1982 Volume 51 Issue 3 Pages 705-706
In the thermal desorption spectra (TDS) of molecular oxygen, three peaks of isotopically exchanged molecules 16O18O at 210, 260 and 650 K and a single peak of 16O2 at 690 K are observed after adsorption of 18O2 on UV-irradiated MgO powders. The formation of exchanged species is shown to be related to the presence of Fs+ centers on the surfaces.
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