High-entropy
rare-earth (RE) sesquioxides (RE2O3) containing
five cations in equimolar amounts have been investigated
for a variety of applications, but little is known about their polymorphic
behavior and coefficient of thermal expansion. Here, we evaluate the
effect of the average ionic radius (AIR) on the polymorphism of high-entropy
RE2O3. Powder samples of compositions 1 (Lu,Y,Ho,Nd,La)2O3 (AIR = 0.938 Å) and 2 (Gd,Eu,Sm,Nd,La)2O3 (AIR = 0.982 Å) were synthesized via a
wet chemical method, and bead samples were prepared for aerodynamic
levitation by melting the powders in a copper hearth. Structural transitions
were monitored upon cooling from the melt to 1000 °C via in situ
X-ray diffraction on aerodynamically levitated samples. The phase
evolution was liquid, hexagonal H-type, and monoclinic B-type for
composition 1 and liquid, cubic X-type, H-type, and B-type for composition
2. Based on their AIR, the general polymorphic transformations of
the high-entropy RE2O3 follow the trend of single-RE
RE2O3, but the transition temperatures differ
from those of single-RE RE2O3. The coefficient
of thermal expansion values of the B-type phase of compositions 1
and 2 are similar to those of Gd2O3 and previously
published high-entropy RE2O3.