The
adsorption of small molecules containing two different organic
functional groups at terrace and step sites on the {101̅4} surface
of calcite at the interface with aqueous solution was studied using
free energy methods. For comparison, the adsorption free energies
of the component ions of calcium carbonate were also determined at
the same sites. Polarizability was taken into account through using
a force field developed for calcium carbonate based on the AMOEBA
model that contains static multipoles and self-consistent induced
dipoles. The influence of including polarization was examined by comparing
to data obtained with a fixed charge rigid-ion model. The strong hydration
layers above the basal plane of calcite were shown to hinder the direct
attachment of the small species studied, including the constituent
ions of the mineral. Only the species bearing an amino group, namely,
methylammonium and glycine, demonstrated favorable adsorption free
energies. The ability of amino groups to more readily pass through
the hydration layers than carboxylate and carbonate groups can be
explained by their weaker solvation free energies, while the carbonate
ions within the calcite surface with which they bind are also less
strongly hydrated than calcium ions. Acetate, glycine, and methylammonium
were all found to be able to directly bind to one growth site at the
acute step of calcite. This is at variance with results obtained with
a rigid-ion model in which all binding free energies are endergonic.
Thus, including polarization allows for a description of the adsorption
process that is more consistent with experimental observations, particularly
at calcite steps, and for determination of more reliable atomic-scale
mechanisms for calcite growth and its modification by organic additives.
Even with polarization, the organic functional groups considered only
exhibit moderate binding to calcite steps with adsorption free energies
not exceeding −13 kJ/mol.