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
C<sub>3ν</sub> and C<sub>2ν</sub> symmetry, while the
C<sub>3ν</sub> and C<sub>2ν</sub> 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 HCrO<sub>4</sub><sup>–</sup> 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.