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Lecture 5 – Crystal structure and diffraction

based on chapters 12–14, (up to and including 14.2) of the book
Exercises 12.3, 12.4, 13.3, 13.4, 14.2

Learning goals

After this lecture you will be able to:

  • Describe any crystal using crystallographic terminology, and interpret this terminology
  • Compute the volume filling fraction given a crystal structure
  • Determine the primitive, conventional, and Wigner-Seitz unit cells of a given lattice
  • Determine the Miller planes of a given lattice

Crystal classification

  • Lattice
    • periodic pattern of lattice points, which all have an identical view
    • lattice points are not necessarily the same as atom positions
    • there can be multiple atoms per lattice point
    • freedom of translation
    • multiple lattices with different point densities possible
  • Lattice vectors
    • from lattice point to lattice point
    • vectors for dimensions
    • multiple combinations possible
    • not all combinations provide full coverage
  • Unit cell
    • spanned by lattice vectors
    • has 4 corners in 2D, 8 corners in 3D
    • check if copying unit cell along lattice vectors gives full lattice
  • Primitive unit cell
    • smallest possible no identical points skipped
    • not always most practical choice
  • Basis
    • only now we care about the contents (i.e. atoms)
    • gives element and position of atoms
    • properly count partial atoms choose which belongs to unit cell
    • positions in terms of lattice vectors, not Cartesian coordinates!

Example: graphite

  1. Choose origin (can be atom, not necessary)
  2. Find other lattice points that are identical
  3. Choose lattice vectors, either primitive (red) or not primitive (blue)
    • lengths of lattice vectors and angle(s) between them fully define the crystal lattice
    • for graphite: = 0.246 nm = 2.46 Å, = 60
  4. Specify basis
    • using and : C, C
    • using and : C, C, C, C

An alternative type of unit cell is the Wigner-Seitz cell: the collection of all points that are closer to one specific lattice point than to any other lattice point. You form this cell by taking all the perpendicular bisectrices or lines connecting a lattice point to its neighboring lattice points.

Stacking of atoms

What determines what crystal structure a material adopts? To good approximation, atoms are solid incrompressible spheres that attract each other. How will these organize?

We start with the densest possible packing in 2D: Will the second layer go on sites A, B or C?

ABCABC stacking cubic close packed, also known as face centered cubic (fcc):

  • One atom on the center of each side-plane: 'a dice that always throws 1'
  • Conventional unit cell primitive unit cell
  • Cyclic ABC all atoms identical 1 atom per primitive unit cell
  • Conventional cell: atoms

Examples of fcc crystals: Al, Cu, Ni, Pb, Au and Ag.

Filling factor

Filling factor = # of atoms per cell volume of 1 atom / volume of cell

, where we have used that .

Compare this to body centered cubic (bcc), which consists of a cube with atoms on the corners and one atom in the center (Fig. 1.12): filling factor = 0.68. Examples of bcc crystals: Fe, Na, W, Nb.

Question: is 74% the largest possible filling factor? Kepler conjecture (1571 – 1630). Positive proof by Hales et al. in 2015!

Crystal structures that are related to fcc:

  1. ionic crystals (Fig. 1.13), e.g. NaCl
  2. zincblende (Fig. 1.15), e.g. diamond

ABABAB stacking hexagonally close-packed (hcp), e.g. Co, Zn. In this case there is no cubic symmetry (Fig. 1.11).

Miller planes

We start with a simple cubic lattice:

(lattice constant)

The plane designated by Miller indices intersects lattice vector at , at and at .

Miller index 0 means that the plane is parallel to that axis (intersection at ""). A bar above a Miller index means intersection at a negative coordinate.

If a crystal is symmetric under rotations, then , and are physically indistinguishable. This is indicated with . is a vector. In a cubic crystal, is perpendicular to proof in problem set.

Learning goals

After this lecture you will be able to:

  • Define the reciprocal space, and explain its relevance
  • Construct a reciprocal lattice from a given real space lattice
  • Compute the intensity of X-ray diffraction of a given crystal

Reciprocal lattice

For every real-space lattice

where , and are integers, there exists a reciprocal lattice

where , and are also integers.

(Note that in previous years we used the notation instead of .)

The two lattices are related as follows:

The above relation holds if

giving

which is clearly 1.

Example of a two-dimensional reciprocal lattice

Compose reciprocal lattice vectors. Directions:

Lengths:

,

Normalization is arbitrary in reciprocal space.

The reciprocal lattice vectors can be composed directly from their real-space counterparts:

Note that the denominator is the volume of the real-space unit cell. These definitions are cyclic, because .

The reciprocal lattice can also be described as a Fourier transform. We imagine the real-space lattice as a density function consisting of delta peaks, first in 1D:

We take the Fourier transform of this function to find:

This sum is non-zero only if , so when is in a recoprocal lattice point. Therefore, it can be rewritten as:

The above can be generalized to three dimensions:

Periodicity of the reciprocal lattice

Any wave in a crystal with wave vector can also be described with wave vector , where .

A primitive unit cell of the reciprocal lattice contains a set of unique vectors. Convention: 1st Brillouin zone. All vectors outside the 1st BZ have a copy inside the 1st BZ. So any wave process with arbitrary can be described inside the 1st BZ.

The 1st Brillouin zone = the Wigner Seitz cell of the reciprocal lattice.

Diffraction

We will now discuss how incoming waves incident onto a crystal can be scattered by the lattice. These waves can be x-rays, neutrons or electrons.

We assume that the incoming wave has wave vector and the scattered wave has wave vector . Furthermore, we assume only elastic scattering, meaning that . In this case, a scattering atom at position can be seen as a radiation sources emitting a wave . A complete atomic lattice will then emit a total wave amplitude:

We find that this sum will only yield a finite value if:

in other words, if the difference between the outgoing and incoming wave vectors coïncides with a reciprocal lattice point. We can then expect constructive interference due to the lattice points. This requirement is known as the Laue condition. Note that the total intensity measured by the detector goes like .

In the above we have assumed that at each lattice point there is one single atom. But what if there are multiple atoms per unit cell? In that case each atom acquires a phase shift of its own and the total amplitude becomes:

where is a phenomenological form factor that may be different for atoms of different elements. The second sum is called the structure factor:

The structure factor can cause destructive interference due to the contents of the unit cell, even though the Laue condition is met. Examples:

  • Simplest case: 1 atom at each lattice point, . In this case each reciprocal lattice point gives one interference peak, none of which is cancelled.
  • Example 2: conventional cell of the fcc lattice.

Basis contains 4 identical atoms:

Parameters , , are integers all terms are either or puzzle. Solution:

if , , are all even or all odd

in all other cases