Abstract
The 57Fe spectrum of the title cationic sandwich compound has been recorded at various temperatures in the range 4.2–350 K. At low temperatures it consists of a simple quadrupole doublet and a magnetically perturbed spectrum at 4.2 K reveals that Vzz is positive. At T 273 K additional absorption to low energy is observed. As the temperature is increased a four-peak spectrum gradually develops which has an inner quadrupole doublet of magnitude approximately half that of the outer doublet. The spectrum is fully developed at 321 K but further heating brings about an inward collapse onto a single peak of much reduced intensity. This critical temperature is associated with a phase change of the solid. These processes are reversible. A model has been developed to account for the variation of spectrum with temperature. The organometallic cation is assumed to lie at an eight-co-oridnate site made up of eight PF6 groups. At low temperatures the symmetry axis of the cation is collinear with the Z axis of the tetragon. As the temperature is raised, the X and Y orientations are Boltzmann populated and jump reorientations XY take place at a significant rate giving rise to the inner doublet. These reorientations become faster with increasing temperature and on further heating those from ZX and ZY become significant on the Mössbauer time scale and the spectrum becomes broadened and confused. Finally, all reorientations are so rapid that the cation is effectively spherical: this brings about a catharsis for the tetragonal phase in the form of a transition to one of cubic symmetry and the Mössbauer spectrum collapses to a narrow single peak.