Compound | Appearance | Reactions |
Fe2O3 (hematite, rouge) | rust red to brown | 4 Fe(s) + 3 O2(g) ![]() |
FeO (wüstite) | jet black powder | |
FeO·Fe2O3 (magnetite) | black to brown | 3 Fe(s) + 2 O2(g) ![]() |
FeS (iron sulfuret) | gray to gray brown | Fe(s) + S(s) ![]() FeS(s) + 2 HCl(aq) ![]() |
FeS2 (pyrite, fool's gold) | shiny gold or brassy crystals | 4 FeS2(s) + 11 O2 ![]() |
FeSO4·7H2O (green vitriol) | blue-green crystals | Fe(s) + H2SO4(aq) ![]() |
Fe2(SO4)3 | gray powder | Fe2O3(s) + 3 H2SO4(aq) ![]() ![]() Fe2(SO4)3(s) ![]() |
FeCl2·4H2O | blue-green crystals | Fe(s) + 2 HCl(aq) ![]() |
FeCl3·6H2O | orange-yellow crystals | 2 FeCl2(aq) + Cl2(g) ![]() |
Iron oxides. The best known reaction of iron is rusting, in which iron reacts with oxygen and water to form red hydrated Fe2O3. Wrapping a thermometer bulb in wet steel wool results in a small but noticeable temperature rise; rusting is exothermic. The color of dried Fe2O3 is intense, and it is used as a red pigment in pints, rubber, ceramics, and glass. Burning the dry steel wool in air results in magnetite, FeO·Fe2O3, a black addition compound that is weakly magnetic.
Iron sulfides. Heating iron filings with powdered sulfur results in a strongly exothermic reaction that produces a charcoal-grey substance. While the substance is commonly identified as iron(II) sulfide, FeS, it has a complex structure and is not a stoichiometric compound (see Cotton and Wilkinson for details). FeS2 (pyrite) is a brassy, shiny mineral sometimes mistaken for gold. It is not iron(IV) sulfide; the iron is in a +2 oxidation state, combined with an S22- ion (the sulfur analog of the peroxide ion). Pyrite burns when heated to form sulfur dioxide and iron(III) oxide:
4 FeS2(s) + 11 O2 2 Fe2O3(s) + 8 SO2(g)
Iron sulfates. Iron is a fairly active metal and can easily displace hydrogen from mineral acid solutions. It reacts vigorously and exothermically with sulfuric acid to produce iron(II) sulfate:
Fe(s) + H2SO4(aq) FeSO4(aq) + H2(g)
Iron halides. Iron displaces hydrogen from hydrochloric acid to form pale green iron(II) chloride:
Fe(s) + 2 HCl(aq) FeCl2(aq) + H2(g)
Iron thiocyanates. When iron(III) ions are added to a solution containing thiocyanate ions, a series of brilliantly red complexes form (Fe(SCN)3, Fe(SCN)63-, FeSCN+2...) Thiocyanate is a sensitive test for iron(III) only- iron(II) does not cause a color change. This makes iron(II) thiocyanate useful as a quick test for the presence of peroxides and oxygen, which rapidly oxidize pale green Fe(SCN)2·3H2O crystals to red iron(III) thiocyanate.
Iron complex cyanides Both iron(II) and iron(III) ions form very stable complexes with the cyanide ion (in fact, iron is used to complex waste cyanides to render them less toxic.) The ferrocyanide (Fe(CN)64+) and ferricyanide ion (Fe(CN)63+) contain covalent iron-carbon bonds arranged octahedrally around the central iron. An intensely colored pigment can be made by combining these ions with iron in a different oxidation state:
K4Fe(CN)6(aq) + Fe3+(aq) KFe[Fe(CN)6](s) + 3 K+(aq)
K3Fe(CN)6(aq) + Fe2+(aq) KFe[Fe(CN)6](s) + 2 K+(aq)
Copyright © 1997-2010 by Fred Senese
Comments & questions to fsenese@frostburg.edu
Last Revised 02/23/18.URL: http://antoine.frostburg.edu/chem/senese/101/inorganic/faq/print-iron-reactions.shtml