Abstract
We report continuous measurements of the sound velocity along the principal Hugoniot curve of quartz between 0.25 and 1.45 TPa, as determined from lateral release waves intersecting the shock front as a function of time in decaying-shock experiments. The measured sound velocities are lower than predicted by prior models, based on the properties of stishovite at densities below , but agree with density functional theory molecular dynamics calculations and an empirical wide-regime equation of state presented here. The Grüneisen parameter calculated from the sound velocity decreases from at 0.25 TPa to 0.66 at 1.45 TPa. In combination with evidence for increased (configurational) specific heat and decreased bulk modulus, the values of suggest a high thermal expansion coefficient at , where is thought to be a bonded liquid. From our measurements, dissociation of the molecular bonds persists to , consistent with estimates by other methods. At higher densities, the sound velocity is close to predictions from previous models, and the Grüneisen parameter approaches the ideal gas value.
- Received 25 December 2017
DOI:https://doi.org/10.1103/PhysRevLett.120.215703
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