• Product NameFerric oxide
  • CasNo. 1309-37-1
  • MFFe2O3
  • MW159.70
  • Purity
  • Appearancered to reddish-brown powder
  • Packing
  • Contact usInquiry

Product Details

CasNo: 1309-37-1

MF: Fe2O3

Appearance: red to reddish-brown powder

Quality Factory Supply Ferric oxide 1309-37-1, Sale with Competitive Price

  • Molecular Formula:Fe2O3
  • Molecular Weight:159.70
  • Appearance/Colour:red to reddish-brown powder 
  • Melting Point:1538 °C 
  • Flash Point:>230°F 
  • PSA:43.37000 
  • Density:5.24 g/cm3 
  • LogP:-0.31100 
  • IDLH: 2500 mg/m3 (as Fe)See: 1309371  

Ferric oxide(Cas 1309-37-1) Usage

Description

Ferric oxide is the inorganic compound with the formula Fe2O3. It is one of the three main oxides of iron, the other two being iron(II) oxide (FeO) the rarer form, and iron(II,III) oxide (Fe3O4) which naturally as magnetite.
Pharmaceutical Uses Ferric oxide red (Fe2O3), also known as iron (III) oxide, is a coloring agent for tablets and capsules and is used in the pharmaceutical industry. Ferric oxide red occurs naturally as hematite ore and rust. Iron oxides are also commonly used in the cosmetics industry.

InChI:InChI=1/2Fe.3O/rFe2O3/c3-1-5-2-4

1309-37-1 Relevant articles

The electrical properties of alpha ferric oxide—II.: Ferric oxide of high purity

R.F.G. Gardner, F. Sweett, D.W. Tanner

Journal of Physics and Chemistry of Solids Volume 24, Issue 10, October 1963, Pages 1183-1186, IN1-IN2, 1187-1196

Values are reported for the d.c. conductivity and Seebeck voltage of several specimens of high-purity polycrystalline alpha ferric oxide between 20°C and 1350°C. It is found that carriers arising from deviations in stoichiometry contribute to conduction in fired specimens.

Mechanism of Solid-state Reaction Between Magnesium Oxide and Aluminum Oxide and Between Magnesium Oxide and Ferric Oxide

R. E. CARTER

, Journal of the American Ceramic Society, Volume44, Issue3 March 1961 Pages 116-120

Inert marker experiments have shown that the solid-state reactions forming MgAl2O4 and MgFe2O4 occur by counterdiffusion of the Mg2+, Fe3+, and A13+ ions through the relatively rigid oxygen lattice of the spinel or ferrite. It is suggested that earlier claims that ZnAl2O4 forms by diffusion of Zn2+ and O2- ions were probably due to a splitting of the markers, leaving some marker on the specimen surface.

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