“…For t = 3 and 6 h, the spectra were fitted with a hyperfine field distribution, a discrete sextet and two doublets. The former is related to an ␣-(Fe 1 − w Al w ) 2 O 3 type of solid solution, as previously verified for 24 h milled samples of diverse concentrations [15], and the second one with magnetic ␣-Fe, hence confirming the above pointed out contamination. The Fe 2+ paramagnetic component is attributed to hercynite (FeAl 2 O 4 ), a spinel synthesizable from iron and alumina and, eventually, hematite, through a number of processes including ball-milling [17,18].…”