Conclusions
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1.
The concentrations and mobilities of hydrogen in decationized zeolites of type X and Y with various residual contents of Na+ were determined by the method of isotopic exchange with deuterium.
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2.
The content and mobility of hydrogen are a maximum in the ultrastable type Y zeolite.
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Translated from Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, No. 2, pp. 289–294, February, 1974.
Coworkers of the K. Schorlemmer Higher Technical School, Merseburg, German Democratic Republic.
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Mitiachev, K.M., Bremer, G., Dmitriev, R.V. et al. Exchange of deuterium with hydrogen of the surface of zeolite catalysts. Russ Chem Bull 23, 261–265 (1974). https://doi.org/10.1007/BF00924665
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DOI: https://doi.org/10.1007/BF00924665