Coexistence of structural and magnetic phases in van der Waals magnet CrI3

CrI 3 has raised as an important system to the emergent field of two-dimensional van der Waals magnetic materials. However, it is still unclear why CrI 3 which has a ferromagnetic rhombohedral structure in bulk, changed to anti-ferromagnetic monoclinic at thin layers. Here we show that this behaviou...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Nature communications 2021-11, Vol.12 (1), p.6265-7, Article 6265
Hauptverfasser: Meseguer-Sánchez, Jaume, Popescu, Catalin, García-Muñoz, José Luis, Luetkens, Hubertus, Taniashvili, Grigol, Navarro-Moratalla, Efrén, Guguchia, Zurab, Santos, Elton J. G.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:CrI 3 has raised as an important system to the emergent field of two-dimensional van der Waals magnetic materials. However, it is still unclear why CrI 3 which has a ferromagnetic rhombohedral structure in bulk, changed to anti-ferromagnetic monoclinic at thin layers. Here we show that this behaviour is due to the coexistence of both monoclinic and rhombohedral crystal phases followed by three magnetic transitions at T C1  = 61 K, T C2  = 50 K and T C3  = 25 K. Each transition corresponds to a certain fraction of the magnetically ordered volume as well as monoclinic and rhombohedral proportion. The different phases are continuously accessed as a function of the temperature over a broad range of magnitudes. Our findings suggest that the challenge of understanding the magnetic properties of thin layers CrI 3 is in general a coexisting structural-phase problem mediated by the volume-wise competition between magnetic phases already present in bulk. CrI 3 is a popular van der Waals magnet that exhibits anomalous magnetic properties between bulk and thin layers due to different crystal symmetry. Here, the authors report the coexistence of different magnetostructural phases over the entire range of temperatures, solving a long-standing puzzle.
ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-021-26342-4