The Hugoniot curve and sound velocity of forsterite to 1200 GPa

Abstract

The comprehension of the composition and physical state of the deep interiors of large planets, as well as the impact events pertinent to planetary formation and evolution, necessitates an understanding of the properties of planetary materials under extreme conditions. Forsterite (Mg₂SiO₄), a significant geological mineral, has not been fully characterized in terms of its behavior under shock compression due to a lack of consensus among previous experiments and simulations aimed at determining its Hugoniot, as well as the absence of knowledge of sound velocity at high pressures, a critical parameter indicative of phase transformation and melting.

Keywords

Forsterite / Hugoniot / Sound velocity / First-principles molecular dynamics / Shock compression / Lateral release

References

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