Uptake and molecular speciation of dissolved Hg during formation
of Al- or Fe-ettringite-type and high-pH phases were investigated
in coprecipitation and sorption experiments of sulfate-cement treatments
used for soil and sediment remediation. Ettringite and minor gypsum
were identified by XRD as primary phases in Al systems, whereas gypsum
and ferrihydrite were the main products in Hg–Fe precipitates.
Characterization of Hg–Al solids by bulk Hg EXAFS, electron
microprobe, and microfocused-XRF mapping indicated coordination of
Hg by Cl ligands, multiple Hg and Cl backscattering atoms, and concentration
of Hg as small particles. Thermodynamic predictions agreed with experimental
observations for bulk phases, but Hg speciation indicated lack of
equilibration with the final solution. Results suggest physical encapsulation
of Hg as a polynuclear chloromercury(II) salt in ettringite as the
primary immobilization mechanism. In Hg–Fe solids, structural
characterization indicated Hg coordination by O atoms only and Fe
backscattering atoms that is consistent with inner-sphere complexation
of Hg(OH)20 coprecipitated with ferrihydrite.
Precipitation of ferrihydrite removed Hg from solution, but the resulting
solid was sufficiently hydrated to allow equilibration of sorbed Hg
species with the aqueous solution. Electron microprobe XRF characterization
of sorption samples with low Hg concentration reacted with cement
and FeSO4 amendment indicated correlation of Hg and Fe,
supporting the interpretation of Hg removal by precipitation of an
Fe(III) oxide phase.