The results of Section 4.3.2 demonstrate uncontrovertibly the
inert relationship between incommensurability and temperature
in Bi-2212. While the b axis has a steady linear response,
and the layer mismatch must therefore vary continuously with
temperature, the incommensurate value of the modulation
remains fixed. This demonstrates that the incommensurate state
cannot be considered in the context of a 'floating phase'. The
result is a very precise confirmation of that already suggested
by electron diffraction experiments, while the additional intensity
information provides a new insight. The interplay in behaviour
between the satellite and fundamental reflections indicates the
amplitude of the atomic modulation function to steadily decrease
with temperature with a concordant gain in the order of the
average structure. Although the reverse of what might naively
be expected to be the effect of increasing temperature, the
results make for a straightforward model of the modulation's
behaviour which is illustrated in Figure 4.14. With the
incommensurate value pinned at
0.21
, the real
space period of the modulation becomes solely dependent upon
the value of the b lattice parameter. The effect of increasing
temperature is to increase b and thereby to stretch the
modulation along that direction. The effect, as would be the case
for the stretching of any corrugated plane, is a flattening of the
corrugations, which is observed in the decreasing modulation
amplitude. It is interesting to note that the modulation does not
respond to the c axis, which is increasing at the same time
and might therefore be expected to stretch the modulation amplitude
along with it. This shows that the dominant parameter controlling
the behaviour of the modulation is the in-plane Cu-O bond length
which is also responsible for determining the b axis.
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Despite the common picture of incommensurate modulations, with
wavevectors which vary continuously or discreetly to some degree
with temperature, the phenomenon of systems with temperature
independent wavevectors is well documented [116].
Such phases exist in the 2H-TaSe
system, and also in
NbSe
for example. In the Landau free-energy description of
incommensurate phases, any change of the modulation amplitude
as a function of temperature should also lead to a change of
wavevector. Explanations for such temperature independent
behaviour have been established, however, by considering
the pinning of the wavevector to the underlying lattice.
The mechanism for pinning can arise by two specific means.
Pinning by impurities is one important mechanism, such
as in 1T-VSe
where poor stoichiometry plays an important
role. In cases where the coherence length of the modulation
is large, indicating impurity pinning to be of minor consequence,
then a further mechanism comes about through the properties
of strongly non-sinusoidal functions. The contribution to the
free energy of higher harmonics of a non-sinusoidal modulation
become highly significant in a way in which those of a purely
sinusoidal one do not, and the sum of such terms is able to
effectively pin higher-order commensurate modulations. Or,
to use the language of Chapter 2, these are described as
semi-commensurate modulations.
Such situations commonly arise in systems with competing
periodicities, called discommensurations, the phenomena is
described by the Devils Staircase approach [12].
In the case in question, both approaches could potentially
account for the temperature independent wavevector. The
wavevector value of 0.21
sits close enough to
the commensurate value of
(or
)
to potentially be
semicommensurate, and a theoretical model of the modulation
with discommensurate features has even been developed by
Walker [79]. The strength of the higher order
satellites, observable to third order in these experiments,
is evidence of a strong higher harmonic component. The
sawtooth modulation function proposed to describe the
oxygen occupancy of the BiO layer by Petricek
[86] is strongly deviated from the
sinusoidal modulation which describes the CuO
planes;
this is reflected to an extent in all of the other structural
refinements. However, the coherence of recognised
discommensurate modulations in the chalcogenides is typically
in excess of 4000
. By comparison, pinning due to a
heavily defected structure, possibly by poor stoichiometry
or dislocations, is one which might seem more readily
identifiable in Bi-2212.
The presence of dislocation networks in Bi-2212 has been
confirmed in electron microscopy studies by Lee [117] and
discussed in detail by Shang [118]. They were first
identified by Fung [119] who described them as
anti-phase boundaries. They involve extended boundaries in the
plane across which sites in the BiO layer are displaced
by a 1/2
1 1 0
. They effectively correspond to a dislocation
in the BiO ribbons and could therefore be a potential source of
pinning. The disappearance of the dislocations upon heating
between 400 and 460
C was suggested to be evidence of a
structural transition in this range by Yang [120], and
it is indeed in this temperature window that the changes in the
modulation wavevector have been observed. Another effect
claimed to occur in this region by Bidkin [92] is the
disappearance of the diffuse streaks. Unfortunately, the
data here is not conclusive due to the much stronger mosaic
scattering which obscures their measurement. The possibility
cannot be eliminated that the streaks merely reduce in intensity
in accord with the other reflections but to a level too low to
be detectable. If the disappearance of the streaks is authentic,
it would suggest that their origin relates in some way to the
dislocations, and that both changes are a consequence of
the increased mobility of the oxygen in the Bi
O
layers
at the initiation of the second oxygen diffusion process.
Their disappearance was described as being permanent by
Yang, however, while the streaks are observed to be at least
partially restored upon cooling in these measurements
(Bdikin [92] also described the transition as fully
reversible).
A further pinning mechanism, potentially the dominant one,
which could be realisable in Bi-2212 derives from the structural
model of Le Page. The model is one which has strongly
non-sinusoidal characteristics, involving a random sequence of
5
or 4.5
commensurate blocks which duplicate the
incommensurate period. Instead of a semicommensurate phase
pinned by discommensuration though, it is more reminiscent
of a chaotic phase where the interaction with the underlying
CuO
layers is so strong as to cause the modulation to
lock-on to the periodicity of these layers at random (the
situation was shown in Figure 2.1(c) of Chapter
2). A chaotic phase model would account for the dominance
of the Cu-O bond length, the temperature independence of the
wavevector, and the random sequencing of the proposed
commensurate blocks. If this picture is correct, then it would
indicate that a peculiarly strong inter-layer interaction is at
work in the Bi-systems. The absence of long range order in
the modulations of other compounds such as the Tl-systems,
might then be explained by a weaker inter-layer interaction in
these systems.
Above 300
C oxygen diffusion processes enact the dominant
influence upon the structure. The combined results of the two
experimental sections presented show there to be two quite
distinct oxygen diffusion processes at work, each exerting its
own particular authority. This has also been evidenced
in many experiments which have found the effects
of annealing upon other properties, such as T
, to be
very different above and below about 450
C
[121,122,113]. The first of the processes
commences close to 300
C and is observed in this experiment
as a growing inhomogeneity in the sample. The loss of oxygen
is also responsible for a permanent extension of approximately
0.4
in both b and c lattice parameters. Such an
extension in the c axis is the most commonly observed
feature to be associated with oxygen loss, and likewise a
comparable contraction upon oxygen absorption (see the review
of this in Section 5.2). The observations made by electron diffraction
methods of vacuum annealing in the vicinity of 300
C, supports
the assumption that the changes observed in this work are also due
to oxygen diffusion. The results here confirm that such diffusion
mechanisms have little or no influence upon the
period of the incommensurate modulation.
The second phase of oxygen diffusion commences above
400
C, and in this temperature range at least, appears to be
much slower than the first diffusion process. Its different nature
is also seen in the reversal of the c axis extension which was
effected in the first. The measurements over the prolonged period
of time at 450
C appear to be monitoring the controlled
decomposition of the sample, due to this slow but continuous
escape of oxygen from the structure. It is during this period that
changes in the modulation period are finally induced, close to
the amorphisation as has been reported in all previous studies
(although it is usually observed only fleetingly as a rapid transition
at much higher temperatures). The change involves the gradual
appearance of diffuse scattering, and eventually new satellites,
with
wavevector components
.
Although a diffuse distribution of scattering is found from
0.20
to 0.10
, very strong, well defined
reflections were found at
. This
corresponds to a new modulation wavelength of
, or
x4.7 the old wavelength. Assuming
this is the result of the reducing oxygen content, then it is
strong evidence to suggest a phase transition to a new oxygen
deficient state, intermediate on the route to decomposition.
It is noted, that the value observed here for this new period
is close to that also observed to appear, by many authors, in electron
diffraction studies of rare-earth doped
Bi-systems. For instance, Chen [123] has measured the
appearance of satellites at
in
when
exceeds 0.6, and Inoue [124] observed a
similar long period modulation in
.
The appearance of these new modulations are observed, as is also
the case here, as a phase separation, the new modulation coexisting
with the original modulation in the same sample. Changes
in the lattice parameters very like those presented here
in Figure 4.13 (i.e. contraction of the c axis
and expansion of the basal plane) are also commonly reported
to accompany the appearance of this new modulation period.
The important question which must be answered is to which
oxygen sites in the structure do these two separate diffusion
processes relate. The same conclusions of distinct diffusion
mechanisms at these temperatures have also been reached by other
means [111,125,112] (reviewed
in Section 5.2), but without any knowledge as to the structural
changes involved. The sequence of diffusion as a function of
temperature and time is determined by the activation energy
of the different oxygen sites; precise data does not exist for
this but a good indication [126] of how tightly
bound a particular oxygen will be is its bond length. Data on
oxygen bond lengths is available from the structural refinements
discussed in Chapter 3. In ascending order of expected activation
energy the oxygen sites would be: inter-ribbon and bridging,
rocksalt, apical, and the most tightly bound of all, Cu planar. It
can be surmised from this that the first diffusion process must
almost certainly be associated with any interchain oxygens or
with the bridging sites, and this is a frequent assertion of
many oxygen studies. The persistence of the modulation well
beyond this initial oxygen diffusion process is strong evidence
to conclude that the modulation remains stable and well
ordered even when the excess oxygen of the Bi
O
layers has been removed. This is just as would be expected
in the picture of the BiO layer being strongly pinned to the
potential of the CuO
layer, and would account for the
very similar descriptions of the modulation given by all the
structural refinements despite very different values being
determined for oxygen content; even one, for example, in which
the bridging positions were observed to be entirely vacated
[83].
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However, the much slower second process did produce a very
definite effect upon the modulation and it might be argued that
this could therefore correspond to the change in the bridging
oxygens. The change, though, involved the transition of the
incommensurate period to a preferred value of
,
and this value does not seem consistent with a change due to
the absence of the bridging positions alone. To illustrate this,
in Figure 4.15 the modulation periods have been
approximated to their nearest semicommensurate counterparts,
and the position of the bridging sites, repeating once for every
five unit cells, is indicated. If the modulation is considered to still
be pinned then it cannot adjust continuously to the changing
oxygen content, and the first discontinuous change in period which
is possible is then when every second bridging position has been
vacated and the modulation relaxes to a value of
or 0.10, which could after further oxygen removal be followed by
. But, in order to achieve a change to
the value which is observed in this experiment, of
, a change in the structure of the central
rocksalt sites of the Bi
O
layers is also required. A fact
which then suggests that the bridging positions have already been
vacated by the first diffusion process and that the second diffusion
corresponds to the rocksalt oxygen sites. This is a more dramatic
reorganisation of the structure and hence the transition is
coincident with an extension of the b axis and the collapse
of the c axis. This behaviour can also be accounted for
in this picture of oxygen removal by considering the bonding
between adjacent BiO layers. In the fully oxygenated structure
there is little bonding between adjacent layers, with the Bi
lone pair believed to be directed along the c axis forcing
the layers apart. However, under substantially reduced oxygen
conditions, the Bi could only maintain the favoured oxygen
coordination by forming bonds with oxygens in the adjacent
layer and directing the lone pair instead within the basal
plane and thus expanding the rocksalt region.
The above interpretation does run contrary to the assumptions
made in the high-temperature electron diffraction studies
discussed at the start of this chapter. In these it was asserted
that the deference of the satellites to the low temperature oxygen
diffusion indicated that the oxygen was not removed from the
BiO layers but rather from the perovskite block. From the wider
discussion of the modulations properties though, there appears
no compelling reason to assume that the structure does not
remain impervious to the removal of the bridging oxygens. This
then overcomes the apparently anomalous requirement that the
most tightly bound oxygen sites should be those which become
mobile at the lowest temperature. The ordering responsible
for the 2
x2
superstructure observed in electron diffraction
experiments must therefore be either the result of some additional
interaction between the electron beam and the oxygen of the
CuO
planes, although this is thought not to be the case,
or it is located elsewhere in the structure. The same
argument must also be applied to the twinning reported by
Yang [110] after vacuum annealing. Indeed,
they note themselves that the proposed CuO
twinning
model is of a previously unknown character for a perovskite
structure. It should also be pointed out that oxygen
vacancies, of the density suggested by the twinning
and the 2
x2
models within the CuO
planes
would surely be highly detrimental to the superconducting
properties. Whilst Gao [109] has observed these
features to be present in samples with close to optimum
values of T
.
In conclusion, the fundamental properties of the incommensurate
modulation of Bi-2212 have been investigated using x-ray
scattering to observe
in situ the response of the structure to high temperature
(over the range room temperature to 450
C). The
results have conclusively demonstrated the temperature independent
nature of the incommensurability, and several pinning mechanisms
which would offer explanations for this have been discussed. The
strong influence exerted by oxygen diffusion over the structure
has also been highlighted, and the results clearly indicate
the existence of two distinct oxygen diffusion processes, the
first being dominant over the temperature
range 300-400
C, and the second commencing above
400
C. However, it has also been found that the
wavevector of the modulation is in no way a continuous
function of oxygen content; a result contrary to the
assumptions which have previously been widespread
in the literature. Only after very prolonged
annealing at 450
C under vacuum was evidence for a
structural transition observed, which involved the appearance
of satellite reflections with a new wavevector of
. It is tentatively
suggested that this transition may relate to the formation
of a new oxygen-deficient structure, due to the removal of oxygen
from both the bridging and rocksalt sites of the Bi
O
layer.