Abstract
The oxidation of crystals and polycrystalline thin films was investigated with electron paramagnetic resonance (EPR) and photoelectron spectroscopy (PES). An EPR signal assigned to evolves when the samples were stored under ambient conditions for a few months, independent of the morphology of the specimens. The formation of a native oxide layer consisting of and was observed in PES during the initial stage of oxidation. Only after long term oxidation for several months an additional copper hydroxide phase, , was detected. When the phase was reduced by annealing in vacuum at or removed by etching in KCN also the EPR signal disappeared. It is shown that the EPR signal originates from the phase and the activation energy for the thermal reduction of to nonparamagnetic is . A model for the native oxidation of will be presented and implications for solar cell device performance discussed.
2 More- Received 1 April 2004
- Corrected 23 November 2004
DOI:https://doi.org/10.1103/PhysRevB.70.205321
©2004 American Physical Society
Corrections
23 November 2004