| Section2 = {{Chembox Properties
| Formula = Cr2O3
| MolarMass = 151.99 g/mol
| Density = 5.22 g/cm3
| Solvent =
alcohol
| SolubleOther = insoluble
| Solubility = insoluble
| MeltingPtC = 2435
| BoilingPtC = 4000
| RefractIndex = 2.5
}}
}}
Chromium(III) oxide is the
inorganic compound of the
formula Cr2O3. It is one of principal oxides of
chromium and is used as a pigment. In nature, it occurs as the rare mineral eskolaite.
Structure and properties
Cr2O3 adopts the
corundum structure, consisting of a hexagonal close packed array of oxide anions with 2/3 of the octahedral holes occupied by chromium. Similar to corundum, Cr2O3 is a hard, brittle material (
Mohs hardness 8-8.5).
It is
antiferromagnetic up to 307 K, the Neel temperature.J.E Greedon, (1994),
Magnetic oxides in Encyclopedia of Inorganic chemistry R. Bruce King, Ed. John Wiley & Sons. ISBN 0471936200A. F. Holleman and E. Wiberg "Inorganic Chemistry" Academic Press, 2001, New York. ISBN 0-12-352651-5. It not readily attacked by acids or bases, although molten alkali gives chromites (salts with the CrO anion, not to be confused with the related mineral
chromite).
Occurrence
Cr2O3 occurs naturally in mineral
Eskolaite, which is found in chromium-rich termolite skarns, metaquartzites, and chlorite veins. Eskolaite is also a rare component of chondrite meteorites. The mineral is named after Finnish geologist
Pentti Eskola.
Production
The Parisians Pannetier and Binet first prepared the transparent hydrated form of Cr2O3 in 1838 via a secret process, sold as a pigment.{{cite book
| title = The pigment compendium: a dictionary of historical pigments
| first1 = Nicholas | last1 = Eastaugh
| first2 = Tracey | last2 = Chaplin
| first3 = Ruth | last3 = Siddall
| publisher = Butterworth-Heinemann
| year = 2004
| isbn = 0750657499
| page = 391
}} It is derived from the mineral
chromite, (Fe,Mg)Cr2O4. The conversion of chromite to chromia proceeds via
Na2Cr2O7, which is reduced with sulfur at high temperatures:Gerd Anger, Jost Halstenberg, Klaus Hochgeschwender, Christoph Scherhag, Ulrich Korallus, Herbert Knopf, Peter Schmidt, Manfred Ohlinger, "Chromium Compounds" in Ullmann's Encyclopedia of Industrial Chemistry, Wiley-VCH, Weinheim, 2005.
Na2Cr2O7 + S → Na2SO4 + Cr2O3
The oxide is also formed by the decomposition of chromium salts such as chromium nitrate or by the exothermic decomposition of ammonium dichromate.
(NH4)2Cr2O7 → Cr2O3 + N2 + 4 H2O
The reaction has a low ignition temperature of less than 200 C and is frequently used in "volcano" demonstrations.
Ammonium dichromate volcano Retrieved 2009-06-06.
Chromium oxide can be converted into elemental chromium metal through a
thermite-like reaction: unlike iron oxide thermites, chromium oxide thermites creates few or no sparks, smoke or sound, but glow brightly. Because of the very high melting point of chromium, chromium thermite casting is impractical.
Applications
Because of its considerable stability, chromia is commonly used pigment and was originally called
viridian. It is used in paints, inks, and glasses. It is the colourant in "chrome green" and "institutional green." Chromium(III) oxide is the precursor to the magnetic pigment
chromium dioxide, according to the following reaction:
Cr2O3 + 3 CrO3 → 5 CrO2 + O2
Reactions
Chromium(III) oxide is
amphoteric. Although insoluble in water, it dissolves in acid to produce hydrated chromium ions,
Cr(H2O)63+. It dissolves in concentrated alkali to yield chromite ions. When heated finely divided aluminium or carbon, it is reduced to chromium metal and
aluminum oxide:
Cr2O3 + 2 Al → 2 Cr + Al2O3
Heating with chlorine and carbon yields
chromium(III) chloride:
Cr2O3 + 3 Cl2 + 3 C → 2 CrCl3 + 3 CO
References
See also