Magnetic hexamers interacting in layers in the (Na,K)CuO(SO minerals
arXiv:2005.02028 · doi:10.1103/PhysRevB.102.184405
Abstract
Magnetic properties and underlying magnetic models of the synthetic ACuO(SO fedotovite (A = K) and puninite (A = Na) minerals, as well as the mixed euchlorine-type NaKCuO(SO are reported. We show that all these compounds contain magnetic Cu hexamer units, which at temperatures below about 100 K act as single spin-1 entities. Weak interactions between these magnetic molecules lead to long-range order below = 3.4 K (A = Na), 4.7 K (A = NaK), and about 3.0 K (A = K). The formation of the magnetic order is elucidated by ab initio calculations that reveal two-dimensional inter-hexamer interactions within crystallographic planes. This model indicates the presence of a weakly distorted square lattice of magnetic ions and challenges the earlier description of the ACuO(SO minerals in terms of Haldane spin chains.
published version, re-worked compared to the initial submission
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- Long range 3D magnetic structures of the spin =1 hexamer cluster fedotovite-like ACuO(SO) (A=K, NaK, Na): a neutron diffraction study
- High-field NMR study of the spin correlations in the spin-cluster mineral NaCuO(SO)
- Pressure-tuned spin chains in brochantite, CuSO(OH)
- Geometrical frustration and incommensurate magnetic order in NaRuO with two triangular motifs