
or

A real 3-dimensional crystal contains many sets of planes. For diffraction, crystal must have the correct orientation with respect to the incoming beam.
Perfect, infinite crystal and perfectly collimated beam: diffraction condition must be satisfied ``exactly.''
Strains, defects, finite size effects, instrumental resolution: diffraction peaks are broadened.
More formally, the scattered intensity is proportional to the square of the Fourier transform of the charge density:

where
is the charge density.
For perfect crystals, I(q) consists of delta functions (perfectly sharp scattering). For imperfect crystals, the peaks are broadened. For liquids and glasses, it is a continuous, slowly varying function.
To achieve all of the above, will need lots of intensity in the primary beam together with sensitive detection systems.
Put a crystal in the beam, observe what reflections come out at what angles for what orientations of the crystal with what intensities.
In principle you can learn everything there is to know about the structure.
You may not have a single crystal. It is time-consuming and difficult to orient the crystal. If more than one phase is present, you will not necessarily realize that there is more than one set of reflections.
Samples consists of a collection of many small crystallites with random orientations. Average over crystal orientations and measure the scattered intensity as a function of outgoing angle.
Inversion of the measured intensities to find the structure is more difficult and less reliable.
It is usually much easier to prepare a powder sample. You are guaranteed to see all reflections. The best way to follow phase changes as a function of temperature, pressure, or some other variable.
Last updated December 30, 1996
Paul A. Heiney, heiney@dept.physics.upenn.edu