Iron(II) oxide
From Wikipedia, the free encyclopedia
Iron(II) oxide |
---|
![]() |
![]() |
Names |
Iron(II) oxide |
Other names Ferrous oxide,iron monoxide |
Identifiers |
CAS Registry Number |
ChEBI |
ChemSpider |
InChI[show] |
Jmol-3D images |
PubChem |
SMILES[show] |
UNII |
Properties |
Chemical formula |
Molar mass |
Appearance |
Density |
Melting point |
Boiling point |
Solubility in water |
Solubility |
Refractive index(nD) |
Hazards |
Main hazards |
Safety data sheet |
NFPA 704 |
Autoignition temperature |
Related compounds |
Other anions |
Other cations |
Related compounds |
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa). |
![]() ![]() ![]() |
Infobox references |
Iron(II) oxide is the inorganic compound with the formula FeO. Its mineral form is known as wüstite. One of several iron oxides, it is a black-colored powder that is sometimes confused with rust, which consists of hydrated iron(III) oxide (ferric oxide). Iron(II) oxide also refers to a family of related non-stoichiometric compounds, which are typically iron deficient with compositions ranging from Fe0.84O to Fe0.95O.[2]
Contents
[hide]
Preparation[edit]
FeO can be prepared by the thermal decomposition of iron(II) oxalate.
FeC2O4 → FeO + CO2 + CO
The procedure is conducted a protective atmosphere to avoid the formation of ferric oxide. A similar procedure can also be used for the synthesis of manganous oxide and stannous oxide.[3][4]
Stoichiometric FeO can be prepared by heating Fe0.95O with metallic iron at 770 °C and 36 kbar.[5]
Reactions[edit]
FeO is thermodynamically unstable below 575 °C, tending to disproportionate to metal and Fe3O4:[2]
4FeO → Fe + Fe3O4
Structure[edit]
Iron(II) oxide adopts the cubic, rock salt structure, where iron atoms are octahedrally coordinated by oxygen atoms and the oxygen atoms octahedrally coordinated by iron atoms. The non-stoichiometry occurs because of the ease of oxidation of FeII to FeIIIeffectively replacing a small portion of FeII with two thirds their number of FeIII, which take up tetrahedral positions in the close packed oxide lattice.[5]
Below 200 K there is a minor change to the structure which changes the symmetry to rhombohedral and samples becomeantiferromagnetic.[5]
Occurrence in nature[edit]
Iron(II) oxide makes up approximately 9% of the Earth's mantle. Within the mantle, it may be electrically conductive, which is a possible explanation for perturbations in Earth's rotation not accounted for by accepted models of the mantle's properties.[6]
Uses[edit]
Iron(II) oxide is used as a pigment. It is FDA-approved for use in cosmetics and it is used in some tattoo inks. It can also be used for filtering phosphates from home aquaria.
References[edit]
Jump up^ Pradyot Patnaik. Handbook of Inorganic Chemicals. McGraw-Hill, 2002, ISBN 0-07-049439-8
^ Jump up to:a b Greenwood, Norman N.; Earnshaw, Alan (1997). Chemistry of the Elements (2nd ed.). Butterworth-Heinemann. ISBN 0080379419.
Jump up^ H. Lux "Iron (II) Oxide" in Handbook of Preparative Inorganic Chemistry, 2nd Ed. Edited by G. Brauer, Academic Press, 1963, NY. Vol. 1. p. 1497.
Jump up^ Practical Chemistry for Advanced Students, Arthur Sutcliffe, 1930 (1949 Ed.), John Murray - London
^ Jump up to:a b c Wells A.F. (1984) Structural Inorganic Chemistry 5th edition Oxford University Press ISBN 0-19-855370-6
External links[edit]
|
---|
|
---|
|
---|
Navigation menu
Not logged in
Początek formularza
Dół formularza
Interaction
Tools
Print/export
Languages
This page was last modified on 17 September 2015, at 16:45.