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CREEP DEFORMATION MODELLING OF SUPERALLOY
SINGLE CRYSTALS
J. SVOBODA{ and P. LUKAÂ SÏ
Institute of Physics of Materials, Academy of Sciences of the Czech Republic, ZÏ izÏ kova 22, CZ-61662Brno, Czech Republic
(Received 15 January 1999; accepted 22 February 2000)
AbstractÐA model of creep deformation in arbitrarily oriented nickel-base superalloy single crystals hasbeen developed. This model extends the preceding model of the present authors [Svoboda, J. and Luka sÏ ,P., Acta mater., 1998, 46, 3421] covering the case of creep in h001i oriented crystals. The calculated creepcurves were compared with the creep curves of single crystals CMSX-4 of the orientations h001i, h011i andh111i measured at 7508C; a fair agreement was found. 7 2000 Acta Metallurgica Inc. Published by ElsevierScience Ltd. All rights reserved.
Keywords: Superalloys; Creep; Di�usion; Dislocations; Theory & modelling
1. INTRODUCTION
Superalloy single crystals have been used up to now
for production of critical parts of aero-engine gas
turbines. They are now considered also for use in
industrial gas turbines in order to achieve the
required increase in working temperature. The
behaviour of the superalloy single crystals is highly
anisotropic. Several experimental studies have
shown that the creep resistance depends strongly on
crystal orientation [1±7]. In the majority of studied
cases the orientation h001i has the highest creep re-
sistance. Nevertheless, this is not a generally valid
rule. For example, MacKay and Maier [1] found
for MAR-M247 and MAR-M200 single crystals
tested in the temperature range 760±7748C that the
rupture life was longest for h111i orientation, some-
what shorter for h001i orientation and shortest for
h011i orientation. On the other hand, Caron et al.
[3] found for CMSX-2 single crystals tested at
7608C considerably shorter creep lives for h111iorientation than for h001i orientation. Later they
showed [8] that the creep life of h111i oriented crys-
tals is highly dependent on the size of the g ' precipi-tates, while the creep life of h001i oriented crystals
depends on the size of g ' precipitates weakly. The
creep life of h111i crystals can be longer or shorter
than that of h001i crystals in dependence on the g 'particle size. Several papers show a drop in creep
rupture lives for crystals having orientation near to
h001i with increasing misorientation from the exact
h001i orientation. For example, Sass et al. [2] tested
CMSX-4 single crystals at 8008C under a constant
stress of 767 MPa. The longest lives were reached
by crystals with an orientation in close proximity of
[001]. With increasing misorientation from [001] the
creep strength dropped signi®cantly, with crystals
having an orientation close to the [001]±[011]
boundary of the standard stereographic triangle
exhibiting longer lifetimes than crystals having an
orientation closer to the [001]±[111] boundary.
Generally, it can be stated that the ranking of
orientations from the point of view of their creep
resistance depends on stress and temperature [7]
and on the size of the g ' precipitates [8].The proposed semi-phenomenological models of
creep in the superalloy single crystals are based
either on visco-plastic ¯ow of the softer matrix
around the hard particles or on crystal plasticity
assuming slip activity not only on octahedral slip
systems, but also on other types of systems. These
models do not consider the basic mechanisms active
during the creep process; their success in describing
the creep anisotropy is only partial [9±12].
In our preceding paper [13] we have proposed a
model based on the basic mechanisms for h001ioriented single crystals. In that paper it was shown
that the complicated creep curve is a result of inter-
action between the deformation processes and the
evolution of morphology of the g ' particles. The
aim of this paper is to present an extension of the
model for arbitrarily oriented crystals crept at low
Acta mater. 48 (2000) 2519±2528
1359-6454/00/$20.00 7 2000 Acta Metallurgica Inc. Published by Elsevier Science Ltd. All rights reserved.
PII: S1359 -6454 (00 )00078 -1
www.elsevier.com/locate/actamat
{ To whom all correspondence should be addressed.
temperature and to compare the theoretical creepcurves with the experimentally determined ones for
the temperature of 7508C on CMSX-4 single crys-tals.
2. DESCRIPTION OF THE MODEL
First of all it is necessary to list the mechanismswhich are dominant during creep of CMSX-4 singlecrystals at 7508C. It is generally accepted that the
creep deformation starts by generation and glide ofdislocations of the type {111}h110i in g channels.Without co-operation with other mechanisms this
mechanism can cause plastic deformation in the gchannels of the same order as the mis®t d and thusthe plastic deformation of the whole crystal up to0.1%. Without dynamic recovery the process of
plastic deformation would stop at this level. Thereare two possible mechanisms of the dynamic recov-ery.
(i) The dislocations overcome the g ' particle bycombination of slip and climb; the dislocationloops annihilate in the vicinity of the apices of
the g ' particle.(ii) The dislocations or their reaction productscut through the g ' particle and then either an-
nihilate with the dislocations on the opposite g/g ' interface or they cut through the next g ' par-ticle.
In our preceding paper [13] the creep curves forthe orientation [001] could be well simulated by themechanism (i). This mechanism does not change the
shape of the g ' particles; during plastic deformationthe vertical g channels get narrower and thus thefurther plastic deformation becomes more di�cult.This results in the experimentally observed dramatic
decrease of the creep rate by two orders of magni-tude and the transition from quick creep to slowcreep. Modelling using the mechanism (i) success-
fully describes this transition [13]. Application ofthe mechanism (ii) did not lead to any hardening.Such a hardening could be explained only by a
change of cutting mechanism during transition fromquick to slow creep [14]. Sass et al. [5] studied themechanisms of creep in CMSX-4 single crystals at8508C. During creep of single crystals mainly with
the orientations near to h011i they identi®ed cuttingof the g ' particle by partial dislocation a=3�211�which left another partial dislocation a=6�211� onthe g/g ' interface and a superlattice stacking fault inthe g ' particle. After creeping h011i crystals to thestrain of 1.8% one to two cutting events were ident-
i®ed in each g ' particle; this corresponds to plasticdeformation of the g ' particle by less than 0.1%.Thus, there must be a dominant recovery mechan-
ism which does not leave traces; this is most prob-ably the mechanism (i) described above. Moreover,Sass et al. [5] observed only very infrequent cuttingfor the orientation h001i and practically no cutting
for the orientation h111i. This strongly supports theassertion that the mechanism (i) is dominant for all
the orientations. Cutting by the dislocation pairs,which was also observed in Ref. [5], is dominant athigh temperatures. It can, therefore, be expected
that it is not dominant at 7508C. In the modelling,the following mechanisms will be taken intoaccount.
1. Dislocation slip in g channels and concurrentmultiplication of dislocations. These dislocationsremain deposited on the g/g ' interfaces.
2. Dynamic recovery of the dislocation structure.The dislocation loops spanning around the g 'particles move by the combination of slip and
climb along the g/g ' interfaces and shrinktowards the apices of the g ' particles.
3. Morphological changes of g ' particles by mi-gration of g/g ' interfaces.
The preceding model assumed tensile stress in thedirection [001] and made use of considerable sym-metry of the case of the [001] oriented crystals. In
the general case the degree of symmetry is lower,the model will have to be more complicated andwill contain more parameters. To describe the
actual state of the structure in the [001] case it wasnecessary to use three parameters concerning dislo-cation density on the g/g ' interfaces and four par-
ameters describing the dimensions of the unit cell.
2.1. Speci®cation of the structure parameters
As well as in the model for h001i oriented crys-tals, also in the presented general model we assume
that only octahedral slip systems {111}h110i areactivated in the g channels. There are 12 slip sys-tems determined by the normalized vector of theslip direction aK � h110i=
���2p
and the normalized
vector of the normal to the slip plane cK �h111i= ���
3p: We shall distinguish between the g chan-
nels normal to x, y and z directions; that is why we
must consider 36 parameters characterizing densityof dislocations deposited on the g/g ' interfacesrs,K �s � x,y,z�:
Fig. 1. Scheme of the unit cell.
2520 SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS
The morphology of the unit cell can be describedby the dimensions of the g ' particle Lx, Ly, Lz and
by the thickness of g channels hx, hy, hz (Fig. 1).The g channels are deformed plastically and thechannels and the precipitates are mutually shifted
along the interfaces due to recovery. For the gchannel normal to the x axis the plastic strains ofthe channel ex,12, ex,13 and the shifts along the g/g 'interfaces wx,2, wx,3 must be introduced for the fulldescription of the morphology. Analogous par-ameters must be introduced for the g channels nor-
mal to the y and z axes. Thus altogether 54independent parameters are needed to describe thestructure of the unit cell. The stress and elasticstrain components in the g channels and in the g 'particles can be considered as dependent par-ameters, which can be evaluated from the appliedstress, mis®t parameter, elastic constants and struc-
ture parameters.
2.2. Stress±strain analysis
Altogether there are 24 (6 in the g ' particle and 3� 6 in the g channels) stress and 24 elastic strain
components in the unit cell. Thus, 48 equations areneeded for their evaluation. Hook law represents 24equations (similar to equations (20)±(26) in Ref.
[15]); the elastic constants c11, c12, c44, c '11, c '12 andc '44 have to be employed. Let us consider equili-brium conditions between the applied stress and theinternal stresses for cross-sections marked in Fig. 1.
For each cross-section we get one equation for thenormal components (similar to equation (16) inRef. [15]) and two equations for the shear com-
ponents. A further four cross-sections are normal tothe x and z axes. For all the cross-sections weobtain 18 equations altogether. However, three
couples of the equations for shear components inthe cross-sections of type No. 2 in Fig. 1 are identi-cal for the initial state with the cubic symmetry and
very similar in the deformed state. That is why eachcouple of these equations was summed and con-sidered as one equation. As a result, the equilibriumcondition o�ers 15 equations. The remaining nine
equations are the contact conditions on the g/g 'interfaces analogous to equations (13)±(15) in Ref.[15]. For the g/g ' interface normal to the x axis it
holds that
ex,ij ÿ eP,ij � d dij ÿX12K�1
rx,KbK,ij �1�
where ij � 22, 33, 23 and
bK,ij � 1=2�aK,icK,j � aK,jcK,i �: �2�
Two further triplets of equations for the g/g ' inter-faces normal to the y and z axes can be obtained ina similar way. The set of 48 linear equations for 48unknown stress and elastic strain components can
be solved. Fortunately, the set can be analyticallypre-solved; the remaining set, which has to be
solved numerically, consists of six equations.
2.3. Calculation of the total energy of the system
To be able to calculate the kinetics of the recov-ery and of the migration of the g/g ' interfaces, it isnecessary to calculate the total energy of the system(of the unit cell) as a function of the state par-ameters and the applied stress. The total energy
consists of the elastic energy, the energy of depos-ited dislocations and the potential energy of theloading system. The elastic energy can be calculated
from the stress and elastic strain componentsobtained. The energy of dislocations can be calcu-lated from the dislocation densities rs,K (see
Appendix A.2). The energy of the loading system isgiven by the tensorial product of the applied stresssapp,ij and the total strain of the unit cell �eij multi-plied by the volume of the unit cell. The total strain
component �e11 is given by
�e11 � ln
� �Lx � hx ��L0 � h0 � �1� �e11 �
��3�
The components �e22 and �e33 can be calculated in asimilar way. The component �e12 is given by
�e12 � ln
�wx,2 � wy,1 � hxex,12 � hyey,12
2�L0 � h0 � �1� �e12 ���4�
The components �e13 and �e23 can again be calculatedin a similar way. The components of the mean elas-tic deformation �eij are given by
�eij �ÿVPeP,ij � Vxex,ij � Vyey,ij � Vzez,ij
�ÿVP � Vx � Vy � Vz
� : �5�
2.4. Dislocation slip in the g channels
Now we can assume that the stress tensor is
known in each g channel. For the Kth slip systemthe resolved shear stress in the g channel normal tothe x axis is given by:
tx,K �X3i,j�1
sx,ijbK,ij �6�
Part of the energy released by slip is deposited inthe form of the energy of dislocations on the g/g 'interfaces. This results in the threshold stress tx,K0(see Appendix A.2). Then, following the lines of lin-ear thermodynamics of irreversible processes, the
rate of dislocation slip is proportional to �tx,K ÿtx,K0� and to the dislocation density at the g/g ' inter-faces corresponding to the slip system. The slip ratecan be expressed by:
SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS 2521
_gx,K �Wÿrx,K � ry,K � rz,K
��tx,K ÿ tx,K0 � �7�
The rate of deposition of dislocations is pro-portional to the slip rate and can be expressed byequation (8) (analogous to equation (6) in Ref.
[15]):
_r�1�x,K � _gx,K
��������2=3pb
: �8�
The total rate of the plastic deformation in the gchannel is given by
_ex,ij �X12K�1
_gx,KbK,ij �9�
and the change of the width of the g channel isgiven by:
_h�1�x � hx_ex,11: �10�
The upper index in parentheses denotes the serialnumber of the mechanism contributing to thechange of the parameter. This index is omitted
when only one mechanism operates. The slip in theg channels normal to the y and z axes can bedescribed analogously.
2.5. Dynamic recovery
Recovery requires motion of dislocations alongthe g/g ' interfaces. Let us consider dislocations onthe g/g ' interfaces corresponding to one slip system.
Interfaces of one orientation are occupied by screwdislocations, while interfaces of the remaining orien-tations are occupied by mixed dislocations. Thescrew dislocations can move along the interface by
combination of cross-slips. The motion of themixed dislocations is possible only if layers ofatoms are deposited and collected on interfaces
with di�erent orientations. Jogs on dislocations pro-duced by thermal activation act as the only sourcesand sinks of vacancies. The jogs can be considered
to be ideal point sources or sinks of vacancies.During the recovery the vacancies must be emittedby the jogs on interfaces of one orientation, trans-ported by di�usion and absorbed by jogs on inter-
faces of the other orientation. The areal density ofjogs on the g/g ' interfaces is decisive for the rate ofrecovery. It is not important whether the dislo-
cations mutually interact or form the network.The kinetics of recovery can be calculated in the
same way as in Ref. [13]. Di�usion connected with
the recovery dissipates the total energy of the sys-tem and the amount of the dissipated energy mustbe equal to the amount of the energy released in
the system due to recovery. In Ref. [13] the rate ofenergy dissipation is expressed by equation (16).The ®rst two terms in the equation correspond toradial ¯uxes around jogs; the third and the fourth
terms correspond to the transport of vacancies inthe g channels. For typical values of p120b and
r110ÿ7 m the ®rst two terms dominate. Thismeans that the recovery is controlled by the di�u-sive transport of vacancies in the area surrounding
jogs. This enables the energy dissipation connectedwith the transport of vacancies in g channels to beneglected and assumes that the recovery processes
in individual slip systems are mutually independent.In the preceding papers [13, 15] it was proved
that the recovery decreases the dislocation densities
rx,K, ry,K, and rz,K by the same amount DrK. Thenit is possible to calculate the value of ÿDE=DrK nu-merically. This value represents the driving forcefor the recovery. It is necessary to stress that DrKcauses the changes in thickness of g channels, causesshifts along the g/g ' interfaces and in¯uences thecontact conditions at the g/g ' interfaces. All these
changes must be involved in the calculation of DE.In the ®nal form the rate of change of dislocationdensities owing to recovery is given by:
_r�2�x,K � _r�2�y,K � _r�2�z,K �DEDrK
2pDOL30kTpb
� bK,11Lx
rx,K� bK,22Ly
ry,K� bK,33Lz
rz,K
!ÿ1: �11�
The change in the thickness of the g channel isgiven by:
_h�2�x �
X12K�1
bK,11Lxb _r�2�x,K: �12�
Shifts along the g/g ' interfaces caused by the recov-
ery can be expressed by:
_wx2 �X12K�1
bK,12Lxb _r�2�x,K �13�
_wx3 �X12K�1
bK,13Lxb _r�2�x,K: �14�
For the y and z directions the correspondingequations are analogous.
2.6. Migration of g/g ' interfaces
The physical substance of the migration of g/g 'interfaces leading to the morphological changes insuperalloys is described in detail in Ref. [13]. In the
present model we assume that the g ' particle canchange its shape with two degrees of freedominstead of only one as shown in Ref. [13].
Migration of the g/g ' interfaces is a di�usion-con-trolled process dependent on temperature andapplied stress. At temperatures above 9008C therate of migration is very high and the migration
2522 SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS
leads to rafting. At 7508C the rate of migration issubstantially slower, but nevertheless it plays a role
in the creep process. For example, in h001i orientedcrystals a deformation of 20% would completelyclose the vertical g channels if the g ' particles were
perfectly rigid. It is just the migration of the g/g 'interfaces which keeps the vertical g channels openduring the slow creep. The change in width of the
vertical g channels is at most several tens of percent. This cannot be experimentally measuredowing to the inherent irregularity of the distribution
of the g ' particles in the CMSX-4 single crystals.The rates of migration _Dx, _Dy, and _Dz normal to
the g/g ' interfaces are bound by the condition ofvolume conservation:
_Dx
Lx�
_Dy
Ly�
_Dz
Lz� 0 �15�
The rate of energy dissipation due to di�usion ofatoms connected with the migration of g/g ' inter-faces is given by:
RM � kTL60
12DjO
24� Ly
hxLz� Lx
hyLz
� _Dx
Lxÿ
_Dy
Ly
! 2
��
Lz
hxLy� Lx
hzLy
� _Dx
Lxÿ
_Dz
Lz
! 2
��
Lz
hyLx� Ly
hzLx
� _Dy
Lyÿ
_Dz
Lz
! 235 �16�
The substitutions
U � Dx
Lxÿ Dy
Lyand V � Dx
Lxÿ Dz
Lz�17�
enable the number of kinetic variables to bereduced to two and the rate of energy dissipation
gains the form:
RM � kTL6
12DjO
"�Ly
hxLz� Lx
hyLz
�_U2
��
Lz
hxLy� Lx
hzLy
�_V2
��
Lz
hyLx� Ly
hzLx
�ÿ_Uÿ _V
� 2# �18�
The rates U.and V
.can be calculated from the set of
two linear equations of motion for the system:
ÿ @E@U� 1
2
@RM
@ _Uand ÿ @E
@V� 1
2
@RM
@ _V�19�
The partial derivative @E=@U was calculated nu-merically as DE=DU keeping DV � 0: DU causeschanges in the dimensions of Lx, Ly, Lz and hx, hy,
hz. This is the reason that the total energy E ischanged. @E=@V is calculated analogously. After U
.
and V.are evaluated, the values of _Dx, _Dy, and _Dz
can be expressed. The evolution of the morphologyof the system is then given by:
_Lx � _Dx, _h�3�x � ÿ _Dx, _Ly � _Dy,
_h�3�y �ÿ _Dy, _Lz � _Dz,; _h
�3�z � ÿ _Dz �20�
2.7. Calculation of creep curves
The coordinates in the preceding calculations are
identical with the crystal directions of the typeh001i. The applied stress has to be expressed in thiscoordinate system. Then the evolution of the state
parameters (the relevant equations for individualcontributions are given in previous paragraphs) canbe calculated by integration in time. From the ten-
sor of the total strain given by equations (3) and (4)it is then possible to calculate the component of thetotal strain in the direction of the uniaxial appliedstress. This is the sought value.
3. RESULTS AND DISCUSSION
In this section the experimental creep curves arecompared with the theoretically calculated ones.
For the comparison we have chosen creep curvesfor three multiple-slip oriented crystals (h001i, h011iand h111i) measured at a ``low temperature'' of
7508C under constant load conditions. These exper-imental curves (points) are presented in Figs 2±4 indi�erentiated form (total strain rate vs total strain)
together with the theoretically calculated curves(full lines).The calculation of the theoretical creep curves
was performed along the lines shown in Section 2.
This requires a large number of parameters. Someof the parameters can be measured by microscopicmethods. These concern the dimensions of the
structure before loading �L0 � 0:45 mm andh0 � 0:05 mm), atomic volume �O � 1:1� 10ÿ29 m3�and Burgers vector �b � 2:5� 10ÿ10 m). The initial
density of the grown-in dislocations in each slip sys-tem is taken to be 1 � 104/m. The elastic constantsc11, c12, c44, c '11, c '12 and c '44 in g and g ' phases forthe temperature of 7508C were taken from the
paper by Pollock and Argon [16]. The remainingparameters are listed in Table 1.For the di�usion coe�cient we have chosen the
value corresponding to the di�usion coe�cient of
Table 1. Values of the constants used in the computation�T � 7508C)
G (GPa) d D (m2/s) W (m/s/Pa) p (m) j
40 ÿ1.1� 10ÿ3 7.8� 10ÿ19 2� 10ÿ21 5� 10ÿ9 10
SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS 2523
nickel in an alloy of a composition similar to the gphase in the superalloy CMSX-4 [17].
There are three ®t parameters, the values ofwhich cannot be taken from independent sources,namely W (which determines slip in the g channels;
p (which determines the kinetics of recovery); and j(which determines the kinetics of migration of theg/g ' interfaces. These parameters, their choice and
their physical acceptability were discussed in detailin Ref. [13].Results of the modelling are shown in Figs 2±7.
The parameters W, p and j were chosen in such away to obtain the best agreement between the ex-perimental creep curve for h001i orientation and thecalculated creep curve for this orientation. Both the
curves in di�erentiated form are shown in Fig. 2.Using then the same values of all the parametersthe creep curves for the orientations h011i and
h111i were computed. The agreement for these twoorientations (Figs 3 and 4 ) is somewhat looser, butstill it is possible to speak about a fair agreement
especially when taking into consideration the factthat the inherent scatter of the creep rates in nomin-ally the same creep tests can reach factor 3.
The modelling also makes it possible to identifythe mechanisms involved in the particular stages ofthe creep deformation. The case of h001i orientationwas discussed in Ref. [13]. The mechanisms for
h011i and h111i orientations will be described in thefollowing. In the case of h011i orientation the gchannels within the unit cell can be divided into
two roof channels and one vertical channel. At theapplied stress of 650 MPa all the channels are plas-tically deformed and the recovery process takes
place. The creep acceleration at the beginning ofthe test is caused by the multiplication of the dislo-
cations. The slip and recovery processes lead to thewidening of the roof channels and to a narrowing
of the vertical channel. The sharp decrease of thecreep rate (at about 4% strain) is due to the nar-rowing of the vertical channel to such an extent
that slip becomes di�cult. Slow creep, controlled bythe widening of the vertical channel due to the mi-gration of the g/g ' interfaces, starts at a strain of
about 5%. In the case of the h111i orientation allthe channels are equivalent and the simultaneousactivity of the slip systems in the g channels leads
to shear in directions h011i. The recovery of thedeposited dislocations on the g/g ' interfaces doesnot cause any change of channel thickness, butcauses shifts in the g/g ' interfaces in the directions
h011i. Owing to the symmetry there is no migrationof the g/g ' interfaces. The model does not predictany hardening of the crystal for the discussed h111iorientation. The experimental creep curve (Fig. 4)exhibits a hardening after about 0.5% deformation.This might be due to the decrease of the distance
between the tips of the g ' particles. This processmay cause narrowing at various points in the chan-nels and might result in the hardening. For all the
orientations it holds that the theoretically predictedonset of creep (increase of creep rate) at the begin-ning of the tests is more revealing than the exper-imentally measured prediction. This is probably due
to the fact that the model assumes the multipli-cation of dislocations within every unit cell. In rea-lity the dislocations have to spread out from the
nests of the grown-in dislocations. This process isslower [16].The model makes it possible to compute the
times needed to reach a given strain. This is shownin Figs 5±7 for the case of a 2% creep strain.
Fig. 3. Calculated (full line) and experimentally (points)determined di�erentiated creep curves of the superalloysingle crystal CMSX-4 (orientation h011i; 7508C;
650 MPa).
Fig. 2. Calculated (full line) and experimentally (points)determined di�erentiated creep curves of the superalloysingle crystal CMSX-4 (orientation h001i; 7508C;
735 MPa).
2524 SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS
Figure 5 shows how this this time depends on
applied stress for all three crystal orientations. Thebasic structural parameters were chosen to modelthe superalloy single crystals of CMSX-4
�L0 � 0:45 mm, h0 � 0:05 mm, volume fraction of theg ' phase of 72.9%). It is clear that the ranking ofthe orientations is h111i, h001i, and h011i. For a
lower volume fraction of the g ' phase, i.e. 54.8%�L0 � 0:45 mm, h0 � 0:1 mm), the ranking remains(Fig. 6), but the strength decreases by almost a fac-tor of 2. If a structure coarsened by a factor of 1.6
�L0 � 0:72 mm, h0 � 0:08 mm� at the same volume
fraction of the g ' phase as in the ®rst case (72.9%)is assumed, a softer structure (Fig. 7) with respectto the original one (Fig. 5) is obtained. The pre-
sented diagrams show that the model makes it poss-ible to simulate the creep behaviour as dependenton structural parameters.
The model is an idealization of reality. It assumesperfectly periodic structure of the g ' particles. Thisis the reason a decrease of the applied stress
leadsÐaccording to the modelÐin some types of gchannels to deactivation of some slip systems and
Fig. 4. Calculated (full line) and experimentally (points)determined di�erentiated creep curves of the superalloysingle crystal CMSX-4 (orientation h111i; 7508C;
800 MPa).
Fig. 5. Calculated time to 2% creep strain while dependenton the applied stress for three crystal orientations. Theinput parameters �L0 � 0:45 mm, h0 � 0:05 mm, volumefraction of the g ' phase being 72.9%) correspond to single
crystals of CMSX-4.
Fig. 6. Calculated time to 2% creep strain while dependenton applied stress for three crystal orientations. The inputparameters are L0 � 0:45 mm, h0 � 0:10 mm, and volume
fraction of the g ' phase is at 54.8%.
Fig. 7. Calculated time to 2% creep strain while dependenton applied stress for three crystal orientations. The inputparameters are L0 � 0:72 mm, h0 � 0:08 mm, and volume
fraction of the g ' phase is at 72.9%.
SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS 2525
consequently to a halting of the recovery processand thus, to a zero creep rate. In reality the
decrease of the applied stress leads to the deactiva-tion only in narrower channels and the slip/recoveryprocess can continue in the wider channels. In con-
clusion it can be stated that the model is well appli-cable for high enough stresses at which all of the gchannels are activated. To model properly the case
of considerably lower stresses it would probably benecessary to take into account the distribution ofthe width of the g channels.
4. CONCLUSIONS
The modelling and its confrontation with the ex-perimental results make it possible to state the fol-
lowing conclusions.
1. A unit cell model of creep of arbitrarily orientedsuperalloy single crystals taking into account slip
in g channels, dynamic recovery of dislocationstructure and migration of g/g ' interfaces hasbeen developed. The model is based exclusivelyon the concept of linear thermodynamics.
2. The model is applicable for low temperaturesand medium applied stresses. The calculatedcreep curves were compared with the experimen-
tal creep curves of single crystals CMSX-4 of theorientations h001i, h011i and h111i measured at7508C; a fair agreement was found.
3. By varying the input parameters such as dimen-sions and volume fraction of the g ' particles it ispossible to evaluate the e�ect of these parameterson the resulting creep behaviour. As an example,
the e�ect of the dimensions and volume fractionof the g ' particles on the time needed to reach astrain of 2% for the orientations h001i, h011iand h111i has been calculated. The resultsdemonstrate a strong e�ect.
AcknowledgementsÐThis research was supported by theGrant Agency of the Academy of Sciences of the CzechRepublic under contracts A2041608 and A2041002 and bythe Ministry of Education of the Czech Republic undercontracts OC P3.30 and OC 522.80. This support is grate-fully acknowledged.
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in Strength of materials in Proc. ICSMA-10, ed. H.Oikawa et al., 1994, p. 705.
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APPENDIX A
A.1. Nomenclature
Lx, Ly, Lz dimensions of the g ' par-ticle
L0 initial dimension of theg ' particle
hx, hy, hz thickness of the g chan-nels
h0 initial thickness of the gchannels
Vx, Vy, Vz, VP volumes of g channelsand the g ' particle
d mis®t parametersx,ij, sy,ij, sz,ij, sP,ij stress components in the
g channels and the g 'particle
K serial number of the slipsystem �K � 1±12)
tx,K, ty,K, tz,K resolved shear stress forthe Kth slip system in gchannels
tx,K0, ty,K0, tz,K0 threshold resolved shearstress for slip in g chan-nels
aK normalized vector in theslip direction
cK normalized vector normalto the slip plane
ex,ij,ey,ij, ez,ij, eP,ij elastic strain componentsin g channels and the g 'particle
ex,ij, ey,ij, ez,ij plastic strain componentsin the g channels
dij Kronecker symbolG, c11, c12, c44, c '11, c '12, c '44 elastic constantsrx,K, ry,K, rz,K density of dislocations
deposited on the g/g 'interfaces
2526 SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS
wx,2, wx,3, wy,1, wy,3, wz,1, wz,2 sliding along the g/g 'interfaces due to recoveryof dislocations
W parameter characterizingthe rate of slip in g chan-nels
p mean distance betweenjogs measured along thedislocation line
k Boltzmann constantT absolute temperatureb magnitude of the Burgers
vectorD average coe�cient of
self-di�usion inthe gphase [13]
O atomic volumej parameter characterizing
the di�erence in chemicalcomposition of the g andg ' phases [13]
A.2. Energy of dislocations deposited on the g/g 'interfaces
Let us consider slip system a�� ���2p =2,���2p=2, 0�, c
��ÿ ���3p=3,
���3p=3,
���3p=3� and the g/g ' interfaces lying
in the planes (001) and (010). The direction of thedislocation line in the plane (001) is g1 � �
���2p=2,���
2p=2, 0� and thus the dislocation is of the screw
type. The direction of the dislocation line in theplane (010) is g2��
���2p=2, 0,
���2p=2� and thus the dis-
location is of a mixed type. These two cases rep-
resent all the possible con®gurations of dislocationsof the systems {111}h110i deposited on the g/g 'interfaces. The mutual interaction of dislocations of
the di�erent Burgers vectors and/or di�erent direc-tions of dislocation lines will be neglected. FigureA1 shows the dislocations deposited on two neigh-
bouring g/g ' interfaces. The direction g is perpen-dicular to the paper, the dislocations in the upperinterface have opposite Burgers vector with respect
to the dislocations in the lower interface. We shallcalculate how the energy of the dislocation is chan-ged due to the interaction with other dislocations.For the isolated pair of dislocations produced by
slip we assume that the line energy is Ed � 1=2Gb 2:The procedure worked out by Hirth and Lothe [18]can be used for the evaluation of the change of theenergy when the distance of two parallel dislo-
cations is changed from Ra to R. The value Ra canbe understood as the distance at which the ®eld ofthe dislocation is screened by other dislocations. In
our case we take Ra � L0=2: The change of theenergy Ed is half the interaction energy with all theother dislocations lying close to the distance Ra.
The interaction energy for two screw dislocationscan be expressed as
W12,screw � ÿGb1b2
2pln2R
L�A1�
and for mixed dislocations as
W12,mixed � ÿGb1b2
2p
�1
2� 3
4�1ÿ n��
ln2R
L
� sin 2Y4�1ÿ n�
!�A2�
Fig. A1. Schematic drawing for the calculation of the energy of dislocations deposited on the g/g ' inter-faces.
Fig. A2. Dislocation line energy while dependent on thedislocation density for the con®guration shown in Fig. A1.
SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS 2527
Then it is possible to calculate the function Ed (r )for screw and mixed dislocations. This is shown in
Fig. A2. For typical dislocation density r= 1 2±4� 10
7/m both dependencies can be approximated
by a straight line:
Ed � 1=2Gb 2ÿ1� 1:1� 10ÿ8r
��A3�
(r in mÿ1) The threshold stress for slip can be cal-
culated from the condition that the energy releasedby the slip is equal to the increase of the energy of
dislocations deposited on the g/g ' interface. For thechannel of unit area it holds that:
t0h dg � 2 d�Edr� � Gb 2ÿ1� 2:2� 10ÿ8r
�dr �A4�
Using relation (8) we get
t0 ����2p
Gb���3p
h
ÿ1� 2:2� 10ÿ8r
��A5�
2528 SVOBODA and LUKAÂ SÏ : CREEP DEFORMATION IN SINGLE CRYSTALS