Iron(III) oxide-hydroxide
Samples of iron(III) oxide-hydroxide monohydrate in a vial, and a spoon
Names
IUPAC name
Iron(III) oxide-hydroxide
Other names
Metaferric acid
Ferric oxyhydroxide
Goethite
Identifiers
3D model (JSmol)
ChemSpider
ECHA InfoCard 100.039.754
EC Number
  • 215-176-6
MeSH Goethite
UNII
  • InChI=1S/Fe.H2O.O/h;1H2;/q+1;;/p-1 checkY
    Key: AEIXRCIKZIZYPM-UHFFFAOYSA-M checkY
  • O=[Fe]O
Properties
FeO(OH)
Appearance Vivid, dark orange, opaque crystals
Odor odorless
Density 4.25 g/cm3
insoluble at pH 7
2.79×10−39 for Fe(OH)3[1]
Hazards
NFPA 704 (fire diamond)
NFPA 704 four-colored diamond
1
0
0
Pharmacology
B03AB04 (WHO)
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
checkY verify (what is checkY☒N ?)
Infobox references

Iron(III) oxide-hydroxide or ferric oxyhydroxide[2] is the chemical compound of iron, oxygen, and hydrogen with formula FeO(OH).

The compound is often encountered as one of its hydrates, FeO(OH)·nH
2O [rust]. The monohydrate FeO(OH)·H
2O is often referred to as iron(III) hydroxide Fe(OH)
3,[3] hydrated iron oxide, yellow iron oxide, or Pigment Yellow 42.[3]

Natural occurrences

Minerals

Anhydrous ferric hydroxide occurs in the nature as the exceedingly rare mineral bernalite, Fe(OH)3·nH2O (n = 0.0–0.25).[4][5] Iron oxyhydroxides, FeOOH, are much more common and occur naturally as structurally different minerals (polymorphs) denoted by the Greek letters α, β, γ and δ.

  • Goethite, α-FeO(OH), has been used as an ochre pigment since prehistoric times.
  • Akaganeite is the β polymorph,[6] formed by weathering and noted for its presence in some meteorites and the lunar surface. However, recently it has been determined that it must contain some chloride ions to stabilize its structure, so that its more accurate formula is FeO
    0.833    (OH)
    1.167    Cl
    0.167     or Fe
    6    O
    5    (OH)
    7    Cl    .[7]
  • Lepidocrocite, the γ polymorph, is commonly encountered as rust on the inside of steel water pipes and tanks.
  • Feroxyhyte (δ) is formed under the high pressure conditions of sea and ocean floors, being thermodynamically unstable with respect to the α polymorph (goethite) at surface conditions.

Non-mineral

Goethite and lepidocrocite, both crystallizing in orthorhombic system, are the most common forms of iron(III) oxyhydroxide and the most important mineral carriers of iron in soils.

Mineraloids

Iron(III) oxyhydroxide is the main component of other minerals and mineraloids:

Properties

The color of iron(III) oxyhydroxide ranges from yellow through dark-brown to black, depending on the degree of hydration, particle size and shape, and crystal structure.

Structure

The crystal structure of β-FeOOH (akaganeite) is that of hollandite or BaMn
8O
16. The unit cell is tetragonal with a = 1.048 and c = 0.3023 nm, and contains eight formula units of FeOOH. Its dimensions are about 500 × 50 × 50 nm. Twinning often produces particles with the shape of hexagonal stars. [2]

Chemistry

On heating, β-FeOOH decomposes and recrystallizes as α-Fe
2O
3 (hematite).[2]

Uses

Limonite, a mixture of various hydrates and polymorphs of ferric oxyhydroxide, is one of the three major iron ores, having been used since at least 2500 BC.[8][9]

Yellow iron oxide, or Pigment Yellow 42, is Food and Drug Administration (FDA) approved for use in cosmetics and is used in some tattoo inks.

Iron oxide-hydroxide is also used in aquarium water treatment as a phosphate binder.[10]

Iron oxide-hydroxide nanoparticles have been studied as possible adsorbents for lead removal from aquatic media.[11]

Medication

Iron polymaltose is used in treatment of iron-deficiency anemia.

Production

Iron(III) oxyhydroxide precipitates from solutions of iron(III) salts at pH between 6.5 and 8.[12] Thus the oxyhydroxide can be obtained in the lab by reacting an iron(III) salt, such as ferric chloride or ferric nitrate, with sodium hydroxide:[13]

FeCl
3 + 3 NaOH → Fe(OH)
3 + 3 NaCl
Fe(NO
3)
3 + 3 NaOH → Fe(OH)
3 + 3 NaNO
3

In fact, when dissolved in water, pure FeCl
3 will hydrolyze to some extent, yielding the oxyhydroxide and making the solution acidic:[12]

FeCl
3 + 2 H
2O ↔ FeOOH + 3 HCl

Therefore, the compound can also be obtained by the decomposition of acidic solutions of iron(III) chloride held near the boiling point for days or weeks:[14]

FeCl
3 + 2 H
2O → FeOOH(s) + 3 HCl(g)

(The same process applied to iron(III) nitrate Fe(NO
3)
3 or perchlorate Fe(ClO
4)
3 solutions yields instead particles of α-Fe
2O
3.[14])

Another similar route is the decomposition of iron(III) nitrate dissolved in stearic acid at about 120 °C.[15]

The oxyhydroxide prepared from ferric chloride is usually the β polymorph (akaganeite), often in the form of thin needles.[14][16]

The oxyhydroxide can also be produced by a solid-state transformation from iron(II) chloride tetrahydrate FeCl
2·4H
2O.[6]

The compound also readily forms when iron(II) hydroxide is exposed to air:

4Fe(OH)
2 + O
2 → 4 FeOOH + 2 H
2O

The iron(II) hydroxide can also be oxidized by hydrogen peroxide in the presence of an acid:

2Fe(OH)
2 + H
2O
2 → 2 Fe(OH)
3

See also

References

  1. ↑ "Solubility product constants at 25 oC". Archived from the original on 2015-02-26. Retrieved 2015-02-23.
  2. 1 2 3 A. L. Mackay (1960): "β-Ferric Oxyhydroxide". Mineralogical Magazine (Journal of the Mineralogical Society), volume 32, issue 250, pages 545-557. doi:10.1180/minmag.1960.032.250.04
  3. 1 2 CAS 51274-00-1, C.I. 77492
  4. ↑ "Bernalite".
  5. ↑ "List of Minerals". 21 March 2011.
  6. 1 2 A. L. Mackay (1962): "β-Ferric oxyhydroxide—akaganéite", Mineralogical Magazine (Journal of the Mineralogical Society), volume 33, issue 259, pages 270-280 doi:10.1180/minmag.1962.033.259.02
  7. ↑ C. Rémazeilles and Ph. Refait (2007): "On the formation of β-FeOOH (akaganéite) in chloride-containing environments". Corrosion Science, volume 49, issue 2, pages 844-857. doi:10.1016/j.corsci.2006.06.003
  8. ↑ MacEachern, Scott (1996): "Iron Age beginnings north of the Mandara Mountains, Cameroon and Nigeria". In In Pwiti, Gilbert and Soper, Robert (editors) (1996) Aspects of African Archaeology: Proceedings of the Tenth Pan-African Congress University of Zimbabwe Press, Harare, Zimbabwe, ISBN 978-0-908307-55-5, pages 489-496. Archived here on 2012-03-11.
  9. ↑ Diop-Maes, Louise Marie (1996): "La question de l'Âge du fer en Afrique" ("The question of the Iron Age in Africa"). Ankh, volume4/5, pages 278-303. Archived on 2008-01-25.
  10. ↑ Iron Oxide Hydroxide (GFO) Phosphate Binders
  11. ↑ Safoora Rahimi, Rozita M. Moattari, Laleh Rajabi, Ali Ashraf Derakhshan, and Mohammad Keyhani (2015): "Iron oxide/hydroxide (α,γ-FeOOH) nanoparticles as high potential adsorbents for lead removal from polluted aquatic media". Journal of Industrial and Engineering Chemistry, volume 23, pages 33-43. doi:10.1016/j.jiec.2014.07.039
  12. 1 2 Tim Grundl and Jim Delwiche (1993): "Kinetics of ferric oxyhydroxide precipitation". Journal of Contaminant Hydrology, volume 14, issue 1, pages 71-87. doi:10.1016/0169-7722(93)90042-Q
  13. ↑ K. H. Gayer and Leo Woontner (1956): "The Solubility of Ferrous Hydroxide and Ferric Hydroxide in Acidic and Basic Media at 25°". Journal of Physical Chemistry, volume 60, issue 11, pages 1569–1571. doi:10.1021/j150545a021
  14. 1 2 3 Egon Matijević and Paul Scheiner (1978): "Ferric hydrous oxide sols: III. Preparation of uniform particles by hydrolysis of Fe(III)-chloride, -nitrate, and -perchlorate solutions". Journal of Colloid and Interface Science, volume 63, issue 3, pages 509-524. doi:10.1016/S0021-9797(78)80011-3
  15. ↑ Dan Li, Xiaohui Wang, Gang Xiong, Lude Lu, Xujie Yang and Xin Wang (1997): "A novel technique to prepare ultrafine Fe
    2    O
    3     via hydrated iron(III) nitrate". Journal of Materials Science Letters volume 16, pages 493–495 doi:10.1023/A:1018528713566
  16. ↑ Donald O. Whittemore and Donald Langmuir (1974): "Ferric Oxyhydroxide Microparticles in Water". Environmental Health Perspective, volume 9, pages 173-176. doi:10.1289/ehp.749173
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