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CRYSTAL SYSTEMS AND CRYSTAL STRUCTURE DETERMINATION

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A parallelepiped is generated by the vectors. a , b and c. a. b. 4 ... Lattice points only at the corners of the parallelepiped. Lattice points at the corners ... – PowerPoint PPT presentation

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Title: CRYSTAL SYSTEMS AND CRYSTAL STRUCTURE DETERMINATION


1
CRYSTAL SYSTEMS AND CRYSTAL STRUCTURE
DETERMINATION
  • Shubha Gokhale
  • School of Sceinces
  • IGNOU
  • May 25, 2007

2
CRYSTAL
  • Crystal consists of 3-D periodic arrangement of
    atoms/ combination of atoms/molecules
  • Each repeating 3-D unit is the UNIT CELL of that
    crystal

3
3-D Unit Cell
4
Different lattice systems are created by
varying the lengths a, b and c and the angles
??, ? and ?.
  • To examine the point symmetry, we look for
  • rotation symmetry axes,
  • reflection planes and
  • inversion centre.

SEVEN systems for 3-D lattices.
5
1. TRICLINIC SYSTEM
All three sides different All three angles
different
a ? b ? c
? ? ? ? ?
Point symmetry Inversion
6
  • 2. MONOCLINIC SYSTEM
  • All three sides different,
  • Two right angles,
  • third arbitrary
  • Point symmetry
  • 180? rotation about one axis
  • Inversion.

a ? b ? c
a

? ? 90, ? ? 90
7
  • 3. ORTHORHOMBIC SYSTEM
  • All three sides different,
  • All three right angles
  • Point symmetry
  • 180? rotations about three
  • mutually perpendicular axes
  • 2. Inversion

a ? b ? c
? ? ? 90
8
4. CUBIC SYSTEM All three sides equal, All
three right angles
a b c
? ? ? 90
  • Point symmetry
  • 90? rotations about three axes,
  • 120? rotations about four cube diagonals
  • 180? rotations about six axes
  • Inversion.

9
5. TRIGONAL SYSTEM All three sides equal, All
three angles equal, of arbitrary value,
a b c
? ? ? ? 90
  • Point symmetry
  • 120? rotation about one axis
  • Inversion

10
6.TETRAGONAL SYSTEM Two sides equal, All
three right angles
a b ? c
? ? ? 90
Point symmetry 1. 90? rotation about two
axis, 2. 180? rotation about one axis, 3.
inversion.
11
7. HEXAGONAL SYSTEM Two sides equal, third
arbitrary, Two right angles, third angle 120?
a b ? c
? ? 90, ? 120
  • Point symmetry
  • 60 rotation about one axis
  • Inversion

12
Just like 2-D lattice, here also we can place
additional lattice points in each unit cell and
examine the translation and point symmetry of
the resulting lattice. A new translation
symmetry for the same point symmetry generates
a different type.
13
A complete analysis based on mathematics and
geometry has shown that a single lattice system
can have at the most FOUR types. In all the
seven lattice systems have a total of 14
types. These are called the BRAVAIS LATTICES.
14
P type
PRIMITIVE LATTICE
Lattice points only at the corners of the
parallelepiped.
BASE CENTRED LATTICE
C type
15
I type
BODY-CENTRED LATTICE
Lattice points at the corners of the
parallelopiped and at the centre of the each
unit cell.
FACE- CENTRED LATTICE
F type
Lattice points at the corners of the
parallelepiped and at the centre of each face of
the unit cell.
16
Cubic system has THREE types
cubic P
PRIMITIVE CUBIC LATTICE Lattice points only at
the corners of the cube. Translation symmetry
is
17
BODY-CENTRED CUBIC LATTICE Lattice points at the
corners and at the centre of each
cube. Translation symmetry is
cubic I
e.g. CsCl, Ammonia
18
cubic F
FACE- CENTRED CUBIC LATTICE (FCC) Lattice points
at the corners of the cube and at the centre
of each face of the cube Translation
symmetry
e.g. NaCl, KBr, MnO, Cu, CaF2
19
Cubic C type is NOT POSSIBLE
By placing additional lattice points at one
pair of opposite faces of a cubic unit cell the
system becomes TETRAGONAL.
20
  • Seven systems divide into 14 Bravais lattices
  • Triclinic P
  • Monoclinic P, C
  • Orthorhombic P, C, I, F
  • Trigonal P
  • Hexagonal P
  • Tetragonal P, I
  • Cubic P, I, F

21
Are all the materials around us crystalline?
22
  • Non-crystalline materials
  • amorphous
  • polycrystalline

23
amorphous
24
Polycrystalline
25
How to determine crystal structure?
Use diffraction technique
Similar to optical diffraction from a grating
Difference being the wavelength of the radiation
should be comparable with the inter-atomic
distances in the crystal!
X- rays, neutrons and electrons fit the bill!
26
X-RAY DIFFRACTION
27
Crystal Planes
Family of planes
28
Miller index
a1 intercept is 2 a2 intercept is 3 a3 intercept
is 3
Hence Miller indices are 3,2,2 and are depicted
by ( hkl ) (322)
Calculate reciprocal of these intercepts and
reduce them to smallest three integers having
same ratio.
29
Inter-planer Distance
(hkl) represent a family of planes. All parallel
crystal planes have the same Miller index. These
planes are equally spaced at distance dhkl . This
distance is defined as
30
Crystal planes in a cubic unit cell
(100) dhkl a
31
Crystal representation for X-Ray Diffraction
(XRD)
2-D depiction in layer forms
32
X-ray diffraction Braggs Law
Rays 1 and 2 interfere constructively if Total
Path Difference is integral multiple of the
wavelength, ?
Specular Reflection
O
Total p.d. AB BC
?OAB and ?OCB are equivalent. ?ABBCdhkl sin?
dhkl
Diffraction condition is 2 dhkl sin? n ?
33
We may see more than one family of planes at a
time in the diffraction pattern
dhkl different ? For same ?, different ?
34
Rotating Crystal method of XRD
Monochromatic x-rays
35
Powder Diffraction Method
  • Similar to Rotating Crystal method.
  • Monochromatic X-rays are used.
  • In order to expose various planes in the
  • crystal, rather than a rotating a single
    crystal,
  • a powder sample is use. This exposes
    various
  • crystal planes simultaneously to the
    X-rays.

36
Powder Diffraction Method
Many planes are equivalent (100), (010), (001)
or (110), (101), (011) or (211), (121),
(112) etc.
Monochromatic x-rays

Each of these sets have same dhkl and hence same
?. Hence diffracted rays form a cone.
37
Laue Method of XRD
  • Single crystal sample
  • The X- rays are polychromatic (multiple ?)
  • Though ? is same here, i.e. crystal is
    fixed,
  • due to different ?, different dhkl are
    diffracted
  • in different directions.
  • Crystal geometry can be found out but no
  • crystal parameters like lattice constants.

38
Comparison of XRD Methods
39
  • Analysing X-Ray Diffraction Pattern

40
Diffraction Cone
Incident beam
Reflected beam
2?
Crystal Plane
2?
Reflected beam
This cone results into arcs on the opened up
X-ray film.
41
Analysis of X-ray film
2? 0
2? 180
?1
?1
?1
?1
?2
?2
?3
?2
?2
?3
?3
?3
?R
d3
d3
d3
d3
d2
d2
d2
d2
d1
d1
d1
d1
D
4?3(rad) D / R
4?3(degree) 57.296 D / R
or
42
Calculating Lattice Constant
4? (degree) 57.296 D / R
If radius of the camera R 57.296 mm then, ?
(degree) D (mm) / 4
For first order diffraction, d can be calculated
by
However, (hkl) assignment is not possible here.
Hence
43
Lattice Constant Calculation Contd
? d 2hkl a 2 / N where N h 2 k 2
l 2
Possible values of N can be 1,2,3,4,5,6
44
Prepare a Table
sin2 ? / N
45
  • Thank you!
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