21-Component Compositionally Complex Ceramics: Discovery of Ultrahigh-Entropy Weberite and Fergusonite Phases and a Pyrochlore-Weberite Transition
Mingde Qin, Heidy Vega, Dawei Zhang, Sarath Adapa, Andrew J. Wright,, Renkun Chen, Jian Luo

TL;DR
This study reports the discovery of new ultrahigh-entropy ceramics with complex compositions, including weberite, fergusonite, and pyrochlore phases, revealing a pyrochlore-weberite transition and expanding the landscape of compositionally complex ceramics.
Contribution
It introduces 21-component high-entropy ceramics with novel phases and a transition mechanism, advancing the understanding of complex oxide systems.
Findings
Nine compositions form single high-entropy phases.
A pyrochlore-weberite transition occurs within specific compositional ranges.
Thermal conductivity remains stable across the phase transition.
Abstract
Two new high-entropy ceramics (HECs) in the weberite and fergusonite structures, along with unexpected formation of ordered pyrochlore phases with ultrahigh-entropy compositions and an abrupt pyrochlore-weberite transition, are discovered in a 21-component oxide system. While the Gibbs phase rule allows 21 equilibrium phases, nine out of the 13 compositions examined possess single HEC phases (with ultrahigh ideal configurational entropies: ~2.7kB per cation or higher on one sublattice in most cases). Notably, (15RE1/15)(Nb1/2Ta1/2)O4 possess a single monoclinic fergusonite (C2/c) phase and (15RE1/15)3(Nb1/2Ta1/2)1O7 form a single orthorhombic (C2221) weberite phase, where 15RE1/15 represents Sc1/15Y1/15La1/15Pr1/15Nd1/15Sm1/15Eu1/15Gd1/15Tb1/15Dy1/15Ho1/15Er1/15Tm1/15Yb1/15Lu1/15. Moreover, a series of eight (15RE1/15)2+x(Ti1/4Zr1/4Ce1/4Hf1/4)2-2x(Nb1/2Ta1/2)xO7 specimens all exhibit…
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Taxonomy
TopicsHigh Entropy Alloys Studies · Nuclear materials and radiation effects · Ferroelectric and Piezoelectric Materials
