Dynamics and mechanism of oxygen annealing in Fe$_{1+y}$Te$_{0.6}$Se$_{0.4}$ single crystal

Yue Sun; Yuji Tsuchiya; Toshihiro Taen; Tatsuhiro Yamada; Sunseng Pyon; Akira Sugimoto; Toshikazu Ekino; Zhixiang Shi; Tsuyoshi Tamegai

doi:10.1038/srep04585

arXiv · 1404.0916

Dynamics and mechanism of oxygen annealing in Fe$_{1+y}$Te$_{0.6}$Se$_{0.4}$ single crystal

Yue Sun·Yuji Tsuchiya·Toshihiro Taen·Tatsuhiro Yamada·Sunseng Pyon·Akira Sugimoto·Toshikazu Ekino·Zhixiang Shi·Tsuyoshi Tamegai

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Abstract

Iron chalcogenide Fe(Te,Se) attracted much attention due to its simple structure, which is favorable for probing the superconducting mechanism. Its less toxic nature compared with iron arsenides is also advantageous for applications of iron-based superconductors. By intercalating spacer layers, superconducting transition temperature has been raised over 40 K. On the other hand, the presence of excess Fe is almost unavoidable in Fe(Te,Se) single crystals, which hinders the appearance of bulk superconductivity and causes strong controversies over its fundamental properties. Here we report a systematical study of O$_2$-annealing dynamics in Fe$_{1+y}$Te$_{1-x}$Se$_{x}$ by controlling the amount of O$_2$, annealing temperature, and time. Bulk superconductivity can be gradually induced by increasing the amount of O$_2$ and annealing time at suitable temperatures. The optimally annealed crystals can be easily obtained by annealing with ~ 1.5% molar ratio of oxygen at 400 $^{\circ}$C for more than 1 hour. Superconductivity was witnessed to evolve mainly from the edge of the crystal to the central part. After the optimal annealing, the complete removal of excess Fe was demonstrated via STM measurements. Some fundamental properties were recharacterized and compared with those of as-grown crystals to discuss the influence of excess Fe.

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Yue Sun, Yuji Tsuchiya, Toshihiro Taen, Tatsuhiro Yamada, Sunseng Pyon, Akira Sugimoto, Toshikazu Ekino, Zhixiang Shi, Tsuyoshi Tamegai. 2014-04-03. Dynamics and mechanism of oxygen annealing in Fe$_{1+y}$Te$_{0.6}$Se$_{0.4}$ single crystal. https://doi.org/10.1038/srep04585

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