High-Pressure-Stabilized Post-Spinel Phase of CdFe2O4 with Distinct Magnetism from Its Ambient-Pressure Spinel Phase
α-CdFe2O4 stabilizes its normal spinel structure due to the covalent Cd–O bond, in which all the connections between adjacent FeO6 octahedral are edge-shared, forming a typical geometrically frustrated Fe3+ magnetic lattice. As the high-pressure methods were utilized, the post-spinel phase β-CdFe2O4...
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Published in | Inorganic chemistry Vol. 62; no. 23; pp. 9139 - 9145 |
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Main Authors | , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
American Chemical Society
12.06.2023
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Online Access | Get full text |
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Summary: | α-CdFe2O4 stabilizes its normal spinel structure due to the covalent Cd–O bond, in which all the connections between adjacent FeO6 octahedral are edge-shared, forming a typical geometrically frustrated Fe3+ magnetic lattice. As the high-pressure methods were utilized, the post-spinel phase β-CdFe2O4 with a CaFe2O4-type structure was synthesized at 8 GPa and 1373 K. The new polymorph has an orthorhombic structure with the space group Pnma and an 11.5% higher density than that of its normal spinel polymorph (α-CdFe2O4) synthesized at ambient conditions. The edge-shared FeO6 octahedra form zigzag S = 5/2 spin ladders along the b-axis dominating its low-dimensional magnetic properties at high temperatures and a long-range antiferromagnetic ordering with a high Néel temperature of T N1 = 350 K. Further, the rearrangement of magnetic ordering was found to occur around T N2 = 265 K, below which the competition of two phases or several couplings induce complex antiferromagnetic behaviors. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0020-1669 1520-510X |
DOI: | 10.1021/acs.inorgchem.3c01002 |