Mixed-valent transition-metal compounds display complex structural, electronic and magnetic properties, which often intricately coexist. Here, we report the new ternary oxide GaVO, a structural sibling of skyrmion-hosting lacunar spinels. GaVO contains a vanadium trimer and an original spin-orbital-charge texture that forms upon the structural phase transition at T = 68 K followed by the magnetic transition at T = 35 K.
View Article and Find Full Text PDFThe first triple perovskite with Mn in A- and 1 : 2 B-site order MnMnNbO, prepared using high pressure phase transformation of the magnetodielectric MnNbO, is reported herein. It has a complex magnetic behaviour with a transition from a collinear AFM into an evolving incommensurate spin density wave (SDW) further stabilised into a lock-in structure dictated by the B-site order.
View Article and Find Full Text PDFBiVOF was prepared, characterized, and identified as a unique example of bismuth vanadyl oxyhalide with paramagnetic V centers. Its crystal structure shows 1D magnetic units with rare alternation of edge-sharing O-O and F-F μ bridges along the octahedral chains. Structural pairing across the O edges induces antiferromagnetic spin dimers ( = 0) with / ≈ 300 K, ∼15 times greater than the exchange across the F bridges, within a non-ordered magnetic ground state.
View Article and Find Full Text PDFNew NiTeO-type (NTO) and double perovskite (DPv) polymorphs of CoTeO are synthesised at pressures of 15 GPa. A complex elliptic helical magnetic order is observed in the NTO polymorph (T = 58 K) that reorientates (42 K) and further splits (T = 23.5 K) creating a coexisting helix.
View Article and Find Full Text PDFMnTaO is presented as the first hexagonal A-site manganite. Based on simple rules, the structure is compatible with a 14H-layer () stacking sequence that is related to BaVO and BaCrO high-pressure polymorphs. The A-site overstoichiometry is explained through difference in ionic radii sizes between Ba and Mn.
View Article and Find Full Text PDFA new double perovskite Mn2MnTeO6 has been obtained by high pressure phase transformation of a corundum-related precursor. It is antiferromagnetic below 36 K and develops a magnetic structure with magnetic moments of 4.8 μB and 3.
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