| Summary: | The phenomenon of oxygen incorporation-induced superconductivity in iron telluride (Fe<sub>1+y</sub>Te, with antiferromagnetic (AFM) orders) is intriguing and quite different from the case of FeSe. Until now, the microscopic origin of the induced superconductivity and the role of oxygen are far from clear. Here, by combining in situ scanning tunneling microscopy/spectroscopy (STM/STS) and X-ray photoemission spectroscopy (XPS) on oxygenated FeTe, we found physically adsorbed O<sub>2</sub> molecules crystallized into <i>c</i> (2/3 × 2) structure as an oxygen overlayer at low temperature, which was vital for superconductivity. The O<sub>2</sub> overlayer were not epitaxial on the FeTe lattice, which implied weak O<sub>2</sub> –FeTe interaction but strong molecular interactions. The energy shift observed in the STS and XPS measurements indicated a hole doping effect from the O<sub>2</sub> overlayer to the FeTe layer, leading to a superconducting gap of 4.5 meV opened across the Fermi level. Our direct microscopic probe clarified the role of oxygen on FeTe and emphasized the importance of charge transfer effect to induce superconductivity in iron-chalcogenide thin films.
|
|---|