Transmission electron microscopic study of pyrochlore to defect-fluorite transition in rare-earth pyrohafnates

A structural transition in rare earth pyrohafnates, Ln2Hf2O7 (Ln=Y, La, Pr, Nd, Tb, Dy, Yb and Lu), has been identified. Neutron diffraction showed that the structure transforms from well-ordered pyrochloric to fully fluoritic through the lanthanide series from La to Lu with a corresponding increase in the position parameter x of the 48f (Fd  3¯m) oxygen site from 0.330 to 0.375. As evidenced by the selected area electron diffraction, La2Hf2O7, Pr2Hf2O7 and Nd2Hf2O7 exhibited a well-ordered pyrocholoric structure with the presence of intense superlattice spots, which became weak and diffuse (in Dy2Hf2O7 and Tb2Hf2O7) before disappearing completely as the series progressed towards the Lu end. High resolution electron microscopic studies showed the breakdown of the pyrochlore ordering in the form of antiphase domains resulting in diffused smoke-like superlattice spots in the case of Dy2Hf2O7 and Tb2Hf2O7.

Graphical abstractTransmission electron microscopic studies showed the ordered pyrochlore to defect fluorite transition in rare-earth pyrohafnates to occur via the formation of anti-phase domains to start with.Figure optionsDownload full-size imageDownload as PowerPoint slideHighlights► Pyrochlore to fluorite structural transition in rare earth pyrohafnates. ► La2Hf2O7, Pr2Hf2O7 and Nd2Hf2O7 showed well ordered pyrochlore structure. ► Short range ordering in Dy2Hf2O7 and Tb2Hf2O7. ► Break down of pyrochlore ordering due to antiphase boundaries. ► Rest of the series showed fluoritic structure.