Abstract

The effect of high pressures up to 60 GPa on single-crystal and polycrystalline samples of iron borate 57FeBO3 was studied by Mossbauer absorption spectroscopy (57Fe nuclei) in a diamond anvil cell. Magnetic field Hhf at the 57Fe nuclei increases with pressure but abruptly drops to zero at 46±2 GPa, indicating the crystal transition from the antiferromagnetic to nonmagnetic state. This is accompanied by an abrupt change in the isomer shift and quadrupole splitting. Their values in the high-pressure phase are evidence for the transition of Fe+3 ions from a high-spin (S=5/2, 6A1g) to low-spin (S=1/2, 6T2g) state (spin crossover). This correlates with an abrupt decrease in the unit-cell volume (by ∼9%) and optical gap. The change of the magnetic and electronic structures is explained by Mott’s transition with rupturing of strong d-d-electron correlations.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call