Conclusions
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1.
The mobility of surface hydrogen increases in passing from faujasite to mordenite structure, and increasing the degree of surface dehydroxylation.
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2.
The increase in the zeolite structure stability observed in going from X to Y to mordenite is accompanied by an increase in the OH group thermal stability. Breakdown of the mordenite crystal structure leads to a reduction in the OH group concentration.
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Translated from Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, No. 11, pp. 2426–2430, November, 1976.
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Minachev, K.M., Dmitriev, R.V., Bronnikov, O.D. et al. Deuterium exchange with the surface hydrogen of zeolite catalysts. Russ Chem Bull 25, 2263–2267 (1976). https://doi.org/10.1007/BF00973373
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DOI: https://doi.org/10.1007/BF00973373