Mössbauer Studies of Lattice Dynamics, Fine and Hyperfine Structure of DivalentFe57in FeF2

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Abstract
Mössbauer studies of the isomer shift, recoil-free fraction, and quadrupole splitting for Fe57 in FeF2 between 80 and 300°K are reported. The temperature dependence of the isomer shift and recoil-free fraction are well explained within the harmonic approximation. The ascertained sum of the microscopic force constants acting on the Fe++ ion is K=(1.24±0.07)×105 dyn/cm. The weighted frequency average associated with the classical mean-square displacement of the Fe57 is 〈1ω2〉−12=(2.08±0.05)×1013 sec−1. Analysis of the quadrupole splitting, coupled with an analysis of the magnetic behavior by Lines, leads to a reassessment of the measurable effects of covalency upon the crystal-field, spin-orbit, and hyperfine interaction. The spin-orbit coupling parameter is estimated to be λ=−85 cm−1. Using this value for the spin-orbit coupling parameter, the resulting crystal-field splitting of the T25 orbital levels which describe the temperature dependence of the quadrupole splitting are Δ1=780±40 cm−1 and Δ2=930±70 cm−1. The 〈r−3〉eff=3.0±0.3a0−3 for the d electrons and the contact contribution to the internal field at 4.2°K is Hc=−518±25 kOe.

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