Radiation experiments have established that H+ released in SiO2 migrates to
the Si-SiO2 interface where it can induce new defects. For oxides exposed
first to high-temperature annealing and then to molecular hydrogen, mobile
positive charge believed to be H+ can be cycled to and from the interface b
y reversing the oxide electric field. We report first-principles calculatio
ns that identify atomic-scale mechanisms for the two types of behavior and
the conditions that are necessary for each. Si-Si bonds an the oxide side,
i.e., "suboxide bonds," can trap H+ in deep wells with an asymmetric barrie
r (1.5 eV on the Si side, 1 eV on the SiO2 side). In radiation experiments
these centers can act as fixed positive charge. In the mobile-positive-char
ge experiments, the protons can be cycled between opposing Si-SiO2 interfac
es if the density of suboxide bonds is high.