Abstract
The structure and thermal response of amorphous ion tracks formed along the ½11 20 , ½10 10 , and [0001]-directions in crystalline quartz have been investigated using small angle x-ray scattering. The radii of the ion tracks vary by about 5% (0.3 nm) for tracks along different crystallographic directions. Molecular dynamics simulations reproduce this anisotropy along the ½10 10 and [0001] directions and suggest that differences in thermal conductivity along these directions are partly responsible for this observation. Using in situ annealing, tracks along the ½10 10 and [0001] directions were shown to recrystallize during thermal annealing around 9601020 C with activations energies around 6 eV, while those along the ½11 20 -direction already disappeared at 640 C with a significantly lower activation energy around 34 eV.
Original language | English |
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Journal | Journal of Applied Physics |
Volume | 118 |
Issue number | 22 |
DOIs | |
Publication status | Published - 2015 |