“…This band may originate from a weak dealumination of the structure during the air calcination process, thus producing some extraframework aluminium species (EFALS) [2,3]. Such attribution is fully supported as other dealuminated zeolites also exhibit such 3670 cm −1 band [14,17,[22][23][24][25]. Although this weak band appears clearly in the H-MCM-22 of Delgado et al's sample (see the bold line blank spectrum in bottom inset of their Fig.…”