Structural and valence properties of the amorphous-metallic high-pressure phase of
- 15 May 1988
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 37 (14) , 8130-8137
- https://doi.org/10.1103/physrevb.37.8130
Abstract
Mössbauer spectroscopy (MS) in and was employed to investigate the evolution and properties of the high-pressure amorphous-metallic phase of . Measurements were carried out at pressures up to 27 GPa using diamond-anvil cells. Both MS probes detect the onset of a new high-pressure phase at P≃10 GPa. The relative abundance of the high-pressure phase increases with pressure, reaching 100% at P≥20 GPa. Whereas the isomer shift of Sn in the low-pressure phase has a positive slope, that of the high-pressure phase has a negative slope with an unusual plateau in the 15–20-GPa region. In the 0≤P≤10 GPa range the MS reveals a single site. For P≥10 GPa a spectral component evolves with pressure that coexists with the ‘‘molecular’’ phase and reaches an abundance saturation of ≃50% at P≥18 GPa. In contrast to the low-pressure phase this component shows a positive quadrupole coupling constant, whose magnitude is about half that of the low-pressure phase, a large η value, and nearly identical values. The high-pressure abundance determined by both and shows a dramatic pressure hysteresis. It is unequivocally determined that no →+ dissociation takes place. A model proposed for the high-pressure phase of consists of randomly oriented chains of tetrahedral molecules where two bridging iodines per molecule provide for the intermolecular association. The ground state in this structure is formed by hybridizing the outer 5s5p with the inner 4p4d tin orbitals. This unique molecular association and the high-pressure ground state provide the proper path and mechanism for the one-dimensional charge delocalization.
Keywords
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