The sodium-iron phosphite NaFe 3 (HPO 3 ) 2 (H 2 PO 3 ) 6 is studied by ac-magnetic susceptibility, pulsed-field magnetization, specific heat, and high-frequency electron spin resonance (HF-ESR) measurements combined with Mössbauer spectroscopy and density-functional calculations. We show that this compound develops ferrimagnetic order below T C = 9.5 K and reveals a magnetization plateau at 1/3-saturation. The plateau extends to B c ~ 8 T, whereas above B c the magnetization increases linearly until reaching saturation at B s ~ 27 T. The Mössbauer spectroscopy reveals two magnetically non-equivalent iron sites with the 2:1 ratio. The HF-ESR spectra are consistent with a two-sublattice ferrimagnet and additionally pinpoint weak magnetic anisotropy as well as short-range spin order that persists well above T C . The ferrimagnetic order in the title compound is stabilized by a network of purely antiferromagnetic exchange interactions. The spin lattice comprises layers coinciding with the crystallographic (10-1) planes, with stronger couplings J i ~ 1.5 K within the layers and weaker couplings J i = 0.3−0.4 K between the layers. Both intralayer and interlayer couplings are frustrated. The ensuing ferrimagnetic order arises from a subtle interplay of the frustrated but nonequivalent exchange couplings.
IntroductionThe magnetization of conventional isotropic antiferromagnets increases monotonically in an applied magnetic field. Fewer systems will, however, show a more complex magnetization process with flat or nearly flat regions of the magnetization curve that are known as magnetization plateaus [1]. These plateaus will normally appear at integer fractions of the total (saturation) magnetization and manifest ferrimagnetic order induced by the magnetic field. The stabilization of ferrimagnetic phases is strongly linked to the presence of magnetic frustration. For example, triangular antiferromagnets reveal a 1/3-plateau that is most pronounced in the quantum spin-1/2 regime, where the collinear ferrimagnetic phase is stabilized by quantum fluctuations [2][3][4]. It does, however, persist in the classical regime as well, thanks to the stabilization by thermal fluctuations [5,6], as in the extensively studied spin-5/2 triangular multiferroic RbFe(MoO 4 ) 2 [7][8][9]. On the other hand, even classical spin systems can show magnetization plateaus of putatively quantum nature, such as the 1/3-plateau recently observed in the spin-trimer compound SrMn 3 P 4 O 12 [10][11][12][13].In the following we report a detailed investigation of a novel iron fluorophosphite showing a pronounced magnetization plateau at 1/3-saturation. The true composition, which incorporates a very small amount of fluorine, has been discussed previously (14) but for simplicity in the present work we use an idealized composition NaFe 3 (HPO 3 ) 2 (H 2 PO 3 ) 6 , abbreviated NaFP. This approximation has no bearing on the interpretation of physical properties in the present work.The crystal structure of NaFP [14] comprises two nonequivalent positions of S...