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替代式铁掺杂对MoS₂和WS₂单层磁性的影响。

The effects of substitutional Fe-doping on magnetism in MoSand WSmonolayers.

作者信息

Kang Kyungnam, Fu Shichen, Shayan Kamran, Anthony Yoshimura, Dadras Siamak, Yuzan Xiong, Kazunori Fujisawa, Terrones Mauricio, Zhang Wei, Strauf Stefan, Meunier Vincent, Vamivakas A Nick, Yang Eui-Hyeok

机构信息

Department of Mechanical Engineering, Stevens Institute of Technology, Hoboken, NJ 07030, United States of America.

The Institute of Optics, University of Rochester, Rochester, NY 14627, United States of America.

出版信息

Nanotechnology. 2020 Dec 10;32(9). doi: 10.1088/1361-6528/abcd61.

Abstract

Doping of two-dimensional (2D) semiconductors has been intensively studied toward modulating their electrical, optical, and magnetic properties. While ferromagnetic 2D semiconductors hold promise for future spintronics and valleytronics, the origin of ferromagnetism in 2D materials remains unclear. Here, we show that substitutional Fe-doping of MoSand WSmonolayers induce different magnetic properties. The Fe-doped monolayers are directly synthesized via chemical vapor deposition. In both cases, Fe substitutional doping is successfully achieved, as confirmed using scanning transmission electron microscopy. While both Fe:MoSand Fe:WSshow PL quenching and n-type doping, Fe dopants in WSmonolayers are found to assume deep-level trap states, in contrast to the case of Fe:MoS, where the states are found to be shallow. Usingm- and mm-precision local NVmagnetometry and superconducting quantum interference device, we discover that, unlike MoSmonolayers, WSmonolayers do not show a magnetic phase transition to ferromagnetism upon Fe-doping. The absence of ferromagnetism in Fe:WSis corroborated using density functional theory calculations.

摘要

二维(2D)半导体的掺杂已被深入研究,以调节其电学、光学和磁学性质。虽然铁磁二维半导体在未来的自旋电子学和谷电子学方面具有潜力,但二维材料中铁磁性的起源仍不清楚。在此,我们表明,MoS和WS单层的替代铁掺杂会诱导出不同的磁性。通过化学气相沉积直接合成了铁掺杂单层。在这两种情况下,使用扫描透射电子显微镜证实成功实现了铁的替代掺杂。虽然Fe:MoS和Fe:WS都表现出光致发光猝灭和n型掺杂,但发现WS单层中的铁掺杂剂呈现深能级陷阱态,这与Fe:MoS的情况相反,在Fe:MoS中这些态是浅能级的。使用微米和毫米精度的局部NV磁强计和超导量子干涉装置,我们发现,与MoS单层不同,WS单层在铁掺杂后不会显示出向铁磁性的磁相变。使用密度泛函理论计算证实了Fe:WS中不存在铁磁性。

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