Abstract
Laser resonance enhanced multiphonon ionization spectroscopy was used to measure yields and velocity distributions of the D (S2), O (P2,1,03), and O(D21) produced during low-energy (5–120 eV) electron-beam irradiation of amorphous D2O 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.