In
this study, the adsorption process of Cr(VI) on the hematite
facets was systematically investigated with synchrotron-based Cr K-edge
extended X-ray absorption fine structure (EXAFS) spectroscopy, in
situ attenuated total reflectance Fourier transform infrared (ATR-FTIR)
spectroscopy, density-functional theory calculation, and surface complexation
models. Structural model fitting of EXAFS spectroscopy suggested that
the interatomic distances of Cr–Fe were, respectively, 3.61
Å for the chromate coordinated hematite nanoplates with exposed
{001} facets, 3.60 and 3.30 Å for the chromate coordinated hematite
nanorods with exposed {001} and {110} facets, which were characteristic
of inner-sphere complexation. In situ ATR-FTIR spectroscopy analysis
confirmed the presence of two inner-sphere surface complexes with
C3ν and C2ν symmetry, while the
C3ν and C2ν species were assigned
to monodentate and bidentate inner-sphere surface complexes with average
Cr–Fe interatomic distances of 3.60 and 3.30 Å, respectively.
On the basis of these experimental and theoretical results, we concluded
that HCrO4– as dominated Cr(VI) species
was adsorbed on {001} and {110} facets in inner-sphere monodentate
mononuclear and bidentate binuclear configurations, respectively.
Moreover, the Cr(VI) adsorption performance of hematite facets was
strongly dependent on the chromate complexes formed on the hematite
facets.