The
sample chosen for this
study was the large Beijing crystal which had been previously
well characterised at room temperature, the results having
been presented in Chapter 3. Although of an intermediate
quality, it was chosen as it was not wished to inflict the
irreversible degradation, which could result from high
temperature annealing, upon a crystal of higher quality. The
Beijing sample also has the advantage of allowing the diffuse
scattering around the odd (0 0
) positions, something not
present in the high quality crystals, to be observed.
The alignment for the x-ray measurements was as described
in Chapter 3. Triple crystal geometry was utilised with
graphite monochromator and analyser crystals chosen to
make available the maximum possible x-ray intensity.
The sample was mounted on a ceramic disc using Ge ceramic
cement as the adhesive, and the disc was then screwed into
the copper block support of the high-temperature furnace. The
furnace is specially constructed for the x-ray diffractometer
to allow in situ measurements of this kind. A Lakeshore
temperature controller was used with a chromel-alumel thermocouple
attached to the ceramic mount to monitor temperature. The
temperature was found to be stable to at least
1
C
over the entire scale. The experiment was carried out with
the furnace under a permanent vacuum, which was maintained
in the region 4.0x10
to 1.0x10
bar throughout.
The experiment was performed in two essentially distinct stages,
and the presentation of the results will follow this accordingly.
The first stage involved observations at intervals from room
temperature up to 400
C, at which temperature the sample
was allowed to anneal for a period of 110 hours whilst more
detailed measurements were made. At the end of each stage, the
sample was returned to room temperature for comparison with
the previous set of measurements to allow the extent of any
irreversible changes to be established. The second stage involved the
heating of the sample to 450
C, at which temperature it was then
maintained for an extended period, to allow time evolving
processes induced solely by the vacuum annealing to be
observed. The lattice parameters were determined at frequent
intervals during each of the heating cycles and always before
a set of measurements. The results for this are presented in
their entirety, for the complete experiment, as a final section.