Calcite
is the most stable polymorph of calcium carbonate (CaCO3) under ambient conditions and is ubiquitous in natural systems.
It plays a major role in controlling pH in environmental settings.
Electrostatic phenomena at the calcite–water interface and
the surface reactivity of calcite in general have important environmental
implications. They may strongly impact nutrient and contaminant mobility
in soils and other subsurface environments, they control oil recovery
from limestone reservoirs, and they may impact the safety of nuclear
waste disposal sites. Besides the environmental relevance, the topic
is significant for industrial applications and cultural heritage preservation.
In this study, the structure of the calcite(104)–water interface
is investigated on the basis of a new extensive set of crystal truncation
rod data. The results agree with recently reported structures and
resolve previous ambiguities with respect to the coordination sphere
of surface Ca ions. These structural features are introduced into
an electrostatic three-plane surface complexation model, describing
ion adsorption and charging at the calcite–water interface.
Inner surface potential data for calcite, as measured with a calcite
single-crystal electrode, are used as constraints for the model in
addition to zeta potential data. Ion adsorption parameters are compared
with molecular dynamics simulations. All model parameters, including
protonation constants, ion-binding parameters, and Helmholtz capacitances,
are within physically and chemically plausible ranges. A PhreeqC version
of the model is presented, which we hope will foster application of
the model in environmental studies.