1. Structural characterization of natural U[O.sub.2] at pressures up to 82 GPa and temperatures up to 2200 K
- Author
-
Greaux, Steeve, Gautron, Laurent, Andrault, Denis, Bolfan-Casanova, Nathalie, Guignot, Nicolas, and Haines, Julien
- Subjects
Uranium -- Structure ,Uranium -- Thermal properties ,Crystals -- Structure ,Crystals -- Analysis ,Earth sciences research ,Earth sciences - Abstract
Uranium is one of the main heat sources in the Earth, as about 25% of the total heat is produced by the radioactive decay of U. The location of U in the deep mantle is then essential for a better understanding of the geodynamics and thermal behavior of the Earth. For the first time, the crystal structure of natural simple dioxide U[O.sub.2] uraninite has been studied by X-ray diffraction with synchrotron radiation (ESRF, Grenoble, France), in situ in a laser-heated diamond-anvil cell at pressures and temperatures relevant to the deep Earth's mantle. Fluorite-type U[O.sub.2] displays a new sequence of phase transitions at high P and T, with a cubic modified fluorite Pa[bar.3] observed at 18 GPa, and an orthorhombic Pbca structure from 33 GPa up to 82 GPa. Using a second-order Birch-Murnaghan equation of state, we calculated room-pressure bulk modulus [K.sub.0] = 166(7) GPa with pressure derivative [K'.sub.0] = 4.0 for the Pa[bar.3] structure, and [K.sub.0] = 225(8) GPa with [K'.sub.0] = 4 for the Pbca structure. The expected Pnma cotunnite structure was not observed but is not excluded at pressures higher than 82 GPa. Since U[O.sub.2] displays a Pbca structure stable up to 82 GPa and presents a density much higher than the average density of the surrounding mantle, U[O.sub.2] could be a host of U in the deep lower mantle. Keywords: Heat sources, uranium oxide, X-ray diffraction, crystal structure, deep mantle
- Published
- 2008