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Aluminosilicate
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Aluminosilicate refers to materials containing Si-O-Al linkages. Commonly, the associate cations are sodium (Na+), potassium (K+) and protons (H+). Such materials occur as , coal combustion products and as synthetic materials, often in the form of . Both synthetic and natural aluminosilicates are of technical significance as structural materials, catalysts, and .


Important representatives
is a common aluminosilicate mineral made of potassium, sodium, and calcium cations surrounded by a negatively charged network of silicon, aluminium and oxygen atoms.

Many aluminosilicates are synthesized by reactions of silicates, aluminates, and other compounds. They have the general formula where M+ is usually H+ and Na+. The Si/Al ratio is variable, which provides a means to tune the properties. Many of these materials are porous and exhibit properties of industrial value. Naturally occurring , hydrous aluminosilicate minerals are also referred to as .


See also
  • Aluminium silicate
  • Geopolymer cement
  • Silicate minerals
  • Calcium aluminosilicate
  • Sodium aluminosilicate
  • – a type of aluminosilicate

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