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Mullite or porcelainite is a rare silicate mineral formed during contact metamorphism of clay minerals. It can form two stoichiometric forms: 3Al2O32SiO2 or 2Al2O3 SiO2. Unusually, mullite has no charge-balancing cations present. As a result, there are three different aluminium sites: two distorted tetrahedral and one octahedral.

Key facts

Mineral.name
Mullite
Mineral.category
Nesosilicate
Mineral.image
Osumilite, thick tabulars with Mullite - Ochtendung, Eifel, Germany.jpg
Mineral.imagesize
260px
Mineral.caption
White, filamentous mullite in front of thicker osumilite platelets(Photo width 1.5 mm)Found in Wannenköpfe, Ochtendung, Eifel, Germany
Mineral.formula
Al6Si2O13
Mineral.IMAsymbol
Mul
Mineral.strunz
9.AF.20
Mineral.system
Orthorhombic
Mineral.class
Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m)
Mineral.symmetry
Pbnm, Pnnm
Mineral.unit cell
a = 7.5785(6) Å, b = 7.6817(7) Å, c = 2.8864(3) Å; Z = 1
Mineral.color
Colorless to pale pink or grey
Mineral.habit
Prismatic to acicular crystals
Mineral.cleavage
Good on [010]
Mineral.opticalprop
Biaxial (+)
Mineral.refractive
nα = 1.642–1.653 nβ = 1.644–1.655 nγ = 1.654–1.679
Mineral.birefringence
δ = 0.012–0.026

via Wikipedia infobox

Wikidata facts

Image
Mullite-655833.jpg
Show 6 more facts
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.AF.20
Commons category
Mullite
Nickel-Strunz 9th edition (updated 2009)
9.AF.20
IMA Mineral Symbol
Mul
chemical formula
3Al₂O₃·2SiO₂
Strunz 8th edition (series ID, updated)
VIII/A’.02 – Anhang
Sources (3)

via Wikidata · CC0

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Article

4 sections
Contents
  • Porcellanite
  • Use in porcelain
  • Use as a catalyst
  • References

Mullite or porcelainite is a rare silicate mineral formed during contact metamorphism of clay minerals. It can form two stoichiometric forms: 3Al2O32SiO2 or 2Al2O3 SiO2. Unusually, mullite has no charge-balancing cations present. As a result, there are three different aluminium sites: two distorted tetrahedral and one octahedral.

Mullite was first described in 1924 for an occurrence on the Isle of Mull, Scotland. It occurs as argillaceous inclusions in volcanic rocks in the Isle of Mull, inclusions in sillimanite within a tonalite at Val Sissone, Italy and with emerylike rocks in Argyllshire, Scotland.

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