The effect of Sn on corrosion mechanisms id din advanced …...17th International Symposium on...
Transcript of The effect of Sn on corrosion mechanisms id din advanced …...17th International Symposium on...
17th International Symposium on Zirconium in the Nuclear Industry
The effect of Sn on corrosion mechanisms i d d Z l ddi f PWRin advanced Zr-cladding for PWR
Philipp Frankel, J. Wei, E. Francis, S. Lyon, R.A. Cottis, M. PreussMaterials Performance Centre, The University of Manchester
N Ni S L P C R M GN. Ni, S. Lozano-Perez, C. R. M. GrovenorDepartment of Materials, University of Oxford
R. J. Comstock, L. HallstadiusWestinghouse, USA/SwedenA. Ambard, M. Blat-Yrieix
EDF FranceEDF, France
03-08 February, Hyderabad, India
Oxi
datio
n of
Zr
Allo
ysyWhat w
e know
:
Large compressive stress in oxide
gp
Zr to
ZrO
2transformation ‐volum
e increase
Tw
ooxideph
ases:M
onoclinic,Tetragonal
Two oxide ph
ases: M
onoclinic, Tetragonal
Tetragon
al only stable at 3
60C by stress, grain size (or chem
istry)
Transformation Tet
mon
o, fu
rthe
r volume increase
Gll
Tlh
if
Gen
erally, m
ore Tetragon
al phase near interface
Recent work (M
UZIC program):
Level of transform
ation im
portant to transitio
n
Related to nano‐po
rosity in
oxide
1A
STM
Intl,
Vol
. 8, N
o. 9
, doi
: 10:
1520
/JA
I103
246,
201
1, 6
49-6
812
Jour
nal o
f Nuc
lear
Mat
eria
ls 4
32 (2
013)
, pp.
102
-112
3ActaMateralia, 2013
The
effe
ct o
f Sn:
Del
ayed
tran
sitio
ny
ZIR
LO®
Exp
erim
enta
l Z
IRLO
®E
xper
imen
tal
allo
y
~0.
92 w
t% S
n~
0.01
wt%
Sn
0.92
wt%
Sn
Exp
osur
e at
360
C in
Wat
er (
Day
s)E
xpos
ure
at 3
60C
in W
ater
(D
ays)
Tabl
e 1:
Mea
sure
d ch
emic
al c
ompo
sitio
n of
the
mat
eria
ls.
Allo
y Al
loyi
ng E
lem
ents
Zr
Fe
[wt%
] Sn
[wt%
] N
b[w
t%]
Hyd
roge
n [w
t.ppm
] ZI
RLO
®ba
lanc
e0
090
920
9110
p(
y)
ZIR
LO
bala
nce
0.09
0.92
0.91
10
A-0.
0%Sn
ba
lanc
e 0.
1 0.
01
1.00
17
Syn
chro
tron
X-R
ay D
iffra
ctio
ny
y
ZIR
LO®
A0
0%S
n
Evolution of Residual stress and ph
ase fractio
n
ZIR
LO®
A-0
.0%
Sn
Ex-
situ
XR
DE
x-si
tu X
RD
Ex
situ
XR
DE
xsi
tu X
RD
Exp
osur
e at
360
C in
Wat
er (
Day
s)E
xpos
ure
at 3
60C
in W
ater
(D
ays)
p(
y)
Measure sam
ples after different len
gths of autoclave exposure
Syn
chro
tron
XR
D: P
enet
ratio
n de
pth
H
igh-
ener
gy a
nd h
igh
flux
S
uffic
ient
pen
etra
tion
to s
ampl
e en
tire
oxid
e as
oxi
de th
icke
nsp
p
Labo
rato
ry X
RD
Syn
chro
tron
XR
D
Thin
oxi
deM
tl
(~ 3
µm)
Met
al
Thic
ker o
xide
Syn
chro
tron
XR
D:
H
igh-
ener
gy a
nd h
igh
flux
S
uffic
ient
pen
etra
tion
to s
ampl
e en
tire
oxid
e as
oxi
de th
icke
nsp
p
Fast
cou
ntin
g tim
es
G
ood
sign
al, l
ow b
ackg
roun
dP
hf
ti
Pha
se fr
actio
n
Res
idua
l Stre
ss M
onoc
linic
& T
etra
gona
l pha
ses
Syn
chro
tron
XR
D R
esul
ts: E
ffect
of S
ny
Te
trago
nal P
hase
Fra
ctio
n
ZIR
LOA
-0.0
%S
n
Oxi
deO
idO
xide
Met
alM
etal
Oxi
de
Met
alM
etal
Oxi
de
The
effe
ct o
f Sn:
Res
idua
l stre
ssZ
IRLO
A-0
.0%
Sn
Mon
oclin
ic
Tet
rago
nal
The
effe
ct o
f Sn:
Res
idua
l stre
ssZ
IRLO
A-0
.0%
Sn
Mon
oclin
ic
Not
str
ess
stab
ilise
do
ses
ss
abse
d
Tet
rago
nal
Ex-
situ
syn
chro
tron
XR
DI
id
b
ZIR
LO®
Allo
y
Interesting tren
ds, but…
ZIR
LO®
Allo
y A
Ex-
situ
XR
DE
x-si
tu X
RD
Ex
situ
XR
DE
xsi
tu X
RD
Exp
osur
e at
360
C in
Wat
er (
Day
s)E
xpos
ure
at 3
60C
in W
ater
(D
ays)
p(
y)
Only few points, different sam
ples
relatively high
scatter
No inform
ation from
early in
corrosion
In-S
itu E
xper
imen
t
Sample he
ated
in air at 5
50C during XR
D
Fast eno
ugh grow
th fo
r 12 ho
ur experim
ent
Nid
li
i?
Not ideal com
parison to ex‐situ m
easuremen
ts?
Manydata
pointsfrom
singlepo
into
nsinglesample!
Many data points from
single po
into
n singlesample!
ZIRLO
Hihiii
llh
d
ihi
Tet
rago
nal p
hase
evo
lutio
n at
550
C
ZIRLO: H
igh initial te
tragon
al phase
redu
ces with
time
tion ase fract nal pha Tetrago T
Oxi
datio
n tim
e at
550
C
Tet
rago
nal p
hase
evo
lutio
n at
550
C
Hihiii
llh
d
ihi
Lower te
tragon
al con
tent fo
r A‐0%Sn
High initial te
tragon
al phase
redu
ces with
time
tion ase fract nal pha Tetrago T
Oxi
datio
n tim
e at
550
C
Tet
rago
nal p
hase
evo
lutio
n at
550
C
Plb
df
A0%
S
Plateau ob
served
for A
‐0%Sn
tion ase fract nal pha Tetrago T
Oxi
datio
n tim
e at
550
C
Effe
ct o
f red
uced
Sn
Lower te
t. pha
seA
ihE
ib
if
360C
Agrees with
Ex‐situ observatio
n for 3
60C
Sn
stabilises tetragon
al phase in
engineering
ceram
ics
Plateau with prolon
ged oxidation
Agrees with
Ex‐situ observatio
n for 3
60C
g
Tet. phase uniform
ly distributed
, i.e. not stress stabilised
Hihiitilt
th
didl
High initial tet. p
hase, red
uces ra
pidly
Not observed previously!!!
Tilti
tibl
itTime resolutio
n no
t possible ex‐situ
Mon
oclin
ic r
esid
ual s
tres
s at
550
C
Co
nstant m
onoclinic stress for ZIRLO
Mon
oclin
ic r
esid
ual s
tres
sLower Snalloy –lower stresses that re
lax over time
Re
duced creep strength (impo
rtant b
enefit of Sn!)
pg
(p
)
Mon
oclin
ic r
esid
ual s
tres
sLower Snalloy –lower stresses that re
lax over time
Re
duced creep strength (impo
rtant b
enefit of Sn!)
pg
(p
)
Sh
arp
dro
p in
T
et F
ract
ion
Tet
. Fra
ctio
n
Ph
ase
tran
s?
Tet
rago
nal r
esid
ual s
tres
sg
ZIRLO –large compressive stress, som
e relaxatio
n
Lower te
tpeak intensity
–larger scatter
Re
duced creep strength
Tet
rago
nal r
esid
ual s
tres
sg
A‐0%Sn
–Lower com
pressive stress
Even
lower te
tpeak intensity
–Even
larger scatter!
Tet
rago
nal r
esid
ual s
tres
sg
Stress canno
t be stabilising
mechanism
With
low Sn, only grain size stabilised
tetragon
al present
Not
stressstabilised
Not stress stabilised
Sum
mar
yy
O
bser
vatio
nsat
550
Cco
rrel
ates
wel
lwith
360
CO
bser
vatio
ns a
t 550
C c
orre
late
s w
ell w
ith 3
60C
S
imila
r mec
hani
sm d
espi
te d
iffer
ent e
nviro
nmen
t
R
educ
ed S
n
Low
er te
trago
nal p
hase
frac
tion
N
otst
ress
stab
ilise
d
Not
stre
ss s
tabi
lised
D
elay
ed tr
ansi
tion
with
redu
ced
Sn
R
elat
ed to
lack
of s
tress
sta
bilis
ed T
etra
gona
l
redu
ced
trans
form
atio
n
Pro
pose
d m
odel
Wha
t hap
pens
aro
und
trans
ition
?
Pre
-tra
nsiti
on:
Larg
er T
et g
rain
sLa
rger
Tet
. gra
ins,
Str
ess
stab
ilise
d
Gra
dual
tran
sfor
mat
ion
U
ncon
nect
ed N
ano
poro
sity
Wha
t hap
pens
aro
und
trans
ition
?
Pre
-tra
nsiti
on:
Larg
er T
et g
rain
sT
rans
ition
:R
apid
tran
sfor
mat
ion
Larg
er T
et. g
rain
s,S
tres
s st
abili
sed
Tra
nsfo
rmed
Rap
id tr
ansf
orm
atio
nLo
calis
edin
com
patib
ilitie
s
Lo
wer
str
ess
tr
ansf
orm
atio
n
Vo
lum
e in
crea
se
Gra
dual
tran
sfor
mat
ion
U
ncon
nect
ed N
ano
poro
sity
Wha
t hap
pens
aro
und
trans
ition
?
Pre
-tra
nsiti
on:
Larg
er T
et g
rain
sT
rans
ition
:R
apid
tran
sfor
mat
ion
Larg
er T
et. g
rain
s,S
tres
s st
abili
sed
Tra
nsfo
rmed
Rap
id tr
ansf
orm
atio
nLo
calis
edin
com
patib
ilitie
s
Lo
wer
str
ess
tr
ansf
orm
atio
n
Vo
lum
e in
crea
se
Gra
dual
tran
sfor
mat
ion
U
ncon
nect
ed N
ano
poro
sity
Rap
id tr
ansf
orm
atio
n
Inte
rcon
nect
ed p
oros
ityF
E c
ourt
esy
of P
. Pla
tt
Fur
ther
opt
ions
p
Low
er te
mpe
ratu
re o
xida
tion
S
low
er o
xida
tion
O
xida
tion
in s
team
A
pply
stea
mdu
ring
test
ing
A
pply
ste
am d
urin
g te
stin
g
H
igh
tem
ps. &
Tra
nsie
nts
~
LOC
A co
nditi
ons
Ali
dl
dd
iid
ti
App
lied
load
dur
ing
oxid
atio
n
Effe
ct o
n ox
idat
ion
rate
Ack
now
ledg
men
ts
g
MU
ZIC
par
tner
s:
ED
F, N
atio
nal N
ucle
ar L
abor
ator
y, R
olls
-Roy
ce, A
mec
and
,y,
y,
Wes
tingh
ouse
D
iam
ond
Ligh
t Sou
rce
I12
bli
I1
2 be
am li
ne
Eve
ryon
e th
at h
elpe
d on
Exp
erim
ent!
Fu
ndin
gg
Than
ks to
the
Eng
inee
ring
and
Phy
sica
l Sci
ence
Res
earc
h C
ounc
il (E
PS
RC
) and
MoD
in
the
UK
for f
undi
ng th
e re
sear
ch a
s pa
rt of
the
Mat
eria
ls fo
r Ene
rgy
call
(res
earc
h co
de:
EP
/E03
6171
/1).