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Figure 1
The recommended data correction sequence for most types of samples. Output B for solids is the corrected data in absolute units, and for dispersions it is the dispersant (solvent) scattering in absolute units. Output C for dispersions is the sample scattering in absolute units. The azimuthal averaging step can be considered for isotropically scattering samples.

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 50| Part 6| December 2017| Pages 1800-1811
https://doi.org/10.1107/S1600576717015096
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