Watching a metal collapse: Examining cerium’s γ ↔ α transformation using X-ray diffraction of compressed single and polycrystals

Numerous investigations have been performed on Ce metal since the discovery of the γ → α phase transformation, where a face-centered cubic structure is believed to collapse isostructurally with a volume change of ∼17%. However, two questions have yet to be answered definitively. First, is the transformation truly isostructural or is the face-centered cubic structure lost in α-Ce due to symmetry breaking? Second, if the transformation is isostructural does the face-centered cubic structure stay in crystallographic orientation through the volume collapse? Here, we use high-pressure and high-temperature X-ray diffraction measurements to examine single and polycrystalline samples of Ce in the vicinity of the γ ↔ α transformation. This was achieved by successive continuous compression and decompression in a diamond anvil cell at temperatures under, at and above the critical point. Our results show that the crystal structure remains face-centered cubic for both the γ and α phases. The results also show that the face-centered cubic structure retains its crystallographic orientation, simply reducing in volume during the γ → α phase transformation. Upon transformation to α, polycrystalline samples show increased diffraction peak broadening, while single crystals show increased streaking. These changes in diffraction can be attributed to increased damage and lattice misorientation from the transformation. Using a simple atomic lattice model, we show that a periodic array of misfit edge dislocation is necessary to accommodate the large volume difference at the γ–α interface and this could act as a source of the edge dislocations needed to produced previously observed deformation bands.