Abstract
Laser resonance enhanced multiphonon ionization spectroscopy was used to measure yields and velocity distributions of the D , O , and produced during low-energy (5–120 eV) electron-beam irradiation of amorphous O ice. Electron-stimulated dissociation has a very low energy threshold ( 6–7 eV), and the neutral fragments desorb with low kinetic energies ( 60–85 meV) which are independent of the incident electron energy. The data suggest that desorption of neutral fragments results from dissociation of excited states formed directly or via electron-ion recombination.
- Received 1 May 1995
DOI:https://doi.org/10.1103/PhysRevLett.75.2606
©1995 American Physical Society