Atomically Layered and Ordered Rare-Earth i-MAX Phases: A New Class of Magnetic Quaternary Compounds
Atomically Layered and Ordered Rare-Earth i-MAX Phases: A New Class of Magnetic Quaternary Compounds
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DOI:
10.1021/acs.chemmater.8b05298
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发表时间:
2019-03
影响因子:
8.6
通讯作者:
Q. Tao;Jun Lu;M. Dahlqvist;A. Mockutė;S. Calder;A. Petruhins;Rahele Meshkian;O. Rivin;D. Potashnikov;E. Caspi;H. Shaked;A. Hoser;C. Opagiste;R. Galera;R. Salikhov;U. Wiedwald;C. Ritter;A. Wildes;B. Johansson;L. Hultman;M. Farle;M. Barsoum;J. Rosen
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作者:
Q. Tao;Jun Lu;M. Dahlqvist;A. Mockutė;S. Calder;A. Petruhins;Rahele Meshkian;O. Rivin;D. Potashnikov;E. Caspi;H. Shaked;A. Hoser;C. Opagiste;R. Galera;R. Salikhov;U. Wiedwald;C. Ritter;A. Wildes;B. Johansson;L. Hultman;M. Farle;M. Barsoum;J. Rosen
In 2017, we discovered quaternary i-MAX phases—atomically layered solids, where M is an early transition metal, A is an A group element, and X is C—with a (M12/3M21/3)2AC chemistry, where the M1 and M2 atoms are in-plane ordered. Herein, we report the discovery of a class of magnetic i-MAX phases in which bilayers of a quasi-2D magnetic frustrated triangular lattice overlay a Mo honeycomb arrangement and an Al Kagome lattice. The chemistry of this family is (Mo2/3RE1/3)2AlC, and the rare-earth, RE, elements are Ce, Pr, Nd, Sm, Gd, Tb, Dy, Ho, Er, Tm, and Lu. The magnetic properties were characterized and found to display a plethora of ground states, resulting from an interplay of competing magnetic interactions in the presence of magnetocrystalline anisotropy.