Shock Compressing Diamond to a Conducting Fluid

D. K Bradley, J. H. Eggert, D. G. Hicks, P. M. Celliers, S. J. Moon, R. C. Cauble, and G. W. Collins
Phys. Rev. Lett. 93, 195506 – Published 5 November 2004

Abstract

Laser generated shock reflectance data show that diamond undergoes a continuous transition from optically absorbing to reflecting between Hugoniot pressures 600<PH<1000GPa. The data are consistent with diamond having a thermal population of carriers at PH600GPa, undergoing band overlap metallization at PH1000GPa and melting at 800<PH<1000GPa. The results agree well with an equation of state model that predicts that elemental carbon remains solid throughout the interior of Neptune.

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  • Received 7 April 2004

DOI:https://doi.org/10.1103/PhysRevLett.93.195506

©2004 American Physical Society

Authors & Affiliations

D. K Bradley, J. H. Eggert, D. G. Hicks, P. M. Celliers, S. J. Moon, R. C. Cauble, and G. W. Collins

  • Lawrence Livermore National Laboratory, Livermore, California 94551, USA

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Issue

Vol. 93, Iss. 19 — 5 November 2004

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