Rare earth elements (REEs), the 15
naturally occurring lanthanides
plus yttrium and scandium, are ubiquitously used in modern life as
they are critical components of many advanced devices and technologies.
However, the demand for REEs is not equal, with the heavy rare earth
elements (HREEs) having a higher demand. Xenotime (HREEPO4) is an important HREE ore mineral and globally is an economical
source of HREE. Most of the crystallographic and thermodynamic properties
of xenotime endmembers have been elucidated by calorimetric, solubility,
and high-pressure studies. Yet, in natural systems, endmembers are
rarely encountered, and instead, REE solid solutions are more commonly
observed. In this work, we characterize the crystal chemistry, thermodynamics
of HREE mixing, and high-temperature material behaviors and thermochemistry
of a synthetic erbium (Er)–ytterbium (Yb) binary xenotime solid
solution (Er(x)Yb(1–x)PO4) using a suite of experimental techniques,
including X-ray fluorescence spectroscopy, synchrotron X-ray powder
diffraction implemented with Rietveld analysis, Fourier transform
infrared spectroscopy coupled with attenuated total reflectance, Raman
spectroscopy, thermogravimetric analysis coupled with differential
scanning calorimetry, and high-temperature oxide melt drop solution
calorimetry. Our results shed light on the formation of natural xenotimes
and lay the foundation for their industrial applications as thermal
coating materials.