Mössbauer Study of Magnetic States of KFeF3and Implications for RbFeF3

Abstract
Mössbauer absorption spectra of Fe57 in an unstrained {100} single-crystal platelet of KFeF3 have been measured between 297 and 4.2 °K. The transition to the trigonal antiferromagnetic state occurred at TN=112.5±0.5 °K. The relaxation effects reported near TN in a previous study were absent, but spectra of a strained crystal provided evidence of strong magnetoelastic interactions. A transition to a lower-symmetry weak ferromagnetic phase was found at TR=36.6±0.5 °K. At 4.2 °K the magnetic hyperfine field is Hhf=182.4±0.5 kOe, and the magnitude of the quadrupole splitting is |ΔEQ|=1.97±0.05 mm/sec. Analysis of the data in the antiferromagnetic phase indicates the spin alignment is parallel to the 〈111〉 distortion. The temperature dependence Hhf and ΔEQ in this phase is compared with predictions of self-consistent molecular-field-theory calculations. Only fair agreement is found with the magnetically induced electric-field-gradient (EFG) model, which describes the Fe2+ ions by a Hamiltonian incorporating free-ion terms, a cubic crystal field, and an exchange interaction. A substantially better fit is obtained with a second model which adds to this Hamiltonian an axial distortion term (δ3)(Lz22), where δ is zero above TN and varies below TN as (1TTN)γ, with γ=12 or 13. Application of this second model to the tetragonal antiferromagnetic state of RbFeF3 indicates that the spins align parallel to a 〈100〉 direction rather than the 〈111〉 direction predicted previously by use of the magnetically induced EFG model. The sign obtained for the axil-distortion parameter δ in RbFeF3 is inconsistent with an analysis which attributes the cubic-to-axial transformation to Jahn-Teller stabilization effects.