1. Cyclic silicates:
Silicates which contain (SiO3)n2n- ions which are formed by linking three or more tetrahedral (SiO3)4-n units cyclically are called cyclic silicates. Each silicate unit shares two of its oxygen atoms with other units.
Example: Beryl [Be3Al2(SiO3)6] (an aluminosilicate with each aluminium is surrounded by 6 Structure of Cyclic silicates
2. Ino silicones:
Silicates which contain V number of silicate units liked by sharing two or more oxygen atoms are called inosilicates. They are further classified as chain silicates and double chain silicates. Chain silicates (or pyroxenes) – These silicates contain (SiO3)n2n- ions formed by linking ‘n’ number of tetrahedral (SiO3)n4- units linearly. Each silicate unit shares two of its oxygen atoms with other Structure of Chain silicates units.
Example:
Spodumene – LiAl(SiO3)2 Double chain silicates (or amphiboles) –
These silicates contains [Si4O11]n6n- ions.
In these silicates there are two different types of
3. Tetrahedra:
1. Those sharing 3 vertices
2. Those sharing only 2 vertices.
Examples.
Asbestos – These are fibrous and noncombustible silicates. Therefore they are used for thermal insulation material, brake linings, construction material and filters. Asbestos being carcinogenic silicates, their applications are restricted.