Carbonate
(CO3) interacts with Fe-(hydr)oxide nanoparticles,
affecting the availability and geochemical cycle of other important
oxyanions in nature. Here, we studied the carbonate–phosphate
interaction in closed systems with freshly prepared ferrihydrite (Fh),
using batch experiments that cover a wide range of pH values, ionic
strength, and CO3 and PO4 concentrations. The
surface speciation of CO3 has been assessed by interpreting
the ion competition with the Charge Distribution (CD) model, using
CD coefficients derived from MO/DTF optimized geometries. Adsorption
of CO3 occurs predominately via formation of bidentate
inner-sphere complexes, either (≡FeO)2CO or (≡FeO)2CO··Na+. The latter complex is electrostatically
promoted at high pH and in the presence of adsorbed PO4. Additionally, a minor complex is present at high CO3 loadings. The CD model, solely parametrized by measuring the pH-dependent
PO4 adsorption as a function of the CO3 concentration,
successfully predicts the CO3 adsorption to Fh in single-ion
systems. The adsorption affinity of CO3 to Fh is higher
than to goethite, particularly at high pH and CO3 loadings
due to the enhanced formation (≡FeO)2CO··Na+. The PO4 adsorption isotherm in 0.5 M NaHCO3 can be well described, being relevant for assessing the reactive
surface area of the natural oxide fraction with soil extractions and
CD modeling. Additionally, we have evaluated the enhanced Fh solubility
due to Fe(III)-CO3 complex formation and resolved a new
species (Fe(CO3)2(OH)23−(aq)), which is dominant in closed systems at high pH. The measured
solubility of our Fh agrees with the size-dependent solubility predicted
using the surface Gibbs free energy of Fh.