view article
Figure 9
Result of the new analysis method when applied to the minus-first-order satellite peaks in the φ = 270° profiles shown in Fig. 7. (a) Three different hkl profiles obtained after rescaling of the horizontal axis by cosθc. Each peak position is shifted to the origin. In other words, Δθ = θ − θ(reference peak) and θ(minus-first-order satellite peak) is adopted as the θ(reference peak). (b) The three profiles in (a) replotted by adjusting their peak intensity tops to that of 004 in order to examine more accurately whether the three profiles are the same or not. The background level for each hkl profile is also indicated in (a) and (b). Only the signals above the background levels are significant for the comparison.

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 34| Part 1| February 2001| Page 87
https://doi.org/10.1107/S0021889800020203
Follow J. Appl. Cryst.
Sign up for e-alerts
E-alerts
Follow J. Appl. Cryst. on Twitter
Twitter
Follow us on facebook
Facebook
Sign up for RSS feeds
RSS