“…To our best knowledge, only Bordiga et al assigned this band to “extra lattice or partially extra lattice Al–OH vibrations”. Many researchers associate the appearance of both the ∼3680 cm –1 H-SAPO-34 and ∼3660 cm –1 H-CHA FTIR bands with sample hydrolysis, showing that the intensity of these bands substantially increases in the presence of H 2 O. − ,, It has been also reported that the acidic OH groups of both molecular sieves tend to connect at least 1 molecule, but often 3 or 4 H 2 O molecules, via hydrogen bonds. ,, However, our measurements were carried out on samples calcined at 500 °C or higher temperatures in air, and in addition they were also in situ evacuated at ∼10 –5 Torr at 500 °C before both the TR and the DRIFT measurements, which were carried out at room temperature afterward. This pretreatment removes all molecular water from the zeolites as one could confirm from the lack of any measurable 1640 cm –1 FTIR band, associated with the well-known bending vibration of molecular water.…”