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August 16
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Structure of Crystalline Solids
Instructor:Prof. Sujoy Kumar Kar 1MT30001 Atumn 2016 S K Kar 2MT30001 Atumn 2016 S K Kar
What are we going to discuss?• Atomic arrangement in the solid state
• Concepts of crystallinity and noncrystallinity
• Notion of crystal structure, specified in terms of a unit cellcell
• The scheme by which crystallographic directions and planes are designated
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Fundamental Concepts
• Crystalline material: One in which the atoms/ molecules/ ions are situated in a 3‐dimensional repeating or periodic array over large atomic distances
– All metals, many ceramic materials, and certain polymers form crystalline structures under normal solidification conditions
• Noncrystalline or amorphous materials:
– Do not crystallize
– Long range atomic order absent4MT30001 Atumn 2016 S K Kar
Fundamental Concepts (Continued….)Lattice:
• An imaginary pattern of points in which every point hasan environment that is identical to that of any other pointin the pattern.
l h f b h f d ll l• A lattice has no specific origin, as it can be shifted parallelto itself.
• Although it is an imaginary construct, the lattice is used todescribe the structure of real materials.
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Fundamental Concepts (Continued….)Unit cells:
• Small repeat units of lattice or, crystal structure
– Defines the lattice/ crystal structure by virtue of its geometry andthe atom positions within
• Parallelepipeds having three sets of parallel faces
Ch t t th t f th l tti / t l• Chosen to represent the symmetry of the lattice/ crystalstructure,
– Not unique. Generally use the unit cell having the highest level ofgeometrical symmetry
• All the lattice points or atom positions in the crystalmay be generated by translations of the unit cellintegral distances along each of its edges.
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Fundamental Concepts (Continued….)Lattice Parameters:
• An x, y, z coordinate system isestablished with its origin at oneof the unit cell corners; each ofthe x, y, and z axes coincides withone of the three parallelepipedone of the three parallelepipededges that extend from this corner
• The unit cell geometry iscompletely defined in terms of sixparameters: the three edgelengths a, b, and c, and the threeinter‐axial angles , , and . Theyare termed as Lattice Parameters 7MT30001 Atumn 2016 S K Kar
Fundamental Concepts (Continued….)Crystal systems:
• Classification of crystals according to unit cell geometry.
• There are seven different possible combinations of a, b,and c, and , , and , each of which represents adistinct crystal system
• Defined in terms of highest symmetry elements present
1. Cubic2. Hexagonal3. Tetragonal
4. Trigonal5. Orthorhombic6. Monoclinic7. Triclinic
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Crystallographic Directions and Planes
• All directions and planes are represented in the crystallographic coordinate system.
• This is always a right-handed coordinate systemThis is always a right handed coordinate system based on the unit cell.
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Labeling conventions of crystallographic planes and directions• Three integers or indices are used to designate
directions and planes. • The basis for determining index
values is the unit cell, with a coordinate system consisting ofcoordinate system consisting of three (x, y, and z) axes situated at one of the corners and coinciding with the unit cell edges
• For hexagonal, rhombohedral, monoclinic, and triclinic—the three axes are not mutually perpendicular
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Point Coordinates
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Point Coordinates
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Crystallographic Directions
1. Vector repositioned (if necessary) to pass through origin.
2. Read off projections in terms of unit cell dimensions a, b, and c
3. Adjust to smallest integer values (Multiply or divide by a common factor)
z Algorithm
y
4. Enclose in square brackets, no commas
[uvw]
ex: 1, 0, ½ => 2, 0, 1 => [ 201 ]
‐1, 1, 1
x
where overbar represents a negative index[ 111 ]=>
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f04_03_pg4618MT30001 Atumn 2016 S K Kar
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Miller Indices ‐ Directions
ba
c
-1/3
1/2-1
x1/2
y-1
z-1/3 (x 6)
263
1
1/4
1/2
x1
y1/4
z1/2 (x 4)
214
263
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Equivalent directions
• Equivalent directions -- The spacing of atoms along each direction is the same.
• In cubic crystals, [100], [100], [010], [010], [001], and [001] are equivalent.
• Equivalent directions are grouped together into a family enclosed in angle brackets thus: <100>family, enclosed in angle brackets, thus: <100>.
• Directions in cubic crystals having the same indices without regard to order or sign, for example, [123] and [213], are equivalent.
• In general, not true for other crystal systems. In tetragonal crystal system, [100] and [010] directions are equivalent, whereas [100] and [001] are not.
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Crystallographic Planes• Algorithm
1. If the plane passes through the selected origin, either another parallel plane must be constructed within the unit cell by an appropriate translation or, new origin must be established at the corner of another unit cell. At this point the crystallographic plane either intersects or parallels each of the three axes
2. Read off intercepts of plane with axes in terms of a, b, c
3. Take reciprocals of intercepts
4 Reduce to smallest integer values4. Reduce to smallest integer values
5. Enclose in parentheses, no commas i.e., (hkl)
z
x
y
a b
c
4. Miller Indices (110)
1. Intercepts 1 1 2. Reciprocals 1/1 1/1 1/
1 1 03. Reduction 1 1 0
example a b c
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Crystallographic Planes
Any two planes parallel to each other are equivalent and have identical indices 22MT30001 Atumn 2016 S K Kar
Crystallographic Planes
example a b cz
y
c1. Intercepts 1/2 2. Reciprocals 1/½ 1/ 1/
2 0 03. Reduction 2 0 0
x
y
a b4. Miller Indices (200)
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Crystallographic Planesz
y
a b
c
example
1. Intercepts 1/2 1 3/4
a b c
2. Reciprocals 1/½ 1/1 1/¾
2 1 4/3
3. Reduction 6 3 4
x4. Miller Indices (634)
3. Reduction 6 3 4
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Miller Indices ‐ Planes
41
21
ba
c
41
21
ba
c
x1/44
y0
z-1/2-2
204
interceptreciprocal
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Miller Indices ‐ Planes
31
21
ba
c
41
31
21
ba
c
41
x1/44
y-1/3-3
z-1/2-2
234
interceptreciprocal
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What is this plane?
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Which one is the plane?011
Follow the steps in reverse order: 1) Take reciprocal 2) Determine the intercepts.
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Miller Indices
Planes
Directions
(hkl)
{hkl}
[uvw]
<uvw>
specific
family
specific
family
- No commas- No fractions- Negative
indicated by bar over
bnumberReversing the directions of all indices specifies another plane parallel to, on the opposite side of and equidistant from, the origin.
(001)(010),
Family of Planes {hkl}
(100), (010),(001),Ex: {100} = (100),
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Equivalent Planes
A family of planes includes all planes which are equivalent by symmetry (Same atomic packing) -depends on crystal system.- For cubic: (110) (011) and (101) are all {110}- For cubic: (110),(011) and (101) are all {110}- For tetragonal: (011) and (101) are {101}
but (110) is not (ca)
• In the cubic system only, planes having the same indices, irrespective of order and sign, are equivalent
• Both and belong to the {123} family
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Cubic crystals
• One interesting and unique characteristic of cubic crystals is that planes and directions having the same indices are perpendicular to one anotherone another
• For other crystal systems there are no simple geometrical relationships between planes and directions having the same indices
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Why 4‐index notation for Hexagonal crystals ?
The third index is included to emphasize the symmetry; if the third index were not included, you might not realize that, e.g., the (2 1 0) and (1 1 0)are crystallographically equivalentare crystallographically equivalent.
What are these planes in hexagonal unit cell? :(2 1 0) and (1 1 0)
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Crystallographic Planes (Hexagonal)
• In hexagonal unit cells the same idea is used
example a1 a2 a3 c
1. Intercepts 1 ‐1 12. Reciprocals 1 1/ ‐1 1
z
4. Miller Indices (101)
1 0 ‐1 1
3. Reduction 1 0 ‐1 1
a2
a3
a1
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What is the Miller-Bravais indices of the plane?
(1 -1 0 1)
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a2
a3
Examples to show the utility of the 4 index
notation
a1
Intercepts → 1 1
Plane → (1 1 0)
Intercepts → ½ –1
Plane → (2 1 0)
In 4 index system (2 11 0 ) In 4 index system Plane → (1 12 0)
These planes are crystallographically equivalent. – Not apparent from the 3 index notation
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(hkl) (hkil)
Miller-Bravais indices
i = -(h+k)
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3-indices (Miller indices) and 4-indices (Miller–Bravaisindices), coordinate system
Directions in Hexagonal Crystal
Why we need 4 indexWhy we need 4 index system?
In 4 index system, Indices reveal crystallographicallyequivalent directions
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3 index (Miller indices) to 4 index (Miller‐Bravais indices)
• Hexagonal Crystals
– 4 parameter Miller‐Bravais lattice coordinates are related to the direction indices (i.e., u'v'w') as follows.
]uvtw[]'w'v'u[ z
'ww
t
v
u
)vu( +‐
)'u'v2(3
1‐
)'v'u2(3
1‐
]uvtw[]wvu[
‐a3
a1
a2
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What is this direction CF?
Finding perpendicular projections in Hexagonal crystal system is not always convenient
In three index system: [1 1 1]39MT30001 Atumn 2016 S K Kar
What is the index of the direction CE?
'
t
v
u
)vu( +‐
)'u'v2(3
1‐
)'v'u2(3
1‐
]uvtw[]'w'v'u[ [1 1 1]
In Four index system: 1123
'ww
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MILLER INDICES OF SOME IMPORTANT PLANES
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Angle between two cystallographic directions [u1 v1 w1] and [u2 v2 w2]
Worked ExampleFind the angle between the directions [2 1 1] and [1 1 2] in a cubic crystal
1 2 1 2 1 2
2 2 2 2 2 21 1 1 2 2 2
½ ½
u u v v w wcos
(u v w ) (u v w )
cubic crystal.
The two directions are [2 1 1] and [1 1 2]
In this case, u1 = 2, v1 = 1, w1 = 1, u2 = 1, v2 = 1, w2 = 2
(or) cos = 0.833 = 35° 3530.
2 2 2 2 2 2
(2 1) (1 1) (1 2) 5cos
62 1 l 1 1 2
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Interplanar Distance
222 lkh
adhkl
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If (h k l) is the Miller indices of a crystal plane then the intercepts made by the plane with the crystallographic axes are given as
where a, b and c are lattice parameters
a b c, and
h k l
Bravais Lattices
Named after named after Auguste Bravais
7 Crystal SystemsCentering
14 Bravais Lattices
• Primitive• Body Centering• Face Centering• Base Centering
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BRAVAIS
LATTTICES
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Bravais Lattices (14)
Crystal System
Parameters Primitive (Simple)
Body-Centered
Face-Centered
Base-Centered
Cubic abc
X X X
Tetragonal abc
X X
Orthorhombic abc
X X X X
Rhombohedral abc
X
Hexagonal abc
X
Monoclinic abc
X X
Triclinic abc
X
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HCP Structure
Hexagonal unit cell
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Hexagonal packing49MT30001 Atumn 2016 S K Kar
A sites
B B
B
BB
B BC C
CA
B
B sites
• ABCABC... Stacking Sequence• 2D Projection
Stacking Sequence
C C
CA
C C
C
A
C sites
• FCC Unit CellA
BC
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Cubic closed packing51MT30001 Atumn 2016 S K Kar FCC unit cell BCC unit Cell 52MT30001 Atumn 2016 S K Kar
Atoms Per Unit Cell
• Corners ‐ shared by eight unit cells (x 1/8)
• Edges ‐ shared by four unit cells (x 1/4)(x 1/4)
• Faces ‐ shared by two unit cells (x 1/2)
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Common Metal Structures
• Face‐Centered Cubic (FCC)
– 8 corners x 1/8 + 6 faces x 1/2
– 1 + 3 = 4 atoms/u.c.
B d C t d C bi (BCC)• Body‐Centered Cubic (BCC)
– 8 corners x 1/8 + 1 center
– 1 + 1 = 2 atoms/u.c.
• Hexagonal Close‐Packed (HCP)
– (4 x (1/6) + 4 x (1/12)) = 1 corner + 1 middle
– 1 + 1 = 2 atoms/u.c. 54MT30001 Atumn 2016 S K Kar
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• Rare due to low packing density (only Po has this structure)• Close-packed directions are cube edges.
• Coordination # = 6(# nearest neighbors)
Simple Cubic Structure (SC)
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• APF for a simple cubic structure = 0.52
volume
Atomic Packing Factor (APF)
APF = Volume of atoms in unit cell*
Volume of unit cell
*assume hard spheres
APF =
a 3
4
3 (0.5a) 31
atoms
unit cell
atom
volume
unit cell
volume
close-packed directions
a
R=0.5a
contains 8 x 1/8 = 1 atom/unit cell
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• Coordination # = 8
• Atoms touch each other along cube diagonals.
--Note: All atoms are identical; the center atom is shadeddifferently only for ease of viewing.
Body Centered Cubic Structure (BCC)
ex: Cr, W, Fe (), Tantalum, Molybdenum
2 atoms/unit cell: 1 center + 8 corners x 1/857MT30001 Atumn 2016 S K Kar
Atomic Packing Factor: BCC
a
• APF for a body-centered cubic structure = 0.68
a2
a3
APF =
4
3 ( 3 a/4 ) 32
atoms
unit cell atom
volume
a 3
unit cell
volume
length = 4R =
Close-packed directions:
3 aaR
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• Coordination # = 12
• Atoms touch each other along face diagonals.
--Note: All atoms are identical; the face-centered atoms are shadeddifferently only for ease of viewing.
Face Centered Cubic Structure (FCC)
ex: Al, Cu, Au, Pb, Ni, Pt, Ag
4 atoms/unit cell: 6 face x 1/2 + 8 corners x 1/859MT30001 Atumn 2016 S K Kar
• APF for a face-centered cubic structure = 0.74
Atomic Packing Factor: FCC
maximum achievable APF
Close-packed directions:
length = 4R = 2 a
Unit cell contains:
6 1/2 8 1/8
2 a
APF =
4
3 ( 2 a/4 ) 34
atoms
unit cell atom
volume
a 3
unit cell
volume
6 x 1/2 + 8 x 1/8
= 4 atoms/unit cella
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• ABAB... Stacking Sequence
• 3D Projection • 2D Projection
Hexagonal Close‐Packed Structure (HCP)
c
A sites Top layer
• Coordination # = 12
• APF = 0.74
6 atoms/unit cell
ex: Cd, Mg, Ti, Zn
• c/a = 1.633
c
a
B sites
A sites Bottom layer
Middle layer
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Spheres at: (0,0,0), (⅔, ⅓,½)
Note: Atoms are coloured differently but are the same
c/a = sqrt( 8/3 )
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APF =
4
3 ( R ) 32
atoms
unit cell atom
volume
3/2 a c2
unit cell
volume
Close-packed directions:
length = 2R = a
Unit cell contains:
4 x 1/(3 x 2) + 4 x 1/(6 x 2) + 1
= 2 atoms/unit cell
c/a =( 8/3 )
Atomic Packing Factor: HCP
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Theoretical Density,
Density = =
VC NA
n A =
CellUnitofVolumeTotal
CellUnitinAtomsofMass
where n = number of atoms/unit cellA = atomic weight VC = Volume of unit cell = a3 for cubicNA = Avogadro’s number
= 6.023 x 1023 atoms/mol
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• Ex: Cr (BCC)
A = 52.00 g/mol
R = 0.125 nm
2
Theoretical Density,
65
n = 2
theoretical
a = 4R/ 3 = 0.2887 nm
actual
aR
= a 3
52.002
atoms
unit cellmol
g
unit cell
volume atoms
mol
6.023 x 1023
= 7.18 g/cm3
= 7.19 g/cm3
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ex: linear density of Al in [110] direction
a = 0.405 nm
Linear Density
• Linear Density of Atoms LD =
[110]
Unit length of direction vector
Number of atoms
a# atoms
length
13.5 nma2
2LD
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Planar Density of (100) Iron
At T < 912C iron has the BCC structure.
(100) R3
34a
2D repeat unit
Radius of iron R = 0.1241 nm
= Planar Density =a2
1
atoms
2D repeat unit
= nm2
atoms12.1
m2
atoms= 1.2 x 1019
12
R3
34area
2D repeat unit 68MT30001 Atumn 2016 S K Kar
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Class Work
Find out the Planar Density of (111) plane of Iron
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Planar Density of (111) IronSolution (cont): (111) plane 1 atom in plane/ unit surface cell
atoms in plane
atoms above plane
atoms below plane
ah3
a2
333 2
2
R3
8R
342a323area ÷
÷
ah2
1/2= =
nm2
atoms7.0m2
atoms0.70 x 1019
3 2R3
8Planar Density =
atoms
2D repeat unit
area
2D repeat unit
4
2a2 2
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Octahedral interstitial sites
FCC BCC
The space in the interstices between 6 regular atoms that form an octahedron.
Four regular atoms are positioned in a plane, the other two are in a symmetrical position just above or below.
12/4 +1 = 4 positions per unit cell
12/4 + 6/2 = 6
iti
Will Provide you this slide
unit cellpositions per unit cell
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Tetrahedral interstitial sites
FCC BCC
The center of a tetrahedra formed by four lattice atoms.
Three atoms, touching each other, are in plane; the fourth atom sits in the symmetrical position on top.
8 positions per unit cell(6 · 4)/2 = 12
iti
Will Provide you this slide
positions per unit cell
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Ceramic Crystal Structures
•Greek word “Keramikos” (= burnt stuff) Ceramics •Desired properties obtained through a high temperature heat treatment process called “Firing”
• Composed of atleast two elements –• Crystal structures are more complex than metals
• Bonding is ionic to covalent•Depending on the electro-negativities of the atoms
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Bond characters of ceramics
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For ceramics having ionic bonding • Cation and anions• Charges on them and relative sizes determine the
crystal structure• Cations are smaller than anions• Ions prefer to have maximum number of oppositely
charged ion nearest neighbours • Stable ceramic structure forms when those anions
surrounding a cation are all in contact with that cationsurrounding a cation are all in contact with that cation
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Radius Ratio Rules
•The coordination number (number of anion nearest neighbours for a cation) is related to the cation-anion radius ratio.
•For a specific coordination number, there is a critical or minimum rC/rA ratio for which the cation-anion contact is established.
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Minimum rC/rA ratio for CN=3
cos30°=rA/(rC+rA) rC/rA = 0.155
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Radius Ratio Rules
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Common Ceramic Crystal Structures
FCCFCCSC
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Crystal = Bravais lattice + Base
• A crystal now is obtained by taking a Bravais latticeand adding a base! The base can just be one atom (as in the case of many elemental crystals, most noteworthy the metals), two identical atoms (e.g. Si Ge C(diamond)) two different atoms (NaClSi, Ge, C(diamond)), two different atoms (NaCl, GaAs, ...) three atoms, ... up to huge complex molecules as in the case of protein crystals.
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Rock Salt (NaCl) Structure
(fcc), with twoatoms in the base: one at (0, 0, 0), the other one at (½, ½, ½)
Many salts and oxides have this structure, e.g. KCl, AgBr, KBr, PbS, ...orMgO, FeO, ...
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CsCl Crystal Structure
cubic primitivewith two atoms in the base at (0,0,0)and (½, ½, ½)
Intermetalliccompounds (not p (necessarily ionic crystals), but also common salts assume this structure; e.g. CsCl, ..., or AlNi, CuZn
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ZnS (Zinc Blende) Structure
(fcc) with two atoms in the base at (0,0,0) and (¼, ¼, ¼)
typical lattice of covalently bonded group IV semiconductors (C(diamond form), Si, Ge)
III V dor III-V compounds semiconductors (GaAs, GaP, InSb, InP, ..)
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CaF2 (Fluorite) Structure
(fcc) with three atoms in the base, one kind (the cations) at (0,0,0), and the other two (anions of the same kind) at (¼, ¼, ¼), and (-¼, -¼, -¼)
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Perovskite crystal Structure
cubic primitive:three different atoms in the base. In the example it would be Ba at (0,0,0), O at (½, ½, ,0), at (½, 0, ½), at (0, ½, ½) and Ti at (½, ½, ½).
Barium titanate (BaTiO3) havingBarium titanate (BaTiO3), having both Ba2+ and Ti4+ cations
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Rock Salt (NaCl) Structure
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Close Packed Structure in ceramics
• Close packed planes of anions
• Cations reside at Tetrahedral and/ or Octrahedralinterstitial sites
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Rock Salt (NaCl) Structure
• Close packed arrangement of Cl ions on {111} planes
• Na+ ions areNa ions are at Octahedral sites
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DENSITY COMPUTATIONS—CERAMICS
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DENSITY COMPUTATIONS—CERAMICS
n’ = 4; FCC lattice
Experimental value: 2.16 gm/cc
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Silicate Ceramics• Bulk of soils, rocks, clays, and sand come under the
silicate classification• Characterize crystal structure in terms of various
arrangements of an SiO44- tetrahedron
• Basic unit of the silicates
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• Chemically, the most simple silicate• Structurally, it is a 3d network generated when every corner O
atom in each tetrahedron is shared by adjacent tetrahedra. • Electrically neutral• The ratio of Si to O atoms is 1 : 2, as indicated by the chemical
formula.
Silica (SiO2)
• Three primary polymorphic p y p y pcrystalline forms of silica: quartz, cristobalite and tridymite.
• Strong Si-O bonds high mp• Relatively open str. Low
density
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Silicon dioxide (or silica, SiO2) in the noncrystalline state is called fused silica, or vitreous silicaOther oxides (e.g., B2O3 and GeO2) may also form glassy structures
SILICA GLASSES
Network formers
The common inorganic glasses used for containers Silica glasses to which ghave been added other oxides such as CaO and Na2OCations are incorporated within and modify the SiO4
4- networkNetwork modifiers
structure of a sodium–silicate glass
Lowers the mp and viscosity of glasses easy formation at low temp
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One or two or three corner oxygen atoms are shared by other tetrahedra
Single chain structure Role of +ve
ions? 95MT30001 Atumn 2016 S K Kar
• A 2d sheet or layered structure • By sharing of 3 O ions in each of the tetrahedra• A second planar sheet structure having an excess of
cations Charge neutrality
Sheet or layered silicates
Their basic structure isTheir basic structure is characteristic of clays and other minerals
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Keolinite (Clay): 2 layer silicate sheet structureAl2(Si2O5)(OH)4
TalcMica
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Diamond Cubic Structure
• Extremely hard
• Low electrical conductivity
• Optically Transparent
• High index of refraction
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Graphite
Lubricative property
Electrical conductivity along sheet
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Fullerenes
BuckminsterfullereneBuckyball
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Carbon Nanotube
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Chain Folded model of Polymer crystallite
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Spherulite sructure
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f35_04_pg99
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X‐Ray Diffraction Pattern
(110)
(211)
z
x
ya b
c
y (r
elat
ive)
z
x
ya b
c
z
x
ya b
c
108
(200)
Diffraction angle 2
Diffraction pattern for polycrystalline -iron (BCC)
Inte
nsity
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• Single Crystals
-Properties vary withdirection: anisotropic.
-Example: the modulusof elasticity (E) in BCC iron:
• Polycrystals
Single vs PolycrystalsE (diagonal) = 273 GPa
E (edge) = 125 GPa
110
y y
-Properties may/may notvary with direction.
-If grains are randomlyoriented: isotropic.(Epoly iron = 210 GPa)
-If grains are textured,anisotropic.
200 m
MT30001 Atumn 2016 S K Kar
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Concept of Grains and Grain Boundary: Single crystal vs. polycrystalline
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Modulus of Elasticity values for several metals at various crystallographic orientations
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Questions1. If you are given plots of interatomic force vs. interatomic distance
for two different metal systems, then how would you determine which metal has higher stiffness among the two from the plots?
2. Why are metals electrically conductive while ceramics are not?
3. How is bond energy related to coefficient of thermal expansion?
4. How many valence electrons are there for Boron?
5. What are the relations between lattice parameters for Monoclinic system?
6. For which four crystal systems, the three axes along unit cell edges are not mutually perpendicular?
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Clarifications:Indexing of Crystallographic planes
• Convert to smallest integers (Optional step)
I d d ti i t i d t ( fIndex reduction is not carried out (e.g., for x-ray or electron diffraction studies); for example, (002) is not reduced to (001). In addition, for ceramic materials, the ionic arrangement for a reduced-index plane may be different from that for a nonreduced one.
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Clarification
Can the indices representing directions be irrational numbers? YES
Can the directions represented by irrational numbers b l tti t ? NObe lattice vectors? NO
So, For lattice vectors, indices have to be integers Miller indices of the Crystallographic directions would be integers
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