Isotropic approximation of the distribution of mis-orientation angles
specified in degrees of all the mosaic domain blocks in the crystal,
represented as a standard deviation. Here, a mosaic block is a set of
contiguous unit cells assumed to be perfectly aligned. Lower mosaicity
indicates better ordered crystals. See for example:
Nave, C. (1998). Acta Cryst. D54, 848-853.
Note that many software packages estimate the mosaic rotation distribution
differently and may combine several physical properties of the experiment
into a single mosaic term. This term will help fit the modeled spots
to the observed spots without necessarily being directly related to the
physics of the crystal itself.