Supplementary Material to: Vapor deposition of water on graphitic surfaces: formation of amorphous ice, bilayer ice, ice I and liquid water. Laura Lupi, Noah Kastelowitz and Valeria Molinero A. Calculation of the line tension of mW water on graphite. We calculated the line tension for water in contact with graphite for the size dependence of the contact angle through1,2 cos π = cos π∞ − πΎ π 1 πΏπ π π , (S1) where π is the contact angle of microscopic droplets, π∞ is the contact angle in the limit of very large droplets, π is the line tension, πΎπΏπ is the liquid-vapor surface tension, and π π is the radius of the circumference of contact between the droplet and the surface. The surface tension of mW water droplets with diameters as small as 1 nm was found to be independent on curvature,3 therefore in our calculations we approximated the liquid-vapor surface tension ∞ of the spherical interface with πΎπΏπ (this was taken from ref. 4 at 220 K for mW water). 1 Through linear fitting of cos π versus π of the data of Table 1 we determined cos π∞ = 85° π and π = 12 pN for water in contact with graphite (Figure S1). Table 1. Contact angles, ο±ο¬ο and radius of base, Rb, of droplets containing Nw water molecules in contact with graphite. Nw ο± (°) Rb (nm) 550 89 1.9 1035 87 2.5 5241 86 4.2 1 cos (q) 0.06 Tf droplet 0.04 0.02 0.2 0.3 0.4 1/Rb (1/nm) 0.5 Figure S1. Cosine of the contact angle of mW water on graphite as a function of inverse droplet radius. Blue symbols are the data points and the blue line is the linear fit of the data using equation 1. B. Bilayer ice and graphitic surfaces lattice. Bilayer ice and graphitic sheets have hexagonal symmetry with a lattice domain mismatch of only 3% when two cells of the graphitic surface are compared with one cell of bilayer ice. Nevertheless, we do not observe alignment between the two structures even for the most attractive surfaces of this study. Snaphots of bilayer ice on these graphitic surfaces are shown in Figures S2 to S4. 2 Figure S2. Bilayer ice deposited on graphite at T = 180 K. The first layer of water molecules from the surfaces is showed with red sticks, the second in blue, carbon atoms of the graphite surface are shown in silver. Only the first layer of water is shown in left panel, and both layers are shown in right panel. Figure S3. Bilayer ice deposited on graphitic surface with ε = 0.16 kJ/mol at T = 200 K. The first layer of water molecules from the surfaces is showed with red sticks, the second in blue, carbon atoms of the graphite surface are shown in silver. Only the first layer of water is shown in left panel, and both layers are shown in right panel. 3 Figure S4. Bilayer ice deposited on graphitic surface with ε = 0.18 kJ/mol at T = 210 K. The first layer of water molecules from the surfaces is showed with red sticks, the second in blue, carbon atoms of the graphite surface are shown in silver. Only the first layer of water is shown in left panel, and both layers are shown in right panel. Supporting References. (1) (2) (3) 4508 (2014). (4) J. Wang; S. Betelu; B. Law, Phys. Rev. E 63, 031601 (2001). A. I. Rusanov, Surf. Sci. Rep. 23, 173 (1996). M. H. Factorovich; V. Molinero; D. A. Scherlis, J. Am. Chem. Soc. 136, A. Hudait; V. Molinero, J. Am. Chem. Soc. 136, 8081 (2014). 4