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. 2022 Apr 20;16(5):6960–7079. doi: 10.1021/acsnano.1c09150

Figure 30.

Figure 30

(a) Atomic structure of monolayer Fe3GeTe2. The left panel shows the view along [001]; the right panel shows the view along [010]. Bulk Fe3GeTe2 is a layered crystal with an interlayer vdW gap of 2.95 Å. FeI and FeII represent the two inequivalent Fe sites in the +3 and +2 oxidation states, respectively. (b) Optical image of typical few-layer flakes exfoliated on an Al2O3 thin film. (c) Atomic force microscopy image of the area marked by the square in (b). Mono- and few-layer flakes are clearly visible. Scale bar, 2 μm. (d) Cross-sectional profile of the Fe3GeTe2 flakes along the white line in (c). The steps are 0.8 nm in height, or consistent with the thickness (0.8 nm) of monolayer (1L) Fe3GeTe2. (e) Normalized remanent anomalous Hall resistance Inline graphic as a function of temperature obtained from Fe3GeTe2 thin-flake samples with varying numbers of layers. Arrows mark the FM transition temperature Tc. (f) Phase diagram of Fe3GeTe2 as layer number and temperature are varied. Tc values are determined from anomalous Hall effect, Arrott plots and RMCD are displayed in blue, red and magenta, respectively. (g) Remanent RMCD signal as a function of temperature for a sequence of selected few-layer flakes (1 L, monolayer; 2 L, bilayer; 3 L, trilayer; 4 L, four layers; 5 L, five layer). The solid lines are least-squares criticality fits of the form α(1 – T/Tc)β. Inset: derived values of the exponent β plotted as a function of thickness. (h) Thickness-temperature phase diagram. PM denotes the region in which the flake is paramagnetic, FM1 that in which it is FM with a single domain and FM2 that in which the flake exhibits labyrinthine or stripe domains. The transition temperatures, Tc, Tc1, and Tc2, are based on the temperature-dependent RMCD or anomalous Hall effect measurements for each flake thickness. The red dashed line denotes the critical thickness at which a dimensional crossover occurs. All panels are adapted with permission from ref (12). Copyright 2018 Springer Nature.