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Solution of problems, design problems and also computer problems.
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8/25/2008
1
MSE 280: Introduction to Engineering Materials
Reading: Chapter 3Part 1
Metal and Ceramic StructuresPart 1– Defining ordered atoms in crystalline solids.
Unit cells, unit vectors, Coordinates, directions, planes, close packing…
– Densities: Crystal density, Line density, Planar density– Crystal symmetry and families– Crystallography
MSE280© 2007, 2008 Moonsub Shim, University of Illinois1
Part 2– Ionic crystals.– Lattice energy.– Silica & silicates.– Carbon
ENERGY AND PACKING• Non dense, random packing Energy
typical neighbor bond length
• Dense, regular packing
r
bond length
typical neighbor bond energy
Energy
typical neighbor b d l h
MSE280© 2007, 2008 Moonsub Shim, University of Illinois2
Dense, regular-packed structures tend to have lower energy.
r
bond length
typical neighbor bond energy
From Callister 6e resource CD.
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2
Packing atoms together
• atoms pack in periodic, 3D arrayst i l f
Crystalline materials...
• typical of: -metals-many ceramics-some polymers
Noncrystalline materials...Si Oxygen
crystalline SiO2Adapted from Fig. 3.18(a),Callister 6e.
MSE280© 2007, 2008 Moonsub Shim, University of Illinois3
• atoms have no periodic packing• occurs for: -complex structures
-rapid cooling
noncrystalline SiO2"Amorphous" = NoncrystallineAdapted from Fig. 3.18(b),Callister 6e.
Crystalline materials: Unit Cell
Unit Cell: The basic structuralUnit Cell: The basic structural unit of a crystal structure. Its geometry and atomic positions define the crystal structure.
Note: more than one unit cell can be chosen for a given crystal but by
MSE280© 2007, 2008 Moonsub Shim, University of Illinois4
convention/convenience the one with the highest symmetry is chosen.
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Unit cells and unit vectors
bv
cvLattice parameters
axial lengths: a, b, cinteraxial angles: α, β, γunit vectors:
In general: a ≠ b ≠ cα ≠ β ≠ γ
av bv
cv
MSE280© 2007, 2008 Moonsub Shim, University of Illinois5
av
Unit Cells: Bravais Lattices
MSE280© 2007, 2008 Moonsub Shim, University of Illinois6
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(trigonal)
MSE280© 2007, 2008 Moonsub Shim, University of Illinois7
Unit cell types
Primitive Face-centered
Body-centered End-centered
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Number of atoms in a unit cell
Simple cubic
8 atoms but each atom is shared by 8 unit cells.
→ 1 atom per unit cell
MSE280© 2007, 2008 Moonsub Shim, University of Illinois9
p
Coordination NumberNumber of nearest neighbor atoms
MSE280© 2007, 2008 Moonsub Shim, University of Illinois10
Simple cubic: coordination number = 6
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Atomic Packing Factor (APF)
APFVol. of atoms in unit cell
Depends on: • Crystal structure.• How “close” packed the atoms are.
APF =Vol. of unit cell
MSE280© 2007, 2008 Moonsub Shim, University of Illinois11
p• In simple close-packed structures with hard sphere atoms, independent of atomic radius
Close packing of atomsConsider atoms as hard spheres.
MSE280© 2007, 2008 Moonsub Shim, University of Illinois12
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Face-Centered Cubic (FCC)
Atoms at the corners of the cube+
Atoms at the center of each face
a a = ||unit vector||4R
R = atomic radius
MSE280© 2007, 2008 Moonsub Shim, University of Illinois13
a Ra
)R(aa
22
4 222
=
=+
Face-Centered Cubic (FCC)
MSE280© 2007, 2008 Moonsub Shim, University of Illinois14
Adapted from Fig. 3.1(a),Callister 6e.
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Number of atoms in an FCC unit cell
• Each corner atom contributes as 1/8contributes as 1/8.There are 8 corner atoms in an FCC unit cell.
• Each face atom contributes as 1/2.There are 6 face atoms.
MSE280© 2007, 2008 Moonsub Shim, University of Illinois15
cell_unit/atoms)atoms_face()atoms_corner( 46218
81
=×+×
Coordination number for FCC
R22
1 4
32
8
7
6
5
12 11
1092R
R22
R22
MSE280© 2007, 2008 Moonsub Shim, University of Illinois16
8
Total 12 nearest neighbor atomsCoordination number = 12
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Atomic packing factor (APF) for FCC
2R
R22
R22
a 4R
⎟⎠⎞
⎜⎝⎛= 3
344 RVatoms π
MSE280© 2007, 2008 Moonsub Shim, University of Illinois17
a
⎠⎝ 3333
_ 216)22( RRaV cellunit ===
74.023216
316
3
3
_
==⎟⎠⎞
⎜⎝⎛
==π
π
R
R
VVAPF
cellunit
atoms Independent of R and a!
Summary for FCC
a 4R
||unit vector|| =
4 atoms/unit cell
Coordination number = 12
APF = 0.74
Ra 22=
MSE280© 2007, 2008 Moonsub Shim, University of Illinois18
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10
Body-Centered Cubic (BCC)
a2
Atoms at the corners of the cube+
Atom at the center of the cubea
a2
R4
MSE280© 2007, 2008 Moonsub Shim, University of Illinois19
( ) ( )
34
42 222
Ra
Raa
=
=+
Body-Centered Cubic (BCC)
MSE280© 2007, 2008 Moonsub Shim, University of Illinois20
From Callister 6e resource CD.
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Number of atoms in a BCC unit cell
• Each corner atom contributes as 1/8contributes as 1/8.There are 8 corner atoms in an FCC unit cell.
• The center atom contributes as 1.There is only 1 center atom
MSE280© 2007, 2008 Moonsub Shim, University of Illinois21
atom.
cell_unit/atoms)atom_center()atoms_corner( 211881
=×+×
Coordination number for BCC
32
Total 8 nearest neighbor atomsCoordination number = 8
4
7
32
6
1
MSE280© 2007, 2008 Moonsub Shim, University of Illinois22
85
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Atomic packing factor (APF) for BCC
⎟⎠⎞
⎜⎝⎛= 3
342 RVatoms πa2
)4()2( 222 Raa =+
3364)
34(
333
_RRaV cellunit ===
⎞⎛
a R43
4)4()2(
Ra
Raa
=
=+
MSE280© 2007, 2008 Moonsub Shim, University of Illinois23
68.083
336438
3
3
_
==⎟⎠⎞
⎜⎝⎛
==π
π
R
R
VVAPF
cellunit
atoms
Summary for BCC
2
||unit vector|| =
2 atoms/unit cell
Coordination number = 8
34Ra =
a
a2
R4
MSE280© 2007, 2008 Moonsub Shim, University of Illinois24
APF = 0.68
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Hexagonal Close-Packing (HCP)
MSE280© 2007, 2008 Moonsub Shim, University of Illinois25
Find a, c, number of atoms/unit cell, coordination number, and APF for HW.
Point Coordinatesto define a point within a unit cell….Essentially same as Cartesian coordinates except values of x, y, and z are expressed as fractions of the magnitude of unit vector(s) (and x, y, and z not necessarily orthogonal)and z not necessarily orthogonal).
ab
y
zpt. coord.
x (a) y (b) z (c)
A 0 0 0
B 1 0 0
C 1 1 1
MSE280© 2007, 2008 Moonsub Shim, University of Illinois26
c
x
y
= point “A” = origin
= point “B”
= point “C”
= point “D”
D 1/2 0 1/2
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Crystallographic DirectionsTo define a vector:
1. Start at the origin.2 Determine length of vector projection in each of 3 axes in units2. Determine length of vector projection in each of 3 axes in units
(or fractions) of a, b, and c.3. Multiply or divide by a common factor to reduce the lengths to
the smallest integer values.4. Enclose in square brackets: [u v w] where u, v, and w are
integers.
Along unit vectors: a b c
MSE280© 2007, 2008 Moonsub Shim, University of Illinois27
Note: in any of the 3 directions there are both positive and negative directions.Negative directions are denoted with a “bar” over the number.
e.g. [1 1]1
Example 1: Assign the coordinates to the following crystallographic direction
Along x: 1 az
ab
c y
Along y: 1 bAlong z: 1 c
[1 1 1]
MSE280© 2007, 2008 Moonsub Shim, University of Illinois28
x
[1 1 1]
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Example 2: draw [1 0] direction. 1
1 unit vector length along x
-1 unit vector length along y
ab
c y
z
g g y
0 unit vector length along z
MSE280© 2007, 2008 Moonsub Shim, University of Illinois29
c
x
y
[1 0]1origin
Note: for some crystal structures, different directions can be equivalent.
e.g. For cubic crystals:
[1 0 0], [ 0 0], [0 1 0], [0 0], [0 0 1], [0 0 ] are all equivalent
111
Families of crystallographic directionse.g. <1 0 0>
MSE280© 2007, 2008 Moonsub Shim, University of Illinois30
Angled brackets denote a family of crystallographic directions.
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Families and Symmetry• Which directions belong in the same family is determined by the
crystal symmetry.• What is symmetry?
Whi h i t i ?• Which one is more symmetric?
• The more symmetry operations there are the more symmetric it is.
a
a
a a
b
c
1 31 1
MSE280© 2007, 2008 Moonsub Shim, University of Illinois31
• Which is more symmetric, cubic or tetragonal?
23 12
and
23 32equivalentequivalent
etc…
Families and Symmetryz
zCubic symmetry
x
y[100]
Rotate 90o about z-axis
x
y
[010]
z
[001]Rotate 90o about y-axis
MSE280© 2007, 2008 Moonsub Shim, University of Illinois32x
y
[001]y
Similarly for other equivalent directions
Symmetry operation can generate all the directions within in a family.
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Crystallographic directions for hexagonal crystals
Consider vectors q and r….If we keep the 3-coordinate system:
y
z = [1 0 0]= [1 1 0]
qv
rv
Different set of indices. However, these two vectors are equivalent by symmetry (i.e. via 60o rotation).
MSE280© 2007, 2008 Moonsub Shim, University of Illinois33
xqv
rv
Choose a 4-coordinate system!
Crystallographic directions for hexagonal crystals
In the Miller-Bravais (4 axes) coordinate system, We have:
a2
z= [2 0]qv 11
MSE280© 2007, 2008 Moonsub Shim, University of Illinois34
qv
a1
a3
Although the length is different the direction is the same.
2 along a1
-1 along a2 -1 along a3
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Crystallographic directions for hexagonal crystals
Similarly for , in the Miller-Bravais (4 axes) coordinate rvsystem, we now have:
a2
z= [1 1 0]rv 2
-2 along a
MSE280© 2007, 2008 Moonsub Shim, University of Illinois35
rva1
a3
1 along a1
1 along a2
-2 along a3
Again, consistent direction.
Crystallographic directions for hexagonal crystals
Miller-Bravais (4 axes) coordinate system
a2
z
We now have:
= [2 0]= [1 1 0]
qv
rv12
1
MSE280© 2007, 2008 Moonsub Shim, University of Illinois36
qvrv
a1
a3
Indices are now consistent within the family, but where do these numbers come from?
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To transform 3 indices to 4 indices[u’ v’ w’] [u v t w]
u = 1/3 (2u’ – v’)( )v = 1/3 (2v’ – u’)t = - (u + v)w = w’
May need to factor to reduce u, v, t, and w to their smallest integers.
e.g. convert = [1 0 0] to 4-coord. system.
u = 1/3 (2x1 – 0) = 2/3 2
v = 1/3 (2x0 1) = 1/3 1
x 3
x 3
qv z
MSE280© 2007, 2008 Moonsub Shim, University of Illinois37
v = 1/3 (2x0 – 1) = -1/3 -1
t = -(2/3 + (-1/3)) = -1/3 -1
w = 0 0
x 3
x 3
[2 0]1 1 a2
qv a1
a3
transforming 3 indices to 4 indices
convert = [1 1 0] to 4-coord. system. rv
u = 1/3 (2x1 – 1) = 1/3 1
v = 1/3 (2x1 – 1) = 1/3 1
t = -(1/3 + 1/3) = -2/3 -2
w = 0 0
x 3
x 3
x 3
x 3
[1 1 0]
z
2
MSE280© 2007, 2008 Moonsub Shim, University of Illinois38
a2
a1
a3rv
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Crystallographic PlanesTo define a plane (i.e. to assign Miller Indices):
1. If the plane passes through the origin, eitherza) Construct a parallel plane translated
ab
c y
b) choose another origin at the corner of adjacent unit cell
or
2. Now, the plane either intersects or parallels each of the three axes
MSE280© 2007, 2008 Moonsub Shim, University of Illinois39
origin
origin
the three axes.3. Determine length in terms of lattice parameters a, b and c.
x
Parallel to x-axis = length along x ∞Parallel to y-axis = length along y ∞Intercepts z-axis at z = c
Crystallographic Planes4. Take the reciprocal of the lengths
Al i l th 0e.g. Along x-axis: length = 0∞Along y-axis: length = 0∞Along z-axis: length = 1 1
5. If necessary, factor to get the smallest integers.
e g if we had 0 0 3 0 0 1divide through by 3
MSE280© 2007, 2008 Moonsub Shim, University of Illinois40
e.g. if we had 0, 0, 3 0, 0, 16. Enclose indices in parentheses w/o commas
In the example on previous slide, the Miller index would be (0 0 1)
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Example 1Assign Miller indices
1 Shift i i f O t O’
ab
z
c/3O
1. Shift origin from O to O’
z’ 2. Determine lengths along each axis
Along x = ∞Intersects y at -1 Intersects z at 1/3
MSE280© 2007, 2008 Moonsub Shim, University of Illinois41
c
x
yc/3O
O’
x’
3. Take the reciprocal: 0, -1, 3
4. No need to factor.5. (0 3)1
Example 2Draw the (0 1) plane.1
1 along x = 0
y
z1. along x 0
The plane runs parallel to x-axis2. along y = -1 (in units of b)
take reciprocal: -1y-intercept at -1
3. along z = 1 (in units of c)take reciprocal: 1z intercept at 1
|b||c|
MSE280© 2007, 2008 Moonsub Shim, University of Illinois42
x
z-intercept at 1
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Crystallographic planes in FCC
z
MSE280© 2007, 2008 Moonsub Shim, University of Illinois43x
y
(1 0 0) planeLook down this direction (perpendicular to the plane)
Crystallographic planes in FCC
zLook down this direction(perpendicular to the plane)
MSE280© 2007, 2008 Moonsub Shim, University of Illinois44x
y
(1 1 1) plane
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Note: similar to crystallographic directions, planes that are parallel to each other are equivalent
MSE280© 2007, 2008 Moonsub Shim, University of Illinois45
Crystallographic Planes for Hexagonal Crystals
Similar to crystallographic directions for hexagonal crystals, 4-coordinate system is used.
i.e. instead of (h k l) for 3-coordinate systems, use (h k i l).
For integers h, k, and l, same procedure as 3-coordinate
MSE280© 2007, 2008 Moonsub Shim, University of Illinois46
systems is used and i = - (h+k)
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Crystallographic planes in HCPz
Name this plane…
a2
MSE280© 2007, 2008 Moonsub Shim, University of Illinois47
a1
a3(0 0 0 1) plane
Parallel to a1, a2 and a3 -> h = k = i = 0Intersects at z = 1
Crystallographic planes in HCP
z
a2
MSE280© 2007, 2008 Moonsub Shim, University of Illinois48
a1
a3
(1 1 0 0) plane
+1 in a1
-1 in a2
h = 1, l = 0i = -(1+-1) = 0,k = -1,
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(1 1 1) plane of FCCz
x
y
z (0 0 0 1) plane of HCPSAME THING!*
MSE280© 2007, 2008 Moonsub Shim, University of Illinois49a1
a2
a3
Close Packing
MSE280© 2007, 2008 Moonsub Shim, University of Illinois50
Note: whether the atoms of 2nd layer fills B-sites or C-sites does not matter.They are equivalent until the 3rd layer is added!
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FCC
MSE280© 2007, 2008 Moonsub Shim, University of Illinois51
HCP
MSE280© 2007, 2008 Moonsub Shim, University of Illinois52
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Difference between FCC and HCPLooking down (0001) plane
MSE280© 2007, 2008 Moonsub Shim, University of Illinois53
HCPFCC
ABCABC… ABABAB…
Looking down (111) plane!
Densities
C t l d it (i 3D d it ) i it f• Crystals density (i.e. 3D density) in units of mass per volume (e.g. g/cm3).
• Linear density: number of atoms per unit length (e.g. cm-1).
• Planar density: number of atoms per unit area (e g
MSE280© 2007, 2008 Moonsub Shim, University of Illinois54
• Planar density: number of atoms per unit area (e.g. cm-2).
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Crystals density (ρ)Mass of unit cell
VM
=ρ Volume of unit cell
ANnAM =
n = number of atoms in unit cellA = atomic weightNA = Avogadro’s number
MSE280© 2007, 2008 Moonsub Shim, University of Illinois55
VNnA
A
=ρ
Density exampleCalculate density of copper given: R = 0.128 nm
A = 63.5 g/molFCC structure
Recall for FCC, there are 4 atoms per unit cell.
Express unit cell volume in terms of atomic radius R.3aV = 3)22( R= 3216 R=
nAM==ρ
Then we have:
MSE280© 2007, 2008 Moonsub Shim, University of Illinois56
3216 RNV A
==ρ
38123 )1028.1)(216)(10022.6()/3.65(4
cmxmolxmolg
−−= = 8.89 g/cm3
Compare to actual value of 8.94 g/cm3!
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Linear Density (LD)LD =
Number of atoms centered on a direction vectorLength of the direction vector
Example: calculate the linear density of an FCC crystal along [1 1 0].
Length = 4R
Effectively 2 atoms along the
MSE280© 2007, 2008 Moonsub Shim, University of Illinois57
atoms along the [1 1 0] vector.
LD = 2/4R = 1/2R
Planar Density (PD)PD =
Number of atoms centered on a given planeArea of the plane
Example: calculate the planar density on (1 1 0) plane of an FCC crystal.
Ra 22=
MSE280© 2007, 2008 Moonsub Shim, University of Illinois58
R4Count only the parts of the atoms within the plane: 2 atoms
RRarea 422 ×= 2241
)22)(4(2
RRRPD ==
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Example problem(110)
nm 0
(101)0.
(011)
0.39 nm
0.2
.32 nm0.3 nm
36 nm
0.253 nm
Given above information answer the following questions.
MSE280© 2007, 2008 Moonsub Shim, University of Illinois59
g qA) What is the crystal structure?B) If atomic radius is 0.08 nm, what is APF?C) If atomic weight is 43 g/mol, calculate density.D) What is the linear density along [210]?E) What is the planar density of (210)?
How to determine crystal structureThe two slit experiment
Same idea with crystals- Light gets scattered off atoms…
Incoming light
dθ
λ
MSE280© 2007, 2008 Moonsub Shim, University of Illinois60
Constructive interference when nλ = 2d sin θ (Bragg’s Law)λ and d have to be comparable lengths. But since d (atomic spacing) is on the
order of angstroms: x-ray diffraction
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Diffraction Experiment and Signal
Diffraction Experiment Scan versus 2x Angle: Polycrystalline Cu
Measure 2θ
Diffraction collects data in “reciprocal space” since it is the equivalent of
MSE 280: Introduction to Engineering Materials ©D.D. Johnson 2004, 2006-08
How can 2θ scans help us determine crystal structure type and distances between Miller Indexed planes (I.e. structural parameters)?
p p qa Fourier transform of “real space”, i.e., eikr, as k ~ 1/r.
Crystal Structure and Planar Distances
h, k, l are the Miller Indices of the planes of atoms that scatter!
BravaisLattice
Constructive Interference
Destructive Interference
Reflections present
Reflections absent
BCC (h + k + l) = Even (h + k + l) = Odd
Distances between Miller Indexed planes
of atoms that scatter!
So they determine the important planes of atoms, or symmetry.
BCC (h + k + l) = Even (h + k + l) = Odd
FCC (h,k,l) All Odd or All Even
(h,k,l) Not All Odd or All Even
HCP Any other (h,k,l) h+2k=3n, l = Oddn= integer
MSE 280: Introduction to Engineering Materials ©D.D. Johnson 2004, 2006-08
For cubic crystals:
dhkl =a
4
3(h2 + hk + k2 ) + l2 a
c⎛⎝
⎞⎠
2
For hexagonal crystals:
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(h k l) h2+k2+l2 h+k+l h,k,l all even or odd?
100 1 1 No110 2 2 No111 3 3 Yes
Allowed (hkl) in FCC and BCC for principal scattering (n=1)
Self-Assessment:From what crystal structure is this?
111 3 3 Yes200 4 2 Yes210 5 3 No211 6 4 No220 8 4 Yes221 9 5 No300 9 3 No310 10 4 No
MSE 280: Introduction to Engineering Materials ©D.D. Johnson 2004, 2006-08
310 10 4 No311 11 5 Yes222 12 6 Yes320 13 5 No321 14 6 No
h + k + l was even and gave the labels on graph above, so crystal is BCC.
Example problem: X-ray crystallography
• Given the information below, determine the crystal structure. Consider only FCC and BCC structures asstructure. Consider only FCC and BCC structures as possibilities. – Lattice parameter: a = 0.4997nm– Powder x-ray: λ = 0.1542 nm
2θ (o)3136
MSE280© 2007, 2008 Moonsub Shim, University of Illinois
3651.861.664.8
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Diffraction of Single 2D Crystal Grain
Lattice of Atoms: Crystal Grain Diffraction Pattern in (h,k) plane
MSE 280: Introduction to Engineering Materials ©D.D. Johnson 2004, 2006-08
Powder diffraction figures taken from Th. Proffe and R.B. Neder (2001)
http://www.uni-wuerzburg.de/mineralogie/crystal/teaching/pow_a.html
Diffraction of Multiple Single 2D Crystal Grains (powders)
Multiple Crystal Grains:4 Polycrystals
Diffraction Patternin (h,k) plane (4 grains)
Diffraction Patternin (h,k) plane (40 grains)
MSE 280: Introduction to Engineering Materials ©D.D. Johnson 2004, 2006-08
Powder diffraction figures taken from Th. Proffe and R.B. Neder (2001)
http://www.uni-wuerzburg.de/mineralogie/crystal/teaching/pow_a.html
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Example from Graphite
Single Crystal Grain Mutlple Grains: Polycrystal
MSE 280: Introduction to Engineering Materials ©D.D. Johnson 2004, 2006-08
Powder diffraction figures taken from Th. Proffe and R.B. Neder (2001)
http://www.uni-wuerzburg.de/mineralogie/crystal/teaching/pow_a.html
Concepts to remember• Unit cell, unit vector, and lattice parameters.• Bravais Lattices.• Counting number of atoms for a given unit cell.• Coordination number = number of nearest neighbor
atoms.• Atomic Packing Factor (APF) = Volume of atoms in a
unit cell/Volume of unit cell.• Close-packing• FCC BCC HCP
MSE280© 2007, 2008 Moonsub Shim, University of Illinois68
• FCC, BCC, HCP• Crystallographic coordinates, directions, and planes.• Densities• X-ray crystallogrphy