Crystallography- Metal Structures and Silicate Chemistry Flashcards

1
Q

fcc

A
Bravais lattice: cubic F
Aka ccp
Point group: m3m
Space group: Fm3m
Examples: Al, Cu, γ-Fe, Ni
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

bcc

A

Bravais lattice: cubic I
Point group: m3m
Space group: Im3m
Examples: Nb, W, α-Fe, Cr

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

hcp

A

Bravais lattice: hexagonal P
Point group: 6/mmm
Space group: P6sub3/mmc
Examples: Co, Be, Mg, Ti

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Trends in metal structures

A

hcp most frequent. All alkali metals and typical refractory metals are bcc. Noble metals (Pt group) are fcc. Some metals have small energy difference to the 2nd most favourite structure meaning stacking faults and phase transitions via temperature or pressure are facilitated.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Ordered intermetallic alloy structures

A

Ordered bcc: system is cubic, Bravais primitive, has one element on corners of cube and the other in the centre, atoms alternate along space diagonal, example NiAl.
Ordered fcc: system is tetragonal, Bravais primitive, has one element for top and bottom faces and other for remaining 4 face centred midway up, alternating layers of elements, example TiAl.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Disordered intermetallic alloys

A

Do not fulfill strict definition of crystals, can be treated by placing statistical ‘mixed elements’ at lattice points (occupancy factors), then the ordered structures would return to proper bcc and fcc and both be cubic.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Glide systems in alloy structures

A

Determine the direction of dislocation motion. Normal bcc has (110)[111], normal fcc has (111)[110]. For the ordered intermetallic alloys the Burgers vector is twice as long as for pure metals, so plastic deformation is hindered and alloy is more brittle (not as brittle as ceramics).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Tin structure

A

Gray α-Tin: stable under 13C, cubic, diamond-structure, semiconductor.
White β-Tin: stable above 13C, tetragonal, is distorted cubic primitive, metallic.
Both are metastable so don’t immediately change as temperature goes through 13C.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Heusler alloy

A

ABC2. Example MnAlCu2 so no anion. Based on fcc, has all interstitials fully filled, has larger lattice parameter than normal fcc. This is first ferromagnetic alloy known without a ferromagnetic element

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

What is complex stacking?

A

Anything other than ABAB, ABCABC, AAAA

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Nomenclature for cation/anion stacking sequences

A

Main (Bravais lattice) stacking is upper case roman letters ABC.
Interstitial stacking is Greek letter αβγ.
A, B and C are same chemistry
α, β, γ are also the same elements as each other
<> denotes infilled interstitials (layers entirely vacant)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Stacking sequences for ZnS wurtzile, ZnS cubic, NiAs hexagonal, CdI2 hexagonal

A

ZnS wurtzile: AαBβ
ZnS cubic: AαBβCγ
NiAs hexagonal: AγBγ
CdI2 hexagonal: AγB<>

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Rare earth elements stacking sequences

A

Mixed stacking sequences
ABCB
Examples: La, Pr, Nd, Pm

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Complex stacking in molybdenite

A

AβA<>BγB<>. This is height of one unit cell. Is MoS2. System is hexagonal, Bravais primitive. Sheet structure, rather loose S-S cross-layer bonds so good lubricant as can exfoliate into single 2D sheets. Get pairs of hexagonal primitive layers with rather loose packing. Interstitial layers are not oct or tet but are trigonal prismatic

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Basics of silicates

A

Polymerisation via Si-O-Si bonds. Stoichiometry varies within SiOx depending on how many O shared. 1D, 2D, 3D network structures. Tetrahedra robust and angles and distances vary little and are close to ideal mathematical tetrahedron. Al can sub in silica lattices but needs extra caution to balance charge which are often in interstitial positions.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Structures of silicates

A

Monomer is SiO4 tetrahedron. Dimer is two tetrahedra sharing one O. Trimer 3 tetrahedra forming ring. Can get other rings made of more tetrahedra linked together. Single chain and double chain (2 chains sort of cross-linked). Layer/sheet/net of many hexagon shapes seen in double chains. 3D framework can form a ball.

17
Q

How to count oxygens in silicates

A

Bridging oxygen shared by 2 tetrahedra counts 1/2

Non-bridging oxygen is unshared and counts 1

18
Q

Different Si:O ratios

A

1: 4- extreme 1, is the monomer where all O non-bridging, e.g CaSiO4, dimensionality is zero.
1: 2- extreme 2, framework SiO2, all O bridging, e.g quartz, dimensionality is 3D.
1: 3- intermediate, chain silicate SiO3, 2 O in line with chain are bridging, out of chain are non-bridging (x2), e.g MgSiO3, dimensionality 1D.
1: 2.5- intermediate, sheet silicate, 3 O in plane of sheet are bridging, other out of plane is non-bridging, e.g Na2Si2O5, dimensionality 2D

19
Q

Al as tetrahedral framework cation

A

Can replace Si. E.g NaAlSi3O8 albite feldspar, is 3D framework silicate with 4 bridging O atoms, Na fills large gaps.

20
Q

Al and Mg as octahedral cation

A

Either can fill holes in silicate polymer, especially in combination with OH- ions.

21
Q

Olivine

A

Mg2SiO4. 3D island silicate. Si:O is 1:4. No bridging O. Oxygen in near hcp packing but trigonal distorted. Si in centre of tetrahedra. Is basically ionic structure between Mg cation and negative SiO4 ions.

22
Q

Cristobalite

A

SiO2. 3D framework silicate. All 4 O shared so no non-bridging O. Si:O is 1:2. Alpha phase is tetragonal. Cubic structure and Si atoms sit on diamond lattice. Metastable a time room temperature.

23
Q

Serpentine and Kaolinite

A

Mg and Al respectively. Sheet silicates. Has SiOx tetrahedral layer. Oxygens sticking out of bottom of layer are bonded to 2 Mg or Al atoms which are octahedrally coordinated. Mg or Al atoms bonded to OH- ion as well. Lattice contants mismatch between octahedra/tetrahedra and induce curvature/rolling up

24
Q

Differences between silicate crystal and glass

A

For normal silicate glass, maintains high Si:O ratio (about 2:1) and has only few non-bridging oxygens, no long range order.
Alkali silicate glass has alkali ions that break Si-O-Si chains and form pairs with non-bridging oxygens. E.g Na+ to SiO4- charge balance