“…On this background appear several sharp reflection peaks at 2θ 26.7, 28.5, 29.7 31.8, 36, 39, 7.6, and 56.5°. These peaks may be assigned to quartz SiO 2 (main peak at 26°; OCD: 96-900-0776) [ 20 ], calcite (main peak at 29.7°; OCD: 96-101-0963), albite, NaAlSi 3 O 8 (25.2, 26, 28.5 and 29.7°; OCD: 96-900-3703) and sphalerite, ZnS (28.5, 36, 47.6 and 56.5°; OCD: 96-900-0108), which are assumed to be remains of the filler materials, or formed after pyrolysis [ 21 ]. The diffractogram of M-AC shows peaks at 2θ of 30, 35.5, 53.6, 57.6, and 62.8°, which indicate the crystalline patterns of magnetite (Fe 3 O 4 ; 96-900-2317) or maghemite (γ-Fe 2 O 3 ; OCD: 96-900-6317) [ 22 ], which indicates that both the magnetic oxides of iron, i.e., magnetite and maghemite, are impregnated on the surface of the AC.…”