Raman spectra of concentrated aqueous solutions of ferric chloride were recorded in the spectral range 50 to 500 cm −1 . In near-saturated solutions, spectra show a four-line pattern typical of the tetrahedral FeCl 4 – complex: 390 cm −1 (w); 335 cm −1 (vs, p); 135 cm −1 (w); 110 cm −1 (s). At lower concentrations a new species dominates the spectrum, showing characteristic Raman lines at 318 cm −1 (s, p) and 165 cm −1 (vw). Conventional investigations of spectral changes with concentration of Fe(III) and chloride, coupled with group theoretical arguments, indicate that the stoichiometry of the complex must be FeCl 3 or lower. Of the several symmetries that a FeCl 3 complex might assume (C 2v , C 3v , D 2h (dimer), and D 3h ), the D 3h trigonal bipyramid structure FeCl 3 ·2H 2 O with three equatorial chloride ligands and two axial waters is most compatible with the spectral evidence.
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Marston et al. (1972) studied this question.
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