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This investigation reveals complex magnetic behaviors in mixed-valence iron phosphate Fe7(PO4)6, indicating intricate interactions between magnetic ions.
Mixed-valence iron compounds are fascinating materials exemplified by ferrimagnetic Fe₃O₄, multiferroic LuFe₂O₄, and a pigment Fe₄[Fe(CN)₆]₃. Mixed-valent iron (oxy)phosphates also provide a large variety of different connections between magnetic ions, which are responsible for complex magnetism. Fe₇(PO₄)₆ (Fe₃²⁺Fe₄³⁺(PO₄)₆) has well-defined Fe²⁺ and Fe³⁺ sites and shows two antiferromagnetic transitions at TN1 = 47 K and TN2 = 16 K. Here, we investigated magnetic structures of Fe₇(PO₄)₆ (at zero magnetic field) using neutron powder diffraction and constructed a temperature-magnetic-field phase diagram. Below TN1, magnetic propagation vector is k1 = (1/2, 0, 1/2), and magnetic moments on Fe³⁺ sites are nearly fully ordered; while moments on Fe²⁺ sites are significantly reduced. Below TN2, the second propagation vector appears k2 = (0, 1/2, 0) and coexists with k1; moments on Fe²⁺ sites are fully ordered (at 2 K) reaching 4.5 μB suggesting noticeable spin-orbital contributions. Coexistence of two propagation vectors and triclinic symmetry results in variations of total magnetic moments on each site. Magnetic measurements up to 300 kOe detected one field-induced transition near 55.5 kOe. Data showed that TN1 is nearly magnetic-field independent up to 90 kOe, while a more complex behavior was observed near TN2 at magnetic fields around 50 kOe.
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Dönni et al. (2026) studied this question.
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