Diamond, as the densest
allotrope of carbon, displays a range of
exemplary material properties that are attractive from a device perspective.
Despite diamond displaying high carbon–carbon bond strength,
ultrashort (femtosecond) pulse laser radiation can provide sufficient
energy for highly localized internal breakdown of the diamond lattice.
The less-dense carbon structures generated on lattice breakdown are
subject to significant pressure from the surrounding diamond matrix,
leading to highly unusual formation conditions. By tailoring the laser
dose delivered to the diamond, it is shown that it is possible to
create continuously modified internal tracks with varying electrical
conduction properties. In addition to the widely reported conducting
tracks, conditions leading to semiconducting and insulating written
tracks have been identified. High-resolution transmission electron
microscopy (HRTEM) is used to visualize the structural transformations
taking place and provide insight into the different conduction regimes.
The HRTEM reveals a highly diverse range of nanocarbon structures
are generated by the laser irradiation, including many signatures
for different so-called diaphite complexes, which have been seen in
meteorite samples and seem to mediate the laser-induced breakdown
of the diamond. This work offers insight into possible formation methods
for the diamond and related nanocarbon phases found in meteorites.