Experiment
-
Take diffractograms (10o to 90) of three forms of silica, SiO2:
- quartz sand
- a slice of flint, a very fine-grained from of quartzite
- fumed silica powder, a glassy form of silica
-
Take a diffractogram of an empty sample holder as a background reading.
Report
-
Subtract the background from all diffractograms. Take care to scale the background reading to
coincide with the baseline around the peaks in your diffractograms.
-
Use Scherrer's formula to derive the column length in different crystallographic orientations
and estimate an average particle size in the flint sample.
-
Determine the characteristic length scale of the major atomic pair correlation in the amorphous
sample by rescaling the diffractogram in terms of the momentum transfer, q.
- Is the apparent particle size dependent on crystal orientation? If so, why?
- Which pair correlation is the strongest contribution to the amorphous diffractogram? Does it relate to
any of the crystalline lattice spacings?