Abstract
Laser generated shock reflectance data show that diamond undergoes a continuous transition from optically absorbing to reflecting between Hugoniot pressures . The data are consistent with diamond having a thermal population of carriers at , undergoing band overlap metallization at and melting at . The results agree well with an equation of state model that predicts that elemental carbon remains solid throughout the interior of Neptune.
- Received 7 April 2004
DOI:https://doi.org/10.1103/PhysRevLett.93.195506
©2004 American Physical Society