Selenite Uptake by Ca–Al LDH: A Description of Intercalated Anion Coordination Geometries

Layered double hydroxides (LDHs) are anion exchangers with a strong potential to scavenge anionic contaminants in aquatic environments. Here, the uptake of selenite (SeO 3 2– ) by Ca–Al LDHs was investigated as a function of Se concentration. Thermodynamic modeling of batch sorption isotherms shows that the formation of SeO 3 2– -intercalated AFm (hydrated calcium aluminate monosubstituent) phase, AFm-SeO 3, is the dominant mechanism controlling the retention of Se at medium loadings. AFm-Cl 2 shows much stronger affinity and larger distribution ratio ( R d ∼ 17800 L kg –1 ) toward SeO 3 2– than AFm-SO 4 ( R d ∼ 705 L kg –1 ). At stoichiometric SeO 3 2– loading for anion exchange, the newly formed AFm-SeO 3 phase results in two basal spacing, i.e., 9.93 ± 0.06 Å and ∼11.03 ± 0.03 Å. Extended X-ray absorption fine structure (EXAFS) spectra indicate that the intercalated SeO 3 2– forms inner-sphere complexes with the Ca–Al–O layers. In situ X-ray diffraction (XRD) shows that basal spacing of Ca–Al LDHs have a remarkable linear relationship with the size of hydrated intercalated anions (i.e., Cl –, SO 4 2–, MoO 4 2–, and SeO 3 2– ). Contrary to AFm-SeO 3 with inner-sphere SeO 3 2– complexes in the interlayer, the phase with hydrogen-bonded inner-sphere complexed SeO 3 2– is kinetically favored but thermodynamically unstable. This work offers new insights about the determination of intercalated anion coordination geometries via XRD analyses.