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 inInorganic chemistry Vol. 62; no. 23; pp. 9139 - 9145
Main Authors Li, Beihong, Ye, Xubin, Wang, Xiao, Zhang, Jie, Lu, Dabiao, Zhao, Haoting, Pi, Maocai, Hu, Zhiwei, Lin, Hong-Ji, Chen, Chien-Te, Pan, Zhao, Qin, Xiaomei, Long, Youwen
Format Journal Article
LanguageEnglish
Published American Chemical Society 12.06.2023
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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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content type line 23
ISSN:0020-1669
1520-510X
DOI:10.1021/acs.inorgchem.3c01002