
Using the atomic form of
as
a starting function, the intensity
is compared to the data to extract a first guess for
for each reflection. A new
is then obtained using the Kramers-Krönig relation. This
procedure is iterated [6] until
a stable
is found for each reflection.
Each resonant crystallographic site contributes to the diffraction
intensity differently at each reflection due to the exp(i Q.R)
term, thus linear combinations of the
from
different reflections are made to isolate contributions from the
different sites.
Last modified: Wed Feb 18 15:56:11 EST 1998