
562  Chapter 
6 
specimen was prepared by  filling a  1 mm deep cavity of  a sample holder 
without  applying  any  pressure  (see  section  3.5)  to  minimize  preferred 
orientation effects. 
Regardless  of  all  precautions  in  the  sample  preparation,  the  pattern 
(Figure  6.26) contains two  distinct Bragg peaks,  which  are  substantially 
stronger than all others. The first peak at 
-9.4O 
(d 
= 
9.308 A) is shown at one 
fourth of its height, and the second at -19.1" 
(d 
= 
4.640 A) has intensity -4 
times  lower than  the first, yet it is -3  times higher  than  any other Bragg 
reflection. The intensities of the remaining Bragg reflections are below 10% 
of the strongest. The d-spacing ratio for the two  strongest peaks is 2.006, 
which clearly indicates that they belong to the same zone, for example, 001 
and 002 in the 001 zone. Combined with the markedly planar shape of the 
crystallites  (inset  in 
Figure  6.26),  these  features  strongly  suggest  the 
presence of a substantial preferred orientation, which may create problems in 
solving the structure and in refining structural and profile parameters. On the 
other hand, the  fact that the  two  strongest reflections belong to the  same 
zone  can  be  used  to  correct the  observed peak  positions  for  the  sample 
displacement  or  zero  shift  errors  during  the  ab initio  indexing,  as  was 
actually done in the original 
work.] 
Semi-manual  profile  fitting  was  conducted  using  WinCSD  (see  the 
footnote on page 515). The first 41 peaks in the range below 
20 
= 
39" were 
indexed using the IT0 program in a monoclinic unit cell 
(Mzo 
= 
37), 
which 
was the best  and the  only solution with all  peaks  indexed. The unit  cell 
refinement resulted in a 
= 
18.453 A, 
b 
= 
6.560 A, 
c 
= 
8.437 A, 
P 
= 
91.12O, 
and 
V 
= 
1021.1 A3. Analysis of the systematic absences results in h 
+ 
1 
= 
2n 
for h01 reflections and 1 
= 
2n for 001 reflections, which unambiguously points 
out to  P2Jn  (P2Jc  in  standard setting) as  the  only possible  space  group 
symmetry. Moreover, 
P2,Ic  is  one of  the  most  common groups observed 
among natural and man-made materials. 
Due to the complexity of the pattern, multiple overlaps (e.g, about 90 
Bragg reflections are possible in the range of the  first 40  observed peaks 
below 
20 
= 
40")  and the relatively broad peaks, the pattern decomposition 
was carried out using a semi-manual profile fitting. For each group of Bragg 
reflections,  located  within  the  manually  selected  ranges  of  the  powder 
This example can be used to illustrate an interesting approach that may be helpful in the 
indexing  from first  principles.  Assume that  two  patterns  were  collected  from the  same 
powder.  The first, using  a specimen  with  minimum or no preferred  orientation, and the 
second  with  artificially  induced  strong texture. Provided  the texture  axis coincides with 
one  of  the  principal  crystallographic  directions 
(e.g.  [OOl],  [OlO],  or  [OOl]),  the 
comparison  of two patterns may provide  critical information about the indices of certain 
peaks, whose intensity was affected (increased or reduced) the most. Once their indices are 
determined by analyzing the ratios between the corresponding d-spacings, the problem of 
finding the remaining lattice parameters is simplified by eliminating one unknown.