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Daniel Caillard, J.L. Martin
To cite this version:
Some
aspects
of
cross-slip
mechanisms
in metals and
alloys
D. Caillard
(1)
and J. L. Martin(2)
(1)
Laboratoired’Optique Electronique
du CNRS, B.P. 4347, F-31055 Toulouse Cedex, France(2)
Institut de GénieAtomique,
EcolePolytechnique
Fédérale de Lausanne, CH-1015 Lausanne,Switzerland
(Reçu
le 6 mars 1989,accepté
sousforme définitive
le 24 mai1989)
Résumé. 2014 Des modèles ont été
proposés
pour décrire leglissement
dévié des dislocations dans les métaux de structure CFC et HC. On montre comment ces modèles se sontdéveloppés
et comment des résultatsexpérimentaux
récents confirment leursprédictions. Quelques
aspectsmacroscopiques
de laplasticité
des cristaux tels que lesénergies
d’activation defluage,
les anomalies de limiteélastique
et les stades de durcissement sont discutés à la lumière de cesmodèles
microscopiques.
Abstract. 2014 Dislocation crossslip
in FCC and HCP metals has been described in terms of various models. Thedevelopment
of these models is reviewed and theirpredictions
arecompared
withrecent
experimental
observations. Somemacroscopic
features ofplastic
deformation(creep
activationenergies, strength
anomalies and deformationstages)
are examined in thelight
of thesemicroscopic
mechanisms. ClassificationPhysics
Abstracts 62.20H1. Introduction.
Cross
slip
occurs when the local stressespush
a dislocation into aplane
which is different fromthe
original plane
ofsplitting.
It has been evidencedlong
agoby
the observation ofslip
traces atsample
surfaces. The outlines of the first realistic models were then derivedby
Friedel,
both for face-centered cubic
(FCC)
metals[1]
in 1956 on the basis of calculations of Stroh(1954) [2]
and forhexagonal close-packed
(HCP)
metals[3]
in 1959. In the meantime,
another
theory
for dislocation crossslip
wasdeveloped
(see
e.g. Refs.[4]
and[5]).
Later on, similar
slip
traceobservations,
after creep at intermediatetemperatures,
led someauthors to
interpret
thecorresponding
activationenergies
in terms ofcross-slip
(Lytton et
al. ,
1958[6] ;
Friedel,
1959[3]
and 1964[7]).
This mechanism has also been claimed to be thekey
process at the transition stress ’iII1 between thehardening stages
II and III of FCC metals(Schoeck
andSeeger,
1955[4] ;
Friedel,
1956[1]
andHaasen,
1967[8]).
More
recently,
theimportance
of crossslip
in theplasticity
of metals has however beenignored
or underestimated.In the
present
paper, weattempt
to describe how these first ideasdeveloped
with time into detailedmodels,
and how these have been confirmed orimproved recently through
FCC metals and then consider Peierls
type
friction related toslip
inbody
centred cubic(BCC)
metals and noncompact
slip
in metals with a closepacked
structure. We then summarize the resultsconcerning
anewly
observedtype
offriction,
the «locking-unlocking
mechanism »,both for
prismatic slip
ofberyllium
andslip
inL12
ordered structures.Macroscopic
aspects
ofplastic
deformation such asstrength
anomalies,
creep activationenergies,
deformationstages
of the FCC metals are then discussed in terms of the above dislocation mechanisms.
2. Cross
slip
in FCC metals.The
elementary
process of dislocation crossslip
from acompact
plane
onto anothercompact
plane although frequently
observedexperimentally,
is a verypoorly
known process.The theoretical
aspects
of crossslip
have been studiedby Escaig
(1968 [10, 11]),
following
Friedel’s view. In his
model,
crossslip
occursthrough
the mechanism sketched infigure
1. It starts from aprimary
constriction on a screw dislocation. Under the influence of theapplied
stress aidedby
thermalactivation,
the two halves of the constriction areseparated
and,
assuggested by
Friedel(1956 [1],
1957[12]),
the dislocationsegment
betweenthem, splits
at once on the crossslip plane.
This model seems to be more realistic than the former one ofSchoeck and
Seeger
(1955) [4].
Inparticular,
Escaig
has shown that the processdepends
mainly
on the ratio of the width ofsplitting
under stress on theprimary
and the crossslip
planes.
This causes the process to be orientationdependent,
which will be discussed below.Fig.
1. - Successivestages of
cross-slip starting
at a constriction, in Friedel’s andEscaig’s
model[1, 10,
11].
The activation energy
AGcs
has been derived for weak effective stresses :with i = 1 or 2
depending
on how many constrictions are necessary to initiate the process ;bo
is the width of a recombined screwdislocation ; 1£
the shearmodulus, a
(i )
an orientationDo
the dissociation width at zero stress ; A is aslowly
variable function of IL,b,
f.
The activation volume of the process is :A new
experimental technique
has beendeveloped
toproduce
a burst of crossslip
at theyield point
[13] :
a coppersingle crystal
is deformed incompression along
[110]
to the end ofstage
II toproduce
ahomogeneous
dislocation forest. Newsamples
are then cut out of thiscrystal,
in asingle slip
orientation. The newprimary
dislocations areexpected
to crossslip
at theyield point
because of the numerous forest dislocationsacting
as obstacles. The tensioncompression asymmetries predicted by
themodel,
as well as the orientationdependence
ofthe critical stress for cross
slip,
are ingood
agreement
withexperimental
results obtained at roomtemperature.
As thetemperature
ischanged,
load relaxationexperiments
areperformed along
the stress strain curves to obtain activation volumes. Anexample
is shown infigure
2 for apredeformation experiment
at 473 K. The corrected activation volume exhibits aminimum as a function of strain. This
corresponds
to a value of about 300 atomicvolumes,
infairly
good agreement
withequation (2)
and the width ofsplitting
of copper. The stresscorresponding
to this minimum is then considered to be the critical stress for crossslip,
which is confirmedby slip
trace observations. The variation as a function oftemperature
of this critical stress and of thecorresponding
activationvolume,
is shown infigure
3[14].
The barrier energy for crossslip
in copper was estimated to be :AG§s
= 1.15 ± 0.37eV,
which falls between the two valuespredicted by equation
(1)
for i = 1 and 2respectively.
Animportant
conclusion is that after the above measurements, it became obvious that the TIII stress and its variation as a function oftemperature
are different from the critical stress forcross
slip
betweencompact
planes.
The aboveexperimental
results,
especially
the orientationdependance
of the critical stress for crossslip,
areclearly
in favor of Friedel’s andEscaig’s
views. Thecomparison
with the secondtype
oftheory
for crossslip
[4]
and[5]
hasalready
been
given
elsewhere[13].
Similar orientation effects have also been found inNi3Al
andinterpreted successfully using
theFriedel-Escaig
crossslip theory
[15].
Fig.
2. - Resolved shear stress and corrected activation volume as a function of resolved shear strain.Fig.
3. -Critical stress for cross
slip
andcorresponding
activation volume as a function of temperature in Cu. Crossslip
takesplace
at the macro elastic limit T between 250 and 410 K. v is the atomic volume[14].
3. Friction forces of the Peierls
type.
The
principle
of this kind of friction force is that the energy ofmoving
dislocationsnecessarily
variesaccording
to the latticeperiodicity.
Dislocations thus have their minimum energy in theso called « Peierls
valleys »,
and their movement can be described as a series ofjumps
betweenadjacent valleys, through
the nucleation andpropagation
of kinkpairs.
In the
early
model of Peierls andNabarro,
the dislocations are assumed tospread only
in theirglide planes.
This results in very low frictionforces,
especially
for dislocations which arelargely split
(case
ofglide
on the mostcompact
planes).
More recent studies have shown that even
larger
frictional forces canoriginate
when dislocationsspread
out of theirglide plane.
Under suchconditions,
the Peierls mechanism canplay
a veryimportant
role in theplasticity
ofmaterials,
even athigh
temperatures.
This is for instance the case ofL12
orderedalloys,
for which friction forces arepresent
up to 0.7Tm
(Tm :
melting
temperature).
These
higher
friction forces are found to concernmainly
screwdislocations,
which canspread
moreeasily
in differentplanes,
because of theirhigher symmetry
within thecrystal
lattice. In order to move the
dislocation,
it is necessary to recombine its core, which involves the same fundamental mechanisms as for crossslip.
The first ideas about this mechanism were
suggested by
Hirsch(1960) [16]
andYoshinaga
and Horiuchi(1963) [17]
for BCC and HCPmetals, respectively.
Detailedmodels,
based onthe recombination of dislocations dissociated into several
partials,
have been derivedby
Kroupa
(1963) [8],
Schottky
et al.(1965) [19],
Vitek(1966) [20]
andEscaig
(1968) [21].
Recent calculationsby Seeger
(1984) [22]
based onsophisticated
kink-kinkinteractions,
do not use anydescription
of the recombination process of dislocationsspread
out of theirglide
plane
(cross
slip
description).
The similitudes and differences between the
early
« classical » model of Peierls andNabarro,
and the modelincluding
thespreading
of dislocations out of theirglide plane
(sometimes
called« pseudo
Peierls » or « kinkpair
mechanism »)
have been discussedby
Friedel
(1968) [23].
The differences between this and the classical Peierls caseonly
concerndetails :
- the
- the
long
range interaction between kinksdepends
on the way the kinkslocally
affect thesplitting ;
- the active
applied
stresses are both in theslip plane
and in thesplitting planes
(«
Escaig
effect
»).
Experimental
data on the Peierls mechanism are summarized below.3.1 PEIERLS STRESSES IN BCC METALS. - The dislocation movement has been studied in situ
in a
high voltage
electronmicroscope by Furubayashi
(1969) [24]
andLouchet,
Kubin andVesely
(1979) [25].
The Peierls mechanism wasclearly
identified for the first timeby
therectilinear
shape
and the slow and smooth movement of the screws.3.2 PEIERLS STRESSES IN HCP METALS (PRISMATIC SLIP). - In the
case of
titanium,
whichglides
moreeasily
on theprismatic
than the basalplane,
the observations of Naka et al.(1988)
[26]
also revealstrong
frictional forces on screw dislocationsgliding
inprismatic planes.
This frictioncorresponds
to a nonplanar spreading
as in BCC metals.The Peierls mechanism has also been
clearly
identifiedby in
situ observations inmagnesium,
in whichglide
is easier on the basal than on theprismatic plane,
above roomtemperature
[27].
The tensile axis was chosenparallel
to the basalplane,
so that the latter wasunstressed and
prismatic
glide only
is activated. The dislocationbehaviour,
observed in a200 kV electron
microscope
corresponds
to a smooth movement of rectilinear screwdislocations,
unlike non screwportions,
whichglide
much faster(see
Fig.
4).
Fig.
4. -Dislocation
glide
in theprismatic plane
ofmagnesium.
Evidence of friction forces on screwdislocations a, f3 and y. In situ
experiment
120 kV, 300 K[27].
The
corresponding
mechanism is detailed infigure
5. Screw dislocations arespread
in the basalplane
andglide
in theprismatic plane by nucleating
andpropagating
kinkpairs.
More
clearly
than in BCCmetals,
it appears inmagnesium
that thegeneralized
Peierls mechanism involves crossslip.
In theconfiguration 5c,
screw dislocations areglissile
in thebasal
plane. Large amplitude
basal to and fro movements thus occur under internal stresses and add toprismatic
movements(Fig. 6).
Thisexperiment clearly
shows that screwdislocations
really
crossslip
between basal andprismatic planes during
the process.Quantitative
evaluations of the dislocation velocities as a function of stress andtemperature
yield
an activation area of 9b 2 at
roomtemperature
and an activation energy at zero stressFig.
5. - Schematicrepresentation
of a sctew dislocationgliding
on theprismatic plane
P of an HCPcrystal following
the kinkpair
mechanism. L = distance betweencompact rows
(L
=c/2).
Thehatched
portions
of the dislocation lie on the basalplane
(perpendicular
toP).
Fig.
6. -Wavy
movement of a screw dislocation(S)
inMg
(in
situ TEMexperiment
120kV),
20 °C. Arrows underline oscillations of the two dislocation traces,parallel
to the basal trace(B).
(b :
Burgers
vector).
From[27].
3.3 PEIERLS STRESSES IN FCC METALS (NON COMPACT SLIP). -
Although
these metals deformeasily by glide
on the octahedralplanes, slip
line observationslong
ago revealed thatglide
can also takeplace
on noncompact planes
(see
reviewby
Carrardet al.,
1987[28]).
In aluminium above
200 °C,
forexample,
these noncompact
planes
were of the{100}, { 110 } , {112} and {113}
type.
A detailedquantitative study
of {110}
slip
waselectron
microscopy
(TEM)
and showed that{ 110 }
slip
exists per se and is not the net result ofcomposite
slip
on {111}.
It was alsoshown,
through
constant strain rate tests, that{110}
slip
isthermally
activated. It startsoperating
above a criticaltemperature.
For lowstacking
fault energymetals,
thistemperature
is ahigher
fraction of the absolutemelting
point.
Thissuggests
that some kind of crossslip
process is involved in theoperation
of noncompact slip.
A detailed
study
of the mechanism related to(001)
slip
in 112 aluminiumsingle crystals
has been undertaken morerecently
[28] [30].
Although
thehigh symmetry
of the FCCcrystals
makes it
impossible
to neutralize théfour {111}
planes
at the sametime,
the[112]
orientation allows extensive[110] (001)
glide
to be activated(see
stereographic projection
ofFig.
7 andFig.
8).
Stress strain curves of different
shapes
are observed as a function of the activeslip system
(see
Fig.
9).
Ifcompact
slip only
isoperating,
a monotonic increase of stress is observed as afunction of
strain,
the curvesexhibiting
anapproximately parabolic shape.
If(001)
slip
operates,
the curves start with asteep
increase in stress and then exhibit asharp
decrease inhardening
rate. It could be established that the lattercorresponds
to the critical stressTooi at which
(001)
slip
startsoperating
for agiven temperature
and strain rate. The stressTooi was
plotted
as a function oftemperature
for different strain rates(Fig. 10).
It can be seenthat an athermal
plateau
is reachedslightly
above400 °C,
that TOO1 isstrongly temperature
dependent
below 400 °C and that it cannot be measured below 270 °C wherecompact slip
takes over. It waspossible
to measure anapparent
activationenthalpy
for(001)
glide,
AHOO,
= 1.74eV,
from the curves offigure
10.These conclusions where confirmed
by in
situexperiments
[28, 32]
andby
the observation oflong
straight
screw dislocationspinned
under load after creep of Al-Znsingle crystals
[31].
A
microscopic
mechanism of the Peierlstype
for(001)
slip
wasproposed taking
into account the abovemacroscopic
and microstructural observations. Itpresents
some similaritieswith the
preceding
mechanism in HCPmetals,
and caneasily
be extended to othertypes
ofFig.
7. -[112]
stereographic projection.
(Pl, bl)
and(p2, b2)
are theprimary
octahedral systems.Fig.
8. - Two 90° views of a[112]
aluminiumsingle crystal
after deformation at 314 °C withy = 12 x
10- 4 s-1.
(001)
and { 111 }
slip
systems are activated in the tworegions
1 and II,respectively
[30].
Fig.
9. - Stress-strain curves at different temperatures in[112]
aluminiumsingle crystals :
y = 12 x
10- 4 S-I.
When(001) glide
is activated, the critical stress is indicatedby
an arrow[30].
non
compact systems.
It considers the motion on(001)
of screwdislocations,
which arenormally
dissociated oncompact
planes,
as the ratecontrolling
process. Under theapplied
stress, the dislocation recombines over acritical length
toglide
on(001).
Under low stresses,Fig.
10. - Variation in the CRSSTwi for
(001)
glide
with temperature for three strain rates in[112]
aluminiumsingle crystals :
(+) y = 12 x 10’ s’ ;
(8)
= 12 x 10- 4 s-1;
(0)
=12 x 10- 3 s-1.
The curves
correspond
to thekink-pair
model[30].
screws which was evidenced
above,
indicates that the kinkpair propagation
is easier than itsnucleation.
Analysis
of the curves offigure
10 in terms of the rateequation
of § 3.4 belowyielded
avalue of the activation energy at zero stress of
AGooi
= 1.40 eV.It can also be seen in
figure
10 that theagreement
betwen the rateequations
and theexperimental
data issatisfactory,
at least in the 150 °Ctemperature
interval over which(001)
glide
could be observed.Finally,
the rateequations
have been used to estimate the athermaltemperature
for{ 110 }
slip
in various FCC metals[30].
This agreesreasonably
well withexperimental
values[33].
3.4 COMMON FEATURES OF THE GENERALIZED PEIERLS MECHANISM. - These can be summarized as follows :
- mechanical
properties
areclosely
related to individual dislocation mobilities and coregeometries
(see Fig. 11) ;
- the
corresponding
screw dislocations arestraight
asthey
movesmoothly
andcontinu-ously ;
- there
are intensive
multiplication
processes,through
the formation anddevelopment
of closedloops
(see
Ref.[27]
formagnesium) ;
- the
velocity
of screwdislocations,
as derivedby Escaig
[11]
under low effective stresses,2
AGp
is
given by : v
= a v(
b
L
exp -20132013 ,
where the critical distance between two kinks islc-
kit1/2
lc
=(
R 1l2
,Lb/2
7TT*; v
is theDebye frequency,
âge
is the activation energy forÎ
J-Lb2
Peierls
glide,
R the recombination energy per unitlength
ofdislocation,
T * the effective stressand g
is the shear modulus. Thevelocity
of dislocations isproportional
to theirlength
L,
which has beendirectly
verified in the case ofmagnesium
[27] ;
-
the activation energy can be
expressed
as :AGp
=AGp -
T *V,
whereAG’
equals
twicethe kink energy, i.e.
G; ’" 2 L’ (J-Lb2 R)1/2 + 2 U
(U
= constriction energy, L = distanceFig.
11. -Comparison
between theFriedel-Escaig
mechanism in BCC and HCP metals. The screwdislocation is seen end-on.
- the activation
area A is of the order of b .
fc
and is small. Thisimplies
astrong
increaseof the elastic limit at low
temperatures,
whichexplains why
noncompact slip
cannot be observed in FCC metals at lowtemperature ;
- because of the
complex
coresplitting
and theEscaig
effect,
Schmid law is oftenviolated,
as in the case of
simple
crossslip
of § 2. Someaspects
of thisproblem
have been discussed fornon
compact slip
in aluminium[30].
4. The
locking-unlocking
mechanism.This new mechanism has been
experimentally
detected on the basis of in situexperiments
onprismatic slip
ofberyllium
for the first time[34, 35].
It appears to beoperative
in many different structures.As in the case of the
generalized
Peierlsmechanism,
a screw coresplitting
occurs out of theglide plane.
However,
a metastableglissile
coreconfiguration
exists,
which allows freeglide
over several interatomic distances before the dislocation is lockedagain.
The fundamentalidea at the
origin
of the Peierlsmechanism,
i.e. thenecessity
of aperiodic
variation of thedislocation energy
according
to the latticeperiodicity,
is then lost.4.1 BERYLLIUM. - The mechanism was first
suggested by Régnier
andDupouy
(1970) [36]
and thenexperimentally
studied andfully
described,
in the case of theprismatic glide
ofberyllium
[34, 35].
The screws exhibit ajerky
movement(Fig. 12),
at variance with the Peierls mechanism. It is sketched infigure
12. It can be shown that theglissile configuration
in theprismatic plane
is metastable and ofhigher
energy than the sessileconfiguration spread
in the basalplane.
It thus appears that dislocations have a « fundamental state » which is theonly
one observed under static conditions and « excited states » of short
lifetime,
which can beobserved under
dynamic
conditionsonly.
Unlocking
andlocking correspond
to twoelementary
crossslip
processes. The first is crossslip
to aplane
ofhigher
energy. Thedescription
of Friedel[1,
3,
7]
leads to lower activationFig.
12. -Locking-unlocking
on screw dislocations inprismatic glide
ofberyllium
at 300 K.a)
toe) :
in situ sequenceillustrating
thejerky
movement of the screws. Schematicrepresentation
of theunlocking
process
f)
toh)
and of thelocking
processi)
tok).
From[34, 35].
study
of thewaiting
times of locked dislocations has beenmade,
which leads to asingle
value for theprobability
ofunlocking
per unittime,
at agiven
stress andtemperature
(Fig. 13).
In the same way, the statistics of thejump lengths
leads to a constantprobability
oflocking
per unit time. Theseprobabilities
are observed to varyaccording
to the stress and thetemperature,
inagreement
with the crossslip
models.When the
temperature
increases,
theprobability
oflocking
increases and thelength
of thejump
thusdecreases,
until it becomesequal
to one interatomic distance(Peierls mechanism).
Reciprocally,
a Peierls mechanism can bereplaced by
thelocking-unlocking
mechanism at lowertemperatures,
provided
a metastableglissile
configuration
exists. This has been demonstratedrecently
in the case ofmagnesium
below 200 K[37].
The Peierls mechanismthus appears,
surprisingly
as a« high temperature »
mechanism,
withrespect
tolocking-unlocking.
Locking-unlocking
being really
a crossslip
mechanism,
thiscontinuity again emphasizes
theimportance
of the crossslip description
of the Peierls mechanism.4.2
Ni3Al.
- InFig.
13. - Data about screw dislocations in thelocking-unlocking glide
process in Be.a)
andb),
waiting
time measurements in the lockedconfiguration.
AN is the number of screwdislocations
waiting during
time t, to tB +AtB.
(a)
linear scaleillustrating
anexponential
decrease ; and(b)
semilogarithmic
scale.Slope
=PUL
= 3.5 s-1.c)
andd),
jump length
measurements(proportional
to theflight
time)
in the unlockedconfiguration.
AN is the number of screw dislocationsjumping
over a distance À to À + AÀ.(c)
linear scaleillustrating
an
exponential
decrease ; and(d)
semilogarithmic
scale, thereciprocal
of theslope
is À = 0.068 >m.From
[35].
Fig.
14. -In the case of
glide
in {100}
planes,
core structurecomputations
[40]
lead to aconfiguration
of minimum energy with the APBin {100}
and eachsuperpartial spread
in oneof the two
possible
intersecting {111}
planes
(Fig. 15).
Weak beam andhigh
resolution observations of dislocation cores[41]
confirm thissplitting
geometry.
Tointerpret
theobserved
jerky
movements,by analogy
with the case ofberyllium,
it is thus necessary to assume that a secondconfiguration
ofhigher
energy,glissile
andspread
in the{ 100 }
plane,
existsduring
very short times(Fig. 15).
The movement is thusinterpreted
as a series of crossslip
events between these twoconfigurations,
as in HCP metals. Thishypothesis
is confirmedby
thewaiting
times andjump
lengths
measurements, whichobey
the same law as inberyllium
[38].
In the case of
glide
in{ 111 }
planes,
thelocking-unlocking
movement isinterpreted
in asimilar way, with a stable sessile
configuration spread
intothé {111}
crossslip plane
and ametastable
glissile
configuration spread
inthé {111}
glide plane
[39].
Fig.
15. -Schematic
configuration
of the core dissociation of a screwin {100}
planes
of theLl2
structure. 1 = metastableconfiguration
(planar
=glissile).
2 and 2’ = stableconfiguration
(non
planar
=sessile).
4.3 COMMON FEATURES OF THE LOCKING-UNLOCKING MECHANISM. - The
common features
of the
generalized
Peierls mechanism alsoapply
tolocking-unlocking, except
for thefollowing
points :
- the movement of dislocations is
no
longer
smooth andcontinuous,
butjerky ;
- their
velocity
is v = v VPUL
where
v is
the instantaneousvelocity
in theglissile
0 PL
0configuration
andPuL
andPL
are theprobabilities
ofunlocking
andlocking, respectively.
P uL
andP L
can beexpressed
as :and thus :
independent
of the dislocationlength
L.-
The activation energy is the difference between the activation
energies
of the two cross(except
for veryhigh
stresses)
which leads to a smaller elastic limit increase atdecreasing
temperatures.
5. The
origin
ofstrength
anomalies.Several
materials,
including beryllium
inprismatic glide
andL12
orderedalloys,
exhibit ananomalous flow stress increase at
increasing temperature.
The most current models for this behaviour are based on thethermally
activated and irreversiblelocking
of dislocationsby
cross
slip
[36, 42].
Thiscorresponds
to the firststep
only
of thelocking, unlocking
mechanism. Astudy
of theglide
of dislocations inprismatic planes
ofberyllium
reveals a behaviourwhich is at variance with this
prediction,
sincelocking-unlocking
is observed over the whole,
temperature
range,including
the domain of the anomalous flow stress increase[34, 35].
Theorigin
of thestrength anomaly
is thus an increase in thedifficulty
of crossslipping
as thetemperature
rises due to an increase of the recombination energy R. In the elasticapproximation,
this wouldcorrespond
to a decrease of thestacking
fault energy as thetemperature
is increased. Similar behaviour has also been observed in a nickel basedalloy
[38],
in the case ofglide
in {100}
planes,
and the same mechanism could also be at theorigin
of thestrength anomaly
ofNi3Al,
in the caseof {111 }
glide
[39].
It can also account for thethermally
activated dislocation motion evidenced at thestrength anomaly
[43].
It is clear that since all crossslip
mechanisms are very sensitive to the recombination energyR,
i.e. thestacking
fault energy, thepossible
temperature
variation of theseparameters
should be included in the models.6.
Creep
at intermediate andhigh
temperature.
The variation of the creep activation
energies
withtemperature,
as reviewedby
Poirier in pure FCC and HCP metals[44],
suggests
that different mechanisms are ratecontrolling
in differenttemperature
domains(see Fig. 16).
In the case of aluminium and FCCmetals,
theFig.
16. -Creep
activationenthalpies
measuredby Sherby et
al.(1957)
in aluminiumpolycrystals
[50].
The results obtained in[112]
single crystals
between 200 and 320 °C are alsoreported
for 001glide
plateau
of activation energy at intermediatetemperature
has been attributed to crossslip
(Friedel [3],
Lytton
et al.[6]),
while thehigh temperature
range has been considered to be climb controlledthrough
self diffusion.Conversely,
for HCPmetals,
the intermediatetemperature regime
was attributed to selfdiffusion,
while thehigher
activation energy in thehigh temperature
domain wasthought
tocorrespond
to dislocation crossslip
from the basal to theprism plane
[44].
More recent detailed models have been
proposed
forcross-slip-controlled
creep mechan-isms. Friedel(1977) [45]
suggests
that creep is controlledby
the dissociation of dislocationsalong
theplane
of thenetwork,
their escapenecessarily
involving
cross-slip
to the morehighly
stressed
glide
plane.
Poirier[46]
considers that the creep rate is controlledby
a recoverymechanism inside the
subgrains :
this can occur eitherby
the annihilationthrough
crossslip
ofthe screw
portions
of theloops
at intermediatetemperature,
orthrough
climb of theedge
portions
athigher temperatures.
These
suggestions
can now bepursued
in more detail thanks tonewly
available transition electronmicroscope
observations.6.1 ALUMINIUM (AND THE Al-Zn SOLID SOLUTION) AT INTERMEDIATE TEMPERATURES. -Strain is associated with the
glide
of dislocationsescaping
from subboundaries[47],
which necessitateshigh
local internal stresses.They
have been measureddirectly
[48]
andthey
originate
in thesubboundary migration
process[49].
The creep rate is thus controlled
by
theglide
of some of thesubboundary segments
on{001}
planes
and the activation energycorresponds
to the energy of one kink in{001} (see
Fig.
17)
with a value at zero stressAGO -
0.7 eV. This is in reasonableagreement
with theenthalpies
offigure
16,
after theentropy
correction has been made[50].
Fig.
17. - Schematicrepresentation
of thesubboundary migration
process.a)
xi(i
= 1, 2,3)
are the 3dislocation families of the
subboundary
mesh.b,
are theirrespective burgers
vectors,Pi
thererespective
glide planes.
b)
Onset ofmigration
while the screw segment xiglides
on(100).
From[49].
6.2 ALUMINIUM AT HIGH
TEMPERATÙRE. -
The creep rate is controlledby
noncompact
slip
of screw dislocations across the
subgrains
at least at the onset of thehigh
temperature
domain. This issupported experimentally by
the observation oflong
rectilinear screwdislocations,
which were
pinned
under load at the end of the creep test in an Al-Zn solid solution(see
Fig.
18. -Straight
screw dislocation substructure after creep. Al-11 wt. % Znpolycrystal.
T =250 ’C, o,
= 17 MPa, e = 22 %. Dislocations arepinned
under load[48].
6.3 MAGNESIUM AT INTERMEDIATE TEMPERATURE. - The results of the in situ
experiments
described in § 3 lead to activation energy values forprismatic glide,
that are notcompatible
with those measured in creep athigh
temperatures.
The creep mechanism athigh
temperatures
is therefore notyet fully
understood.However,
at intermediatetemperatures,
figure
19 shows that the activation energy values forprismatic glide
as a function oftemperature
arecompatible
with those measured in creep[27].
Prismaticslip
can therefore bean alternate mechanism for creep at intermediate
temperatures.
Fig.
19. -Comparison
of activationenthalpies
inmagnesium,
for creep ofpolycrystals
and forprismatic
7. Déformation
stages.
In face centred cubic metal
single crystals,
three deformationstages
on the stress strain curveshave been evidenced at
temperatures
below orequal
to roomtemperature
(Friedel, 1956 [1]
and 1959
[3]).
Asalready
discussed in §2,
recentexperimental
information about crossslip
in copper shows that the critical stress for this mechanism isclearly
different from Tjjj, as well as its variation with thetemperature
[14].
Crossslip
isprobably
activeduring
stage III,
but mixedtogether
with other mechanisms such as the destruction of sometypes
ofjunction
reactions[51].
However,
atlarge
strains and roomtemperature,
astage
IV isobserved,
which ischaracterized
by
a new linearhardening [52].
Athigher
temperatures, stage
IV has also beenobserved in covalent materials
[53].
The same authors have detected a similar behavior in facecentered cubic
metals,
by analysing previously published
stress strain curves on Al[54]
and onAu
[55].
In a recentstudy
of[112]
coppersingle crystals
above 200°C,
it has been shown thatstage
IV is alsopresent,
and followedby
additionalstages
[56].
A careful examination of theslip
traces has shown that the onset ofstage
IVcorresponds
to the activation of noncompact
slip
which itself involves crossslip
(§ 3.3).
8. Conclusions.
In this
review,
we haveattempted
to show how realistic ideas about basic crossslip
mechanisms,
which were formulated aboutthirty
years ago, are stillenlightening.
This isquite
remarkable
nowadays,
as thegeneral
tendency
is toignore
the literature which is more than ten years old.These ideas stimulated the
complete
derivation of the crossslip
mechanism when thedislocation is dissociated in the
glide plane
or out of it.Later,
experimental
data wereproduced, mostly
based on in situ observations in the electronmicroscope
and accurate mechanical tests.They
have confirmed the crossslip
model both in copper and inmagnesium
oriented for
prismatic glide.
In these two cases, realistic values of activationenergies
and volume values have been obtained. The kinkpair
mechanism forprismatic glide
could also be extended with success to noncompact
slip
in aluminium. Intermediate andhigh temperature
domains have been determined for which the cross
slip
mechanisms seem toimpose
well established creep activation energy values. A new mechanism oflocking-unlocking
of the screws has been evidencedexperimentally.
The latter seems to be rather common, the kinkpair
mechanismbeing
aspecial
case. It accounts foryield
stress anomalies in avariety
ofsituations such as
prismatic slip
inberyllium,
titanium,
etc... and in theNi3Al
compound
oriented for 111 or 001slip.
The amount of work needed to
complete
the above results isquite large.
In the FCCstructure, cross
slip
should beexperimentally
studied incrystals
with variousstacking
faultenergies ;
the same remark holds for noncompact slip
on variousplanes.
This will allow abetter check of the models. In
prismatic
glide
of HCPcrystals
and in theL12
structures,accurate mechanical tests should be
performed
to detectmacroscopic
evidence of thelocking-unlocking
versus kinkpair
mechanism. The connection between the former mechanism andyield
stress anomalies should be better established incrystals
other thanberyllium.
Acknowledgements.
The authors
acknowledge stimulating
discussions with Dr. P. W. Hawks about this paper.They
thank Fonds National Suisse de la RechercheScientifique
for the financialsupport
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