摘要
在压缩应变双层镍酸盐薄膜中,通过连续调控氧化学计量,研究人员发现了一个超导半圆顶。从最优超导态出发,增加氧含量会逐渐抑制超导,使其向金属相转变;而减少氧含量则驱动颗粒状超导体-绝缘体转变,但超导起始温度保持不变。这种半圆顶结构源于间隙氧与氧空位的不同作用:前者主要通过掺杂效应调控载流子浓度,后者则引入强散射导致电子不均匀性。实验表明,这一半圆顶在不同稀土组合及有无碱土掺杂的样品中一致出现,揭示了双层镍酸盐相图的普遍特征。该发现为理解相关电子体系中超导的涌现与消亡提供了新视角。
材料
方法
- PLD
- Molecular beam epitaxy (MBE)
- Electron energy-loss spectroscopy (EELS)
- X-ray absorption spectroscopy (XAS)
- Transport measurements
- Resistivity and Hall effect
- Cryo-FIB
关键词
- half dome
- oxygen stoichiometry
- granular superconductor insulator transition
- interstitial oxygen
- oxygen vacancies
- spin density wave (sdw) state
亮点
- 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.
结论
- 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.
主要论断
- Oxygen excess suppresses superconductivity toward a metallic phase through doping; oxygen deficiency drives a granular superconductor-insulator transition.
- 证据: 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.
- 证据: 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.
- 证据: Abstract,Full text: The pronounced asymmetry suggests that oxygen vacancies play a fundamentally different role from oxygen interstitials.
研究流程
- sample_preparation
- 材料: LSNO; LPNO; LPCNO; SLAO substrate
- 方法: pulsed laser deposition; molecular beam epitaxy
- oxygen_stoichiometry_tuning
- 方法: ozone annealing; vacuum annealing; EELS; XAS
- 观察: two-stage evolution of transport
- transport_characterization
- 方法: resistivity measurements; Hall effect measurements
- 观察: superconducting half-dome; SIT scaling
- phase_diagram_construction
- 方法: normalization of conductivity; contour mapping
- 观察: universal half-dome across different compositions