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High-temperature mechanical behavior of polycrystalline yttrium-doped barium cerate perovskite

Abstract

The high-temperature mechanical properties of the mixed ionic-electronic conductor perovskite BaCe0.95Y0.05O3-δ with average grain size of 0.40μm have been studied in compression between 1100 and 1300°C in air at different initial strain rates. The true stress-true strain curves display an initial stress drop, followed by an extended steady-state stage. As the temperature decreases and/or the strain rate increases, there is a transition to a damage-tolerant strain-softening stage and eventually to catastrophic failure. Analysis of mechanical and microstructural data revealed that grain boundary sliding is the primary deformation mechanism. The strength drop has been correlated with the growth of ultrafine grains during deformation, already present at grain boundaries and triple grain junctions in the as-fabricated material.

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High-temperature mechanical behavior of polycrystalline yttrium-doped barium cerate perovskite

Author: Vaquero Aguilar, Cristina; López Robledo, Manuel Jesús; Martínez Fernández, Julián; Real Pérez, Concepción; Jiménez Melendo, Manuel
Publisher: Elsevier
Year: 2011
DOI: 10.1016/j.jeurceramsoc.2010.05.023
Source: https://idus.us.es/bitstreams/3e68e34e-8824-491f-8873-549e0a6111d0/download
1
High- empe a u e mechanical beha io o polyc ys alline y ium-doped ba ium
ce a e pe o ski e
C. Vaque o-Aguila (a), M.J. López-Robledo (a), J. Ma ínez-Fe nández (a), C. Real
(b), M. Jiménez-Melendo (a)
(a) Depa amen o de Física de la Ma e ia Condensada, Uni e sidad de Se illa, Ap do.
1065, 41080 Se illa, Spain
(b) Ins i u o de Ciencias de Ma e iales de Se illa, Uni e sidad de Se illa-CSIC, A .
Ame ico Vespucio 49, 41092 Se illa, Spain
Abs ac
The high- empe a u e mechanical p ope ies o he mixed ionic-elec onic conduc o
pe o ski e BaCe0.95Y0.05O3−δ wi h a e age g ain size o 0.40 μm ha e been s udied
in comp ession be ween 1100 and 1300 °C in ai a di e en ini ial s ain a es. The ue
s ess– ue s ain cu es display an ini ial s ess d op, ollowed by an ex ended s eady-
s a e s age. As he empe a u e dec eases and/o he s ain a e inc eases, he e is a
ansi ion o a damage- ole an s ain-so ening s age and e en ually o ca as ophic
ailu e. Analysis o mechanical and mic os uc u al da a e ealed ha g ain bounda y
sliding is he p ima y de o ma ion mechanism. The s eng h d op has been co ela ed
wi h he g ow h o ul a ine g ains du ing de o ma ion, al eady p esen a g ain
bounda ies and iple g ain junc ions in he as- ab ica ed ma e ial.
Keywo ds
D. Pe o ski es; C. C eep; A. Sin e ing; B. Mic os uc u e- inal; A. G ain g ow h
1. In oduc ion
Pe o ski e-s uc u ed oxides o gene ic o mula ABO3 (whe e A and B deno e si e
ca ions) ha e ecei ed inc easing a en ion in he las yea s because he selec i e A and
B si e doping p o ides a unique oppo uni y o ailo ing hei p ope ies o impo an
p ac ical applica ions, pa icula ly in he ield o elec ochemical ene ge ics as
elec oly es in solid oxide uel cells (SOFCs) and chemical senso s.1, 2, 3, 4, 5, 6 and 7
Subs i u ion o B4+ si es by i alen ions in hese pe o ski e oxides causes he
o ma ion o oxygen acancies, which allow o p o onic conduc ion (hyd ogen ion
anspo ) a he han he mo e amilia oxygen ion conduc ion. Because o he highe
mobili y o p o ons, he ope a ing empe a u e o SOFCs can be sa ely educed wi hou
deg ading pe o mance.8 and 9
Y ium-doped ba ium ce a e (BCY) is a p o o ype o his class o p o on conduc ing
oxides. I exhibi s one o he highes p o on conduc i i ies a ele a ed empe a u es, as
2
well as an excellen chemical s abili y o e a la ge ange o empe a u es and oxygen
pa ial p essu es.10, 11 and 12 In addi ion, i has been ecen ly disco e ed ha BCY
also exhibi s ema kable s eam-pe mea ion capabili ies unde app op ia e condi ions,13
and 14 ha can be used o imp o e he pe o mance o a a ie y o ene gy con e sion
echnologies including SOFCs, memb ane e o me s and coal gasi ica ion. Mos o he
in es iga ions on BCY a e conce ned wi h i s p ocessing, s uc u e, de ec chemis y
and conduc i i y cha ac e is ics. Only wo s udies, howe e , ha e ocused on he high-
empe a u e mechanical p ope ies o hese high- empe a u e p o on conduc o s.15 and
16 These p ope ies a e o special ele ance in he design o componen s and sys em
a chi ec u es in SOFCs and o he high- empe a u e ope a ing de ices, which a e
ypically submi ed o c eep condi ions: de o ma ion, mechanical deg ada ion and
ailu e de e mine he ma e ial beha io and ul ima e o e all pe o mance. C eep s udies
o pe o ski es a e also impo an o unde s anding he de o ma ion beha io o he
Ea h's lowe man le.17 and 18 In addi ion, high- empe a u e plas ic de o ma ion is
usually con olled by di usion, and can hus p o ide basic in o ma ion abou mass
anspo in he compound. Since sin e ing and g ain g ow h a e go e ned by di usional
p ocesses, such an in o ma ion can be used o de ise op imum p ocessing schedules.
The e o e, he objec i e o his wo k was o in es iga e he high- empe a u e
mechanical beha io o ine-g ained BaCe0.95Y0.05O3−δ polyc ys als ab ica ed by
solid s a e eac ion. De o ma ion cu es we e ob ained in ai a a ious cons an
displacemen a es in he empe a u e ange be ween 1100 and 1300 °C. The mechanical
da a we e co ela ed wi h mic os uc u al obse a ions o deduce he de o ma ion
mechanisms.
2. Expe imen al p ocedu e
2.1. Sample p epa a ion
BaCe0.95Y0.05O3−δ (BC5Y) powde s we e p epa ed by solid-s a e eac ion o BaCO3,
CeO2 and Y2O3 powde s (Ald ich, pu i y >99.0%). The aw ma e ials we e weigh ed
in he equi ed s oichiome ic a io, mixed and g ounded in aga e media o 1 h using a
plane a y ball mill. The esul ing powde was calcined o 10 h a 1200 °C in ai and
hen manually c ushed o educe agglome a es. X- ay di ac ion analysis con i med
ha he esul ing powde was pu e o ho hombic pe o ski e phase. The powde was
uniaxially p essed a 150 MPa in o 20 mm-diame e pelle s and hen isos a ically cold
p essed a 210 MPa. A wo-s ep sin e ing p ocess was pe o med on he pelle s in ai
a mosphe e a low hea ing and cooling a es: a i s s ep a 600 °C o 2 h o elimina e
wa e and hyd oxides o med du ing in e media e s ages, and a second sin e ing s ep a
1550 °C o 10 h. The inal densi y o he samples, de e mined using A chimedes’
me hod, was abou 90% o he heo e ical alue (6310 kg/m3).
2.2. Mechanical es s and mic os uc u al obse a ions
Specimens o 5 × 3 × 3 mm in size we e cu om he sin e ed pelle s wi h a low-speed
diamond saw and used o mechanical es ing. Comp ession es s we e ca ied ou a
3
empe a u es T be ween 1100 and 1300 °C (0.74Tm < T < 0.85Tm, whe e Tm = 1850 K
is he mel ing empe a u e o BaCeO3) in ai a cons an c oss-head speed. The
specimens we e sandwiched be ween CSi pads in o de o educe he ic ion wi h he
alumina push ods o he de o ma ion machine, which ends o cause plas ic
cons ic ions a ei he end o he specimen. The eco ded da a, load s ime, we e
plo ed as σ–ɛ cu es, whe e σ is he ue s ess and ɛ is he ue s ain. Mechanical es s
we e discon inued a e eaching a o al ue s ain o 50% o subsequen
mic os uc u al obse a ions.
The da a we e analyzed using he s anda d high- empe a u e powe law o s eady-s a e
de o ma ion:
(1)
whe e A is a pa ame e depending on he de o ma ion mechanism, d is he g ain size, n
is he s ess exponen , p is he g ain size exponen , Q is he ac i a ion ene gy o low
and R is he gas cons an .
2.3. Mic os uc u al obse a ions
The mic os uc u al cha ac e iza ion o as- ab ica ed and de o med polyc ys als was
ca ied ou using con en ional (SEM) and high- esolu ion (HRSEM) scanning elec on
mic oscopy (Mic oscopy Se ice, Uni e si y o Se illa, Spain). To e eal g ain
bounda ies, longi udinal sec ions we e cu om he samples and mechanically polished
using up o 1 μm g ade diamond pas e, and hen he mally e ched a 1200 °C o 2 h in
ai . The ele an mo phological pa ame e s, g ain size d ( aken as he equi alen plana
diame e d = (4(g ain a ea)/π)1/2) and o m ac o F (de ined as F = 4π(g ain
a ea)/(g ain pe ime e )2) we e measu ed by using a semiau oma ic image analyze .
F ac u e su aces we e also analyzed by HRSEM; in as- ab ica ed and non- ac u ed
s ained specimens, ac u e su aces we e ob ained h ough b eaking he samples by
impac a oom empe a u e.
3. Expe imen al esul s
Fig. 1 shows a HRSEM mic og aph o a polished and he mally e ched c oss-sec ion o
he ab ica ed ma e ial. The g ains appea o ha e an equiaxed shape (F = 0.80), wi h an
a e age g ain size d o 0.40 μm. Po osi y consis ed in ca i ies a mul iple g ain
junc ions, wi h po e sizes o a ew mic ome e s.
Typical ue s ess σ– ue s ain ɛ cu es a e shown in Fig. 2 o di e en de o ma ion
condi ions o s ain a e and empe a u e. As no ed abo e, es s we e usually ended a
50% s ain o a be e obse a ion o he esul ing mic os uc u e, unless p ema u e
ac u e occu ed. The compound exhibi s a ansi ion om duc ile o agile beha io as
he ini ial s ain a e inc eases o he empe a u e dec eases. Se e al cha ac e is ics may
be no iced om his igu e:
4
In he duc ile egion ( ha is, a lowe s ain a es and highe empe a u es), he cu es
exhibi a peak s ess a he beginning o he de o ma ion, ollowed by a con olled s ess
d op and hen by an ex ensi e seconda y c eep egime (cha ac e ized by a posi i e slope
o he σ–ɛ cu e due o he inc ease in specimen sec ion and ue s ain a e du ing
comp ession). The e is a p og essi e ansi ion om duc ile o agile beha io when
inc easing he ini ial s ain a e and/o dec easing he empe a u e. The onse o ma e ial
deg ada ion is cha ac e ized by a slow dec ease in low s ess wi h inc easing s ain, as
can be seen in he σ–ɛ cu e o View he Ma hML sou ce in Fig. 2a. Despi e he
damage, he ma e ial s ill e ains a ela i ely high s eng h a e he comple ion o he
es in his semib i le egime (cu e o T = 1200 °C in Fig. 2b), indica ing he
a ainmen o a damage- ole an egime in such expe imen al condi ions E en ually, a
he wo s es ing condi ions o s ain a e and empe a u e, ca as ophic ailu e occu ed
a e ela i ely small s ains.
The magni ude o he s ess d op ( he di e ence be ween uppe and lowe yield
s esses) dec eases when dec easing he s ain a e and/o inc easing he empe a u e.
The a io be ween he peak s ess and he minimum s ess is, howe e , p ac ically
cons an wi h a alue o 1.10. This esul sugges s ha he mechanism esponsible o
he ini ial s eng h d op is he same a all de o ma ion condi ions.
The c i ical s ain ɛp a which he peak s ess σp and subsequen so ening akes place
also shi s sligh ly o lowe s ains wi h inc easing empe a u e and/o dec easing s ain
a e.
The mechanical cha ac e is ics o BC5Y polyc ys als in he duc ile egion (s eng h
d op ollowed by s eady-s a e de o ma ion, and a ia ion o σp and ɛp wi h he wo
con ol a iables View he Ma hML sou ce and T) a e e y simila o hose epo ed o
a ious me als and alloys a ho de o ma ion condi ions. 19, 20, 21, 22 and 23 On he
con a y, e y ew s udies ha e epo ed he occu ence o yield d op in ce amic
polyc ys als, 24 and 25 pa icula ly a small g ain sizes.26 To ou knowledge, no such a
beha io has been ound on simila ly s uc u ed pe o ski es.
The mac oscopic aspec o he s ained samples is well co ela ed wi h he mechanical
beha io displayed by he co esponding s ess–s ain cu es. Excep o he mos
se e e de o ma ion condi ions whe e ca as ophic ailu e occu ed, he samples
unde wen a a he homogeneous de o ma ion wi hou ba eling. No special ea u es
we e obse ed o samples exhibi ing s eady-s a e low. As he empe a u e dec eased
and/o he ini ial s ain a e inc eased, mac oscopic c acks pa allel o he loading
di ec ion we e isible on he la e al su aces, co esponding o samples wi h con olled
deg ada ion. As no ed p e iously, he ma e ial was ole an o hese mac oc acks e en
a e s ains o 50% in comp ession. Finally, hese c acks de eloped as e a highes
s ain a es and lowes empe a u es, ac u ing he sample in o small pieces.
Fig. 3 shows a polished and he mally e ched longi udinal c oss-sec ion o a sample
de o med in s eady-s a e condi ions (T = 1300 °C, View he Ma hML sou ce, ɛ = 50%).
The g ains emain equiaxed, indica ing ha g ain bounda y sliding is he p ima y
5
de o ma ion mechanism a such expe imen al condi ions, as usually ound in ine-
g ained supe plas ic me als and ce amics. 27 and 28 As T dec eases o View he
Ma hML sou ce inc eases, g ain bounda y sliding is no as enough o accommoda e
he de o ma ion imposed, and c acks de elop along g ain bounda ies leading e en ually
o ailu e. A close inspec ion o Fig. 3 e eals ha he a e age g ain size is sligh ly
smalle han ha o he as- ab ica ed ma e ial due o he p esence o new ine g ains o
abou 100 nm in size. This inding can be be e obse ed in Fig. 4, which shows
HRSEM mic og aphs o e ical ac u e su aces ob ained unde a ious expe imen al
condi ions. In he as- ab ica ed ma e ial (Fig. 4a), he g ain bounda ies and iple
junc ions a e deco a ed wi h ul a ine g ains smalle han 20 nm in size; hese g ains
inc ease up o abou 100 nm in size du ing s eady-s a e de o ma ion (Fig. 4b). A simila
e olu ion o he g ain s uc u e was obse ed in samples ha ailed du ing es ing (Fig.
4c).
4. Discussion
The mechanical cha ac e is ics displayed by he σ–ɛ cu es o BC5Y indica e he
occu ence o a so ening mechanism p io o he es ablishmen o he s eady-s a e low,
leading o a peak in s ess. Mo i a e al.26 ha e ecen ly epo ed yield d op in a ine-
g ained (d < 1 μm) e agonal Z O2–30 ol% spinel composi e, which was a ibu ed o
a sudden inc ease in he mobile disloca ion densi y in spinel g ains. Simila ly, Dokko
and Pask24 asc ibed he yield d op in la ge-g ained MgO (d > 10 μm) o disloca ion
mul iplica ion in di e en slip sys ems. These in ag anula disloca ion- ela ed
mechanisms, also ound in single c ys als, usually esul in a he sha p s ess d ops,
which a e li le a ec ed by s ain a e. In he p esen wo k, all yield cu es a e o
ounded con igu a ion, and he yield s esses s ongly depend on he s ain a e (and
empe a u e). This beha io is e y simila o wha has been epo ed in he ho
de o ma ion o me als and alloys, 19, 20, 21, 22 and 23 in which he peak s ess and
s eady-s a e low esul om a dynamic balance be ween disloca ion eco e y and
dynamic ec ys alliza ion. The mic os uc u al e olu ion obse ed du ing mechanical
es ing o BC5Y (Fig. 4), along wi h he a ia ion in peak s ess and s ain alues wi h
empe a u e and s ain a e condi ions, sugges s ha he g ow h o he ul a ine g ains
unde de o ma ion is esponsible o he peak s ess and subsequen con olled s eng h
d op. A he beginning o he de o ma ion, he ul a ine g ains a e so small ha
“no mal” neighbo g ains a e in con ac wi h each o he ; hese no mal g ains, wi h an
a e age g ain size d, hus will ca y he imposed load a a s ess le el gi en by Eq. (1).
As he de o ma ion p og esses, he ul a ine g ains will g ow and pa icipa e in he
p ocess suppo ing some o he load. The e ec i e a e age g ain size in he ma e ial is,
he e o e, e ined, leading o a dec ease in low s ess wi h s ain acco ding o he
in e se dependence o he s eady-s a e s ain a e wi h g ain size (Eq. (1)), as
expe imen ally obse ed (Fig. 2).
Wi h he p e ious s a emen , he mic os uc u e o he samples can be ega ded as
cons an up o he peak s ess σp, ega dless o es ing condi ions. The s eady-s a e
equa ion o low (Eq. (1)) can be hus w i en as:

6
whe e B is a cons an independen o s ess. The s ess exponen n can be es ima ed
om a plo o log View he Ma hML sou ce e sus peak s ess σp a a gi en
empe a u e, as shown in Fig. 5 o T = 1300 °C. A alue o n = 1.8 was ound, which is
in close ag eemen wi h he alue o 2 sys ema ically epo ed in ine-g ained me als
and ce amics, 27 and 28 whe e g ain bounda y sliding is he dominan de o ma ion
mechanism. A s ess exponen o 2 has been also p edic ed by many heo e ical models
de eloped o explain he supe plas ic beha io o ine-g ained ma e ials based on
di usion and/o disloca ion slip.28 None o hem, howe e , is able o explain
success ully he body o expe imen al da a; his is p esen ly a ma e o in ense deba e.
The alue o n = 1.8 expe imen ally ound in ine-g ained BC5Y subs an ia es he
p e ious conclusion, based on mic os uc u al obse a ions abou he e en ion o
equiaxed g ain shapes du ing c eep, ha g ain bounda y sliding plays a key ole in he
de o ma ion o hese compounds.
When de o ma ion is achie ed by g ain bounda y sliding, he s eady-s a e low
gene ally is con olled by he di usion necessa y o accommoda e he s esses gene a ed
du ing sliding.27 and 28 Thus, he ac i a ion ene gy o low Q (Eq. (1)) mus
co espond o he ac i a ion ene gy o he slowes mo ing species in he compound. A
alue o Q = 390 ± 40 kJ/mol was de e mined om an A henius plo o log σp e sus
ecip ocal empe a u e 1/T a ixed ini ial s ain a es. Un o una ely, he e a e no
enough di usion da a a ailable o BCY o make a p ecise compa ison. Only he
ac i a ion ene gy o oxygen bulk di usion Q ≈ 60 kJ/mol has been epo ed,15 which
is subs an ially smalle han he alue o c eep, and sugges s ha ca ion di usion is he
a e-limi ing p ocess. The lack o comp ehensi e ca ion bulk and g ain bounda y
di usi i ies p ecludes a de ini i e iden i ica ion o he a e-con olling species.
Two p e ious wo ks15 and 16 ocused on he high- empe a u e de o ma ion o
BaCe1−xYxO3−δ, wi h x a ying be ween 0.05 and 0.20, g ain sizes anging om 2 o
9 μm and ela i e densi ies o abou 90% o heo e ical alues. In hese s udies, a s ess
exponen close o uni y and an ac i a ion ene gy o c eep o 360 ± 60 kJ/mol we e
epo ed. These alues, along wi h he ac ha g ains did no change shape du ing
es ing, allowed he au ho s o conclude ha he de o ma ion was achie ed by g ain
bounda y sliding accommoda ed by ca ion la ice di usion. The same conclusion was
d awn in he de o ma ion o o he oxide pe o ski es wi h g ain sizes anging be ween 2
and 50 μm, whe e a s ess exponen o abou 1 was sys ema ically ound:
La0.9S 0.1MnO3,29 La0.8S 0.2Ga0.85Mg0.15O2.825,30 BaTiO3,31
La0.2S 0.8Fe0.8C 0.2O332 and S Co0.8Fe0.2O333. The di e ence in s ess exponen
alues be ween hese s udies (n ≈ 1) and he p esen wo k (n ≈ 2) can be ela ed wi h he
di e ence in g ain sizes. A ansi ion om n = 1 owa ds n = 2 wi h dec easing g ain
size has been no ed o o he ce amic oxides 27 and 34; he c i ical g ain size seems o
be abou 1 μm, in ag eemen wi h he p esen esul s. Ne e heless, di usion is he a e-
limi ing s ep in bo h cases; he alues o Q measu ed in ine- and la ge-g ained BCY
(390 and 360 kJ/mol, espec i ely) compa e e y well and sugges ha ca ion la ice
7
di usion is also he a e-con olling mechanism o g ain bounda y sliding in he n = 2
egion. I is wo h no ing ha he same mechanism was p oposed o he supe plas ic
beha io o ine-g ained e agonal zi conia.27
5. Conclusions
Polyc ys alline BaCe0.95Y0.05O3−δ wi h a e age g ain size o 0.40 μm was s ained in
comp ession be ween 1100 and 1300 °C in ai a a ious cons an ini ial s ain a es.
The ue s ess– ue s ain cu es sys ema ically displayed an ini ial s eng h d op
ollowed by an ex ensi e s eady-s a e egime, excep a he mos se e e de o ma ion
condi ions (lowes empe a u es and highes s ain a es) whe e ca as ophic ac u e
occu ed. The yield s ess showed s ong dependence on empe a u e and on he applied
s ain a e. No change in g ain shape was obse ed a e 50% s ain, indica ing ha
g ain bounda y sliding is he main de o ma ion mechanism in his compound, as also
ound in ine-g ained supe plas ic ma e ials. The s ess d op has been co ela ed wi h
he g ow h o ul a ine g ains p esen p e iously a g ain bounda ies and iple g ain
junc ions in he as- ab ica ed ma e ial. A s ess exponen n = 1.8 and an ac i a ion
ene gy o low Q = 390 kJ/mol we e es ima ed om mechanical. The n alue is
consis en wi h g ain bounda y sliding accommoda ed by di usion. By compa ison wi h
la ge-g ained oxide pe o ski es, i is sugges ed ha de o ma ion is a e-con olled by
bulk ca ion di usion.
Acknowledgmen
This wo k was suppo ed by he P ojec no. MAT2009-13979-C03-01, Minis e io de
Ciencia e Inno ación, Spain.
8
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man le
16
Figu e 3

17
Figu e 4
18
Figu e 5