Thermal oxidation of atomic defects on a graphite surface, produced by low energy (50–200 eV) impact of Ar+ and Kr+ ions, leads to the formation of pits with a diameter of several nm. These pits are generated from both carbon vacancy defects and interstitial defects, the latter formed by trapping of incident ions in-between graphite layers. The probability of the pit formation is measured for each type of defect. Nearly all vacancy defects (>90%) are developed into pits by thermal oxidation in air at 560 °C, while only a small portion (<15%) of the interstitial defects are converted into pits.
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Hahn et al. (1999) studied this question.
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