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RESEARCH PRODUCT
The high-pressure, high-temperature phase diagram of cerium
Steve McguireIngo LoaDaniel ErrandoneaKeith MunroDominik DaisenbergerS. G. MacleodS. G. MacleodS. G. MacleodCatalin PopescuPablo BotellaPablo BotellaMalcolm McmahonMalcolm Mcmahonsubject
Phase boundaryMaterials scienceTriple pointThermodynamicsDiamondchemistry.chemical_element02 engineering and technologyengineering.material021001 nanoscience & nanotechnologyCondensed Matter Physics01 natural sciencesCeriumchemistryPhase (matter)0103 physical sciencesX-ray crystallographyengineeringGeneral Materials ScienceOrthorhombic crystal system010306 general physics0210 nano-technologyPhase diagramdescription
Abstract We present an experimental study of the high-pressure, high-temperature behaviour of cerium up to ∼22 GPa and 820 K using angle-dispersive x-ray diffraction and external resistive heating. Studies above 820 K were prevented by chemical reactions between the samples and the diamond anvils of the pressure cells. We unambiguously measure the stability region of the orthorhombic oC4 phase and find it reaches its apex at 7.1 GPa and 650 K. We locate the α-cF4–oC4–tI2 triple point at 6.1 GPa and 640 K, 1 GPa below the location of the apex of the oC4 phase, and 1–2 GPa lower than previously reported. We find the α-cF4 → tI2 phase boundary to have a positive gradient of 280 K (GPa)−1, less steep than the 670 K (GPa)−1 reported previously, and find the oC4 → tI2 phase boundary to lie at higher temperatures than previously found. We also find variations as large as 2–3 GPa in the transition pressures at which the oC4 → tI2 transition takes place at a given temperature, the reasons for which remain unclear. Finally, we find no evidence that the α-cF4 → tI2 is not second order at all temperatures up to 820 K.
year | journal | country | edition | language |
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2020-05-15 | Journal of Physics: Condensed Matter |