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

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

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
what is a typical clay material
montmorillonite
26
In framework silicates the SiO4 units share how many oxygen atoms
4 Oxygen atoms | - to give a 3D framework silicate eg. silica (SiO2)
27
what does silica occur naturally as
SiO2 occurs naturally as quartz
28
what does granite consist of?
micro crystals of feldspar, mica and quartz
29
What are zeolites?
- 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
structure of zeolite
porous, open, tunnels and channels (4-20 A in diameter)
31
what are zeolites useful for?
catalysts and absorbants