Grebenchuk Sergey Y, Grzeszczyk Magdalena, Chen Zhaolong, Šiškins Makars, Borisov Vladislav, Pereiro Manuel, Katsnelson Mikhail I, Eriksson Olle, Novoselov Kostya S, Koperski Maciej
Institute for Functional Intelligent Materials, National University of Singapore, Singapore, 117544, Singapore.
Department of Materials Science and Engineering, National University of Singapore, Singapore, 117575, Singapore.
Adv Sci (Weinh). 2025 Jul;12(26):e2500562. doi: 10.1002/advs.202500562. Epub 2025 Apr 11.
Traditional magnetic phase diagram represents a transition between the ferromagnetic and paramagnetic states of a material under the influence of varied temperature, magnetic field, and pressure. So far, the ferromagnetic phase has been considered predominantly as a single type of magnetization texture extending macroscopically in the bulk of a crystal, existing as a ground state determined by the interactions between localized magnetic moments arranged in a lattice. Here, it is demonstrated that an unconventional magnetic order composed of vertically correlated planar magnetic sub-domains occurs intrinsically in mechanically exfoliated layers of van der Waals ferromagnet CrBr. Based on the visualization of the magnetic textures through magnetic force microscopy in conjunction with the ab initio calculations of the crystal structure in the magnetic phase and micromagnetic simulations, the origin of the magnetic sub-domains is attributed to stacking faults isolating a van der Waals ferromagnetic well from the bulk film due to modifications in the interlayer exchange coupling. This enables to create a phase diagram describing the magnetic states unique to van der Waals ferromagnets in terms of the degree of correlation between the magnetic sub-domains, dependent on the exchange coupling constants and tuneable by magnetic field and temperature.
传统的磁相图表示材料在温度、磁场和压力变化的影响下,铁磁态和顺磁态之间的转变。到目前为止,铁磁相主要被认为是一种在晶体主体中宏观延伸的单一类型的磁化纹理,作为由晶格中局域磁矩之间的相互作用所决定的基态而存在。在此,研究表明,由垂直相关的平面磁子域组成的非常规磁序,在范德华铁磁体CrBr的机械剥离层中固有地出现。基于通过磁力显微镜对磁纹理的可视化,结合磁相晶体结构的从头算计算和微磁模拟,磁子域的起源归因于由于层间交换耦合的改变,堆叠缺陷将范德华铁磁阱与体膜隔离开来。这使得能够创建一个相图,该相图根据磁子域之间的相关程度来描述范德华铁磁体特有的磁态,该相关程度取决于交换耦合常数,并可通过磁场和温度进行调节。