Fouling

Aluminosilicate

Phase diagram of Al2SiO5
(nesosilicates).[1]

Aluminosilicate minerals are minerals composed of aluminium, silicon, and oxygen, plus countercations. They are a major component of kaolin and other clay minerals.

Andalusite, kyanite, and sillimanite are naturally occurring aluminosilicate minerals that have the composition Al2SiO5.[2][3][4] The triple point of the three polymorphs is located at a temperature of 500 °C and a pressure of 0.4 GPa. These three minerals are commonly used as index minerals in metamorphic rocks.

Hydrated aluminosilicate minerals are referred to as zeolites and are porous structures that are naturally occurring materials.

The catalyst silica-alumina is an amorphous substance which is not an aluminosilicate compound.

Aluminosilicate glasses

There exist a wide variety of glass types. The characteristics of these different types depend on the chemical composition of the glass with a special focus on the oxide composition. Glasses can be categorized into many different groups, one of them including the so-called aluminosilicate glasses.

Properties of this glass family

The maximum allowable temperatures of aluminosilicate glasses of up to 800 °C are far above those of borosilicate glasses and reach the level of glass ceramic materials. The relevant property to decide about maximum temperatures for glasses is the transformation temperature. The thermal expansion of this glass family can be adjusted to common electrode materials such as molybdenum. A matched thermal expansion allows for a extremely tight and gas-proof glass to metal seal which is achieved by hot forming.

This glass type can be further differentiated:

Alkaline earth aluminosilicate glasses

Characteristically, these glasses are free of alkali oxides and contain 15-25% AI2O3, 52-60% SiO2 and about 15% alkaline earths. Very high transformation temperatures and softening points are typical features. Main fields of application are glass bulbs for halogen lamps, high-temperature thermometers and thermally and electrically highly loadable film resistors.

Alkali aluminosilicate glasses

The AI2O3 content of alkali aluminosilicate glasses is typically 10-25% and the alkali content over 10%. The high alkali content prepares the glass for ion exchange with bigger alkali ions in order to improve the surface compressive strength. Due to this particular feature, this glass type is especially suitable for the use in touch displays, solar cells cover glass and laminated safety glass. High transformation temperatures and outstanding mechanical properties, e.g. hardness and scratch behavior, are characteristic of this glass type.[5]

See also

References

  1. ^ Whitney, D.L. (2002), “Coexisting andalusite, kyanite, and sillimanite: Sequential formation of three Al2SiO5 polymorphs during progressive metamorphism near the triple point, Sivrihisar, Turkey”, American Mineralogist, 87 (4): 405–416 
  2. ^ “Andalusite, Handbook of Mineralogy” (PDF). Archived (PDF) from the original on 2012-05-16. 
  3. ^ “Kyanite, Handbook of Mineralogy” (PDF). Archived (PDF) from the original on 2012-02-24. 
  4. ^ “Sillimanite, Handbook of Mineralogy” (PDF). Archived (PDF) from the original on 2011-11-19. 
  5. ^ “Archived copy” (PDF). Archived (PDF) from the original on 2017-08-24. Retrieved 2017-08-24. 

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