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The following statement is incorrect with respect to 57Fe Mössbauer spectra of FeCl3.6H2O and FeCl2.4H2O :

  • A.Both the compounds show doublet with equal quadrupole splitting
  • B.Both are compounds show doublet with unequal quadrupole splitting
  • C.Both the compounds are high spin complexes of Fe(II) and Fe(III) respectively
  • D.Valence contribution is present in \(\mathrm{FeCl_{2}.4H_{2}O}\) while lattice contribution is present in \(\mathrm{FeCl_{3}.6H_{2}O}\)

Answer: A

The incorrect statement is (A): the two compounds do not show equal quadrupole splitting.

Quadrupole splitting measures the electric field gradient at the iron nucleus, and in both compounds the I = 3/2 excited state splits into two levels, so each gives a doublet. FeCl3.6H2O contains high-spin Fe(III), d5, whose half-filled t2g3eg2 shell is spherical, so the valence electrons add no field gradient and only the lattice (ligand) contribution acts: the splitting is small. FeCl2.4H2O contains high-spin Fe(II), d6, whose extra electron sits in a non-spherical d orbital and adds a large valence contribution, so its splitting is much larger. The splittings are therefore unequal, which makes (B) true, and (D) states exactly this valence versus lattice difference.

Statement (C) is true in substance: both salts are high-spin, and the pair is one Fe(III) and one Fe(II) complex. As printed, 'respectively' pairs Fe(II) with the first formula, FeCl3.6H2O, which is the wrong way round; the question evidently means only the pair of oxidation states, so (A), false on any reading, is the answer. The splitting values themselves are not quoted here; the argument rests on the d5 versus d6 electronic structure.

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