“…Bands at 805 cm − 1 , 688 cm − 1 , and 568 cm − 1 ascribed to -Si-O-Al(IV), -Si-O- Al(V), and -Si-O-Al(VI), respectively, appeared in the spectra of calcined kaolin. ese bands disappeared after geopolymerization, and new bands at 726 cm − 1 , indicative of the formation of -P-O-Al-, were observed in the spectra of PAG [12]. e bands at 926 cm − 1 are attributed to -P-O-Pvibrations [12,13].…”