Summary
In compressively strained bilayer nickelate thin films, by continuously tuning the oxygen stoichiometry, researchers have discovered a superconducting half-dome. Starting from the optimal superconducting state, increasing the oxygen content progressively suppresses superconductivity, driving a transition toward a metallic phase; conversely, decreasing the oxygen content induces a granular superconductor-insulator transition while the onset superconducting temperature remains unchanged. This half-dome structure originates from the distinct roles of interstitial oxygen and oxygen vacancies: the former primarily regulates carrier concentration through doping effects, whereas the latter introduces strong scattering that leads to electronic inhomogeneity. Experiments show that this half-dome consistently appears across different rare-earth combinations and with or without alkaline-earth doping, revealing a universal feature of the bilayer nickelate phase diagram. This finding offers new perspectives for understanding the emergence and suppression of superconductivity in correlated electron systems.
Materials
Methods
- PLD
- Molecular beam epitaxy (MBE)
- Electron energy-loss spectroscopy (EELS)
- X-ray absorption spectroscopy (XAS)
- Transport measurements
- Resistivity and Hall effect
- Cryo-FIB
Keywords
- half dome
- oxygen stoichiometry
- granular superconductor insulator transition
- interstitial oxygen
- oxygen vacancies
- spin density wave (sdw) state
Highlights
- The study reveals a half-dome structure consistently across samples with different rare-earth combinations and doping.
- Oxygen stoichiometry exhibits two qualitatively distinct manifestations: excess oxygen acts as an electronic tuning parameter, while oxygen deficiency introduces strong scattering and electronic inhomogeneity.
Conclusions
- A superconducting half-dome is observed in compressively strained bilayer nickelate thin films as a function of continuous tuning of oxygen stoichiometry.
- Increasing oxygen stoichiometry suppresses superconductivity toward a metallic phase, whereas decreasing oxygen stoichiometry drives a granular superconductor-to-insulator transition while leaving the superconducting onset intact.
- The half-dome structure arises from contrasting roles of interstitial oxygen (doping) versus oxygen vacancies (scattering).
- The half-dome emerges consistently across samples with different rare-earth combinations, with or without alkaline-earth doping, revealing a general feature of the bilayer nickelate phase diagram.
Main claims
- Oxygen excess suppresses superconductivity toward a metallic phase through doping; oxygen deficiency drives a granular superconductor-insulator transition.
- Evidence: Abstract,Full text: increasing oxygen stoichiometry gradually suppresses superconductivity toward a metallic phase, whereas decreasing oxygen stoichiometry drives a granular superconductor-to-insulator transition.
- The superconducting half-dome is a universal feature across different rare-earth combinations and alkaline-earth doping.
- Evidence: Abstract,Full text: half-dome emerges consistently across samples with different rare-earth combinations, with or without alkaline-earth doping.
- Interstitial oxygen acts as a dopant while oxygen vacancies introduce strong disorder.
- Evidence: Abstract,Full text: The pronounced asymmetry suggests that oxygen vacancies play a fundamentally different role from oxygen interstitials.
Workflow
- sample_preparation
- Materials: LSNO; LPNO; LPCNO; SLAO substrate
- Methods: pulsed laser deposition; molecular beam epitaxy
- oxygen_stoichiometry_tuning
- Methods: ozone annealing; vacuum annealing; EELS; XAS
- Observations: two-stage evolution of transport
- transport_characterization
- Methods: resistivity measurements; Hall effect measurements
- Observations: superconducting half-dome; SIT scaling
- phase_diagram_construction
- Methods: normalization of conductivity; contour mapping
- Observations: universal half-dome across different compositions