“…The band at 830 cm −1 on the magnetite NPs belongs to the Fe–O group, while the vibrational peaks at 990 and 1100 cm −1 represent the C–H and C–O bending vibration modes [ 1 , 72 ]. The band at 1000 cm −1 that occurred on zeolite A and MAGZA composite was assigned to the asymmetric stretching vibrations of all zeolite materials such as Si–O and Al–O that may be attributed to tetrahedron bond frequencies of (Si, Al)–O along the connecting lines of [(Si, Al)O 4 ] 4-tetrahedron oxygen atoms with Si/Al central atoms [ 42 , 69 , 70 ]. Specifically, the characteristic peak at 1343 cm −1 substantiated the presence of iron corresponding to the formation of magnetite, hematite and lepidocrocite on the surfaces of Fe 0 and the MAGZA composite surfaces [ 42 ].…”