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具有大谷极化和压电极化的二维铁磁半导体Janus 2H-ZrTeI单层的预测

Prediction of the two-dimensional ferromagnetic semiconductor Janus 2H-ZrTeI monolayer with large valley and piezoelectric polarizations.

作者信息

Li Jie, Chen Ya-Qing, Yuan Hong-Kuan, Tian Chun-Ling

机构信息

School of Physical Science and Technology, Southwest University, Chongqing 400715, China.

出版信息

Nanoscale. 2024 Oct 10;16(39):18504-18517. doi: 10.1039/d4nr01692k.

Abstract

Two-dimensional room-temperature Janus ferrovalley semiconductors with valley polarization and piezoelectric polarization offer new perspectives for designing multifunctional nanodevices. Herein, using first-principles calculations, we predict that the Janus 2H-ZrTeI monolayer is an intrinsic ferromagnetic semiconductor with in-plane magnetic anisotropy and a Curie temperature of 111 K. The Janus ZrTeI monolayer possesses a significant valley polarization of 141 meV due to time-reversal and inversion symmetry breaking. Based on the valley-contrasting Berry curvature, the anomalous valley Hall effect can be observed under an in-plane electric field. Meanwhile, the breaking of the inversion symmetry and mirror symmetry results in large longitudinal and transverse piezoelectric coefficients. By applying biaxial strain, the Janus 2H-ZrTeI monolayer can also be transformed into a Weyl nodal line semimetal. Furthermore, bilayers of ZrTeI with AB and BA stacking configurations allow the coexistence of valley polarization and ferroelectricity, enabling the manipulation of magnetism, ferroelectric polarization, and valley polarization through interlayer sliding. Our work provides a platform for studying valley polarization, piezoelectricity, and multiferroic coupling, which is significant for the application of multifunctional devices.

摘要

具有谷极化和压电极化的二维室温Janus铁谷半导体为多功能纳米器件的设计提供了新的视角。在此,通过第一性原理计算,我们预测Janus 2H-ZrTeI单层是一种具有面内磁各向异性且居里温度为111 K的本征铁磁半导体。由于时间反演和空间反演对称性破缺,Janus ZrTeI单层具有14 meV的显著谷极化。基于谷对比贝里曲率,在面内电场下可观测到反常谷霍尔效应。同时,空间反演对称性和镜面对称性的破缺导致了较大的纵向和横向压电系数。通过施加双轴应变,Janus 2H-ZrTeI单层还可转变为外尔节线半金属。此外,具有AB和BA堆叠构型的ZrTeI双层允许谷极化和铁电性共存,从而能够通过层间滑动来操控磁性、铁电极化和谷极化。我们的工作为研究谷极化、压电性和多铁性耦合提供了一个平台,这对多功能器件的应用具有重要意义。

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