Wüstite

Wüstite (FeO) is a mineral form of iron(II) oxide found with meteorites and native non-stoichiometric compound.

Wüstite was named for Fritz Wüst (1860-1938), a German metallurgist and founding director of the Kaiser-Wilhelm-Institut für Eisenforschung. ^[1]

In addition to the type locality in Germany, it has been reported from Disko Island, Greenland; the Jharia coalfield, Bihar, India and as inclusions in manganese nodules.

Its presence indicates a highly reducing environment.

Wüstite Redox Buffer

Main article: Mineral redox buffer

Wüstite, in geochemistry, defines a redox buffer of oxidation within rocks at which point the rock is so reduced that Fe³⁺ and thus hematite is absent.

As the redox state of a rock is further reduced, magnetite is converted to wüstite. This occurs by conversion of the Fe³⁺ ions in magnetite to Fe²⁺ ions. An example reaction is presented below;

1. FeO.Fe₂O₃ + C --> 3FeO + CO

magnetite + graphite/diamond --> wüstite + carbon monoxide

The formula for magnetite is more accurately written as FeO.Fe₂O₃ than as Fe₃O₄. Magnetite is one part wüstite (FeO) and one part hematite (Fe₂O₃), rather than a fugacity. This is similar to buffering in the H⁺/OH^- acid-base system of water.

Once the Fe³⁺ is consumed, then oxygen must be stripped from the system to further reduce it and wüstite is converted to native iron. The oxide mineral equilibrium assemblage of the rock becomes wüstite-magnetite-iron.

In nature, the only natural systems which are chemically reduced enough to even attain a wüstite-magnetite composition are rare, including carbonate-rich graphite.

Effects upon silicate minerals

Main article: Normative mineralogy

The ratio of Fe²⁺ to Fe³⁺ within a rock determines, in part, the silicate mineral assemblage of the rock. Within a rock of a given chemical composition, iron enters minerals based on the bulk chemical composition and the mineral phases which are stable at that temperature and pressure. Iron may only enter minerals such as olivine if it is present as Fe²⁺; Fe³⁺ cannot enter the lattice of fayalite olivine and thus for every two Fe³⁺ ions, one Fe²⁺ is used and one molecule of magnetite is created.

In chemically reduced rocks, magnetite may be absent due to the propensity of iron to enter olivine, and wüstite may only be present if there is an excess of iron above what can be used by silica. Thus, wüstite may only be found in silica-undersaturated compositions which are also heavily chemically reduced, satisfying both the need to remove all Fe³⁺ and to maintain iron outside of silicate minerals.

In nature, carbonate rocks, potentially kimberlites, carbonate-bearing melilitic rocks and other rare alkaline rocks may satisfy these criteria. However, wüstite is not reported in most of these rocks in nature, potentially because the redox state necessary to drive magnetite to wüstite is so rare.

Related minerals

Wüstite forms a solid solution with serpentinite metamorphic reactions.

Oxidation of wüstite forms goethite-limonite.

Zinc, aluminium and other transition metals may substitute for Fe in wüstite.

Wüstite in dolomite skarns may be related to magnesite.

See also

• Normative mineralogy
• Redox
• Kimberlite
• Skarn
• Periclase

References

1. ^ Schenck, Rudolf & Dingmann, Th.; 1927: Gleichgewichtsuntersuchungen über die Reduktions-, Oxydations- und Kohlungsvorgänge beim Eisen III, in: Zeitschrift für anorganische und allgemeine Chemie 166, p. 113-154, here p. 141.

• Mineral Data Pub. PDF file Accessed 3/5/2006
• Euromin Accessed 3/5/2006
• Wüstite on Mindat.org Accessed 3/5/2006
• Webmineral data Accessed 3/5/2006