Abstract

1. The IR spectra of some decationized and dealuminized mordenite samples in the 400–1800 cm−1 region were studied and an assignment of the absorption bands was made. 2. A change in the state of the water, OH groups and hydroxonium ions occurs with increase in the degree of decationization and dealuminization. 3. Both decationization and dealuminization affect the characteristic “chainlet” vibrations. The skeletal structure of mordenite is retained at high degrees of dealuminization.

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