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Guinier-Preston zones in Al-3 at.% Ag
B. Schönfeld, A. Göcmen, G. Kostorz
To cite this version:
B. Schönfeld, A. Göcmen, G. Kostorz. Guinier-Preston zones in Al-3 at.% Ag. Journal de Physique
I, EDP Sciences, 1992, 2 (6), pp.1075-1081. �10.1051/jp1:1992197�. �jpa-00246589�
Classification
Physics
Abstracts61.55H 81.30M
Guinier-Preston
zonesin Al-3 at.fli Ag
B.
Sch6nfeld,
A. G6cmen and G. KostorzInstitut flit
Angewandte Physik,
ETH Zorich, CH-8093 Zorich, Switzerland (Received 7Janua~y
1992, accepted infinal form
17Februa~y
1992)Rdsumk. on a mesur£ la diffusion de rayons X aux
grands angles
pour un monocristal d'Al- 3 9bat.Ag.
L'£chantillon a £t£ vieilli pour produire des zones de Guinier-Preston (« zones E »). Apant
d'une combinaison des intensit£s diffusescorrespondant
h l'ordre h courte distance, qui ont£t£
s£parses
des intensit£s mesur6es, avec des rdsultats ant£rieurs de diffusion de rayons X auxpetits angles,
des cristaux ont £t6 simul£s sur ordinateur.L'analyse
de ladisposition
des atomes dans ces cristaux semble supporter laproposition
r£cente d'un enrichissementd'argent
dons unecouche extdrieure des zones E,
Abstract. Diffuse wide-angle X-ray
scattering
has been measured from an Al-3 at.9bAg single
crystal.
Thesample
wasaged
for 4 min at 453 K toproduce
Guinier-Preston zones (« e-zones »).Combining
theseparated short-range
orderintensity
withprevious small-angle X-ray scattering
results,crystals
were computer modelled. Ananalysis
of the atomic arrangements in these modelcrystals
tends to support the recentsuggestion
of a silver enrichment in the shell of the E-zones.Introduction.
Guinier-Preston zones
(GP zones)
are metastablephases
foundduring
theearly
stages ofdecomposition.
InAl-Ag they
were first observedby
Guinier[II
withsmall-angle X-ray scattering (SAXS).
His basic model of these zones as silver-richspheres
has been refined over the years(for
a recent review, see, e-g-[2]).
In
subsequent investigations
the existence of two types of GP zones wasintroduced,
so-called q-zones below about 443K and e-zones for
higher temperatures.
This idea wassupported by
SAXS andatom-probe
field ionmicroscopy (AP-FIM),
where asignificant change
in the zonecomposition
was determined around 443 K(Baur
and Gerold[3],
Osamura et al.[4]).
Naudon and Caisso[5]
and alsoDubey
et al.[6], however,
did not observe such a distinctchange
in the zonecomposition
withaging
temperature. But from the presence of twopeaks
in a Porodrepresentation
of SAXS data for the eregime,
both groupssuggested
a different silver distribution in ~- and e-zones- The q-zones are
homogeneous (possibly short-range ordered),
and the e-zones have a morecomplex
structure : while a silver-enrichedcore and a
depleted
shell weresuggested by
Naudon and Caisso[5],
adepleted
core and anouter shell of
nearly
pure silver tumed out to be moreappropriate [6],
based on a detailedcomparison
of simulations withexperimental
results.1076 JOURNAL DE PHYSIQUE I N° 6
Small-angle scattering
is suited for aninvestigation
on alarger
than atomic scale. It was found useful to also includewide-angle
diffusescattering
in order to determine morereliably
the small-scale
Ag
distribution within the e-zones.One
quantitative wide-angle scattering study
onAl-Ag
has beenperformed by Gragg
andCohen
[7]
whoinvestigated
an Al-5at.fbAg single crystal aged
for 14h at 383 K andobserved no intemal order within the silver
agglomerates
that werereported
to be octahedral inshape
and to have an averageAg
content of 68 at.9b. It istempting
toaccept
these results asbeing fully
characteristic for q-zones. But as notedby Dubey
et al.[6],
the heat treatmentchosen was too short, and
quenched-in
silveragglomerates
areprobably
stilldominating.
That zones are octahedral and bounded
by ( ii1) planes
issupported by high
resolutionelectron
microscopy [8]. Using
transmission electronmicroscopy
afaceting
on(100) planes
in addition to the dominant
(111)
facets was found for somewhatlarger
zonesby
Alexander et al.
[9]
and followed as a function of temperature. Withincreasing
temperaturefaceting
decreases and theshape
of the zoneschanges
from a truncated octahedron to atruncated
sphere.
Similar results were deduced from SAXS[6],
with aslightly higher
percentage of
( ii1)
facets thangiven
in[9].
For a
wide-angle
diffusescattering experiment
it had to bekept
in mind that the e-zones should not be toosmall,
in order to be able to demonstrate apossible
silverinhomogeneity
within the zones in
computer-modelled crystals,
but smallenough
to avoid that themodulation in the diffuse
scattering
would be toosharp
close to the direct beam and theBragg
reflections.Furthermore,
a combination of thewide-angle scattering
with the SAXS data ofDubey
et al.[6]
was to beattempted.
Theory.
The
diffusely
scattered elastic coherentintensity
from abinary alloy
has two contributions :one due to the presence of two
types
of elements(short-range order/decomposition)
and the other due to the staticdisplacements
of these atoms from the mean lattice sites(size effect).
The
displacement scattering
cannot berepresented
in closed form and isusually
as in the present caseapproximated by
a seriesexpansion
up to termsquadratic
in the static atomicdisplacements (Bone
andSparks [10],
see also Schwartz and Cohen[11]).
For a cubic substitutional solid solution the chemical order which willonly
be of interest in thefollowing, gives
rise to ascattering intensity Is~o according
to~SRO
(h)
"
£ £ £
"fmn C°S("hl
C°S ("h2
m)
CDS(Wh3
n)
t
m n
where h=
(hi h~h~)
is thescattering
vector inreciprocal
lattice units(r.I.u.)
andai~~ are the
Warren-Cowley short-range
order parameters[12]
definedby
"fmn " 1~
P©/CB
P£$
is the conditionalprobability
offinding
a B atom(the
concentration of B atoms isc~)
at animn site,
if an A atom is atposition
000.Thus,
door has to beequal
to one. For ahomogeneous
solid solution ai~~~~y~~ =0,
andIs~o(h)
is the monotonic Lauescattering (defined
as one Laueunit).
Ashort-range
ordered fccalloy
has aj Jo <0,
but a~~o ~ 0 for a
decomposed
one.The various
scattering
contributions can beseparated taking
into account their differentsymmetries
inreciprocal
space. ForX-rays
thistechnique
was introducedby Georgopoulos-
Cohen
[13]
who extended theBorie-Sparks
evaluation[10] by explicitly including
a variationof the form factor ratios for
X-ray scattering.
TheGeorgopoulos-Cohen technique
wasapplied
in the presentinvestigation.
Experiment.
An Al-3 at.fb
Ag single crystal
was grownby
strainannealing [6].
A slice 9 mm in diameter and 2.5 mm thick was cutby spark
erosion. Thesample
washomogenized
at 848 K for 2h, quenched
into water andaged
at 453 K for 4min in a silicon oil bath. With such a heat treatment, the formation of thesubsequent
metastabley'-phase
is still avoided. Thesample
surface was
finally polished using
a 3 ~m diamond spray.The
wide-angle scattering
was measured on a four-circlediffractometer, using
MoK~ radiation,
apyrolitic graphite
monochromator and ahigh-purity
Ge detector. Thesample
was mounted under an evacuated
Be-hemisphere
to reduce airscattering.
For a detaileddescription
of theset-up,
see Klaiber et al.[14].
Data were taken at about 8 000
positions
inreciprocal
space(I.e.
diffractometersettings),
with more than 10 000 counts perposition.
The varioussettings
were chosenappropriate
to aGeorgopoulos-Cohen analysis,
with about 50symmetry-equivalent positions
for oneposition
within the minimum
separation
volume forshort-range
orderion
agrid
of 0.Ir-I-u-)-
The data were corrected for
background,
thermal diffusescattering
andCompton
scattering.
Thermal diffusescattering
up to third order was calculatedusing
the interatomic force constants up toeight neighboring
shells as determinedby
Gilat and Nicklow[15]
for pure aluminum.Compton scattering
was calculated from the data of Cromer[16]
and Cromer and Mann[17].
The atomicscattering
factors were taken fromDoyle
and Tumer[18]
withdispersion
correctionsgiven by
Sasaki[19].
Absolute intensities were calculatedusing
thescattering
ofpolystyrene
at sin MIA=0.5A~' (&
is half thescattering angle
andA the
wavelength).
The calibration before and after theexperiment agreed
within 2 9b.Results and discussion.
The
separated short-range
orderintensity
ispartly (there
is a total of 153 datapoints
in the presentcase)
shown infigure
I. It tumed out to beappropriate
toplot
the intensities versus themagnitude
of thescattering
vector, h. This couldalready
beanticipated
because the SAXSexperiment
showed a ratherisotropic intensity
distribution[20].
The data are ingood
agreement with the SAXS results obtained from asample
with acomparable
heat treatment.These intensities were
averaged
within a(110) plane. Surely, they
are notjust short-range
order
intensities,
but the static atomicdisplacement scattering
for such small values of h is small for analloy
with a small lattice misfit of 2 to 3 x10~~ [21].
12
iQ O
O
8
d °.
£ 6
o 2
°$Y
0
0.2
h
Fig. I.- SAXS [20] (.)
of
1078 JOURNAL DE
PHYSIQUE
I N° 6The
separated short-range
order intensities were fitted with theWarren-Cowley
short- range order parameters. About 20 to 30 of them could thus be determined. As the standard deviationssteadily
increased for alarger
number ofparameters,
a set of 23 ai~~ was chosen(weighted
R-value=
0.045, x~=1.4). Figure
2 compares theintensity
fromsmall-angle scattering
with the recalculatedshort-range
orderintensity.
It is obvious that a distinctunderestimation is observed close to the
origin
which is reflectedby
a~y~~=
0.831(7).
If one adds the SAXS data to theseparated short-range
orderintensity,
about 90 ai~~ can be fitted(weighted
R-value=
0.086, x~
=
7.2).
With alarger
number of ai~~ thesystem
ofequations
now becomes
unstable, indicating
that a volume and notjust
aplane
of SAXS datamight
berequired
for theleast-squares fitting.
With91ai~~
the recalculatedIs~o(h) reproduces
thegeneral
behaviour of the SAXSdata,
but notunexpectedly
fails toreproduce
the interferencepeak.
With door =1.038(12)
the theoretical value is reached within three times the standard deviation that wassolely
determined fromcounting
statistics. The a i~~~~y~~ are all
positive, decreasing monotonically
within one standard deviation towards zero, the value for astatistically
uncorrelatedarrangement.
Figure
2 also allows the radius ofgyration R~
to be estimated(for spherical particles
theparticle
radius isR~
=fi R~).
Theexperimental
value from SAXS isR~
=14. 5
(6) A,
andthe value determined from
Is~o(h)
recalculated from91ai~~
isonly slightly
lower(R~
= 11.81).
For sucha
particle
size a modelcrystal
with 32 x 32 x 32 unit cells(the
lattice parameter is 4.05A)
will besufficiently large.
Several
crystals
were modelled with all «i~~ ~~y~~starting
from a randomarrangement
andusing periodic boundary
conditions. Analgorithm
was used toexchange
Al andAg
atoms if acloser
approach
to theexperimental
a i~~ is
reached,
aprocedure
first realizedby
Gehlen and Cohen[22].
All the 90 ai~~finally
obtained were within the standard deviation of theirexperimental value,
with atypical agreement
of 0.1 9b or better.s
4
- *O
j °@
~ 3 ~O
~ °m
- ~
*ii
Do
_ *,
* ~.
- O *
c O ~ *O~
~ * _
l °
O ° O * * .
O o ~ *° ~
b J
0 o
0 0.03 0.06 0.09 0.12 0.15
h~,(r.I.u.)~
Fig.
2. Guinierplot
of the SAXSintensity
[20] (.), theshort-range
orderintensity
from 23 ai~~ (*) and from 91 ai~~ (o).Figure
3 shows aplot
ofeight
consecutive(100) planes
of a modelledcrystal,
where eachfigure represents
twoplanes.
One finds that the size of the e-zonescorresponds
to the radii found from a Guinierplot (Fig. 2). However,
the modelledparticles
are notreally spherical.
Especially,
it seems difficult to define aprecise interface,
and thus theparticle composition
cannot be
given exactly.
The value of71(10)
at.9bAg
determinedby Dubey
et al.[6]
from theintegrated intensity
ofSAXS,
issurely
consistent for the zones shown.Conceming
thea b
c d
Fig.
3. Four consecutive (100) doubleplanes
of acrystal
modelled from 90 ai~~ (. ;Ag,
o : Al).discussion about the intemal structure of the e-zones, a silver
depletion
in the cores is found to be moreplausible
even if theparticle
surface is notprecisely
known.Thus,
thethree-phase
model of
Dubey
et al.[6]
should represent the average characteristicparticle
structure. It is obvious that thepresent
atomictype
ofmodelling
is on a scale too fine togive
the «typical
»structure of the zones in an easy way. A different
algorithm
formodelling involving
notjust
atoms but
appropriately
chosenagglomerates
is morepromising
and will bedeveloped.
For
comparison
consecutive(100) planes
of one out of severalcrystals
modelled with all theWarren-Cowley short-range
order parameters ofGragg
and Cohen(Tab.
II of[7])
are shown infigure
4.Up
to the shell indeximn
=
510,
the agreement between the modelled and theexperimental
ai~~ was « 3 9b. Beside theexpected
difference in theparticle
size(the
radius ofgyration
is 5.9A [7])
it isstriking
that theseparticles
have ahigher
silver concentration(nearly
1009b)
thangiven
in[7].
Thusthey
represent silveragglomerates. Surely
the silver1080 JOURNAL DE PHYSIQUE I N° 6
a b
c d
Fig.
4. Four consecutive (100) doubleplanes
of acrystal
modelled with the 26 ai~~ of [7] (. : Ag, OAl).
content can be reduced to about 70 9b if additional
assumptions
about theshape (sphere
ortruncated octahedron) are
imposed.
Acknowledgement.
The authors thank Ph. A.
Dubey
formaking
available thesingle crystal
and for communicat-ing
the SAXS data.References
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Phys.
Rad. Paris 8 (1942) 124.[2] COHEN J. B., Solid St.
Phys.
39 (1986) 131.[3] BAUR R. and GEROLD V., Acta Metall. 10
(1962)
637.[4] OSAMURA K., NAKAMURA T., KOBAYASHI A., HASHIzUME T. and SAKURAI T., Scr. Metall. 21 (1987) 255.
[5] NAUDON A. and CAlsso J., J.
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[7] GRAGG J. E. and COHEN J. B., Acta Metall. 19
(1971)
507.[8] GRONSKY R., VAN TENDELOO G. and THOMAS G.,
Decomposition
of Alloys TheEarly Stages,
Proc. 2nd
Acta-Scripta
metall. Conf., P. Haasen, V. Gerold, R.Wagner
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SCHWARTz L. H. and COHEN J. B., Diffraction from Materials(Springer,
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A 24 (1968) 390.[19] SASAKI S., KEK
Report
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private
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