Iron(II) hydroxide

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Iron(II) hydroxide
Mg(OH)2Xray.jpg
Names
IUPAC name
Iron(II) hydroxide
Other names
Ferrous hydroxide, green rust
Identifiers
3D model (JSmol)
ChemSpider
ECHA InfoCard 100.038.581 OOjs UI icon edit-ltr-progressive.svg
PubChem CID
UNII
  • InChI=1S/Fe.2H2O/h;2*1H2/q+2;;/p-2 Yes check.svgY
    Key: NCNCGGDMXMBVIA-UHFFFAOYSA-L Yes check.svgY
  • InChI=1/Fe.2H2O/h;2*1H2/q+2;;/p-2
    Key: NCNCGGDMXMBVIA-NUQVWONBAV
  • O[Fe]O
Properties
Fe(OH)2
Molar mass 89.86 g/mol
Appearancegreen solid
Density 3.4 g/cm3 [1]
0.000052 g/100 g water (20 °C, pH 7) [2]
8.0 x 10−16 [3]
Acidity (pKa)17 [4]
Hazards
Flash point Non-flammable
Related compounds
Related compounds
Iron(II) oxide
Iron(III) hydroxide
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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Iron(II) hydroxide or ferrous hydroxide is an inorganic compound with the formula Fe(OH)2. It is produced when iron(II) salts, from a compound such as iron(II) sulfate, are treated with hydroxide ions. Iron(II) hydroxide is a white solid, but even traces of oxygen impart a greenish tinge. The air-oxidised solid is sometimes known as "green rust".

Contents

Preparation and reactions

Iron(II) hydroxide is poorly soluble in water (1.43 × 103 g/L), or 1.59 × 10−5 mol/L. It precipitates from the reaction of iron(II) and hydroxide salts: [5]

FeSO4 + 2 NaOH → Fe(OH)2 + Na2SO4

If the solution is not deoxygenated and iron not totally reduced in Fe(II), the precipitate can vary in colour starting from green to reddish brown depending on the iron(III) content. Iron(II) ions are easily substituted by iron(III) ions produced by its progressive oxidation.

It is also easily formed as a by-product of other reactions, a.o., in the synthesis of siderite, an iron carbonate (FeCO3), if the crystal growth conditions are imperfectly controlled.

Structure

Fe(OH)2 adopts the brucite structure, i.e. the arrangement of the atoms in the crystal are the same as the arrangement of the atoms in Mg(OH)2. The Fe(II) centers are bonded to six hydroxide ligands. Each hydroxide ligand bridges to three Fe(II) sites. The O-H bonds are perpendicular to the planes defined by the oxygen atoms, projecting above and below these layers. [6]

Reactions

Under anaerobic conditions, the iron(II) hydroxide can be oxidised by the protons of water to form magnetite (iron(II,III) oxide) and molecular hydrogen. This process is described by the Schikorr reaction:

3 Fe(OH)2 → Fe3O4 + H2 + 2 H2O

Anions such as selenite and selenate can be easily adsorbed on the positively charged surface of iron(II) hydroxide, where they are subsequently reduced by Fe2+. The resulting products are poorly soluble (Se0, FeSe, or FeSe2).

Natural occurrence

Iron III hydroxide staining caused by oxidation of dissolved iron II and precipitation, Perth, Western Australia. Limestone building with pollution.jpg
Iron III hydroxide staining caused by oxidation of dissolved iron II and precipitation, Perth, Western Australia.

Iron dissolved in groundwater is in the reduced iron II form. If this groundwater comes in contact with oxygen at the surface, e.g. in natural springs, iron II is oxidised to iron III and forms insoluble hydroxides in water. [7] The natural analogue of iron(II) hydroxide compound is the very rare mineral amakinite, (Fe,Mg)(OH)2. [8] [9]

Application

Iron(II) hydroxide has also been investigated as an agent for the removal of toxic selenate and selenite ions from water systems such as wetlands. The iron(II) hydroxide reduces these ions to elemental selenium, which is insoluble in water and precipitates out. [10]

In a basic solution iron(II) hydroxide is the electrochemically active material of the negative electrode of the nickel-iron battery.

See also

Related Research Articles

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<span class="mw-page-title-main">Ferric</span> The element iron in its +3 oxidation state

In chemistry, iron(III) or ferric refers to the element iron in its +3 oxidation state. Ferric chloride is an alternative name for iron(III) chloride (FeCl3). The adjective ferrous is used instead for iron(II) salts, containing the cation Fe2+. The word ferric is derived from the Latin word ferrum, meaning "iron".

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2
, consisting of divalent cobalt cations Co2+
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3
), chloride (Cl
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4
), in a layered double hydroxide (LDH) structure. The most studied varieties are the following:

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References

  1. Lide, David R., ed. (2006). CRC Handbook of Chemistry and Physics (87th ed.). Boca Raton, FL: CRC Press. ISBN   0-8493-0487-3.
  2. CRC Handbook of Chemistry and Physics, 84th Edition, CRC Press, 2004, pg 4-62
  3. Stumm, Werner; Lee, G. F. (February 1961). "Oxygenation of Ferrous Iron" (PDF). Industrial & Engineering Chemistry. 53 (2): 143–146. doi:10.1021/ie50614a030 . Retrieved 17 November 2022.
  4. Perrin, D. D., ed. (1982) [1969]. Ionisation Constants of Inorganic Acids and Bases in Aqueous Solution. IUPAC Chemical Data (2nd ed.). Oxford: Pergamon (published 1984). Entry 130. ISBN   0-08-029214-3. LCCN   82-16524.
  5. H. Lux "Iron(II) Hydroxide" in Handbook of Preparative Inorganic Chemistry, 2nd Ed. Edited by G. Brauer, Academic Press, 1963, NY. Vol. 1. p. 1498.
  6. Lutz, H.D.; Möller, H.; Schmidt, M. (1994). "Lattice vibration spectra. Part LXXXII. Brucite-type hydroxides M(OH)2 (M = Ca, Mn, Co, Fe, Cd) — IR and Raman spectra, neutron diffraction of Fe(OH)2". Journal of Molecular Structure. 328: 121–132. doi:10.1016/0022-2860(94)08355-x.
  7. lenntech.com
  8. "Amakinite".
  9. "List of Minerals". 21 March 2011.
  10. Zingaro, Ralph A.; et al. (1997). "Reduction of oxoselenium anions by iron(II) hydroxide". Environment International. 23 (3): 299–304. doi:10.1016/S0160-4120(97)00032-9.