Recently, several putative quantum spin liquid (QSL) states were
discovered in {\tilde S} = 1/2S̃=1/2
rare-earth based triangular-lattice antiferromagnets (TLAF) with the
delafossite structure. In order to elucidate the conditions for a QSL to
arise, we report here the discovery of a long-range magnetic order in
the Ce-based TLAF KCeS_22
below T_{\mathrm N} = 0.38TN=0.38 K,
despite the same delafossite structure. Finally, combining various
experimental and computational methods, we characterize the crystal
electric field scheme, the magnetic anisotropy and the magnetic ground
state of KCeS_22.
The recent realizations of the quantum anomalous Hall effect (QAHE) in MnBi2Te4 and MnBi4Te7 benchmark the (MnBi2Te4)(Bi2Te3)n family as a promising hotbed for further QAHE improvements. The family owes its potential to its ferromagnetically (FM) ordered MnBi2Te4 septuple layers (SLs). However, the QAHE realization is complicated in MnBi2Te4 and MnBi4Te7 due to the substantial antiferromagnetic (AFM) coupling between the SLs. An FM state, advantageous for the QAHE, can be stabilized by interlacing the SLs with an increasing number n of Bi2Te3 quintuple layers (QLs). However, the mechanisms driving the FM state and the number of necessary QLs are not understood, and the surface magnetism remains obscure. Here, robust FM properties in MnBi6Te10 (n = 2) with Tc ≈ 12 K are demonstrated and their origin is established in the Mn/Bi intermixing phenomenon by a combined experimental and theoretical study. The measurements reveal a magnetically intact surface with a large magnetic moment, and with FM properties similar to the bulk. This investigation thus consolidates the MnBi6Te10 system as perspective for the QAHE at elevated temperatures.
We have carried out a structural and magnetic characterization of Co 8 Zn 8+y Mn 4−y−x Fe x by means of bulk techniques, powder neutron scattering and Mössbauer spectroscopy. From our data, we derive the main magnetic parameters and carry out a detailed structural characterization. We observe that disorder is present in our samples in various forms and that this seems to be generic for this class of materials. However, the disorder appears to have little impact on the character of the magnetic phases, and thus seems to be of no relevance for the skyrmionic phases established for these types of materials.
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