1969 Volume 26 Issue 3 Pages 674-680
Neutron inelastic scattering experiments show that the phase transition of KMnF3 at 184°K is a result of the softening of the Γ25 phonon mode at the [111] zone boundary. The over-all characteristics of the Γ25 mode are similar to those that have been observed for this same mode in SrTiO3 near its 110°K phase transition. We also observe that the M3 mode at the [110] zone boundary has the very low energy of 3.1±0.2 MeV at room temperature, and condenses not at 184°K but rather in the vicinity of its Néel temperature, 88°K. The X-ray studies by Beckman and Knox indicate that the space group of KMnF3 below 184°K is the orthorhombic PbnmD(2h16). This orthorhombic phase is consistent with our observation that the Γ25 mode is responsible for the 184°K transition in that the dominant contribution to the rotation of the fluorine octahedra is a superposition of two of the three triply degenerate modes of Γ25 condensing at the transition temperature.
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