REEXAMINATION OF THE SCALING OF HOMOGENEOUS NUCLEATION RATES FOR WATER B. N. HALE1 Physics Department and Cloud & Aerosol Science Laboratory, Missouri University of Science & Technology, Rolla, MO 65409 U. S. A 1 Keywords: NUCLEATION, SCALING, WATER, EXPERIMENT, THEORY INTRODUCTION The temperature dependent scaling of the homogeneous nucleation rate, J, offers a comprehensive comparison of rates over a range of temperature ratios, T/Tc (where Tc is the critical temperature) and supersaturation ratios, S = P/P₀ (where P and P0 are the ambient and equilibrium vapor pressures). Experimental rates are often obtained via physically different background processes while the theoretical predictions range from classical analyses to Monte Carlo (MC) and Molecular Dynamics (MD) computer simulations with several choices of effective pair potentials. The scaling plot enables one to examine all these data simultaneously using two parameters: , the excess surface entropy per molecule (in units of k, the Boltzmann constant) and the critical temperature for the substance or the model potential in the case of the theoretical predictions. We examine here the scaling plot for water (Hale, 2004) and (Wyslouzil and Wölk, 2016) together with recent MD (Tanaka, 2014), (Angelil, 2015) and MC predictions at higher rates (Hale and DiMattio, 2017). The latter higher rates place the physical process in the realm of smaller critical cluster sizes where the discreteness of the cluster size can play a significant role and affect the scaling exponents. THE SCALING PLOT In the scaling plot (Hale, 2004) -log [J/JS] is plotted vs. the scaled free energy of formation (Hale, 1986) [16π/3] Ω³ [Tc/T-1]³/(lnS)² where JS is a typical monomer flux factor times the monomer number density -- often taken to be 10²⁶ in the cgs system of units. The excess surface entropy per molecule, Ω, is approximately 1.5 for substances with a dipole moment and 2.0 for normal substances. The scaling plot for the experimental and theoretical water data is shown in Fig. 1. MC NUCLEATION RATES FOR THE TIP4P POTENTIAL MODEL AT LARGE SUPERSATURATION RATIOS In the interest of generating Monte Carlo simulation based nucleation rates near 1023 cm-3s-1 the free energy differences for small TIP4P clusters (Hale and DiMattio, 2004) at 260K, 280K and 300K (see Fig. 2) are used to predict nucleation rates at high supersaturation ratios. The results are added to Fig. 1. Details of this process are in (Hale, 2010). The predicted nucleation rates are given in Table I. Table I T/K S J/cm-3s-1 260 260 260 260 260 260 260 260 260 6 6.2 6.4 6.6 6.8 18.7 46 10.4 150 2.70E+09 1.52E+10 6.71E+10 2.44E+11 2.44E+11 1.45E+20 3.32E+23 2.77E+16 1.40E+26 T/K S J/cm-3s-1 T/K S J/cm-3s-1 280 280 280 280 280 280 280 280 4.3 4.5 4.7 4.9 5.1 9.7 19.2 6.3 1.85E+09 4.83E+10 7.97E+11 8.24E+12 5.57E+13 1.86E+20 3.74E+23 5.26E+16 300 300 300 300 300 300 300 300 3.5 3.6 3.7 3.8 3.9 5.9 9.9 4.4 2.45E+11 2.11E+12 1.53E+13 9.31E+13 4.70E+14 2.54E+20 4.33E+23 1.68E+17 Fig.1. Homogeneous nucleation rates, J, for water vs. the scaled free energy of formation. Much of the data in this plot was presented in Fig. 12 of (Wyslouzil and Wölk, 2016) who generously shared data files for creating the present figure which now includes data for the MD generated nucleation rates, (Tanaka et al, 2014), (Angelil et al. 2015), (Dumitrescu et al. 2017) and MC generated nucleation rates (Hale and DiMattio, 2017). See Fig. 10 of (Wyslouzil and Wölk, 2016) for remaining data sources identified at the side. Fig 2. Helmholtz free energy differences for small TIP4P clusters scaled with [Tc/T – 1] (Hale and DiMattio, 2004). The -f = ln[Q(n)/(Q(n-1)Q(1)vn/V)] where Q(n) are the n- cluster canonical configuration integrals and vn and V are the small n-cluster volume and system volumes respectively. The free energy differences are calculated via the Bennett technique. See (Hale, 2010) for additional formalism details. COMMENTS AND CONCLUSIONS For inclusion in Fig. 1 the nucleation rates in Table I were plotted vs. the scaled energy of formation using the literature reported value of the critical temperature for TIP4P, Tc = 588K (Vega, 2011). There was no convincing value of Tc with which the free energy differences scaled in the Monte Carlo simulations. For purposes of demonstrating the scaling analysis Tc = 588K is used in Fig 2. It is essential to note the importance of the intercept at infinite n cluster size in Fig. 2. This intercept is equal to ln [liquid/vapor monomer] and enters crucially into the determination of the n-cluster number density and subsequently the nucleation rate. Scaling does not occur unless this intercept reliably reproduces the ratio of liquid to vapor monomer number densities, with the correct temperature dependence. See (Hale, 2010) for further details. The TIP4P data points in Fig. 1 from the present MC analysis appear to agree reasonably with the results of (Merikanto et al.2004) and surprisingly with a range of experimental data points. A feature of note is that the present TIP4P MC nucleation rates appear to have an slightly larger than 1.47. At high nucleation rates the TIP4P MC data points are consistent with the MD results of (Dumitrescu et al. 2017) and not far from the MD results for the SPC/E potential (Tanaka et al, 2014) and (Angelil et al., 2015). Angelil et al. have found an exponent of 1.7 at high nucleation rates whereas the experimental data at lower rates are more aligned with the 3/2 value. This very interesting result will no doubt have important consequences in understanding the role which the effective potential model and the critical cluster size play in the scaling analysis. REFERENCES Angelil, R., Diemand, J., Tanaka, K. K., and Tanaka, H. (2015), Homogeneous SPC/E water nucleation in large molecular dynamics simulations, J. Chem. Phys. 143, 064507. Dumitrescu, L. R., Smeulders, D. M. J., Dam, J. A. M., Gaastra-Nedea, S. V.(2017), Homogeneous nucleation of water in argon. Nucleation rate computation from molecular simulation of TIP4P and TIP4P/2005 water model, accepted for publication, J. Chem. Phys. 2017 Hale, B. N. (1986), Application of a scaled homogeneous nucleation-rate formalism to experimental data at T << Tc, Phys. Rev A 33, 4156. Hale, B. N. (1992), The Scaling of Nucleation Rates, Metallurg. 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