Mosaic spread values for crystals grown in microgravity were measured using
synchrotron radiation. Full width at half maximum (FWHM) values for diffra
ction line profiles in the range 10-20 " (arc seconds, 1 " = 1 degrees/3600
) were observed. These values are similar to these measured for crystals gr
own on earth using the gel-acupuncture method. The crystals analysed are co
mposed of from two to five domains producing peaks having widths from 5 to
15 ". The distribution of these domains is neither homogeneous (with domain
s of lower quality concentrated in the centre of the crystal) nor isotropic
(producing peaks whose width changes depending on the observation directio
n). Methodological aspects are also discussed, with special consideration o
f the effects of mosaic spread on the data-collection procedures for high-r
esolution (low-intensity) reflections.