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SHEETAL SEQUEIRA
198227
INTRODUCTION
 A Silicate is an anions consisting of silicon and oxygen.
 General formula [SiO4-x
(4-2x)- ]n .
 Silicates occur in earth’s crust in abundantly in the form of silicate minerals
and aluminosilicate clay.
 Silicate anions are often large polymeric molecules with an extense variety
of structures, including chains and rings, double chains and sheets.
 Silicates are extremely important materials, both natural and artificial, for all
sorts of technological and artistic activities.
STRUCTURE OF SILICATE
 Silicate structure consists of (SiO4)4- units which are formed by sp3 hybridisation of Si
orbitals.
 The electron configuration of Silicon atom in the excited state is 3s1 p1
x p1
y p1
z thus it forms
four bonds with oxygen atoms by utilizing sp3 hybrid orbits and yielding (SiO4)4- units.
 The oxygen atoms pickup one electron each from some metal in order to complete their
octets.
PROPERTIES OF SILICATES
 Most of the silicates are insoluble in water.
 Sodium silicate, Na2SiO3, is the only common silicate which is soluble in
water.
 The electronegativity of oxygen is 3.5 and that of silicon is 1.9 . The
electronegativity difference of 1.6 suggests that Si-O bond, though covalent
,has an appreciable degree of ionic character.
DIFFERENT TYPES OF SILICATES
 ORTHO SILICATES.
 PYRO SILICATES.
 CHAIN SILICATES.
 CYCLIC SILICATES.
 SHEET SILICATES.
 THREE-DIMENSIONAL SILICATES.
ORTHO SILICATES
 These simplest silicates which contain discrete (SiO4)4- units.
 Example; 1) Phenacite - Be2SiO4
2) Willemite - Zn2SiO4
3) Olivine - (Fe/Mg)2SiO4 : The cations are octahedrally coordinated to the
oxygen atoms of the silicate.
4) Zircone - ZrSiO4 : The coordination number of Zr4+ is 8.
PYRO SILICATES
 These contains disilicate anions , (Si2O7)6- units.
 These (Si2O7)6- units are formed by joining two tetrahedral (SiO4)4- units through
one oxygen atom.
Example; Thortveitite - Sc2Si2O7
Hemimorphite- [Zn4(OH)2Si2O7]
CHAIN SILICATES
 Chain silicates or pyroxenes contain (SiO3)n
2- ions which are formed by linking ‘n’ number of tetrahedral
SiO4
4- units linearly. Each unit shares two oxygen atoms with other units.
 Examples;
1) Spodumene - LiAl(SiO3)2
2) Diopside - CaMg(SiO3)2
3) Enstatite - MgSiO3
DOUBLE CHAIN SILICATES
 The general formula of double chain silicates (or Amphiboles) is (Si4O11)n
6- . There are two types of
tetrahedra: those sharing 3 vertices and those sharing only 2 vertices.
 EXAMPLES;
1) Tremolite - Ca2Mg5(Si4O11)2(OH)2
2)Amosite – ( MgFe)7Si8O22(OH)2.
3)Crocidolite
CYCLIC SILICATES
 These contain (SiO3)n
2n- ions which are formed by linking three or more tetrahedral SiO4
4- units cyclically.
 Each unit shares two oxygen atoms with other units.
Examples; 1) Bentonite - BaTi(SiO3)3 : contain three
tetrahedra arranged cyclically
2) Beryl - Be3Al2(SiO3)6 : contain six-silicate rings.
It is an aluminosilicate. Each aluminium is
surrounded by 6 oxygen atoms octahedrally.
SHEET SILICATES
 The general formula of Sheet or Phyllo
silicates is (Si2O5)n
2n- . Each SiO4 tetrahedron
shares three oxygen atoms with others and thus
by forming two-dimensional sheets. These
silicates can be cleaved easily just like graphite.
 Examples; 1)Kaolinite - AlSiO5(OH)4
2) Talc – Mg3Si4O16(OH)3
THREE DIMENSIONAL SILICATES
 The general formula of three dimensional or tecto silicates is (SiO2)n . All the
oxygen atoms of SiO4 are shared with other tetrahedra and thus by forming three-
dimensional network.
 E.g. SiO2 - Quartz, Tridymite and Crystobalite - These are the crystalline forms of
silica.
 When SiO4
4- units are replaced by AlO4
5- units, three
dimensional aluminosilicates are formed.
 E.g. Feldspar, Zeolites, Ult etc.,
Silicates - Sheetal Sequeira

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Silicates - Sheetal Sequeira

  • 2. INTRODUCTION  A Silicate is an anions consisting of silicon and oxygen.  General formula [SiO4-x (4-2x)- ]n .  Silicates occur in earth’s crust in abundantly in the form of silicate minerals and aluminosilicate clay.  Silicate anions are often large polymeric molecules with an extense variety of structures, including chains and rings, double chains and sheets.  Silicates are extremely important materials, both natural and artificial, for all sorts of technological and artistic activities.
  • 3. STRUCTURE OF SILICATE  Silicate structure consists of (SiO4)4- units which are formed by sp3 hybridisation of Si orbitals.  The electron configuration of Silicon atom in the excited state is 3s1 p1 x p1 y p1 z thus it forms four bonds with oxygen atoms by utilizing sp3 hybrid orbits and yielding (SiO4)4- units.  The oxygen atoms pickup one electron each from some metal in order to complete their octets.
  • 4. PROPERTIES OF SILICATES  Most of the silicates are insoluble in water.  Sodium silicate, Na2SiO3, is the only common silicate which is soluble in water.  The electronegativity of oxygen is 3.5 and that of silicon is 1.9 . The electronegativity difference of 1.6 suggests that Si-O bond, though covalent ,has an appreciable degree of ionic character.
  • 5. DIFFERENT TYPES OF SILICATES  ORTHO SILICATES.  PYRO SILICATES.  CHAIN SILICATES.  CYCLIC SILICATES.  SHEET SILICATES.  THREE-DIMENSIONAL SILICATES.
  • 6. ORTHO SILICATES  These simplest silicates which contain discrete (SiO4)4- units.  Example; 1) Phenacite - Be2SiO4 2) Willemite - Zn2SiO4 3) Olivine - (Fe/Mg)2SiO4 : The cations are octahedrally coordinated to the oxygen atoms of the silicate. 4) Zircone - ZrSiO4 : The coordination number of Zr4+ is 8.
  • 7. PYRO SILICATES  These contains disilicate anions , (Si2O7)6- units.  These (Si2O7)6- units are formed by joining two tetrahedral (SiO4)4- units through one oxygen atom. Example; Thortveitite - Sc2Si2O7 Hemimorphite- [Zn4(OH)2Si2O7]
  • 8. CHAIN SILICATES  Chain silicates or pyroxenes contain (SiO3)n 2- ions which are formed by linking ‘n’ number of tetrahedral SiO4 4- units linearly. Each unit shares two oxygen atoms with other units.  Examples; 1) Spodumene - LiAl(SiO3)2 2) Diopside - CaMg(SiO3)2 3) Enstatite - MgSiO3
  • 9. DOUBLE CHAIN SILICATES  The general formula of double chain silicates (or Amphiboles) is (Si4O11)n 6- . There are two types of tetrahedra: those sharing 3 vertices and those sharing only 2 vertices.  EXAMPLES; 1) Tremolite - Ca2Mg5(Si4O11)2(OH)2 2)Amosite – ( MgFe)7Si8O22(OH)2. 3)Crocidolite
  • 10. CYCLIC SILICATES  These contain (SiO3)n 2n- ions which are formed by linking three or more tetrahedral SiO4 4- units cyclically.  Each unit shares two oxygen atoms with other units. Examples; 1) Bentonite - BaTi(SiO3)3 : contain three tetrahedra arranged cyclically 2) Beryl - Be3Al2(SiO3)6 : contain six-silicate rings. It is an aluminosilicate. Each aluminium is surrounded by 6 oxygen atoms octahedrally.
  • 11. SHEET SILICATES  The general formula of Sheet or Phyllo silicates is (Si2O5)n 2n- . Each SiO4 tetrahedron shares three oxygen atoms with others and thus by forming two-dimensional sheets. These silicates can be cleaved easily just like graphite.  Examples; 1)Kaolinite - AlSiO5(OH)4 2) Talc – Mg3Si4O16(OH)3
  • 12. THREE DIMENSIONAL SILICATES  The general formula of three dimensional or tecto silicates is (SiO2)n . All the oxygen atoms of SiO4 are shared with other tetrahedra and thus by forming three- dimensional network.  E.g. SiO2 - Quartz, Tridymite and Crystobalite - These are the crystalline forms of silica.  When SiO4 4- units are replaced by AlO4 5- units, three dimensional aluminosilicates are formed.  E.g. Feldspar, Zeolites, Ult etc.,