Crystal and electronic structures of BiS2-based compounds Sr0.5X0.5FBiS2 (X=rare earth) under pressure: Correlation with the change in the superconductivity from unconventional to conventional
Hitoshi Yamaoka, Aichi Yamashita, Yuki Nakahira, Masayuki Ochi, Kazuhiko Kuroki, Hiroto Arima, Kazuyuki Matsubayashi, Hirofumi Ishii, Nozomu Hiraoka, Yoshikazu Mizuguchi
DOI 10.1103/PhysRevB.106.205122 · Physical Review B
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Abstract
Sr1−xXxFBiS2 (X:rare earth) is considered to show a pressure-induced structural transition around 1 GPa where the superconductivity changes from unconventional in the low-pressure phase to conventional in the high-pressure phase with increasing the superconducting transition temperature (Tc). We clarified the monoclinic crystal structure (P21/m) in the high-pressure phase which is the same as the high-pressure phase of XO1−xFxBiY2 (Y: chalcogen) systems. We performed high-resolution x-ray absorption spectroscopy (XAS) to study the electronic structure of Sr1−xXxFBiS2 systematically, indicating the Bi charge state of nearly 3+. The pressure dependence of the XAS spectra of Sr0.5La0.5FBiS2 and Sr0.5Nd0.5FBiS2 indicate a large change in the electronic structure around the structural transition pressure, which corresponded to the transition from semiconductorlike to more metallic states. The increase of the empty states of Bi s and d (t2g) bands above the Fermi level was observed in the high-pressure phase. Density functional theory calculations showed that the density of the states at the Fermi level did not show a significant change in the high-pressure phase, where higher Tc was observed.
Source-reported materials — not catalogue approval
| Formula | Reported Tc (K) | Pressure (GPa) | Type |
|---|---|---|---|
| Sr0.5La0.5FBiS2 Archive — visibility unverified Source-occurrence policy only; no material identity or catalogue acceptance is inferred from the formula. | 10 | 1 GPa | onset |
| Bi4O4S3 Archive — visibility unverified Source-occurrence policy only; no material identity or catalogue acceptance is inferred from the formula. | 8.6 | Pressure unresolved | unknown |
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