structure 3
TRANSCRIPT
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1
Chapter 3:
The Structure of Crystalline Solids
ISSUES TO ADDRESS...
• How do atoms assemble into solid structures?
(for now, focus on metals)
• How does the density of a material depend on
its structure?
• When do material properties vary with the
sample (i.e., part) orientation?
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!
Materials and Packing
• atoms pac& in periodic, ' arraysCrystalline materials...
$metals
$many ceramics
$some polymers
• atoms have no periodic pac&in%
Noncrystalline materials...
$comple structures$rapid coolin%
crystalline *i+!
noncrystalline *i+!Amorphous - oncrystalline
Si Oxygen
• typical of/
• occurs for/
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0hapter ' $
Crystal Systems'
crystal systems
12 crystal lattices
3nit cell/ smallest repetitive volume whichcontains the complete lattice pattern of a crystal.
a, b, and c are the lattice constants
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0hapter ' $
Crystal Systems2
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"
Metallic Crystal Structures
• 4end to be densely pac&ed.• 5easons for dense pac&in%/
$ 4ypically, only one element is present, so all atomic
radii are the same.
$ Metallic bondin% is not directional.$ earest nei%hbor distances tend to be small in
order to lower bond ener%y.
$ lectron cloud shields cores from each other.
• Have the simplest crystal structures.
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6
Simple Cubic Structure (SC)• 5are due to low pac&in% density (only 7o has this structure)
• 0lose$pac&ed directions are cube ed%es.
• 0oordination 8 - 6
(8 nearest nei%hbors)
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Atomic Packing actor (AP)
• 97: for a simple cubic structure - #."!
97: -a'
2
'π (#."a) '1
atoms
unit cellatom
volume
unit cell
volume
97: -;olume of atoms in unit cell<
;olume of unit cell
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=
!ody Centered Cubic Structure (!CC)
• 0oordination 8 - =
• 9toms touch each other alon% cube dia%onals.$$ote/ 9ll atoms are identical the center atom is shaded
e/ 0r, W, :e (α), 4antalum, Molybdenum
! atoms>unit cell/ 1 center @ = corners 1>=
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A
Atomic Packing actor: !CC
a
97: -
2
'π ( 'a>2)'!
atoms
unit cell atom
volume
a'
unit cell
volume
len%th - 2R -
0lose$pac&ed directions/
' a
• 97: for a body$centered cubic structure - #.6=
aR
a2
a3
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1#
ace Centered Cubic Structure (CC)
• 0oordination 8 - 1!
• 9toms touch each other alon% face dia%onals.$$ote/ 9ll atoms are identical the face$centered atoms are shaded
e/ 9l, 0u, 9u, 7b, i, 7t, 9%
2 atoms>unit cell/ 6 face 1>! @ = corners 1>=
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11
Atomic Packing actor: CC• 97: for a face$centered cubic structure - #.2
maimum achievable 97:
97: -
2
'π ( !a>2)'2
atoms
unit cell atomvolume
a'
unit cell
volume
0lose$pac&ed directions/
len%th - 2R - ! a
3nit cell contains/ 6 1>! @ = 1>=
- 2 atoms>unit cella
! a
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0hapter ' $
1!
9 sites
B B
B
BB
B B
0 sites
0 0
0 9
B
B sites
• 9B09B0... *tac&in% *eCuence
• ! 7roDection
• :00 3nit 0ell
:00 *tac&in% *eCuence
B B
B
BB
B B
B sites
0 0
0 9
0 0
0 9
A
BC
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1'
"e#agonal Close$Packed Structure ("CP)
• 0oordination 8 - 1!
• 9B9B... *tac&in% *eCuence
• 97: - #.2
• ' 7roDection • ! 7roDection
6 atoms>unit cell
e/ 0d, M%, 4i, En• c >a - 1.6''
c
a
9 sites
B sites
9 sites Bottom layer
Middle layer
4op layer
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Theoretical %ensity& ρ12
where n - number of atoms>unit cell
A - atomic wei%ht
V C - ;olume of unit cell - a' for cubic
N 9 - 9vo%adroFs number
- 6.#!' 1#!' atoms>mol
ensity - ρ -
V C N 9
n Aρ -
0ell3nitof ;olume4otal
0ell3nitin 9tomsof Mass
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Theoretical %ensity& ρ1"
'#: Cr (!CC) A *+,, g-mol
R ,+.* nm
n *
ρtheoretical
a - 2R > ' - #.!== nm
ρactual
aR
ρ -a'
"!.##!
atoms
unit cell mol
%
unit cell
volume atomsmol
6.#!' 1#!'
- .1= %>cm'
- .1A %>cm'
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0hapter ' $
%ensities of Material Classes16ρmetals
Gρceramics
Gρpolymers
Why?
ρ
( % > c m
) '
raphite>0eramics>
*emiconductor
Metals> 9lloys
0omposites>fibers
7olymers
1
!
!#
'#
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1
Crystals as !uilding !locks
• Some en%ineerin% applications reCuire sin%le crystals/
• 7roperties of crystalline materials
often related to crystal structure.
$$/ uartN fractures more easily
alon% some crystal planes thanothers.
$$diamond sin%le
crystals for abrasives
$$turbine blades
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1=
Polycrystals• Most en%ineerin% materials are polycrystals.
• b$Hf$W plate with an electron beam weld.
• ach %rain is a sin%le crystal.• Lf %rains are randomly oriented, overall component properties are not directional.
• rain siNes typically ran%e from 1 nm to ! cm
(i.e., from a few to millions of atomic layers).
1 mm
Lsotropic
9nisotropic
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1A
Single /s Polycrystals• *in%le 0rystals
$7roperties vary with direction/ anisotropic.
$ample/ the modulus
of elasticity () in B00 iron/
• 7olycrystals
$7roperties may>may not
vary with direction.
$Lf %rains are randomly
oriented/ isotropic. (poly iron - !1# 7a)
$Lf %rains are tetured,
anisotropic.
!## µm
(dia%onal) - !' 7a
(ed%e) - 1!" 7a
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Polymorphism!#
T0o or more distinct crystal structures for the samematerial (allotropy-polymorphism)
titanium
α& β$Ti
carbon
diamond& graphite
B00
:00
B00
1"'=O0
1'A2O0
A1!O0
-:e
γ-:e
-:e
liCuid
iron system
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0hapter ' $
Point Coordinates!1
Point coordinates for unit cellcenter are
a-*& b-*& c-* 1 1 1
Point coordinates for unit cellcorner are ...
Translation: integer multiple oflattice constants identicalposition in another unit cell
z
x
y
a b
c
###
111
y
z
•
2c
•
•
•
b
b
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Crystallographic %irections!!
1. ;ector repositioned (if necessary) to pass
throu%h ori%in.
!. 5ead off proDections in terms of
unit cell dimensions a, b, and c
'. 9dDust to smallest inte%er values
2. nclose in sCuare brac&ets, no commas
Puvw Q
e/ 1, #, R -G !, #, 1 -G P !#1 Q
$1, 1, 1
z
x
9l%orithm
where overbar represents a
ne%ative inde
P 111 Q-G
y
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0hapter ' $
Crystallographic Planes!"
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0hapter ' $
Crystallographic Planes!6
Miller 2ndices: eciprocals of the (three) a#ialintercepts for a plane& cleared of fractions 4common multiples+ All parallel planes ha/esame Miller indices+
Algorithm.+ ead off intercepts of plane 0ith a#es in
terms of a& b& c
*+ Take reciprocals of intercepts3+ educe to smallest integer /alues5+ 'nclose in parentheses& no
commas i+e+& (hkl )
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0hapter ' $
Crystallographic Planes!
z
x
y a b
c
2. Miller Lndices (11#)
eample a b c z
x
y a b
c
2. Miller Lndices (!##)
1. Lntercepts 1 1 ∞!. 5eciprocals 1>1 1>1 1>∞
1 1 #'. 5eduction 1 1 #
1. Lntercepts 1>! ∞ ∞!. 5eciprocals 1>R 1>∞ 1>∞
! # #'. 5eduction ! # #
eample a b c
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0hapter ' $
Crystallographic Planes!=
z
x
y a b
c •
•
•
2. Miller Lndices (6'2)
eample1. Lntercepts 1>! 1 '>2
a b c
!. 5eciprocals 1>R 1>1 1>S
! 1 2>'
'. 5eduction 6 ' 2
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0hapter ' $
6inear %ensity '#
6inear %ensity of Atoms≡
6%
e/ linear density of 9l in P11#Q
direction
a - #.2#" nm
a
P11#Q
3nit len%th of direction vector
umber of atoms
8 atoms
len%th
1'." nma!
!K −==
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0hapter ' $
Crystallographic Planes'1
7e 0ant to e#amine the atomic packing ofcrystallographic planes
2ron foil can be used as a catalyst+ Theatomic packing of the e#posed planes is
important+a) %ra0 (.,,) and (...) crystallographic planes
for e+
b) Calculate the planar density for each of theseplanes+
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0hapter ' $
Planar %ensity of (.,,) 2ron'!Solution: At T 8 9.*°C iron has the !CC structure+
(1##)
5adius of iron R - #.1!21 nm
R '
'2a =
9dapted from :i%. '.!(c), Callister 7e.
! repeat unit
-7lanar ensity - a!
1
atoms
! repeat unit
-nm!
atoms1!.1
m!atoms
- 1.! 1#1A 1
!
R '
'2area
! repeat unit
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Planar %ensity of (...) 2ron
''Solution (cont): (...) plane 1 atom in plane> unit surface cell
'''
!
!
R '
16R
'
2!a'ah!area =÷÷
===
atoms in plane
atoms above plane
atoms below plane
ah23=
a2
! (
r e p e a t u n i t
1
- -nm!
atoms.#
m!atoms
#.# 1#1A
' !R '
167lanar ensity -
atoms
! repeat unit
area
! repeat unit
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$ay %iffraction'2
%iffraction gratings must ha/e spacings comparable tothe 0a/elength of diffracted radiation+
Can;t resol/e spacings
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0hapter ' $
$ays to %etermine Crystal Structure'"
T$rayintensity(fromdetector)
θ
θc
d =n λ
! sinθc
Measurement ofcritical an%le, θc,allows computation of
planar spacin%, d .
• Lncomin% T$rays diffract from crystal planes.
9dapted from :i%. '.1A,
Callister 7e.
reflections mustbe in phase fora detectable si%nal
spacin%betweenplanes
d
i n c o m i n %
T $ r a y s
o u t %
o i n %
T $ r a
y s
d e t e c t o r
θλ
θetra
distancetravelledby wave U!V
U 1 V U ! V
U 1 V
U ! V
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$ay %iffraction Pattern'6
(11#)
(!##)
(!11)
z
x
y a b
c
iffraction an%le !θ
iffraction pattern for polycrystalline α$iron (B00)
L n t e n s i t y ( r
e l a t i v e )
z
x
y a b
c
z
x
y a b
c
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'
S
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'=
S