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.