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Some diffusive properties of oxygen in Y-Ba-Cu-O systems
D. Djurek, V. Manojlović, Z. Medunić, M. Prester, E. Babić, K. Zadro
To cite this version:
D. Djurek, V. Manojlović, Z. Medunić, M. Prester, E. Babić, et al.. Some diffusive properties of oxygen in Y-Ba-Cu-O systems. Journal de Physique I, EDP Sciences, 1992, 2 (1), pp.63-67.
�10.1051/jp1:1992123�. �jpa-00246463�
Classification
Physics
Abstracts74.30C 74.70V 74.705 74.70Y
Some diffusive properties of oxygen in Y-Ba-Cu-O systems
D.
Djurek (~),
V.Manojlov16 (~),
Z. Medun16(1),
M.Prester(2),
E.Bab16(3)
andK.Zadro(3)
(1) Volta
Applied
Ceramics, 41000Zagreb,
Croatia,Yugoslavia
(2) Institute of
Physics
of tile University ofZagreb,
41000Zagreb,
Croatia,Yugoslavia
(3)Department
ofPhysics, Faculty
of Natural Sciences, 41000 Zagreb, Croatia,Yugoslavia
(Received 21
August
1991,accepted
4 October I991)Abstract. We have studied tile diffusive
properties
of oxygen in Y-Ba-Cu-O systems at 940 °Cby measurements of tile resistive response time r of the
samples subjected
to tilestep-lflce
increaseof tile oxygen pressure
Apo~~
I to 5 bars. Thesuperconducting
(SC) transition widtlis AT~plotted
versus inverse diffusion constant D robey
the universal lineardependence.
Thecharacteristic
protruded
tail of the real part of ACsusceptibility
which exhibits the feature at 86 K is absent insamples
with the nominalcomposition
Y~Ba~CU~O~(Y-336)
in theregime
r < 3 s as result of
weakly
connectedgrains
of YBa~CU~O~ s (Y-123) nucleated fromdecomposed
Y-336
phase.
Introduction.
The oxide
superconductor YBa~CU~O~
~
(Y-123)
is still thesubject
of an intensiveresearch,
because ofcomparatively simple preparation procedure
and attractive extension of conventio- nal ceramicproperties
tosuperconductivity.
There is less evidence in scientific literature on the correlations ofphysical properties
recorded at 900-940 °C and SC data observed below 90 K. Thecommonly accepted
result thatO~
favours the SCproperties
in Y-Ba-Cu-Osystems
is less evidentby
in siturecording
of oxygen diffusionduring
theannealing
athigh
temperatures
anddiffusivity
data don't form a coherentpicture
in detail with considerable differencesexisting
from group to group[I].
While
therrnogravimetric (TGA) analysis
offers aninsight
in the amount ofcaptured
orreleased oxygen in the
sample
the diffusiveproperties
of oxygen are less accessibleby
TGA.Recently
we have introduced[2]
the measurements of the electrical resistance(R)
ofsamples during
the heat treatment andreported
the close correlation of R with the mass of absorbed or released02
in Y-123. The timedependence
of R may elucidate the mechanism of the diffusion of02
and/or O. In this paper wereport
the results of the measurements of theresistive response in the
samples subjected
to astep
like increase ofO~
pressureApo~ (
~0.5 s for 90 9b of
Apo )
atsintering temperature (~
940°C)
aftersintering procedure
(~
12h)
has been finished. An increaseApo~
from I to 5 bars results in the decrease of R from64 JOURNAL DE PHYSIQUE I N° I
Ro
in time and this decrease can be fitted to anexponential dependence
3R=
(Ro R~)
exp(- t/r).
Thetemporal
andspatial dependence
of oxygen concentration(n)
in thinsample
of the area S is
governed by
the diffusionequation
3n/3t= D
3~n/3x~
withdiffusivity
D related to(r
= S/D
).
The diffusive
properties
of oxygen in Y-Ba-Cu-O can be considered in two respects.Firstly, intragrain
diffusion ismainly govemed by
oxygen-oxygenrepulsion
energy E~ 0,16 eV[3]
which contributes to diffusion times
r
10~?
s
[4] according
toexpression
r= To exp
E/kT
with To 8 x10~ ~~s
[5].
Otherwise the activation energyE~
whichcorresponds
to the site oxygen removed from thegrain
boundaries(GB)
to the interior isE~
2 2.5 eV[6]
withcorresponding
diffusion times r~ lo s.
In
fact,
diffusion rate 3n/3t of the oxygen in Y-123 is related to the strain rate3e/3t since strain fluctuations 3e are
suppressed by removing
of variations 3n ofconcentration no
according
toNabarro-Herring expression 3n/no
= wo 3 e/kT. wo is the lattice
site volume wo ll
i~
forunoccupied
vacancy or the volume 4wrj3
for oxygenoccupied
vacancy site. ro stands for the effective distance of
long-range
elastic interaction and exceeds at least 20 atomic coordination shells[7].
Experiment.
Y-Ba-Cu-O
samples
wereprepared
frompowders Y~O~,
CUO andBaCO~
mixed in an agatmortar and fused at 940 °C for 24
h, usually
in two heatcycles,
in order tocomplete
the solidstate reaction. After
cooling
to roomtemperature (RT)
the fusedcompound
wasreground
and
subsequently compacted
inpellets (S
= 0.2-0.4
calf,
200 ~ inthickness).
Thesintering
was
performed
at 940 °C in air after which the resistive response toApo~
=5 bars was recorded.
By cooling
to RT weadditionally
annealed thesamples
at 430 °C for 12 h in theflowing O~ (~
l bar in order to remove the variations ofO~
concentration among differentsamples
as a result ofirreproducibility
of the fumacecooling
rate.The
powders
of Y-123 werecompacted
with different pressures in order toprovide
the different time constants at 940 °C. Therespective compaction
pressures at RT forsamples
a, b and c with resistive SC transitions shown infigure
I were 0.8GPa,
3. I GPa and 8.2 GPa. Theheating
up to 940 °C andannealing
for 12 h resulted in three different values of diffusionconstants D as it is shown in
figure
2.The fusion of Y-336 differs in some
respects
from Y-123.Iqbal
and coworkers[8] reported
that
single phase Y-336,
aspreviously reported by
Raveau and coworkers[9]
can't be obtained as a stable oneby
the solid state reaction and authorssuggested sol-gel
method aspreparation procedure
forobtaining
stable Y-336.We fired the
powder
mixture of nominalcomposition Y~Ba~CU~O~
at 880 °C for 20 h and X- raydiffractograms
taken onsamples quenched
to RT from 880 °Cby simple pulling
from thefumace reveal the presence of Y-336
phase
characterizedby hki
= lll
(20
=24°)
diffraction. The
reground
andcompaction
withsubsequent sintering
for 12 h at 940 °C in air revealed acomparatively
small time constants(r
=
2-4
s)
recorded at 940 °C andcooling
to 430 °C withsubsequent annealing
at this temperature in I bar offlowing O~
confirmed thepresence of
Y-123, Y2BaCu05 (insulating phase)
and CUO. To the lowestr =2s
corresponds comparatively
narrow resistive transition widthAT~
= 0.4 K(inset
ofFig. 3).
In addition to low resistiveAT~
thediamagnetic
transition in Y-336 isqualitatively
different from that in Y-123(Fig. 3).
The transition is smooth with an absence of theprotruded
tail andnearly
80 fb of transitions is finished in 1.5 K.-The
samples
of mixedphase Yi_~Bao_~CUO~ a',
b' and c' wereprepared by application
of differentcompaction
pressures to thepowders
withrespective
values I.4GPa,
2.2 GPa andmiic m
~: ~~'~
~~~ ~ $(, 6
~~
...'""
b
~
~~
f~ b
;;:.'"
,.
;.. $
..""
T b
«
~
~
~
i ° plGPaJ
) Y-336
10 ~iis«ctm21 3.102
Fig.
2.goK go
Fig.
I.Fig,
I. Resistive transitions to SC state insamples
Y-123subjected
to three differentcompaction
pressures : a ~p = 0.8 GPa), b ~p = 3. I
GPa),
c ~p = 8.2 GPa).Fig.
2. SC transition width AT~plotted
versus inverse diffusion constant D ~' The inset shows thedependence
of AT~ in Y-123 oncompaction
pressure as referred infigure
I.1'". 0
a2 .'
ohm f
." z
01 j
0 ""100
TjK 200 ~~
;""~~~
T£/(~!~li":"::.".":"?"',()~~~
3,,,, .;..~. .~~" '~.
T/K
Fig.
3.-Diamagnetic
transition in Y-336decomposed
in real part Xm andimaginary
partX,m. The inset shows the resistive transition in Y-336 to SC state.
3.8 GPa, The
corresponding
D and transition widths areplotted
infigure
2.Similarly
as in the case of Y-123AT~
and D~ areincreasing
functions ofapplied
pressure.Discussion.
An increase of r with
applied
uniaxial pressure in Y-123 for p~ lo kbars may be
explained by
appearance of dislocation creep
commonly
introducedby
twins on twin-twin andtwin-grain boundary
intersections. Animportance
of twins as apossible
dislocation source in Y-123 wasstressed
recently [10].
While at
high temperatures (T~
0.5T~
;T~
ismelting temperature
ofY-123)
dud low normalized stress«/J~ (~
is shearmodulus)
the dislocation strain ratek~ig~
is dominatedby
lattice diffusion
k~tg~
~(«/~)~ [l I] (n
is aninteger)
at lowtemperatures (T~
0.3T~)
dudhigh
stresses(«/~ ~10~~)
the dislocation strain is smaller and varies ask~tg~ («/~ )~+~
66 JOURNAL DE PHYSIQUE I N°
An
application
of stress at T~ 0.3
T~
locks theintergrain viscosity (Cottrell
type oflock)
upto
sintering temperatures
withcorresponding suppression
of oxygendiffusivity.
The
comparatively high diffusivity
of oxygen indecomposed
Y-336 sounds for the minorimportance
of strains locked ongrain
boundariesduring
the nucleation of Y-123phase by heating
from 880 °C to 940 °C and formation ofloosely
connectedgrains
in the matrix ofinsulating phase Y~BaCUOS.
Thisimplies
aqualitatively
different situation from that in mixedphase Yi,~Bao_~CUO~
where Y-123phase
is formedby
the solid state reaction in solidsolution of
starting
oxides.Since the elastic contribution G~~ to Gibbs free energy G is of minor
importance
in formation of new nuclei with radius r the interfacial energy E~ =4
wr~,
y is balanced
by
thevolume energy introduced
by
O-Orepulsion
energy E~=
4
wr~Eo/3 (Eo~ 0.16eV)
withcorresponding
reduction of termr
~exp(G/kT).
A ratherrough
estimation for thegrain
radius r
=
3
y/E~ gives
for y lJ/m~ [12]
r 2 ~L, ingood
agreement with the result of themicroscopic
observation ofdecomposed
Y-336.The
picture
ofloosely
connectedgrains
in Y-336 is contrastedby
the measurements of ACsusceptibility.
Whereas
susceptibility
in ceramicsamples
exibits twosteps [13, 14] (Fig. 4)
associated with theproperties
ofgrains
andintergranural
links[15]
the transition in Y-336 reveals a rathernarrow
single
step(AT~~2.7K)
followed with a tailprotruded
to lower temperatures.Furthermore,
in ceramicsamples
these steps are shiftedapart
onincreasing
theamplitude
of theapplied magnetic
field in theexplored
range(0.02
~Ho
< IDe). Therefore,
this step may be associated with theproperties
ofYBa~CU~O~
~
grains
in accordance with above discussion and withprevious findings [15].
We note however that the transition in Y-336 is alsoqualitatively
different from those observed inpowdered YBa~CU~O~_~ samples,
where thetransition, although
rather insensitive toHo [15],
isusually
broad(AT~
~ loK)
and continuessmoothly
into tail. Thisprobably
arises from a wide distribution in thesize, shape,
orientation andpossibly quality
of the individualgrains. Therefore,
rather narrowdiamagnetic
transition observed forsample
Y-336 indicates much narrower distribution of the above parameters.The same conclusion is also reached from the
imaginary
part(Xim)
of the ACsusceptibility (associated
withloss)
also shown in thefigure
3. Whereas inpowdered samples only
a smallbump
in the broad loss distribution appears[3]
a rather narrow maximum centered at around 0.5 Xim is observed forsample
Y-336.Therefore,
the distribution of thegrain
sizes in Y-336 isnarrower
and/or
the averagegrain
sizelarger (larger
x~~ at maximum in respectx~~ at low
temperature (x~~/x~~~ 0.05))
than that in usual Y-123 ceramicsamples.
AsX,miaUJ
,_
x,~
;' :
,: foul
: ; :
,.: :"
.. ; :.
,;." ,,..:j"
:~Y
,;°f
...." z
... .."
.: ".
:"
.:
...
.,,,
,,.. ...:..
VK
Fig.
4. Diamagnetic transition to SC state of Y-123 : sample a ~p = 0.8 GPa)decomposed
in real part X andimaginary
part Y. The continuous line Z is diamagnetic transition in Y-336 plotted in figure 3.evidenced from the absence of the second
peak
in xj~ and ofcorresponding
secondstep
in x~~ theintergrain coupling
is either far to weak or thiscoupling
does not influence the SCproperties
in Y-336. The existence of very weakintergrain coupling
is however inferred from the slow increase of x~ and nonzero X~n at lowertemperatures.
In
conclusion,
the resistive response of thesamples
Y-Ba-Cu-O to thestep
like increase of the oxygen pressuregives
an usefulinsight
in elasticproperties
ongrain
and twin boundaries.The SC transition widths are in close correlation with these elastic
properties.
Acknowledgments.
We are indebted to
Ministry
of Science andTechnology
ofRepublic
Croatia for financial support under contract No 1-03-069 and to Dr. D. Duzevic forhelpfull
discussions.References
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