Title: Kinetic phase diagrams for island nucleation and growth using accelerated dynamics
1Kinetic phase diagrams for island nucleation and
growth using accelerated dynamics M. Basham and
P.A. Mulheran Department of Physics University of
Reading
2Simplistic Mesoscopic simulations (DDA)
3Scaling in the Island Size Distribution
4Capture Zones beyond mean field
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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
11Self-learning kinetic Monte Carlo simulation for
small island dynamics
12Island mobility parameters from self-learning KMC
13Some tetramer island dissociation pathways
discovered by the SL-KMC
14Island dissociation parameters from self-learning
KMC
15Enhanced DDA Simulation
- Lattice-based Monte Carlo simulation
16Enhanced DDA Simulation
- Lattice-based Monte Carlo simulation
- Deposition, Diffusion and Aggregation of monomers
17Enhanced 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
18Enhanced 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
19Enhanced 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
20Enhanced 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
21DDA simulations T300, D1/F 2e8
22DDA simulations T300, D1/F 2e8
Diffusion only
23DDA simulations T300, D1/F 2e8
Dissociation only
Diffusion only
24DDA simulations T600, D1/F 2e8
25DDA simulations T600, D1/F 2e8
Diffusion only
26DDA simulations T600, D1/F 2e8
Diffusion only
Dissociation only
27Kinetic Phase Diagram
- Can we predict what the dominant growth process
is for a given temperature and deposition rate?
28Kinetic 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
29Kinetic 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
30n1 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
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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
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39Theory 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
41Improving order in the JPD with temperature
42Variance of JPD with coverage test of scaling