Highly ordered graphite (HOPG) to hexagonal diamond (lonsdaleite) phase transition observed on picosecond time scales using ultrafast x-ray diffraction

Michael R. Armstrong*, Harry B. Radousky, Ryan A. Austin, Oliver Tschauner, Shaughnessy Brown, Arianna E. Gleason, Nir Goldman, Eduardo Granados, Paulius Grivickas, Nicholas Holtgrewe, Matthew P. Kroonblawd, Hae Ja Lee, Sergey Lobanov, Bob Nagler, Inhyuk Nam, Vitali Prakapenka, Clemens Prescher, Evan J. Reed, Elissaios Stavrou, Peter WalterAlexander F. Goncharov, Jonathan L. Belof

*Corresponding author for this work

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2 Scopus citations

Abstract

The response of rapidly compressed highly oriented pyrolytic graphite (HOPG) normal to its basal plane was investigated at a pressure of ∼80 GPa. Ultrafast x-ray diffraction using ∼100 fs pulses at the Materials Under Extreme Conditions sector of the Linac Coherent Light Source was used to probe the changes in crystal structure resulting from picosecond timescale compression at laser drive energies ranging from 2.5 to 250 mJ. A phase transformation from HOPG to a highly textured hexagonal diamond structure is observed at the highest energy, followed by relaxation to a still highly oriented, but distorted graphite structure following release. We observe the formation of a highly oriented lonsdaleite within 20 ps, subsequent to compression. This suggests that a diffusionless martensitic mechanism may play a fundamental role in phase transition, as speculated in an early work on this system, and more recent static studies of diamonds formed in impact events.

Original languageEnglish
Article number055901
JournalJournal of Applied Physics
Volume132
Issue number5
DOIs
StatePublished - 7 Aug 2022
Externally publishedYes

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