Synthesis of (MgCoNiCuZn)O entropy-stabilized oxides using solution-based routes: influence of composition on phase stability and functional properties

被引:16
作者
Mnasri, Walid [1 ,2 ]
Berardan, David [2 ]
Tusseau-Nenez, Sandrine [1 ]
Gacoin, Thierry [1 ]
Maurin, Isabelle [1 ,3 ]
Dragoe, Nita [2 ]
机构
[1] Ecole Polytech, CNRS, IP Paris, Phys Matiere Condensee,UMR 7643, F-91128 Palaiseau, France
[2] Univ Paris Saclay, Inst Chim Mol & Mat Orsay, UMR CNRS 8182, F-91405 Orsay, France
[3] Univ Grenoble Alpes, Inst NEEL, Grenoble INP, CNRS, BP 166, F-38042 Grenoble, France
关键词
SOLID-SOLUTION FORMATION; THERMODYNAMICS; POWDERS; CO;
D O I
10.1039/d1tc03287a
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Formation of the (MgCoNiCuZn)O entropy-stabilized oxide and of the related 4-cation derivatives is achieved using a Pechini route based on cation chelation and subsequent immobilization in a polymer gel. Calcination of the as-obtained resins yields a phase separation into fine-grained oxide precursors, but the extent of this phase separation depends on the formulation. In particular, absence of copper leads to the formation of a multi-element oxide with a rock-salt structure including most of the cations except for Zn at a temperature as low as 450 degrees C. Starting from these charred resins, the temperature-composition phase diagram of the equimolar mixtures is investigated by in situ powder X-ray diffraction. This study highlights the specific role of copper, with an onset of phase transformation into a phase-pure (MgCoNiZn)O mixed oxide at a temperature 25 degrees C lower than the one found for the 5-cation reference. Removal of the magnesium and nickel elements has also a pronounced impact on phase stability and lattice distortions after quenching, suggesting a description in terms of site percolation within a (MgNi)O templating network. The optical, dielectric and magnetic properties of the 4-cation compositions with respect to the 5-element high-entropy oxide are discussed in relation with the structural distortions induced at the local scale by the Jahn-Teller Cu2+ ions and at longer range through the destabilization of the rock-salt cubic structure.
引用
收藏
页码:15121 / 15131
页数:11
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