This lecture explains one of the most important conceptual bridges in structural biology:
π How diffraction spots (reciprocal space) relate to electron density inside the crystal (real space).
We start in reciprocal space.
It has:
|d^*| = rac{1}{d_}
where ( d_ ) is the distance between crystal planes with Miller indices (hkl).
When diffraction occurs:
So:
β A diffraction spot = one specific set of lattice planes contributing to scattering.
Now comes the key idea:
π If we take one reflection (one reciprocal point) and Fourier transform it back to real spaceβ¦
We get:
This wave has:
And crucially:
β The peaks lie exactly on the crystal planes that produced that reflection.
Example:
So one reflection creates one periodic density modulation in the unit cell.
There is also an opposite vector pointing to:
F_{-h -k -l}
These two reflections produce:
Thus:
π They cannot normally be distinguished in diffraction.
This is related to Friedelβs law.
Only special cases (like anomalous scattering) can break this symmetry.
The phase determines:
π Where the sinusoidal wave begins inside the unit cell.
Examples:
So:
β Phase shifts move the entire density pattern relative to the lattice.
This is extremely important later.
If a Miller index becomes negative:
Example:
This flips the orientation of the density modulation inside the unit cell.
This is the heart of crystallography.
Each reflection contributes:
[
ho(x,y,z) = sum ext{all electron density waves} ]
This process is called:
When all waves are summed:
Produces:
Produces:
When collecting diffraction data:
We measure:
β Intensities β give amplitudes
But we do NOT measure phases.
This is catastrophic because:
π Without phase information π We cannot correctly sum electron density waves π We cannot reconstruct the structure.
This is known as:
Solving it is a major part of structure determination methods such as:
As we include reflections with:
We obtain:
So:
β Resolution = ability to include high-frequency density waves
This lecture teaches the core pipeline:
More precisely: