Iron(III) oxide: Wikis


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From Wikipedia, the free encyclopedia

Iron(III) oxide
CAS number 1309-37-1
PubChem 518696
RTECS number NO7400000
Molecular formula Fe2O3
Molar mass 159.69 g/mol
Appearance red-brown solid
Odor odorless
Density 5.242 g/cm3, solid
Melting point

1566 °C (1838 K) decomp.

Solubility in water insoluble
Crystal structure rhombohedral
Std enthalpy of
−825.50 kJ/mol
EU classification not listed
Flash point non-flammable
Related compounds
Other anions iron(III) fluoride
Other cations manganese(III) oxide, cobalt(III) oxide
Related compounds iron(II) oxide, iron(II,III) oxide
Except where noted otherwise, data are given for materials in their standard state (at 25 °C, 100 kPa)
Infobox references

Iron(III) oxide is the inorganic compound with the formula Fe2O3. It is of one of the three main oxides of iron, the other two being FeO, which is rare, and Fe3O4, which also occurs naturally as the mineral magnetite. As the mineral known as hematite, Fe2O3 is the main source of the iron for the steel industry. Fe2O3 is paramagnetic, reddish brown, and readily attacked by acids. Rust is often called iron(III) oxide, and to some extent, this label is useful, because rust shares several properties and has a similar composition. To a chemist, rust is considered an ill-defined material, described as hydrated ferric oxide.


Different forms


Alpha phase

α-Fe2O3 has the rhombohedral, corundum (α-Al2O3) structure and is the most common form. It occurs naturally as the mineral hematite which is mined as the main ore of iron. It is antiferromagnetic below ~260 K (Morin transition temperature), and weak ferromagnetic between 260 K and 950 K (Neel temperature).[1] It is easy to prepare using both thermal decomposition and precipitation in the liquid phase. Its magnetic properties are dependent on many factors, e.g. pressure, particle size, and magnetic field intensity.

Beta phase

Cubic face centered, metastable, at temperatures above 500 °C converts to alpha phase. It can be prepared by reduction of hematite by carbon, pyrolysis of iron(III) chloride solution, or thermal decomposition of iron(III) sulfate.

Gamma phase

Cubic, metastable, converts to the alpha phase at high temperatures. Occurs naturally as the mineral maghemite. Ferrimagnetic. Ultrafine particles smaller than 10 nanometers are superparamagnetic. Can be prepared by thermal dehydratation of gamma iron(III) oxide-hydroxide, careful oxidation of iron(II,III) oxide. The ultrafine particles can be prepared by thermal decomposition of iron(III) oxalate.

Epsilon phase

Rhombic, shows properties intermediate between alpha and gamma. So far has not been prepared in pure form; it is always mixed with the alpha phase or gamma phases. Material with a high proportion of epsilon phase can be prepared by thermal transformation of the gamma phase. The epsilon phase is metastable, transforming to the alpha phase at between 500 and 750 °C. Can also be prepared by oxidation of iron in an electric arc or by sol-gel precipitation from iron(III) nitrate.

Other phases

High pressure, amorphous.[2]


Iron(III) oxide dissolves readily in strong acid, e.g. hydrochloric and sulfuric acids. It also dissolves well in solutions of the chelating agents such as EDTA and oxalic acid.

It also used in an extremely exothermic reaction called a thermite reaction.[3]

2 Al + Fe2O3 → 2 Fe + Al2O3

This process was once used in welding.


Iron industry

The overwhelming application of Iron(III) oxide is as the feedstock of the steel and iron industries, e.g. the production of pure iron, steel, and many alloys.[4]


A very fine powder of ferric oxide is known as jeweler's rouge, red rouge, or simply rouge. It is used to put the final polish on metallic jewelry and lenses, and historically as a cosmetic.

Rouge cuts more slowly than some modern polishes, such as cerium(IV) oxide, but is still used in optics fabrication and by jewelers for the superior finish it can produce. When polishing gold, the rouge slightly stains the gold, which contributes to the appearance of the finished piece. Rouge is sold as a powder, paste, laced on polishing cloths, or solid bar (with a wax or grease binder). Other polishing compounds are also often called "rouge", even when they do not contain iron oxide. Jewelers remove the residual rouge on jewelry by use of ultrasonic cleaning.


Iron(III) oxide is also used as a pigment, under names "Pigment Brown 6", "Pigment Brown 7", and "Pigment Red 101"[5]. Some of them, e.g. Pigment Red 101 and Pigment Brown 6, are Food and Drug Administration (FDA)-approved for use in cosmetics.


Nanoparticles of iron(III) oxide are biocompatible, non-toxic, are chemically active on their surface, and are paramagnetic at particle sizes above a critical limit of about 5 nanometers[citation needed] . They find wide use in biomedical applications. Can be used as contrast agents in magnetic resonance imaging, in labeling of cancerous tissues, magnetically controlled transport of pharmaceuticals, localized thermotherapy (where the tissue is labeled by iron oxide nanoparticles, then heated by application of AC field to particles), and preparation of ferrofluids.[2]


Iron (III) oxide is a product of the oxidation of iron. It can be prepared in the laboratory by electrolyzing a solution of sodium bicarbonate, an inert electrolyte, with an iron anode:

2 Fe + 3/2 O2 + H2O → 2 FeO(OH)
2 FeO(OH) → Fe2O3 + H2O

At about 200 °C, the iron(III) hydroxide converts into Fe2O3.[4]

See also


  1. ^ J.E Greedon, (1994), Magnetic oxides in Encyclopedia of Inorganic chemistry Ed. R. Bruce King, John Wiley & Sons ISBN 0471936200
  2. ^ a b "Oxid železitý, Fe2O3" (in Czech). Retrieved 20. JUN 2009. 
  3. ^ Adlam & Price, Higher School Certificate Inorganic Chemistry, Leslie Slater Price, 1945.
  4. ^ a b Greenwood, N. N.; & Earnshaw, A. (1997). Chemistry of the Elements (2nd Edn.), Oxford:Butterworth-Heinemann. ISBN 0-7506-3365-4.
  5. ^ Paint and Surface Coatings: Theory and Practice William Andrew Inc. ISBN 1884207731

External links

Simple English

Iron(III) oxide

Iron(III) oxide, also known as rust, is a reddish substance. It has a chemical formula of Fe2O3. It is made by the reaction of iron with oxygen. It is found naturally in the ground. It is a major ore of iron (iron comes from this mineral) as haematite. It dissolves in acids.

The iron is in the +3 oxidation state, which is what the III means. If the iron was in the +2 oxidation state, it would be iron(II) oxide.

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