DOE OSTI · 2448560
High-Pressure Polymorphism in Silver Ferrite Delafossite, AgFeO 2
Abstract
The delafossites are a class of layered metal oxides that are notable for being able to exhibit optical trans- parency alongside an in-plane electrical conductivity, making them promising platforms for the development of transparent conductive oxides. Pressure-induced polymorphism offers a direct method for altering the electrical and optical properties in this class, and although the copper delafossites have been studied extensively under pressure, the silver delafossites remain only partially studied. We report two new high-pressure polymorphs of silver ferrite delafossite, AgFeO 2 , that are stabilized above ~6 GPa and ~14 GPa. In situ X-ray diffraction and vibrational spectroscopy measurements are used to examine the structural changes across the two phase transitions. The high-pressure structure between 6–14 GPa is assigned as a monoclinic C2/c structure that is analogous to the high-pressure phase reported for AgGaO 2 . As a result, nuclear resonant forward scattering reveals no change in the spin state or valence state at the Fe 3+ site up to 15.3 GPa.
Explore related subjects
Keep this discovery
Explore connections, maps & timelines
Manganaro, Nicholas S., Ambos, Scott D., DeCapua, Matthew, Thiel, Scott D., Mitchell, Wyatt E., Liu, Zhenxian, Zhang, Dongzhou, Nguyen, Phuong Q. H., Lavina, Barbara, Alp, Esen Ercan, Yan, Jun, Walsh, James P. S.. 2024-05-13. High-Pressure Polymorphism in Silver Ferrite Delafossite, AgFeO 2. https://doi.org/10.1021/acs.inorgchem.3c04631
Cite the original work for its findings. Save a collection to share your selection of sources.