“…A [Fe 2.5+ 2-6δ Fe 3+ 5δeδ ] B O 4 2-. Calculations of the stoichiometry deviation from relative subspectral area with two different reported formulas, δ ) 0.063 in Fe 3-δ O 4 28 and δ ) 0.057 in Fe 3-δ O 4 , 30 give a general formula of Fe 2.94 O 4 . The values of the isomer shift lead to an estimate of the Fe valence state, i.e., the Fe content; assuming the isomer shift of Fe 3+ tetra , Fe 3+ octa , and Fe 2+ octa at 0.25, 0.40, and 1.00 at 300 K, and 0.40, 0.54, and 1.15 at 77 K, respectively, one obtains Fe 2.95 O 4 .…”