Of the two peaks in the temperature-programmed desorption of a copper(II)-exchanged Y-type zeolite, one, at 603 K, was the desorption of oxygen adsorbed in a non-dissociated form and another, at 773 K, resulted from the desorption of lattice oxygen induced by the adsorption of gaseous oxygen.
M. Iwamoto, S. Morita, S. Kagawa and T. Seiyama, J. Chem. Soc., Chem. Commun., 1980, 842 DOI: 10.1039/C39800000842
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