
Fundamentals 
of 
diffraction 
angles, coordination polyhedra, etc. reasonable? If yes, move to step 
9. 
If 
no, go to step 
7 
using the next best solution. 
9. 
The model of the crystal structure is verified and completed by 
computing phases for all available (conventional) structure amplitudes 
using the current structural model (Eq. 2.105) and successive calculation 
of Fourier (Eq. 2.133) 
and/or difference Fourier maps (Eq. 2.135). Once 
all atoms are located, the complete structure is refined using least squares 
technique against all available diffraction data. 
10. If no solution is found, step 2 should be repeated with different 
parameters and 
lists(s) of reflections in the starting sets. It may be 
necessary to expand or reduce the list of reflections under consideration 
by changing the cut-off value of 
Emin 
from a standard value of 1.2. 
2.14.3 
Structure solution from powder diffraction data 
Solving the crystal structure using either heavy atom or direct techniques 
does not  always work  in  a  straightforward fashion  even  when  the  well- 
resolved  and  highly  accurate  diffraction  data  from  a  single  crystal  are 
available. The  complicating factor  in  powder  diffraction is borne by  the 
intrinsic overlap of multiple Bragg peaks. The latter may become especially 
severe when the unit cell volume and complexity of the structure increase. 
Thus, there is a fundamental difference between the accuracy of structure 
amplitudes obtained from single crystal and powder  diffraction data.  The 
former are always resolved, 
i.e. there is only one combination of indices, 
hkl, 
per  Bragg peak,  whereas  in  the  latter  some  reflections may  be  fully  or 
partially overlapped. The intensities of individual reflections 
hkl 
may still be 
recovered  from  powder  diffraction  data  but  their  accuracy  is  critically 
dependent on both the degree of the overlap and the quality of the pattern. 
Obviously, the absolute overlapping of some reflections makes it impossible 
to obtain the individual intensities regardless of the quality of data, and only 
the combined total intensity is known 
(e.g. reflections 431 and 051 in both the 
cubic and tetragonal crystal systems). 
As established above, individual intensities (or structure amplitudes) of 
Bragg reflections are needed in  order to  solve the  crystal structure using 
direct or Patterson methods. 
In 
the first case, accurate normalized structure 
amplitudes  are  required  to  generate  phase  angles  and  to  evaluate  their 
probabilities. In the second case, accurate structure amplitudes result in the 
higher accuracy and resolution on the Patterson map. 
Thus, when reflections overlap to a degree when the individual intensities 
can  no  longer be  considered reliable,  they  may be  dealt with using  two 
different approaches: