This lecture explains how X-rays are produced, how they scatter from protein crystals, and the core theory (Braggβs law, lattice planes, reciprocal space) behind protein crystallography.
To perform X-ray diffraction experiments, we first need an X-ray source.
Two types of X-ray radiation are generated:
X-rays interact with electrons inside the crystal and are scattered.
π Therefore crystallographers focus on elastic scattering only.
Typical crystallography experiment includes:
Only ~1β2% of X-rays are scattered β signals are very weak.
Crystals are flash-frozen to prevent damage.
Common cryoprotectants:
Crystals are tiny (loop size ~0.05β1 mm) and embedded in a thin cryosolution film.
Every point on a wavefront generates a secondary wave.
When waves from multiple scatterers meet:
π Diffraction pattern depends on distance between scatterers β structural information can be deduced.
Inside a crystal:
These planes are labeled using Miller indices (h, k, l):
Example:
Each reflection on the detector corresponds to a specific (hkl) plane.
Modern detectors:
Each diffraction spot:
Common experimental issues:
These can often be tolerated if not too strong.
Constructive interference occurs when:
nlambda = 2d sin heta
Where:
Key consequences:
Typical protein crystal resolutions:
Single molecule β scattering too weak.
Crystal lattice:
Diffraction gives:
But phases are missing.
Determining phases is essential to: β‘ reconstruct the electron density map β‘ build the protein structure.
This will be discussed later in the course.
Crystallography uses two coordinate systems:
Important relationships:
β X-rays are produced via electron acceleration β bremsstrahlung + characteristic lines β Elastic scattering from electrons gives diffraction spots β Crystals amplify weak molecular scattering β Diffraction depends on interference from lattice planes β Braggβs law links resolution β scattering angle β plane spacing β Miller indices label reflections β Reciprocal space is the natural framework for analyzing diffraction