Jr. Rustad et al., Molecular modeling of the surface charging of hematite - II. Optimal proton distribution and simulation of surface charge versus pH relationships, SURF SCI, 424(1), 1999, pp. 28-35
A parameterized classical potential model for the interaction of water and
hydroxide with iron oxide was used to calculate the optimal proton arrangem
ent and proton binding energies on the (012) surface of hematite. Energy mi
nimization calculations with the parameterized potential model indicate tha
t approximately 75% of adsorbed water molecules are dissociated on this sur
face, in agreement with recent TPD and HREELS measurements. Surface protona
tion/deprotonation energies were calculated from the predicted optimal arra
ngement of protons on the neutral (012) surface. A supercell geometry with
translational symmetry in two dimensions and finite in the third dimension
(2-D PBC) was assumed. The calculated surface protonation energies were the
n used to model the experimentally observed surface-charging curve of hemat
ite in aqueous solution. Excellent agreement was found between the calculat
ed and measured surface charge for ionic strengths ranging from 0.001 to 0.
1 M. Our calculations favor the value of 8.5 for the pH of zero charge of h
ematite over the more recent result of 6.7. (C) 1999 Elsevier Science B.V.
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