Abstract

The unit cell volume of periclase (MgO) has been measured under high pressures and high temperatures up to 10 GPa and 1400°C. The measurement was made by an in situ X ray diffraction technique with the DIA-type high multianvil high-pressure apparatus (SAM85) installed at the superconducting wiggler beamline at the National Synchrotron Light Source (NSLS, X17B). In order to avoid the effect of microscopic stress, a chunk of MgO sintered with a piston cylinder apparatus was used for the measurement. Special care was taken to obtain deviatoric-stress-free spectra; for the room temperature measurement, a liquid pressure medium was used, and in the high temperature experiments, the relaxation of deviatoric stress by the heating treatment was always checked. As a result, very precise unit cell volumes of MgO were determined using its six to eight diffraction peaks. MgO showed no structural distortion in the P-T conditions in this study. Fitting the experimental P-T-V data to the high-temperature Birch-Murnaghan equation of state yields K 0 = 153(3) GPa and (∂K T /∂T) p = -0.034(3) GPa/K, assuming a constant value of 4 for K' T,0 . The high temperature equation of state of MgO can be used as an experimental pressure standard in high P-T condition where NaCl scale is useless.

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