“…e) MO calculations suggests 140 ± 30 mJ m -2 (Douillard and Henry, 2003). f) If the enthalpies of formation of the interfaces ∆H surf are proportional with the enthalpies of the corresponding phase transformations (Table 2) as shown in Fig.2.…”
Section: Electronic Annexmentioning
confidence: 97%
“…∆S vap = 119-122 J mol -1 K -1 in the range T = 298-273 K (Table 2). B) For the ice-gas interface, the entropy change in Table 3 has been calculated by combining the experimental surface Gibbs free energy G surf or γ (Vanoss et al, 1992) with a computationally-derived surface enthalpy H surf (Douillard and Henry, 2003). Applying ∆G surf = ∆H surf -T ∆S surf , the resulting molar surface entropy is 15 J mol -1 K -1 at a H 2 O surface density of N H2O = 9.8 nm -2 at 273 K. The calculated surface entropy for the ice-vapor interface is also low but it is larger than for the water-vapor interface ( Table 3).…”
“…e) MO calculations suggests 140 ± 30 mJ m -2 (Douillard and Henry, 2003). f) If the enthalpies of formation of the interfaces ∆H surf are proportional with the enthalpies of the corresponding phase transformations (Table 2) as shown in Fig.2.…”
Section: Electronic Annexmentioning
confidence: 97%
“…∆S vap = 119-122 J mol -1 K -1 in the range T = 298-273 K (Table 2). B) For the ice-gas interface, the entropy change in Table 3 has been calculated by combining the experimental surface Gibbs free energy G surf or γ (Vanoss et al, 1992) with a computationally-derived surface enthalpy H surf (Douillard and Henry, 2003). Applying ∆G surf = ∆H surf -T ∆S surf , the resulting molar surface entropy is 15 J mol -1 K -1 at a H 2 O surface density of N H2O = 9.8 nm -2 at 273 K. The calculated surface entropy for the ice-vapor interface is also low but it is larger than for the water-vapor interface ( Table 3).…”
“…It has been applied with success to the analysis of crystal structure of silicas [17], to hydrogen bonding in supramolecular assemblies [18] and more particularly to the calculation of the surface energy of ice [19] and of some clays, both of industrial [20] and of theoretical [21] interest. This method is very similar to the classic calculation of lattice energy, but uses the partial charges instead of the ionic charges.…”
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