“…The spectral features closely resembled each other containing the same frequency nine representative frequency bands with the following contributors. The C-O (V as C-O ) stretching vibration in carbonate CO 3 2− emerged in the region of 1510 to 1400 cm −1 [63,64,65], the Si-O-Si linkage-associated V as Si-O vibration in silica gel at 1243 cm −1 [66,67,68], the Al-OH bending (δ as Al-OH ) and (δ s Al-OH ) vibrations, and AlO 4 tetrahedral (V Al-O ) stretching in bohmite (γ-AlOOH), were respectively, at 1148, 1068, and 777 cm −1 , reflecting the presence of typical bohmite-related doublet peaks of O-H group at 3307 (V as O-H ) and 3086 (V s O-H ) cm −1 bands (not shown) [69,70,71,72], the M-O (M: Si or Al) (V as M-O ) in amorphous and crystalline Na 2 O-Al 2 O 3 -SiO 2 -H 2 O (N-A-S-H), CaO-Al 2 O 3 -SiO 2 -H 2 O (C-A-S-H), and CaO,Na 2 O-Al 2 O 3 -SiO 2 -H 2 O (C,N-A-S-H) hydrates appeared at 990 and 902 cm −1 [73,74,48], and the Si-O stretching (V s Si-O ) and Si-O bending (δ O-Si-O ) modes in quartz at 738 and 675 cm −1 , respectively with a possible quartz contribution to the band at 1068 cm −1 (V s Si-O ) [62]. The N-A-S-H, C-A-S-H, and C,N-A-S-H phases were assembled by the interactions between Na + and Ca 2+ released by SMS activator and CAC, and the aluminosilicate anhydrous compounds in FAF [75].…”