Phase Transition Mechanism of Hexagonal Graphite to Hexagonal and Cubic Diamond: Ab-initio Simulation
Ranjan Mittal, Mayanak Kumar Gupta, Samrath Lal Chaplot

TL;DR
This study uses ab-initio simulations to uncover the atomic mechanisms behind the phase transition of hexagonal graphite to diamond forms under high pressure, highlighting the role of layer sliding, puckering, and phonon modes.
Contribution
It provides detailed atomic-level insights into the phase transition pathways from hexagonal graphite to both hexagonal and cubic diamond, including the role of phonons and vibrational energies.
Findings
HG to HD transition occurs rapidly within 0.2 ps with layer sliding and puckering.
HG to CD transition involves complex cooperative layer displacements.
Phonon soft modes facilitate the phase transition, and vibrational energies stabilize HG at higher pressures.
Abstract
We have performed ab-initio molecular dynamics simulations to elucidate the mechanism of the phase transition at high pressure from hexagonal graphite (HG) to hexagonal diamond (HD) or to cubic diamond (CD). The transition from HG to HD is found to occur swiftly in very small time of 0.2 ps, with large cooperative displacements of all the atoms. We observe that alternate layers of atoms in HG slide in opposite directions by (1/3, 1/6, 0) and (-1/3, -1/6, 0), respectively, which is about 0.7 {\AA} along the pm[2, 1, 0] direction, while simultaneously puckering by about pm0.25 {\AA} perpendicular to the a-b plane. The transition from HG to CD occurred with more complex cooperative displacements. In this case, six successive HG layers slide in pairs by 1/3 along [0, 1, 0], [-1, -1, 0] and [1, 0, 0], respectively along with the puckering as above. We have also performed calculations of the…
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