multiscale Modelling Cu/Cu(100)
  • High i is preferable because it yields narrower
    size distributions (and better spatial
    organisation), which in turn influences the
    regularity of complete films and multilayer
    growth
  • What influence do temperature and deposition rate
    have on i?
  • Atomistic modelling of island dynamics using
    saddle-point search methods

9
  • Multiscale Modelling Cu/Cu(100)
  • High i is preferable because it yields narrower
    size distributions (and better spatial
    organisation), which in turn influences the
    regularity of complete films and multilayer
    growth
  • What influence do temperature and deposition rate
    have on i?
  • Atomistic modelling of island dynamics using
    saddle-point search methods
  • Self-learning Kinetic Monte Carlo to access the
    long-timescale regime

10
  • Multiscale Modelling Cu/Cu(100)
  • High i is preferable because it yields narrower
    size distributions (and better spatial
    organisation), which in turn influences the
    regularity of complete films and multilayer
    growth
  • What influence do temperature and deposition rate
    have on i?
  • Atomistic modelling of island dynamics using
    saddle-point search methods
  • Self-learning Kinetic Monte Carlo to access the
    long-timescale regime
  • Incorporate dynamics into MC simulations to
    address long lengthscales of film morphology

11
Self-learning kinetic Monte Carlo simulation for
small island dynamics
12
Island mobility parameters from self-learning KMC
13
Some tetramer island dissociation pathways
discovered by the SL-KMC
14
Island dissociation parameters from self-learning
KMC
15
Enhanced DDA Simulation
  • Lattice-based Monte Carlo simulation

16
Enhanced DDA Simulation
  • Lattice-based Monte Carlo simulation
  • Deposition, Diffusion and Aggregation of monomers

17
Enhanced DDA Simulation
  • Lattice-based Monte Carlo simulation
  • Deposition, Diffusion and Aggregation of monomers
  • Island sizes slt9 can hop and dissociate according
    to activation energies and temperature

18
Enhanced DDA Simulation
  • Lattice-based Monte Carlo simulation
  • Deposition, Diffusion and Aggregation of monomers
  • Island sizes slt9 can hop and dissociate according
    to activation energies and temperature
  • Islands grow when monomers or sub-critical
    islands diffuse onto them

19
Enhanced DDA Simulation
  • Lattice-based Monte Carlo simulation
  • Deposition, Diffusion and Aggregation of monomers
  • Island sizes slt9 can hop and dissociate according
    to activation energies and temperature
  • Islands grow when monomers or sub-critical
    islands diffuse onto them
  • Islands sgt8 are immobile and grow as compact
    circles

20
Enhanced DDA Simulation
  • Lattice-based Monte Carlo simulation
  • Deposition, Diffusion and Aggregation of monomers
  • Island sizes slt9 can hop and dissociate according
    to activation energies and temperature
  • Islands grow when monomers or sub-critical
    islands diffuse onto them
  • Islands sgt8 are immobile and grow as compact
    circles
  • Can directly image the impact of the small island
    dynamics

21
DDA simulations T300, D1/F 2e8
22
DDA simulations T300, D1/F 2e8
Diffusion only
23
DDA simulations T300, D1/F 2e8
Dissociation only
Diffusion only
24
DDA simulations T600, D1/F 2e8
25
DDA simulations T600, D1/F 2e8
Diffusion only
26
DDA simulations T600, D1/F 2e8
Diffusion only
Dissociation only
27
Kinetic Phase Diagram
  • Can we predict what the dominant growth process
    is for a given temperature and deposition rate?

28
Kinetic Phase Diagram
  • Can we predict what the dominant growth process
    is for a given temperature and deposition rate?
  • Start with mean-field rate equations for very
    small (point-like) islands

29
Kinetic Phase Diagram
  • Can we predict what the dominant growth process
    is for a given temperature and deposition rate?
  • Start with mean-field rate equations for very
    small (point-like) islands
  • The game is to decide
  • which flux dominates when
  • consequent scaling laws
  • when transitions between regimes occur

30
n1 is monomer density F is deposition rate N is
density of stable islands nj density if
subcritical islands size j Dj is diffusion rate
of island size j Kj is dissociation rate of
island size j Capture numbers O(1) neglected We
can assume terms always negligible
31
  • In general for critical island size i, islands
    si1 stable but smaller ones dissociate before
    they capture monomers

32
  • Consider the early stages of growth island and
    monomer density very low so i8
  • At high enough F, the monomer density becomes
    high enough to make a smaller island size stable
  • Here take theta 0.001 for nucleation regime

33
  • Consider the early stages of growth island and
    monomer density low so i8
  • At high enough F, the monomer density becomes
    high enough to make a smaller island size stable
  • Here take theta 0.001 for nucleation regime
  • Alternatively perhaps the island mobility
    dominates

34
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35
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36
  • i3 -gt i1,2 use i3 density equation for N
  • i3 -gt mobility scaling regime
  • Dimer mobility -gt i1 regime

37
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39
Theory 2/5 3/5 8/10 1/3 3/5
40
  • Summary and Conclusions
  • Multiscale modelling of Cu(100) homoepitaxy
  • Self-learning KMC of small island dynamics
  • Large-scale simulations of island nucleation and
    growth
  • higher temperature yields larger critical island
    size
  • Lower temperature growth can be dominated by
    dimer-island mobility
  • Theory development Kinetic Phase Diagrams
  • Thanks to Francesco Montalenti
  • Work supported by EPSRC grant T18738/01

41
Improving order in the JPD with temperature
42
Variance of JPD with coverage test of scaling
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