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![[Figure 4]](gm5061fig4mag.jpg)
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Figure 4
(a) Mosaicity and (b) Wilson B factor, determined using data acquired 3–5 s after cooling, versus temperature and glycerol concentration for ice-free cubic apoferritin crystals. Mosaicities have a `floor' determined by the incident X-ray beam divergence of ∼0.03°. Actual room-temperature crystal mosaicities are likely to be ∼0.01° or less. The significant scatter in values arises from crystal-size-related variations in illuminated volume and background scatter. Adapted from Supplementary Fig. S11 in the supporting information to Moreau et al. (2019  ). |
![[Figure 4]](gm5061fig4.jpg)
 | STRUCTURAL BIOLOGY |
ISSN: 2059-7983
