Chapter 7
Introduction to
Crystallography
Crystalline Substances: e.g., Diamond and Table Salt
Diamonds
7.1 periodicity and lattices of crystal structure
7.1.1 The characteristics of crystal structure
1. A few definitions:
• Solids can be divided into two primary categories,
crystalline and amorphous.
• Crystalline Solids are built from atoms or molecules
arranged in a periodic manner in space, e.g., rock salt and
diamond.
• Amorphous Solids possess short-range order only. They
are not related through symmetry, e.g. glass, rosin, amber
glass.
• Short-Range Order: Fixed bond lengths and angles
• Long-Range Order: Associated with a lattice point
Crystals:
Crystals are solids that are built from atoms or
molecules arranged in a periodic manner in space.
2. Fundamental characteristics of crystal
a) Spontaneous formation of polyhedral shapes
F+V=E+2
b) Uniformity: periodic distribution of
atoms/molecules
Single crystal gold bead with
naturally formed facets
HRTEM images of hollow beads
•Anisotropy
Different periodicity and density for different direction.
2150 g/mm2
Conductivity
1150 g/mm2
570 g/mm2
Graphite
NaCl
•Definite sharp melting points
T
t
• Symmetry: crystal shape (macroscopic)
lattice arrangement (microscopic)
•X-ray diffraction by crystals:
atomic distances match the wavelength of x-ray.
7.1.2 The lattice and unit cell
Lattice:
• A periodic pattern of points in space, such
that each lattice point has identical
surroundings.
• Can be reproduced by translational motion
along the vector between any two points.
a. The lattice and its unit in 1D:
Tm = ma (m = 0, 1, 2,) a: basic vector.
Each motif in this
1D pattern can be
represented by a
point.
A one-dimensional lattice This 1D system is
represented by a
lattice of repeating
points.
Different choice of unit cell for a 1D lattice
Note: the translation vectors connecting any two lattice
points constitute a translation group.
Examples of 1D lattice
b. Lattice and its unit in 2D:
Tmn = ma + nb(m, n = 0,1, 2, )
a & b: independent basic vectors
•Crystal structure = lattice + structural motif
(basis)
Lattice:
•A periodic pattern of points in space, such that
each lattice point has identical surroundings.
•Can be reproduced by translational motion
along the vector between any two points.
this 2D pattern 2D lattice. 2D lattice.
itself is not a lattice,
but can be
represented by a
2D Lattice.
2D Primitive Cell
Unit Cell Choice
There is always more than one possible
choice of unit cell
By convention the unit cell is chosen so
that it is as small as possible while
reflecting the full symmetry of the lattice
1) The highest symmetry
2) The smallest area (or volume)
Five 2D lattices
ab 90, a=b =90
120 ab =90
ab =90 a=b =120
Primitive
unit cell
Centered
There are literally thousands of crystalline
materials, there are only 5 distinct planar lattices
c. Lattices and its unit in 3D:
T = ma + nb + pc (m, n, p = 0, 1, 2, …)
What’s the smallest structure motif of a graphene sheet?
The Choice of a Unit Cell: Have the highest symmetry
and minimal size
c
b
a
c
a b
The Choice of a Primitive Cell
1) The axial system consisting of the basis
vectors should be right handed.
2) The basis vectors should coincide as much as possible
with directions of the highest symmetry.
3) Should be the smallest volume that satisfies condition 2.
4) Of all lattice vectors none is shorter than a.
5) Of those not directed along a none is shorter than b.
6) Of those not lying in the a, b plane none is shorter than c.
7) The three angles between the basis vectors a,b,c are
either all acute or obtuse.
Crystal structure = lattice + structural motif
(basis)
Atomic Coordinates: Fractional coordinates
Fractional coordinates:
The positions of atoms inside a
unit cell are specified using 0.5
fractional coordinates(x,y,z). i
These coordinates specify the
position as fractions of the unit 0.6
cell edge lengths
i: (1.0, 0.6, 0.5)
Example:
Cubic unit cell of CsCl,
a=b=c
===90
Cs:(0,0,0)
Cl: (1/2,1/2,1/2)
Single Crystal: Composed of only one particular type of space lattice.
Polycrystalline matter: Clusters of multiple crystals.
Chapter 7 Introduction to Crystallography
a. The lattice and its unit in 1D:
T = ma (m = 0, 1, 2,)
unit cell and its choice for one-dimensional lattice
b. Lattice and its unit in 2D:
T = ma + nb(m, n = 0,1, 2, )
•Crystal structure = lattice + structural motif
(basis)
Five 2D lattices
ab 90, a=b =90
120 ab =90
ab =90 a=b =120
Primitive
unit cell
Centered
There are literally thousands of crystalline materials,
there are only 5 distinct planar lattices
c. Lattices and its unit in 3D:
T = ma + nb + pc (m, n, p = 0, 1, 2, …)
c
b
a
c
a b
Crystal structure = lattice + structural motif
(basis)
Atomic Coordinates: Fractional coordinates
Fractional coordinates:
The positions of atoms inside a
unit cell are specified using 0.5
fractional coordinates(x,y,z). i
These coordinates specify the
position as fractions of the unit 0.6
cell edge lengths
i: (1.0, 0.6, 0.5)
7.1.3 Crystal systems and Bravais Lattices
a. Crystal systems
A total of seven types of crystal
systems exist with different symmetry
elements.
Crystal Characteristic Unit cell Choice of axis Lattic
systems symmetry parameters Point
elements Group
Triclinic Nil abc Ci
Monoclinic C2, h abc b // 2-fold axis C2h
==90
Orthorhombic 3C2, 2 h abc a, b, c // 2-fold D2h
===90 axes
Unit cell is chosen in such a way that it contains as many
symmetry elements of the lattice as possible and, meanwhile,
has the smallest volume.
Trigonal 3-fold rotation Rhombohedr D3d
axes al
a=b=c
== are used to specify a set of symmetry-
equivalent directions.
[uvw] zone axis Direction Vector = ua + vb + wc
d. d-spacing dhkl
(010)
(110)
d010
d110
( 2 10)
(210)
( 1 20)
The spacing between adjacent planes in a family is
referred to as a “d-spacing”
Cubic : 1/d2 = (h2+k2+l2)/a2 or d2 = a2/(h2+k2+l2)
Tetragonal: 1/d2 = (h2+k2)/a2 + l2/c2
Orthorhombic: 1/d2 = h2/a2+k2/b2 + l2/c2
Hexagonal: 1/d2 = (4/3)(h2+hk+k2)/a2 + l2/c2
Monoclinic: 1/d2 = [(h/a )2 + (k/b )2sin2 + (l/c )2-
(2hl/ac)cos]/sin2
Triclinic:
7.1.5 Real crystals and Crystal defects:
Real crystals are only close approximations of space lattices
Edge dislocation
Screw Dislocation
• Formed by shear stress
• Also linear and along a
dislocation line
7.2 Symmetry in crystal structures.
7.2.1 Symmetry elements and symmetry
operations
Crystallographers make use of all the symmetry in a
crystal to minimize the number of independent
coordinates
a. Lattice symmetry
b. Point symmetry
c. Other translational symmetry elements: screw axes
and glide planes
a. Lattice symmetry --- translation operation
m
Tmnp=ma+nb+pc
Tmnp=
n
p
b. Point symmetry elements compatible with 3D translations
• Point symmetry operation does not alter at least one
point that it operates on: rotation axes, mirror planes,
rotation-inversion axes
Reflection Mirror Plane m
Rotation operation Rotation axis n = 1, 2, 3, 4, 6
Inversion Center of symmetry 1
Rotatory inversion Inversion axis 3, 4, 6
Translational symmetry of lattice prohibits the presence
of 5-fold axis!
Rotation axes, 1,2,3,4,6 only!! Why ???
ma
B1 B2
Limitation induced by
Translation symmetry!
a a a
A1 A2 A3 A4
Lattice points A1, A2, A3, A4 (m-1)/2 1
Through n-fold operation m-1 2
A1 B1 m= 3, 2, 1, 0, -1
A4 B2 cos =1, 1/2, 0, -1/2, -1
A1A4 // B1B2 = 0º, 60º, 90º, 120º, 180º
B1B2 =a +2acos = ma n= 1, 6, 4, 3, 2
cos = (m-1)/2 rotation axes, 1,2,3,4,6 only!!
The symmetry elements of a cube
Twofold axis
Threefold axis
Fourfold axis
2 3 4 6
Rotation axis
1 0 0 General equivalent positions:
(x,y,z); (-x, y, -z)
R(2) 0 1 0
0 0 1 2-fold axis // b axis
0 1 0
R(3) 1 1 0
0 0 1
general equivalent positions:
(x,y,z), (-y, x-y, z) (-x+y, -x, z)
3-fold axis // c axis
0 1 0 general equivalent positions: (x,y,z),
(-y, x, z), (-x,-y,z), (y,-x,z)
R(4) 1 0 0
0 0 1 4 fold axis // c axis
1 1 0 general equivalent positions: (x,y,z), (x-
y, x, z), (-y, x-y, z), (-x,-y,z), (y-x, -x, z),
R(6) 1 1 0 (y, y-x,z)
0 0 1 6 fold axis // c axis
c. Screw axes nm (m < n) and glide planes:
2 m
A two-fold screw 21 n C T (t );
1
m
1
n C R( ),
1
n T (t ) a
n n
21 // a axis
(x,y,z)(x, –y, -z)
(x+1/2,-y, -z)
Helical
structure
The direction of such an axis is usually along a unit cell edge, and the
translation must be a subintegral fraction of the unit translation in that direction.
Higher order screw axes
Screw 31 Screw 32
41-3, 61-5
Glide operations: An a glide
• a, b, c, n and d glides occur
• The a glide has translational component
of 1/2a
• n glide has translational component a/2
+b/2 or b/2+c/2 or …
• d glide has translational component of the
type a/4 + b/4 + c/4
• e glide (double glide plane).
Mirror: M
Glide operation: G = MT(t)
t= a/2, b/2, c/2, (a+b)/2, (b+c)/2, (a+c)/2, (a+b+c)/4 etc.
GG = [MT(t)]2 = T(2t) , t = 2t ( a basic vector of lattice)
Zig-zag structure
Summary of symmetry elements and
symmetry operations in crystal structure
Symm. operation | Symm. Element
• Rotation operation | Cn rotation axis
• Reflection operation | mirror plane
• Inversion operation | center of symmetry
• Rotation inversion operation | inversion axis
• Translation operation | lattice
• Screw operation | screw axis
• Glide operation | glide plane
(n=1, 2, 3, 4, 6)
Combinations of the 8 point symm. elements (5 n-axis,
i, m, S4) result in 32 crystallographic point groups.
Combining symmetry elements
When a crystal possesses more than one of the above
symmetry elements, these macroscopic symmetry elements
must all pass through a common point. There are 32
possible combinations of the above symmetry elements that
pass through a point and these are the 32 crystallographic
point groups.
7 Crystal systems
14 Bravais lattices
32 crystallographic point groups
230 space groups
7.2.2 Crystallographic point group and space group
1.Crystallographic point group
Combinations of the 8 point symm. elements (5 n-axis, i, m,
S4) result in 32 crystallographic point groups.
e.g., Monoclinic system: point symmetry element -- 2, m.
2 – {E, C2} -- C2 point group ; m -- {E,} --Cs point group.
2,m -- {E, C2, , i} -- C2h point group.
Two notations of crystallographic point group
schonflies notation vs. international notation
C2 2
Cs m
C2h 2/m
• 7 crystal systems.
• Each crystal system contains a set of
distinctive crystallographic point groups.
• A total of 32 crystallographic point groups, e.g.
Crystal Schonflies International Symmetry examples
system notation notation elements
monoclinic C2 2 C2 BiPO4
Cs m KNO2
C2h 2/m C2, h, i, KAlSi3O8
orthorhombic D2 222 3C2 HIO3
C2v mm2 C2, 2 NaNO2
D2h mmm 3C2, 3, i, Mg2SO4
2. Crystallographic space group
Point groups (32) + translational symmetries = Space groups (230)
Schonflies notation and International notation for space group
e.g, D2h16 - P21/n 21/m 21/a C2h5 – P21/c
system directions
1 2 3
Cubic a a+b+c a+b
hexagonal c a 2a+b
Tetragonal c a a+b
Trigonal a+b+c a-b -
Trigonal* c a
Orthorhombic a b c
monoclinic b - -
Example: monoclinic point group C2h-2/m
Six space groups belong to C2h point group, denoted:
C2h1-P2/m, C2h2-P21/m, C2h3-C2/m,
C2h4-P2/c, C2h5-P21/c, C2h6-C2/c,
Equivalent positions: e.g., C2h5 – P21/c
c glide
plane
at b/4.
A set of equivalent positions located within a unit cell!
General equivalent positions :
4 e 1 (x, y, z), (-x, y 1 , 1 z), (-x, y, z), (x,
2 2
1
2 y, 1 z)
2
e.g., C2h5 – P21/c
Special equivalent positions :
2 d 1 ( 1 ,0, 1 ), ( 1 , 1 ,0);
2 2 2 2 2 c 1 (0,0, 1 ), ( 1 ,0,0);
2 2
2 b 1 ( 1 ,0,0),( 1 , 1 , 1 );
2 2 2 2 2 a 1 (0,0,0),(0, 1 , 1 )
2 2
Inversion center
Diamond: face-centred cubic Oh7- Fd3m
41
d glide
plane
1/8,3/8,
5/8,8/7 Sideview topview
Structure motif – 2C
• Lattice points: (0,0,0)+, (1/2,1/2,0)+, (0,1/2,1/2)+, (1/2,0,1/2) +
7.2.3 The description and application of crystal structure
Example 1. Crystal of iodine
Crystal System orthorhombic
Space group D182h-Cmca (or C 2/m 2/c 21/a)
Cell parameters a=713.6 pm b= 468.6 pm c = 987.4 pm
Number of molecules per unit cell Z = 4
Atomic coordinate for I x y z
0 0.15434 0.11741
Lattice points within a unit cell: (0,0,0)+, (1/2, 1/2, 0)+ (C-center).
General equivalent positions:
(x,y,z); (-x, -y, -z); (-x, -y+1/2, z+1/2); (x, y+1/2, -z+1/2)
(0, .15434, .11741) (1/2, .65434, .11741)
(0, -.15434, -.11741) (1/2, .34566, -.11741)
(0, .34566, .61741) (1/2, .84566, .61741)
(0, .65434, 38259) (1/2, .15434, 38259)
a) Bond length (Bond distance)
r1-2= [(x1-x2)2a2+(y1-y2)2b2+(z1-z2)2c2]1/2 = 2.715 A
c) Density of crystal
V = a x b x c = 3.27 x 10 8 pm 3
D = 8 x 127.0 /( 6.02 x 10 23 x 327.0 x 10 –24 ) g cm-3 =5.16 g cm-3
7.3 X-ray diffraction of crystals
7.3.1 The source and property of X-ray
X-ray tube
the wavelengths of X-ray are in the range
of 100-0.01Å
• 1-0.01Å: hard x-ray
• 100~1Å:soft x-ray
• 2.5-0.5Å: used in crystal structure
analysis
• 1-0.05Å: used in medical perspective,
detection of materials wound
X-rays produced by electronic transition between
atomic energy levels
High energy A part of the
electrons are
electron beam
blocked; their
kinetic energies
M giving rise to
L L “white” x-ray.
radiation
As for Cu:
K Cu+ 1s12s22p6…
2S 1s22s22p5…
1/2
e
2P
3/2
K1=1.540594Å
2P K2=1.544422Å
1/2
e
IK1 2IK2
K1
K2
Notice: K2 can not be striped by the monochromator.
Synchrotron Radiation X ray Source
Benefits of Synchrotron radiation X-ray :
• Narrow range of x-ray wave-length– high
monochromicity
• High intensity of x-ray.
• High intensity and high quality of diffraction data
• High resolution – characterization microcrystals
Toooooooo Expensive facility!
SPring-8, at Osaka, Japan. www.spring8.or.jp
ESRF - European Synchrotron Radiation Facility , Polygone
Scientifique Louis Néel - 6, rue Jules Horowitz - 38000 Grenoble
- France , http://www.esrf.fr
The Advanced Photon Source (APS) at Argonne National
Laboratory, http://www.aps.anl.gov/aps.php
7.3.2 Laue equation and Bragg’s Law
1. Laue equations
Laue first mathematically
described diffraction from
crystals
• consider X-rays scattered
from every atom in every
unit cell in the crystal and
how they interfere with each
other
Max Von Laue
• to get a diffraction spot you
must have constructive
interference
Laue equation (Based on diffraction by 1D lattice)
Interference condition:
the difference in path lengths of
adjacent lattice points must be a
multiple integral of the wavelength.
AD-CB = h
AD = a·S = acos
CB = a·S0 = acos0
For each h value, the
a(cos-cos0) = h, h=0, 1, 2 …. diffraction rays from a 1D
lattice make a cone.
Where,
a— lattice parameter 0
0—angle between a and s0
— angle between a and s
Expanded to 3D lattice case
a·(S-S0) = a(cos-cos0) = h
b·(S-S0) = b(cos-cos0) = k
c·(S-S0) = c(cos-cos0) = l
This is the Laue Equation!
where,
a,b,c—lattice parameter
0,0,0—angle between a,b,c and s0
,, —angle between a,b,c and s
h,k,l — indices of diffraction, integers
which may not be prime to each other and are
different from Miller indices for crystal plane!
In the diffraction direction, the difference between the
incident and the diffracted beam through any two
lattice points must be an integral number of
wavelengths.
The vector from (000) to (mnp):
Tmnp = ma + nb +pc
The differences in wavelengths:
=Tmnp · (S-S0)
=(ma + nb +pc) ·(S-S0)
= ma ·(S-S0)+nb ·(S-S0)+pc ·(S-S0)
=mh+ nk+pl
=(mh+nk+pl)
2. The Bragg’s Law
Bragg discovered that you could consider the diffraction
arising from reflection from lattice planes
s0 s
O P
dhkl
Conditions to obtain constructive inferences,
a. the scattered x-ray must be coplanar with the
incident x-ray and the normal of the lattice plane.
b. S=S0
=AD+DB = 2d(hkl)sinn
s0 s
Condition for diffraction:
2d(hkl) sinn = n (n=1, 2, 3, … ) O
dhkl
A
n: the angle of reflection D
n: the order of the reflection B
2dnhnknlsinnh,nk,nl=(dnhnknl = dhkl/n)
However, the reflection order n is
not measurable!
Reformulated Bragg equations: reflection indices
2dhkl sin =
n=2
Virtual reflection plane
2d(hkl) sinn = n (n=1, 2, 3, … )
Lattice plane 2dhkl sin = (dnhnknl = dhkl/n)
indices
Diffraction indices or virtual reflection plane indices.
The Bragg equation defines the direction of diffraction
beams from a given set of lattice planes!
(100)
diffraction
crystal planes -
(100), (200), … (100) (200) (300)
Families of planes (200)
Lattice plane
directions-(100)
The Bragg Law vs. Laue equation:
•Both equations define the relationship between the direction of
diffraction beams, the x-ray wave-length and the parameters of
a crystal lattice.
•The Bragg law: simple, easier to derive lattice parameters from
the direction of diffraction beams.
2dhkl sin =
3. Reciprocal lattice --- Why we need it?
* b c * c a c * a b Basis vectors of a
a b reciprocal lattice
V V V
* * * * *
r ha kb lc r 1 / d hkl
102 112 A reciprocal lattice
101 point corresponds to
111 a diffraction (lattice)
100 110 plane of its original
a* 001 lattice!!!!!!!!!!!!
c* A reciprocal vector r*
b*
000 010 is perpendicular to a
r* lattice plane with the
1 22 indices (hkl).
1 01 1 11
1 00 1 10
4. Ewald sphere (reflection sphere) O1: origin of
crystal lattice
Radius = 1/
G O: origin of
reciprocal lattice
S r* G: a reciprocal
1/dhkl lattice point / a
2 diffraction point!
A S0 O1 1/ O
Only when the
reciprocal lattice
point is located on
the Ewald sphere
can constructive
OG 2 O1O * sin ( 2 ) sin 1 interference occur
d hkl (diffraction) !
2d hkl sin θ λ
Note: very few diffraction data can be
observed when a single crystal is fixed.
How to get more diffraction data?
• Rotate the crystal to enable more reciprocal points
(diffractions) dynamically located on the Ewald
sphere.
• While the crystal is fixed, use x-rays with varying
wavelengths (e.g., white x-ray). By doing so, the
Ewald sphere becomes filled.
The first technique is preferred and has been
widely used in practice!
7.3.3. The intensity of diffraction beam
1. The principle of X-ray scattering
To same your time,
Let’s neglect part 1 and
QR move directly to part 2!
r If you are interested in
s-s0 P s this part, just go
s0 O through it by yourself.
For elastic scattering, each electron scatters the plane wave
causing a spherical wave (exp[2i(kr)]).
The phase difference is: =(r•s - r•so)/λ
The scattered x-ray: exp{2i[r(s-s0)/]} or exp{2i[rq/]}
The contribution of the scattering of all electrons of a given atom:
(r) exp(2iq r / )d
3
r
Rn
For the crystal structure :
(r ) cell (r Rn )
b
n
c
A cell (r Rn ) exp(2iq r / )d 3 r a
n
A cell
( r ) exp(2iq r / )d 3r exp(2iq Rn / )
n
F ( q) exp(2iq Rn / )
n
F(q) --- structure factor
F ( q) cell ( r ) exp(2iq r / )d 3 r
Supposed that there are N1,N2,N3 periods along a,
b,c, and all the atoms locate on the position of lattice
points, F(q) can be replace with a constant ‘f’. f is
scattering factor of atoms.
N1 1 N 2 1N3 1
Amnp f e 2i / ( n1an2bn3c )q
n1 0 n2 0 n3 0
For the case of 1D and f=1,
2iN aq /
N 1
1 e
AN e 2inaq /
2iaq /
n 0 1 e
The intensity:
N
sin 2
a q
sin 2 Nh
I AN AN AN
2 *
sin 2 h
sin 2 a q
30 2
|A| (N=5) 250 |A|2(N=15)
200
20
150
100
10
50
0 h 0 h
-1.0 -0.6 -0.2 0.2 0.6 1.0 -1.0 -0.6 -0.2 0.2 0.6 1.0
In the case of 3-D:
N 1 2 N 2 2 N 3
sin
2
a q sin b q sin c q
I Amnp
2
f
2
sin 2 a q sin 2 b q sin 2 c q
Therefore,
aq/=h,bq/=k,cq/=l (h,k,l should be integer)
or aq=h,bq=k,cq=l
----- Laue conditions for X-ray diffraction
I f N N N
2
I Fhkl N N N
2 2 2 2 2 2 2
1 2 3 1 2 3
Only those scatterings fulfilling these conditions give
rise to measurable diffraction beams.
2. The intensity of diffraction beam
• The directions of the diffraction beams
Bragg Equation
2dhkl sin =
The directions of the diffraction beams are
determined by the cell parameters.
• The intensity of diffraction beam I K F 2
hkl hkl
Structure factor:
Fhkl ρ( x , y , z )e 2 πi ( hx ky lz )
dxdydz
Electron density distribution in a unit cell.
n
f je
2 πi ( hx j ky j lz j )
j 1 atomic coordinates: x,y,z
Sum over all atoms fj: atomic scattering factor defined by
within a unit cell. atomic electron density distribution.
• The intensity of the diffraction beams are determined by
types of atoms and the arrangement of atoms in the cell!
• By measuring the cell parameters and the intensities of
diffraction points, the atomic arrangement within a unit cell
can be derived.
3. systematic absence
Calculation of structure factor
Example A, Body center crystal
Simplified case: Each lattice point is a
metal atom.
n
Fhkl f j e
2i ( hx j ky j lz j )
j 1
1 1 1
2i ( h k l )
f1e 2i ( h 0 k 0l 0 ) f1 e 2 2 2
i ( h k l )
f1 (1 e )
While h+k+l =2n+1,
e πi ( h k l ) e( 2 n 1 )πi 1 Fhkl 0
systematic absence !
Body-center crystal –
A general case: each lattice point contains n atoms
• The total number of atoms within a unit cell is 2n;
• For jth atom in a structure motif (a lattice point): (xj,yj,zj)
• Its body-center equivalent point is: (0.5+xj, 0.5+yj, 0.5+zj)
2n
Fhkl f i e 2πi ( hxi kyi lzi )
i 1
n 1 1 1
2 πi [ h ( x j ) k ( y j )l ( z j )]
{ f j e
2 πi ( hx j ky j lz j )
fj e 2 2 2
}
j 1
n
f je
2 πi ( hx j ky j lz j )
[ 1 eπi( h k l ) ]
j 1
While h+k+l =2n+1,
System
πi ( h k l ) ( 2 n 1 ) πi
e e 1 Fhkl 0 absence
Example B. Unit cell has a 21 screw axis along the c axis at
x=y=0
Equivalent position (x,y,z) and ( -x , -y , z+1/2)
N /2
Fhkl f j {exp[i 2 (hx j ky j lz j )] (x,y,z)
Sum over j 1
all atoms of
a molecule. 1
exp[i 2 (hx j ky j l ( z j ))]}
2
N /2
F00l f
j 1
j exp( i 2πlz j )[( 1 exp( iπl )]
(x , y , z+1/2)
N /2
Note:
F00l 2 f j exp[i 2 lz j ] l = 2n •A structuremotif (lattice
j 1
point) consists of two
F00l 0 l = 2n+1 molecules.
•The two molecules are
correlated by the 21 screw
systematic absence
axis.
systematic absence
• Crystals of the same lattice type exhibit similar behavior
in system absence!
• Crystal structure which contain centering, glide plane
and screw axis will have systematic absences.
• Namely, some reflections/diffractions will be
systematically absent in case the lattice have centering,
glide plane and screw axis.
Please derive the conditions of system absence due to
3-,4-, 6-fold screw axes and d-glide plane by yourself!
systematic absence and sysmmetry
Types of Conditions for extinction Cause of extinction Centering and
reflection symmetry
elements
hkl h+k+l = odd In-centred (bodycentred) I
h+k = odd C-centred C
h+l = odd B-centred B
k+l = odd A-centred A
h,k,l not all even and not all Face-centred F
odd
-h+k+l not multiples of 3 R-centred R(hexagonal)
0kl k =odd Translation in b/2 b
l =odd (100) c/2 c
k+l =odd glide (b+c)/2 n
k+l not multiples of 4 Planes (b+c)/4 d
00l l =odd Translation c/2 21, 42, 63
l not multiples of 3 Along c/3 31, 32, 62, 64
l not multiples of 4 (001) c/4 41, 43
l not multiples of 6 Screw axis c/6 61, 65
7.3.4 Applications of X-ray diffraction
1. Methods
* Single crystal diffraction
Monochromatic camera method -- Monochromatic X-ray
Rotation, Oscillation, Weissenberg …
Laue photography --- white X-ray
Diffractometer -- Monochromatic X-ray
Crystal Diffraction beam
2
Incident beam
* Powder diffraction
Monochromatic X-ray Diffraction beam
powder
2
Incident beam 2
P
Diffraction beam
Incident beam 2
O
sample R
Powder Diffractometer
Radiation sources
X-ray tubes Monochromator – e.g.HOPG
Synchrotron radiation Filter – e.g. Ni for CuK
Detectors
•Film
- poor sensitivity, high background, low dynamic range
•Scintillation counters
- good sensitivity, low background, high dynamic range
•Imaging plates
- good sensitivity, low background, good dynamic range, very
efficient data collection
•CCDs and Multiwire detectors
- fast readout, good sensitivity, low background, good dynamic range,
very efficient data collection
Automated diffractometer method
2. The applications
a. crystal structure determination
Intensity data collection
Indexing Crystal system and
Cell parameters
I hkl K Fhkl
2
Phase problem
F (hkl) ( x, y, z )e 2i ( hx kylz ) dxdydz
( x, y , z ) V 1 F ( hkl)e 2i ( hx kylz )
h k l
Indexing of the cubic system:
a0
d hkl 2dhklsin=
h2 k 2 l 2
sin 2 ( / 2a) 2 (h 2 k 2 l 2 )
sin h k l
2 2 2 2 sin 2 θ1 : sin 2 θ2 : sin 2 θ3 : sin 2 θ4 :
Get the directions of the diffraction beams, i
Get the sin 2 θ1 : sin 2 θ2 : sin 2 θ3 : sin 2 θ4 :
Get the ( h 2 k 2 l 2 )1 : ( h 2 k 2 l 2 )2 : ( h 2 k 2 l 2 )3 ....
Get the lattice type (space group) and unit cell
parameters.
Indexing of the cubic system:
sin 2 ( / 2a) 2 (h 2 k 2 l 2 )
sin h k l
2 2 2 2 sin 2 θ1 : sin 2 θ2 : sin 2 θ3 : sin 2 θ4 :
Characteristic line sequence in cubic system:
P: (hkl) 100, 110, 111, 200, 210, 211, 220, 221, 222, 300, ….
Systematic absence
(h2+k2+l2 ) 1, 2, 3, 4, 5, 6, 8, 9, 10, 11, 12, 13, …
I: (hkl) 100, 110, 111, 200, 210, 211, 220, 221, 222, 300, ….
(h2+k2+l2 ) 2, 4, 6, 8, 10, 12, 14, 16 … (1: 2: 3: 4: 5: 6: 7: 8:…)
F: (hkl) 100, 110, 111, 200, 210, 211, 220, 221, 222, 300, ….
(h2+k2+l2 ) 3, 4, 8, 11, 12, 16, 19, 20 …
Observed diffractions: hkl all odd or all
Example for the indexing of cubic system and its applications
Sample: NaCl Condition: Cu K, =1.5418Å, R=50 mm
(1) Measure sample and relative intensity
(2) Calculate the position of diffraction lines (usually 2 in Ewald
sphere)
(3) Calculate
(4) Calculate sin2
(5) Calculate sin21: sin22 : sin23 : sin24 :…=3:4:8:11:…
(6) Identify Bravais lattice → face cubic
(7) Indexing and calculate h2+k2+l2, calculate dhkl and a.
FC: (hkl) 100, 110, 111, 200, 210, 211, 220, 221, 222, 300, ….
(h2+k2+l2 ) 3, 4, 8, 11, 12, 16, 19, 20 …
(7) Index and calculate h2+k2+l2
No. I 2 sin2 h2+k2+l2 hkl
1 W 27.46 13.73 0.05631 3 111
2 S 31.80 15.90 0.07508 4 200
3 S 45.60 22.80 0.15016 8 220
4 W 54.06 27.03 0.20647 11 311
5 S 57.50 28.75 0.22524 12 222
6 S 66.44 33.22 0.30032 16 400
7 W 73.30 36.65 0.35663 19 331
8 S 77.56 38.78 0.37540 20 420
9 S 84.30 42.15 0.45045 24 422
Measured in Ewald sphere Indexing
by x-ray diffraction
(8) Calculate lattice parameter
1.54182 Why use high angle
sin 2 θ ( h2 k 2 l 2 ) values?
4a 2
1.5418
a h2 k 2 l 2
2 sin θ
Least-square method, plot
method, high angle values,…
a=5.628 Å 0° 90
(9) = 2.165g/cm3 for NaCl °
ρV 2.165 ( 5.628 10 8 )3
n 4
M 23 35 .5
N0 6.022 10 23
One unit cell contains 4 NaCl
Example. Index cubic pattern and calculation lattice parameter
Line 2 sin2 sin2i h2+k2+l2 hkl
/sin21
1 40.26 20.13 0.1184 1 2 110
2 58.26 29.13 0.2370 2 4 200
3 73.20 36.60 0.3555 3 6 211
4 87.02 43.51 0.4740 4 8 220
5 100.64 50.32 0.5923 5 10 310
6 114.92 57.46 0.7109 6 12 222
7 131.16 65.58 0.8290 7 14 321
8 153.58 76.79 0.9470 8 16 400
If =1.5418 Å, body-centred cubic
1.5418
a h k l
2 2 2
42 02 02 3.16 Å
2 sin 2 sin 76.79
b. Applications of powder diffractions
Peak Positions Peak Intensities Peak Shapes and Widths
b. Applications of powder diffractions
Information contained in a Diffraction Pattern
Peak Positions
Crystal system, cell parameters, qualitative phase identification
Peak Intensities
Unit cell contents, quantitative phase fractions
Peak Shapes and Widths
Crystallite size, Non-uniform microstrain
(i) Peak Positions and
Intensities
Qualitative Analysis:
One crystal phase correspond to
a set of diffraction peaks.
( being different from the
spectroscopic analysis)
Phase analysis
Quantitative Analysis:
The peak intensities are
proportional to the weight
percentage of the corresponding
phase.
(ii) Changes of lattice parameters――Solid solution、
doping
Using high angle diffraction data or applying least square method.
Why use high angle
2dsin=n
values?
Maximal
minimal d/
0° 90
°
(ii) Changes of lattice spacing along specific
directions――residue stress
stress
d
d d d’
(iii) The width of diffraction peaks ―― Crystallite
size
30 2
|A| (N=5) 250 |A|2(N=15)
200
20
150
100
10
50
0 h 0 h
-1.0 -0.6 -0.2 0.2 0.6 1.0 -1.0 -0.6 -0.2 0.2 0.6 1.0
I Fhkl N N N Fhkl A
2 2 2 2 2 2
1 2 3
N1, N2, N3 periods along the lattice axes within a microcrystal
(iii) The width of diffraction peaks ―― Crystallite
size
Scherrer formula: (1nm to 100nm) Widely exploited in
research of nanoparticles!
K K
Dhkl
cos ( B B0 ) cos Why use small
angle values?
Dhkl average size along the direction perpendicular to (hkl) plane.
B measured peak width
B0 Instrumental width, using standard sample (e.g. -SiO2 with
crystallite size of 25-44m)
Instrumental width(B0) B0 (B)
[100]
[001]
XRD pattern of ZnO nanowires
(iii) The width of diffraction peaks ―― Lattice
Distortion
晶格的畸变(不均匀应变、微观应变、内应力)
d1 d4 d5 =d /d
d2 d3 2(d+d)sin(+)=
or 2d(1+)sin(+)=
d and are very small,
d1 d2
and hence ,
2=-2tg or
’= 2tg
Separation of the effects of Crystallite size and
Lattice Distortion
K
i '
2tg
D cos
i
cos sin K
2
D
Measuring two or more diffraction peaks.
(iv) The profile of diffraction peaks ―― Crystallite
size distribution
N
sin 2
a S Derived from
I AN
2
AN AN
* Bragg equation
2
sin a S
m
sin 2 ns
f p ( s ) K P ( n)
n 1 sin (s )
2
fp(s) is the line profile of diffraction peak
P(n) is Crystallite size distribution function
Instrumental(B0) Convolution
B0 (B)
h( s ) g (t ) f (s t )dt
or h( s) g ( s) f ( s)
F (h( s)) F ( g ( s)) F ( f ( s))
(vi) Texture (002)
30.0k
25.0k
20.0k
Intensity a.u.
15.0k
10.0k
5.0k
(103) (004)
0.0
30 40 50 60 70 80 90
2-Theta degree
ZnO nano-arrays
140.0k (201)
120.0k
100.0k
Intensity
80.0k
60.0k
40.0k
(002)
20.0k
0.0
30 40 50 60 70 80
2-Theta degree
(vii) Small angle scattering --- Particle size
b. Applications of powder diffractions
Applications
Qualitative Analysis
Quantitative Analysis
Lattice Parameter Determination
Crystallite size / size distribution & Lattice Distortion
Analysis (Non-uniform microstrain)
Crystallinity Analysis
Residue Stress Analysis
Texture analysis
Structure Solution and Refinement
Radical distribution function (for amorphous materials)
7.2.5 Electron Diffraction and Neutron Diffraction
1. Electron Diffraction
de Brogli wave length
of electron in a field V:
h
=
2meeV
100 kV ---- ~ 0.00370 nm
Atom-level resolution!
a) TEM image of the tip part of one TeO2 nanorod. (b)
Enlarged TEM image. (c) The corresponding electron
2. Neutron Diffraction diffraction pattern.
----- Scatterring of atomic nuclear
~ higher atomic resolution
7.4 Quasi-crystal, liquid crystal and amorphous
Quasi-crystal
Liquid crystal
Amorphous
Quasi-crystal
Crystal
There is no translation
symmetry.