Collapse of the charge disproportionation and covalency-driven insulator-metal transition in Sr3Fe2O7 under pressure

Citation
P. Adler et al., Collapse of the charge disproportionation and covalency-driven insulator-metal transition in Sr3Fe2O7 under pressure, PHYS REV B, 60(7), 1999, pp. 4609-4617
Citations number
38
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
PHYSICAL REVIEW B-CONDENSED MATTER
ISSN journal
01631829 → ACNP
Volume
60
Issue
7
Year of publication
1999
Pages
4609 - 4617
Database
ISI
SICI code
0163-1829(19990815)60:7<4609:COTCDA>2.0.ZU;2-A
Abstract
The effect of pressure on electronic properties and crystal structure of Sr 3Fe2O7 was studied up to 45 GPa. Experimental methods employed were Fe-57 M ossbauer spectroscopy (MS), monochromatic synchrotron powder x-ray diffract ion, optical reflectance between 0.6 and 4 eV, and electrical resistance me asurements. Mossbauer spectra of the magnetically ordered as well as of the paramagnetic phase demonstrate that the charge disproportionation of Fe-IV disappears at pressures between 15 and 21 GPa. The diffraction data show t hat the tetragonal Ruddlesden-Popper-type crystal structure (space group I4 /mmm) is retained up to the highest pressure. The optical spectra reveal a continuous increase with pressure of the near-infrared oscillator strength, which indicates a pressure-driven transition from an insulating towards a metallic ground state. This is confirmed by the electrical resistance measu rements which evidence a sluggish pressure-induced insulator-metal (LM) tra nsition with a clear incipient metallic state at P approximate to 20 GPa. T he changes in electronic state are not associated with any detectable anoma ly in the pressure dependence of lattice parameters. The high-pressure beha vior of Sr3Fe2O7 is discussed in terms of a strengthening of the covalent F e(3d)-O(2p)-Fe(3d) interactions under pressure. Within the impurity model f or the electronic structure of transition metal compounds the IM transition in Sr3Fe2O7 can be attributed to the closure of a p-p-type energy gap. The ambient- and high-pressure properties of Sr3Fe2O7 and related Fe-IV oxides are compared. [S0163-1829(99)10531-9].