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Metropolis-type evolution rules for surface growth models

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Presentation on theme: "Metropolis-type evolution rules for surface growth models"— Presentation transcript:

1 Metropolis-type evolution rules for surface growth models
with the global constraints on one and two dimensional substrates Yup Kim, H. B. Heo, S. Y. Yoon KHU

2 1. Motivation In equilibrium state,
Normal restricted solid-on-solid model : Edward-Wilkinson universality class Two-particle correlated surface growth - Yup Kim, T. S. Kim and H. Park, PRE 66, (2002) Dimer-type surface growth J. D. Noh, H. Park, D. Kim and M. den Nijs, PRE 64, (2001) - J. D. Noh, H. Park and M. den Nijs, PRL 84, 3891 (2000) Self-flattening surface growth -Yup Kim, S. Y. Yoon and H. Park, PRE(RC) 66, (R) (2002)

3 nh : the number of columns with height h
2 Partition function, nh : the number of columns with height h Steady state or Saturation regime , 1. Normal RSOS (z =1) Normal Random Walk (1D) (EW) 2. Two-particle correlated (dimer-type) growth (z = -1) nh=even number, Even-Visiting Random Walk (1D)

4 ? ? 3. Self-flattening surface growth (z = 0)
Self-attracting random walk (1D) Phase diagram (1D) z = 0 z = 1 z =-1 Normal Random Walk Even-Visiting ? Self-attracting z Phase diagram (2D) z = 0 z = 1 z =-1 Normal Random Walk Even-Visiting ? Self-attracting z

5 2. Generalized Model Evaluate the weight
4 2. Generalized Model ( nh : the number of sites which have the same height h ) Evaluate the weight in a given height configuration Choose a column randomly. Decide the deposition (the evaporation) attempt with probability p (1-p) Calculate for the new configuration from the decided deposition (evaporation) process Acceptance parameter P is defined by

6 If P  1 , then new configuration is accepted unconditionally.
5 If P  1 , then new configuration is accepted unconditionally. If P < 1 , then new configuration is accepted only when P  R. where R is generated random number 0< R < 1 (Metropolis algorithm) Any new configuration is rejected if it would result in violating the RSOS contraint ( a primitive lattice vector in the i – th direction ) P  R hmax hmin p =1/2 L = 10 z = 0.5 n+2 = 1 n+1 = 3 n 0 = 2 n-1 = 2 n-2 = 2 w n´ +2 = 2 n´ +1 = 2 n´ 0 = 2 n´ -1 = 2 n´ -2 = 2

7  Equilibrium model (1D, p=1/2)
6 3. Simulation Results  Equilibrium model (1D, p=1/2)

8 7 0.22 0.33 1.1 0.9  0.19  0.22 1/4  0.33  0.34 1/2  (L) -1 -0.5 0.5 1 1.5 z

9  Equilibrium model (2D, p=1/2)
7  Equilibrium model (2D, p=1/2) z -1 -0.5 0.5 1 1.5 a 0.176 0.175 0.179

10 Scaling Collapse to in 2D equilibrium state.
7 Scaling Collapse to in 2D equilibrium state. , Z = 2.5

11 Phase diagram in equilibrium (1D)
7 Phase diagram in equilibrium (1D) z =-1 -1/2 z = 0 1/2 z = 1 3/2 z = 0.9 z = 1.1 2-particle corr. growth Self-flattening surface growth Normal RSOS Phase diagram in equilibrium (2D) z z =-1 z = -0.5 z = 0 z = 0.5 z = 1 z = 1.5 Even-Visiting Random Walk Self-attracting Random Walk Normal Random Walk

12 Growing (eroding) phase (1D, p=1(0) )
9 Growing (eroding) phase (1D, p=1(0) ) z  0 : Normal RSOS model (Kardar-Parisi-Zhang universality class) p  (L) 1.5  0.52 0.5  0.51  0.49

13 10 z  0 Normal RSOS Model (KPZ)

14 11 z  0 z=-0.5 p=1 L=128

15  Equilibrium model (1D, p=1/2)
12 4. Conclusion  Equilibrium model (1D, p=1/2) z -1 -1/2 1/2 0.9 1 1.1 3/2 2-particle corr. growth (EVRW) Self-flattening surface growth (SATW) Normal RSOS (Normal RW) Growing (eroding) phase (1D, p = 1(0) ) 1. z  0 : Normal RSOS model (KPZ universality class) 2. z  0 : Groove phase ( = 1) Phase transition at z=0 (?)

16 Scaling Collapse to in 1D equilibrium state. ( = 1/3 , z = 1.5)
12-1 Scaling Collapse to in 1D equilibrium state. ( = 1/3 , z = 1.5)

17 Monomer & Extremal & Dimer & 2-site
7 Monomer & Extremal & Dimer & 2-site 0.175 0.162 Dimer Monomer Slope a Model Extremal 0.174 2-site


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