"Orbital Ground State Inversion in [Fe(H<sub>2</sub>O)<sub>6</sub>](ClO" by W. M. Reiff, Richard B. Frankel et al.
 

Abstract

Mössbauer spectroscopy in external magnetic fields has been used to measure the signs of the principal components of the electric field gradient Vzz in the two forms of [Fe(H2O)6)(Cl04)2. The signs are Vzznegative for low temperature form (A) with quadrupole splitting ΔEA = 3.4 mm/sec, and Vzz positive for high temperature form (B) with ΔEB = 1.4 mm/sec. This implies a trigonally distorted ligand field and the transition (A) → (B) corresponds to compression → elongation with respect to the trigonal axis.

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Physics

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URL: https://digitalcommons.calpoly.edu/phy_fac/221