Abstract
This study shows that the MWW structure is more stable than previously known zeolites. Structural, thermal and spectroscopic analyses have shown that acid MCM-22 zeolite is stable up to 1373K under vacuum and to 1473K in air. The Brönsted hydroxyl groups withstand temperatures up to 1173K. At 1473K there is a phase transition from the MWW structure into α-cristobalite when the sample is under vacuum while for the sample treated in air only a small fraction of the total is transformed to α-cristobalite at 1473K.
| Lingua originale | Inglese |
|---|---|
| pagine (da-a) | 1426-1430 |
| Numero di pagine | 5 |
| Rivista | Studies in Surface Science and Catalysis |
| Volume | 154 B |
| DOI | |
| Stato di pubblicazione | Pubblicato - 2004 |
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