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Computer Simulations, Scaling and the Prediction of Nucleation Rates

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1 Computer Simulations, Scaling and the Prediction of Nucleation Rates
Barbara Hale Physics Department and Cloud and Aerosol Sciences Laboratory University of Missouri – Rolla Rolla, MO USA

2 Nucleation : formation of embryos of the new phase from the metastable (supersaturated) parent phase
K. Yasuoka and M. Matsumoto, J. Chem. Phys. 109, 8451 (1998)

3 “Molecular dynamics of homogeneous nucleation in the vapor phase: Lennard-Jones fluid”, K. Yasuoka and M. Matsumoto, J. Chem. Phys. 109, 8451 (1998);

4 Estimating the nucleation rate, J, from the molecular dynamics simulation at T = 80.3K. Supersaturation ratio = P/Po = 6.8 vol. = ( 60 x 60 x 60) 3;

5 Nucleation is a non-equilibrium process!
●There is no “first principles” theory from which to determine the nucleation rate. ● Most models attempt to treat nucleation as the decay of a near-equilibrium metastable (supersaturated) state. ● The classical nucleation theory (CNT) model was first developed in by Volmer and Weber, and by Becker and Döring in …. following a proposal by Gibbs. ● CNT treats nucleation as a fluctuation phenomenon in which small embryos of the new phase overcome free energy barriers and grow irreversibly to macroscopic size.

6 Classical Nucleation Theory
(vapor-to-liquid) Jclassical = [N1 v 4rn*2/3 ] · Nn* = [Monomer flux] · [# Critical Clusters/Vol.]

7 Estimating Nn Nn / N1 = exp [–Work of formation / kT]
Work of formation of cluster from vapor: W(n) = 4 rn2  n kT ln S S = P/Po

8 n* = critical sized cluster has equal probability of growing or decaying

9 n* = critical sized cluster
at n = n*: dW(n) / dn = 0 Let W(n) = An2/3 -nlnS where A = [36]1/3 liq-2/3  /kT liq= liquid number density

10 Volume / Surface in W(n*)
d/dn [ An2/3 - nlnS]n* = 0 (2/3)A n*-1/3 = lnS n* = [2A/ 3lnS]3 W(n*) /kT = ½ n* lnS = [16/3] [/(liq2/3 kT) ]3 / [lnS]2 liq= liquid number density

11 Classical Nucleation Rate
(T)  a – bT is the bulk liquid surface tension ;

12 Homogeneous Nucleation rate data for water: classical nucleation rate model has wrong T dependence

13 Motivation for Scaling J at T << Tc
The CNT nucleation rate depends exponentially on (T)3 / [ln (P/Po(T))]2 . To obtain a physically realistic T dependence of J, a good starting point is to require functional forms for (T) and Po(T) which reflect “universal” properties of surface tension and vapor pressure.

14 Scaling of the surface tension at T << Tc
Assume a scaled form for :  = o’ [Tc- T]  with  =1 for simplicity. Many substances fit this form and the critical exponent (corresponding to ) is close to 1.  = excess surface entropy per molecule / k  2 for normal liquids  for substances with dipole moment (a law of corresponding states result; Eötvös 1869)

15 Scaled Nucleation Rate at T << Tc B. N. Hale, Phys
Scaled Nucleation Rate at T << Tc B. N. Hale, Phys. Rev A 33, 4156 (1986); J. Chem. Phys. 122, (2005) J0,scaled  [thermal (Tc)] -3 s-1 “scaled supersaturation”  lnS/[Tc/T-1]3/2

16 Water nucleation rate data of Wölk and Strey plotted vs
Water nucleation rate data of Wölk and Strey plotted vs. lnS / [Tc/T-1]3/2 ; Co = [Tc/240-1]3/2 ; Tc = K J. Chem. Phys. 122, (2005)

17 Toluene (C7H8) nucleation data of Schmitt et al plotted vs
Toluene (C7H8) nucleation data of Schmitt et al plotted vs. scaled supersaturation, Co = [Tc /240-1]3/2 ; Tc = 591.8K

18 Nonane (C9H20) nucleation data of Adams et al. plotted vs
Nonane (C9H20) nucleation data of Adams et al. plotted vs. scaled supersaturation ; Co = [Tc/240-1]3/2 ; Tc = 594.6K

19 for most materials (corresponding states)
Comparison of Jscaled with water data from different experimental techniques: plot log[J/J0,scaled] vs. J0,scaled  cm-3 s-1 for most materials (corresponding states)

20

21 Missing terms in the classical work of formation?

22 Monte Carlo Simulations
Ensemble B: n cluster with probe interactions normal Ensemble A: (n -1) cluster plus monomer probe interactions turned off Calculate f(n) =[F(n)-F(n-1)]/kT

23 Monte Carlo Helmholtz free energy differences for small water clusters: f(n) =[F(n)-F(n-1)]/kT B.N. Hale and D. J. DiMattio, J. Phys. Chem. B 108, (2004)

24 Nucleation rate via Monte Carlo
Calculation of Nucleation rate from Monte Carlo -f(n) : Jn = flux · Nn* Monte Carlo = [N1v1 4rn2 ] · N1 exp 2,n(-f(n´) – ln[liq/1o]+lnS) J = [n Jn ]-1 The steady-state nucleation rate summation procedure requires no determination of n* as long as one sums over a sufficiently large number of n values.

25 Monte Carlo TIP4P nucleation rate results for experimental water data points (Si,Ti)

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27 Comments & Conclusions
Experimental data indicate that Jexp is a function of lnS/[Tc/T-1]3/2 A “first principles” derivation of this scaling effect is not known; Monte Carlo simulations of f(n) for TIP4P water clusters show evidence of scaling; Temperature dependence in pre-factor of classical model can be partially cancelled when energy of formation is calculated from a discrete sum of f(n) over small cluster sizes. Can this be cast into more general formalism?

28 Molecular Dynamics Simulations
Solve Newton’s equations, mi d2ri/dt2 = Fi = -i j≠i U(rj-ri), iteratively for all i=1,2… n atoms; Quench the system to temperature, T, and monitor cluster formation. Measure J  rate at which clusters form


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