The presence of diffuse streaks, associated with, but distinct from the satellite reflections, was shown in Chapter 3 to be an intrinsic feature of the reciprocal space pattern of Bi-2212. Their origin, however, was not clear. The x-ray scattering results presented in this chapter have revealed new information about the nature of these streaks and, most importantly, have shown them to be strongly affected by certain annealing treatments. This observation in combination with the compositional analysis of the crystals makes possible some definite judgements about the origin of the diffuse streaks.
As was made clear in Chapter 3, their diffuse character indicates
them to be associated with some structural feature which must
be closely linked to the modulation within the basal a-b
plane and which disrupts its body-centred symmetry, but which
is poorly correlated between layers along the c axis. The
transformation observed in the streaks of the B1 sample indicates
that the annealing treatment has brought about an ordering of this
structural feature along the c axis which results in an
even more distinct violation of the symmetry. The annealing
treatment of the A1 sample, however, brought about little or no
change in the streaks. The compositional analysis identifies
the primary differences between the A and B samples to be the low
Sr, and slightly higher Bi content of the B samples, along with
a greater oxygen content. An annealing induced ordering of either
cation substitutions (possibly Bi on Sr sites) which are not
present in the A1 sample, or an ordering related to the additional
oxygen content of the B1 sample could therefore be potentially
responsible for the observed changes. It is notable, however, that
the Oxford crystal, which has a similar Bi stoichiometry to that
of B1, has a diffuse streak closer instead to that of the A1
crystal in intensity and shape, and also that both the A1 and
Oxford crystals have similar oxygen contents and T
values.
This suggests that the larger oxygen content of the B1 crystal
is the more significant parameter.
In as-grown crystals a large excess of oxygen will most
reasonably be incorporated in a highly disordered manner;
this is evidenced in STM images of oxygen rich BiO layers
for instance [148]. If oxygen is indeed at the
root of the streaks, this lack of coherence in the oxygen
arrangement would explain the very flattened shape of the
diffuse streak observed in the B1 sample before annealing.
Upon annealing, the subsequent ordering may be dependent
upon the extent to which oxygen content has also changed.
The ordering could involve either the excess oxygen atoms
themselves or vacancies created after oxygen loss. The
brief ten minute annealing treatment of the B1 sample is,
on the basis of the results of the many other annealing
experiments discussed at the start of this chapter, too
short a time to have resulted in a substantial change in
the bulk oxygen content of the sample, particularly
considering the sample's large dimensions. The effect of
this brief annealing may then be rather to facilitate
the establishment of a more ordered oxygen distribution,
or to allow a slight oxygen loss which then facilitates
the ordering of the remaining excess of oxygen. Perhaps
this latter explanation is the most reasonable picture. A further
potential experiment would be to investigate the effect
of annealing at some lower temperature where oxygen loss
will be more definitely curtailed. Low-temperature
annealing of Y-123, for instance, has been found necessary
to achieve the most ordered oxygen states [154].
The post-anneal quenching may also have been a factor in
achieving the ordered state, and the effect of slow-cooling
could also be investigated. The behaviour of the A1 sample
in this picture is understandable if the oxygen annealing
leads to oxygen incorporation at other vacant sites, and
not to the additional oxygen positions responsible for the
streaks. This is sensible because sample A1 starts from a
much lower oxygen content, and even after the annealing the
change in T
indicates it's oxygen content remains
lower than B1.
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A schematic representation of the modulated structure in the
[1 0 0] direction in Figure 5.10 illustrates how
a violation of the body-centred ordering of the modulation,
necessary to be consistent with the streaks, may be brought
about (the large circles in the figure). The locations also
correspond to areas of greatest separation between neighbouring
Bi-O planes, and they would therefore be favourable locations
for the incorporation of additional oxygen. The effect of the
annealing is to allow the oxygen to migrate to this more
favoured position, no c axis interaction is required
between the oxygen to achieve the increased correlation,
the guiding potential is provided by the modulation, and
they merely align themselves within this. The readjustments
of the local structure which may then result could include
a closer bonding of the adjacent BiO
layers due to the
linking oxygen, and would reduce the amplitude of the
modulated displacements along the c axis. This effect
would account for the reduction in satellite
intensity observed to accompany the ordering
of the streaks. If this ordering and associated
change in the amplitude of the modulation are anything
other than coincidental with the increase in T
, which
also resulted from the annealing, then it could be effected
through a change in the tilt of the CuO
octahedra.
The tilt angle is known to be an important quantity in
determining superconducting properties [155],
and would certainly alter along with the modulation. The
flattening of the corrugation of the CuO
layers could
also be a factor, and it is interesting to note that a
change in the
axis was also observed to accompany
this, in agreement with the model proposed at the close of
Chapter 4. If there was indeed little change in oxygen
content, the suggested model of ordering could explain the
observed increase in T
of around 3K by these means.
The ordering may also bring about an increase in the
inter-layer coupling. The c axis resistivity
in Bi-2212 is believed sensitive to the coupling and is known
to be highly dependent upon annealing treatment and to vary
considerably between samples. An ordering of the sort
suggested here could explain the relief of interlayer
distortion previously suggested by Yoo [133]
to explain the change in
due to annealing.
The suggestion that structural change induced by annealing
has been responsible for influencing superconductivity and
T
has been made by other experiments when it was
believed that no suitable change in oxygen content to
effect the carrier concentration could have occurred.
Two already mentioned in the review [141,111]
could perhaps be attributed to underestimates in the degree of
oxygen evolution. A result which is harder to explain in this
way is that obtained by Wu [113] who found that the
T
of single crystals could be raised to around 86K by
annealing at 550
C but that the change was independent
of both annealing period and, most striking of all, the
atmosphere (be it oxygen or nitrogen); it was therefore
concluded only a structural modification, and not changing
oxygen content could be responsible. It has similarly
been found in previous annealing studies of the Warwick
samples of the B type used here, that it is difficult to
effect T
any further than the initial rise to 86K,
even with greatly extended periods of annealing.
Evidence of a different kind comes from Mossbauer
studies of Fe doped Bi-2212 by Lin [156]. The
technique probes the local structure of the Fe atoms
substituted onto the Cu sites and is sensitive to the
distortions of the CuO
layer by the modulation.
Vacuum annealing was found to induce changes in these
local distortions, and this was in association
with the rise of T
to its maximum value. It is
always a problem to disentangle the individual effect
of structure from that of carrier concentration upon
the superconductivity, and very rarely are transport
measurements combined with an explicit study of the
affects upon the structure. But these interpretations
are in agreement with the results presented here.
The speculation needs now to be confirmed by careful
measurement of oxygen content both before and after
the annealing, and perhaps in combination with Hall
measurements, to allow a definite conclusion to be made.
The model proposed here cannot be conclusively established by the data available, but it does appear the most viable picture compatible with the current information. Alternative structural modifications can be imagined which might be responsible, such as excess oxygen incorporation into the Ca layer perhaps, or the ordering of cation substitutions in the Ca or Sr layers. However, these alternative models must also be able to account for the associated changes of the modulation amplitude, and it is not so easy to visualise how the ordering of interstitial oxygen in the Ca layer for instance, would be so closely tied to the modulation period. Further studies are clearly warranted.