Abstract
Iron, a transition metal, represents 5% of the earth’s crust. It exists in a variety of oxidation states ranging from the zero-valent metal itself to Fe(VI), occurring in such diverse forms as iron disulfide (FeS2, “fool’s gold”), iron oxides, including magnetite (Fe304), and hemoglobin. However, the Fe(II) and Fe(III) oxidation states (Equation 1) are of the most relevance in the present discussion.
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Bergeron, R.J., Wiegand, J., McManis, J.S., Weimar, W.R., Huang, G. (2002). Structure-Activity Relationships Among Desazadesferrithiocin Analogues. In: Hershko, C. (eds) Iron Chelation Therapy. Advances in Experimental Medicine and Biology, vol 509. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-0593-8_9
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DOI: https://doi.org/10.1007/978-1-4615-0593-8_9
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