The i.r. absorption curve of “deep bed” calcined NH4Y zeolites could be broken down into the same components as HY zeolites. The frequency of the peaks was slightly changed, but their half band width remained constant. In a series of treatments representing increasing hydrolysis non-acidic OH bands around 3680 and 3600 cm–1 increase in intensity, due to surface OH groups near Al defect locations. Polynuclear Al species bridging the cubo-octahedra are suggested to be partly responsible for the increased thermal stability. The non-acidic OH bands in synthetic faujasites exchanged with polyvalent cations are explained on the same basis, since they behave in a similar way as the non-acidic bands on “deep bed” zeolites after different treatments.
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