Brief introduction to Crystallography
Brief introduction to Crystallography
•• • • • • • • • • Crystallography Crystallography Structure Structure Symmetry Symmetry d-spacing d-spacing
Defines results one achieves with XRD, TEM, SEM, etc.
Crystalline vs. Amorphous Materials
Crystalline vs. Amorphous Materials
Crystalline
Crystalline mamaterial –terial – atatoms aroms are situae situated in ated in a periodic array over large distances.
periodic array over large distances. Amorphous
Crystalline vs. Amorphous Materials
Crystalline vs. Amorphous Materials
Crystalline
Crystalline mamaterial –terial – atatoms aroms are situae situated in ated in a periodic array over large distances.
periodic array over large distances. Amorphous
Amorphous (or(or non-crystallinenon-crystalline) ma) mateteriarial –l – whwhereree long range order is absent. Therefore no real
long range order is absent. Therefore no real symmetry.
•
• Close packClose packed dired directions are ections are cube edgescube edges..
SIMPLE CUBIC STRUCTURE (SCC)
SIMPLE CUBIC STRUCTURE (SCC)
•
• Coordination # = 8
Adapted from Fig. 3.2, Callister 6e.
(Courtesy P.M. Anderson)
• Close packed directions are cube diagonals.
--Note: All atoms are identical; the center atom is shaded differently only for ease of viewing.
• Close packed directions are face diagonals.
--Note: All atoms are identical; the face-centered atoms are shaded differently only for ease of viewing.
FACE CENTERED CUBIC STRUCTURE (FCC)
Adapted from Fig. 3.1(a),
• Coordination Number = 12 • Atomic packing factor
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• ABCABC... Stacking Sequence along cube diagonal • 2D Projection: A sites B sites C sites B B B B B B B C C C A A
A
B
C
FCC STACKING SEQUENCE
• Coordination #= 12• Coordination # = 12 • ABAB... Stacking Sequence
• Only difference from FCC is in the stacking (and the
orientation we generally consider when describing/drawing the stacking):
• 3D Projection • 2D Projection
A sites
B sites
A sites Bottom layer Middle layer Top layer
Adapted from Fig. 3.3, Callister 6e.
Lattices and Unit Cells
• What if we want to consider more complicated crystals? • Take advantage of symmetry and well known structures
– A “
identical surroundings (nearest neighbors, etc). – A
• strictly the unit cell is the smallest repeating cell (though this is
sometimes totally impractical and thus more convenient, but larger, unit cells are employed).
– A lattice does not define the crystal, only its symmetry.
– Atoms (or ions, molecules, etc.) will be placed at any number of lattice points . ONLY THEN do we have a crystal.
lattice” is a repeating array of special points in space that have
unit cell defines a repeating unit within the lattice
2-d Lattices
• A lattice repeats in all directions, and defines the symmetry.
• The unit cell is the simplest repeating structure.
Square unit cell
“Basis”
• BUT, a lattice only identifies repeating points and their symmetry.
– What’s the lattice for the wall or floor in the classroom?
• Must be combined with a “basis” to know where atoms are in the crystal
– What kind of bricks are hung at each lattice point? – Are there smaller stones patterned regularly in
between the bricks?
• Only by knowing a lattice AND a basis can a crystal structure (or anything else symmetric) truly be built.
2-d Lattice
• Anions at lattice positions (0,0) • Cations at (½,0) • Cations at (0,½) square Lattice: Basis: tetragonal
and Basi
• Lattice:
– A minimized pattern that will be followed • Basis:
– a) A vector that defines the position of hooks on
which something (atoms, molecules, bricks) will be hung with relation to the underlying pattern
(lattice)
– and b) What exactly will be hung on each hook (atom, molecule)
• Rules:
– At least one hook (basis) per lattice point
• (but can be more than 1)
– Basis vectors must put atoms within the unit cell (not in an adjacent cell)
– Each basis vector applies to every single lattice point
Seven Crystal Systems Cubic a=b=c ===90° Tetragonal a=b≠c ===90° Orthorhombic a≠ b≠c ===90° Hexagonal a=b≠c ==90° =120° Monoclinic a≠ b≠c ==90°≠ Triclinic a≠ b≠c ≠≠ Rhombohedral a=b=c ==≠90°
In 3 dimensions, there are only 7 basic crystal systems. Easily defined by: 3 edge lengths (a, b and c) and 3
interaxial angles ( and ).
This class
Cubic Bravais Lattices
/
Tetragonal a=b≠c
°
/
Orthorhombic Bravais Lattices / / / / / / b / / / /
Other Bravais Lattices
a=b°c
Defining Basis Positions Using
Fractional Co-ordinates
To locate atom positions in cubic unit cells we use rectangular x, y, and z axes.
The FCC Structure
Note: All atoms are not always shown because technically there are only 4/unit cell (for FCC)
Lattice=Face Centered Cubic Basis=red atoms at (0,0,0)
-of course it looks like there are more atoms, but these simply result from the repeating lattice and symmetry; ie they are not distinct
Each position might be provided, but probably the fewest number of positions will be given—the rest fill in as long as you know the Bravais lattice (ie the basic symmetry).
Simple unit cells
Based on Simple Cubic Lattice with a basis of: 1) anions at the SC points 2) cations at the center
[offset by (½, ½, ½)]
Based on FCC Lattice with a basis of: 1) anions at the FCC points
More common unit cells
Based on FCC Lattice with a basis of: 1) anions at the FCC points
2) cations at (¼,¼,¼)
Based on SC Lattice with a basis of: 1) Big cation at the SC points
2) Small cation at (½,½,½)
• Consider CaF2 : based on the CsCl structure.
• BUT: there are half as many Ca2+ as F- ions—how can
we accommodate this?
CsCl structure w/only half of cation sites occupied.
The initial ‘unit cell’ is no longer valid since every lattice site doesn’t have a basis attached to it (some are void). Instead, we use a ‘supercell.’ 2 possibilities here:
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A
mX
pSTRUCTURES
• Consider CaF2 : Based on the CsCl structure, BUT: there are half as many Ca2+ as F- ions
– This is accommodate with ‘empty cubes’.
– i.e. CsCl based structure w/only half of cation sites occupied.
• Thus, the proposed CsCl ‘unit cell’ is no longer valid since every Simple Cubic lattice site doesn’t have a basis attached to it (half are void!).
– Instead, use a ‘supercell.’
– Other
possibilities:
Crystallographic Directions and Planes
• Terminology
– Positions (,,,)
– Directions [] note no commas – Planes () note no commas – Families of directions <> note no
commas
– Families of planes {} note no commas
and NOT “one bar zero zero” 100)=“bar one zero zero”
Directions in Cubic Unit Cells
Position co-ordinates of vector OM = 1, 0.5, 0 (but these aren’t integers)
Position co-ordinates must be multiplied by 2 to obtain integers. Direction indices of OM = 2 (1, 0.5, 0) = [2, 1, 0]
A negative index direction (e.g. see vector ON) is written with a bar over the index
• For cubic crystals, the crystallographic direction indices are the vector components of the direction resolved along each of the co-ordinate axes (x,y,z)
[Directions]
• [100] • [110] • [111] • [021] • [011] • [200] • [210] x y z1. Draw cell + origin 2. Draw vector 3. “ reduce” to smallest integer values 4. [xyz] Group exercise
more [Directions]
• [100] • [011] • [011] x y zFor negative directions : a. Add more unit cells.
OR
Directions in Cubic Unit Cells
z y x z y x z y x z y x z y x z y x [00 1 ] [0 1 1 ] [1 1 1] [112 ] [2 1 2] [22 1 ]The origin may be shifted. Thus:
<Directions> =family of directions
• [100] • [010] • [001] • [100] • [010] • [001] x y zA <family of directions> includes all possible directions with the same basic coordinates.
(Planes)
• (xyz) • (100) • (110) • (111) • (100) • (020) • (040) • (04/ 30) • (½½½) x yz 1. Draw the origin, cell,
and normal vector. 2. Draw the plane at a distance from the origin of 1/sqrt(a2+b2+c2).
{Planes} =family of planes
• {xyz} • {100} • {110} • {111} • {100} x y z How many equivalent planes are therein each family (“multiplicity”)? multiplici ty 3 6 ? ?
For a simple cubic lattice and (0,0,0) basis:
• Along (xyz) plane • (100) • (110) x y z ± ±
Should be able to draw atoms in, and above/below, a given plane in a crystal.
For CsCl (simple cubic lattice, basis of Cl-(0,0,0) and Cs-(½½,½)) • Along (xyz) plane • (100) • (110) x y z ± ± ± ± ± Group exercise
Crystallographic Planes –
Miller Indices
Intercept; 1, ∞, ∞ Reciprocal; 1/1, 1/∞, 1/∞ Simplify; 1, 0, 0 Miller indices; (1 0 0) 1,1, ∞ 1/1,1/1,1/∞ 1,1,0 (1 1 0) 1,1,1 1/1, 1/1, 1/1 1,1,1 (1 1 1 )Crystallographic Planes – Miller
Indices
When planes are more complicated, follow these rules:
1. Choose a plane that does not pass through the origin at (0,0,0)
2. Determine the intercepts of the plane in terms of the x, y, and z axes of the cube. 1/3,2/3,1 3. Form the reciprocals of these
intercepts 3, 3/2, 1 4. Bring to smallest integers by
multiplying or dividing through by a common factor. 6, 3, 2 5. Enclose integers in parentheses