MgO melting curve constraints from shock temperature and rarefaction overtake measurements in samples preheated to 2300 K

ORAL

Abstract

In a continuous effort to determine experimentally the melting curve of MgO at 100-200 GPa, we extended our target preheating capability to 2300 K. The limit was primarily caused by intense sublimation of pure MgO in vacuum above $\sim$2050 K. Completely redesigned Mo capsules holding $\sim$20 mm long MgO crystals with controlled thermal gradients were impacted by thin Ta flyers launched at 6.5 to 7.5 km/s on the Caltech two-stage light-gas gun. Radiative shock temperatures and rarefaction overtake times were measured simultaneously by a 6-channel pyrometer with 3 ns time resolution, over 440-750 nm spectral range. All our experiments showed smooth pressure dependence of MgO sound speed consistent with the solid phase at 204-239 GPa. Observed temperatures are $\sim$1000 K lower than those predicted by the solid phase model, but the plot of measured shock temperature versus pressure exhibits a pattern typical of shock melting at the highest pressure investigated. This may suggest that the Hugoniot of MgO preheated to 2300 K crosses its melting line at 220-240 GPa. Sound speed data indistinguishable from the solid phase model do not exclude the possibility of melting there.

Authors

  • O.V. Fat'yanov

    Division of Geological and Planetary Sciences, Caltech, Pasadena, CA 91125 U.S.A.

  • P.D. Asimow

    Division of Geological and Planetary Sciences, Caltech, Pasadena, CA 91125 U.S.A.