Classes of Silicate structures Flashcards

1
Q

What are the 3 classes of silicate structures?

A
  1. ) discrete anions
  2. ) One dimensional chains
  3. ) Two Dimensional sheets
  4. ) Framework silicates
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2
Q

What are examples of discrete anions (silicate structure)

A
Zircon ZrSiO4
Olivine M2SiO4 (M= Mg (2+), Fe(2+))
Beryl (ring structure) Be3Al2Si6O18
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3
Q

What are one dimensional chains (silicate structure)

A
  • the simplest chain
  • involves the sharing of two O atoms per SiO4 unit
  • each SiO4 has two terminal O atoms
  • so the repeat unit of the chain is SiO3 (2-)
    cations Na+ and Al3+ balance the charge
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4
Q

what cations balance the charge of one dimensional chains (silicate structure)

A

Na+ and Al3+

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5
Q

What happens when two chains link laterally into a ribbon, what is the most common repeating unit?

A

Si4O11 (6-)

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6
Q

what is the purpose of metal ions that bind to the polyionic ribbons together?

A

to form neutral sheaths

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7
Q

why are these polyionic ribbon sheeths occur in fibrous strands (as in the family of asbestos minerals)

A

due to the weak intermolecular forces

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8
Q

What are two dimensional sheets?

A
  • if 3 of the O atoms of each SiO4 unit are shared then INFINITE SERIES are formed.
  • only one O atom per SiO4 unit is terminal and carries a negative charge
  • all the terminal O atoms point in one direction one the same side of the sheet
  • silicate repeat unit: Si2O5 (2-)
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9
Q

what is the repeat unit of 2 dimensional sheets

A

Si2O5(2-)

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10
Q

what is the repeat unit of one dimensional chains?

A

SiO3 (2-)

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11
Q

what is the sheet formula of Talc

A

Mg3(Si2O5)2(OH)2

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12
Q

true or false; all the bonding interactions among the ions and atoms of talc occur in a single layer

A

true

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13
Q

how are the layers of talc sheets attracted to each other?

A

van der waals interactions (intermolecular attractions)

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14
Q

what is the significance of each Talc layer being held by van der waals forces with each other?

A

allows the layers to slip over the other easily and hence talc feels slippery

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15
Q

how are aluminosilicates formed?

A

if some Si atoms in silicates are replaced by Al atoms (plus an appropriate cation)

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16
Q

what is the most abundant aluminosilicate

A

feldspars eg. albite (NaAlSi3O8)

17
Q

true or false, mica is also an aluminosilicate

A

true

18
Q

how are Al ions and other ions arranged in micas

A

they lie between aluminosilicate double layers

19
Q

what is theformula of muscovite mica

A

KAl2(AlSi3O10)(OH)2

20
Q

why do mica sheets not slide over each other so readily as in talc?

A

there is an ionic component to the interactions between the double sheets

21
Q

true or false; mica can still be cleaved into layers

A

true

22
Q

how is clay produced?

A

by weathering of silicate minerals such as talc and micas

23
Q

what structure do clay usually have?

A

sheet structures with the layers held together by ionic interactions and hydrogen bonds

24
Q

what happens when water is added to clay?

A

it causes the layers to SWELL and different cations can be found between the layers

25
Q

what is a typical clay material

A

montmorillonite

26
Q

In framework silicates the SiO4 units share how many oxygen atoms

A

4 Oxygen atoms

- to give a 3D framework silicate eg. silica (SiO2)

27
Q

what does silica occur naturally as

A

SiO2 occurs naturally as quartz

28
Q

what does granite consist of?

A

micro crystals of feldspar, mica and quartz

29
Q

What are zeolites?

A
  • 3 dimensional aluminosilicates
  • the negative charge on the aluminosilicate framework is balanced by G1 or 2 cations
  • usually open, porous structure with tunnels and channels (4-20A in diameter)
  • found in nature but can also be made synthetically
  • useful catalysts and absorbants
30
Q

structure of zeolite

A

porous, open, tunnels and channels (4-20 A in diameter)

31
Q

what are zeolites useful for?

A

catalysts and absorbants