Abstract
The origin of the habit plane of the martensite phase (α′) in low-carbon steels is elucidated by three-dimensional phase-field simulations. The cubic → tetragonal martensitic transformation and the evolution of dislocations with Burgers vector aα′/2〈111〉α′ in the evolving α′ phase are modeled simultaneously. By assuming a static defect in the undercooled parent phase (γ), we simulate the heterogeneous nucleation in the martensitic transformation. The transformation progresses with the formation of the stress-accommodating cluster composed of the three tetragonal domains of the α′ phase. With the growth of the α′ phase, the habit plane of the martensitic cluster emerges near the (111)γ plane, whereas it is not observed in the simulation in which the slip in the α′ phase is not considered. We observed that the formation of the (111)γ habit plane, which is characteristic of the lath martensite that contains a high dislocation density, is attributable to the slip in the α′ phase during the martensitic transformation.
1. Introduction
In ferrous alloys, various types of martensite such as thin plate, lenticular, butterfly, and lath have been observed.1) Among them, the lath martensite appears in most heat-treatable commercial steels and is therefore extremely important from an industrial viewpoint. The characteristics of lath martensite, which is often observed in low-carbon steels, can be summarized as follows:2,3,4,5,6,7,8) (1) the martensite phase (hereafter denoted as α′) contains a high dislocation density; (2) habit planes are close to the {111} or the {557} crystallographic planes of the parent phase (hereafter denoted as γ); and (3) the Kurdjumov–Sachs (K–S) orientation relationship ((111)γ//(011)α′,[101]γ//[1 11]α′) is satisfied between the γ phase (with a face-centered cubic (fcc) lattice) and the α′ phase (with a body-centered tetragonal (bct) lattice). The habit plane of the martensite coincides with the invariant plane because fitting the γ and α′ phases together along the invariant plane causes no elastic strain and minimizes the elastic energy associated with the transformation. The absence of elastic strain enables us to discuss the habit plane formation purely on the basis of crystallographic theory9,10,11,12,13,14,15,16) without resorting to elasticity theory.
The phase-field method is a powerful tool for simulating the evolution of a material microstructure.17) Phase-field models of proper and improper martensitc transformations (MTs) have been proposed by Khachaturyan and his collaborators.18,19,20,21,22) The MT in steels have been simulated by simultaneously modeling the cubic → tetragonal lattice deformation and the plastic deformation in the γ and/or α′ phases.23,24,25,26,27,28,29,30,31,32,33) In most of these studies, the elastic energy calculation is based on the microelasticity theory;14,34) hence, the long-range elastic interaction between the transformation strain (Bain strain), plastic strain, and external applied stress is automatically taken into account and its effect on the microstructure evolution has been successfully simulated. However, the formation of the {111}γ habit plane has not yet been simulated; although Yeddu et al.26) predicted the habit plane of an infinitesimal α′ phase as (111)γ, the final habit plane was determined to be (211)γ after the growth of the α′ phase. A phase-field model that can reproduce the lath-martensite characteristics, one of which is the {111}γ habit plane, seems to be essential for simulating microstructure evolution in practical low-carbon steels. In phase-field simulations, the microstructure evolves so as to reduce the total free energy of the microstructure; hence, the formation of the {111}γ habit plane should be simulated because it is presumably effective for minimizing the elastic energy during the MT.
As mentioned earlier, the lath martensite contains a high dislocation density.2,6) As an inevitable result, the formation of the lath martensite is closely related to the slip in the α′ phase.15,16) Presumably, the elastic energy minimization during the MT plays an important role in the habit plane formation in the lath martensite, where dislocations with Burgers vector aα′/2〈111〉α′ have often been observed.3) There are some phase-field approaches in modeling defects and deformation in materials.35) In the microelasticity theory of dislocations,36) phase fields were defined to characterize inelastic strain field of individual dislocations on slip planes. Zhou et al.37) extended this model to a larger length scale and introduced a new set of phase fields (density functions for dislocation), which describes the plastic deformation produced by dislocations from a specific slip system. In this study, the cubic → tetragonal MT and the evolution of dislocations in the evolving α′ phase are simultaneously simulated by the phase-field method. Notably, for the first time, the elastic energy associated with both the Bain strain and the dislocations with Burgers vectors aα′/2〈111〉α′ in the α′ phase is taken into account; the density functions for dislocation37) are employed as field variables to describe the plastic deformation in the α′ phase. From simulation results with/without consideration of slip in the α′ phase, the origin of the {111}γ habit plane of the lath martensite is explored.
2. Calculation Method
2.1. Phase-field Model
Long-range order parameters {φi(r, t)} = φ1(r, t), φ2(r, t), φ3(r, t) (i = 1, 2, 3 numbering crystallographically equivalent orientation domains) and density functions for dislocation {
p
α
(i)
(r, t)} =
p
1
(i)
(r, t),
p
2
(i)
(r, t), …,
p
n
(i)
(r, t) (α = 1, 2, …, n numbering slip systems in the α′ phase) are adopted as field variables, which are functions of space (r) and time (t). φi(r, t) represents the structural density of each of the three tetragonal martensitic domains derived from the fcc → bct MT. Therefore, φi(r, t) is equal to unity if the vector r is inside a martensitic domain of i and is zero otherwise.
p
α
(i)
(r, t) is related to
m
α
(i)
(r, t), which is the average number of lattice planes between neighboring sheared regions by dislocations of slip system α:
p
α
(i)
(r, t)=
|
b
α
(i)
|
D
α
(i)
(r, t)
=
|
b
α
(i)
|
d
α
(i)
m
α
(i)
(r, t)
,
| (1) |
where
d
α
(i)
is the lattice plane spacing and
b
α
(i)
is the Burgers vector for slip system
α. In
Eq. (1),
D
α
(i)
(
r,
t)=
d
α
(i)
m
α
(i)
(
r,
t) represents the average spacing between neighboring sheared regions by dislocations of slip system
α.
37) The temporal evolution of the field variables is given by the time-dependent Ginzburg–Landau (TDGL) equations:
∂
φ
i
(r, t)
∂t
=-
L
φ
δG
δ
φ
i
(r, t)
, i=1, 2, 3,
| (2) |
∂
p
α
(i)
(r, t)
∂t
=-
L
p
δG
δ
p
α
(i)
(r, t)
, i=1, 2, 3, α=1, 2, ..., n,
| (3) |
where
Lφ and
Lp are kinetic coefficients and
G is the total free energy of the microstructure. The
G is a functional of field variables:
G=
∫
r
[
f
L
(
{
φ
i
}
)
+
κ
φ
2
∑
i=1
3
(
∇
φ
i
)
2
+
κ
p
2
∑
i=1
3
∑
α=1
n
(
n
α
(i)
×∇
p
α
(i)
)
2
]dr+
E
el
(
{
φ
i
},{
p
α
(i)
}
)
,
| (4) |
where
fL is the Landau energy density,
κφ and
κp are gradient energy coefficients,
n
α
(i)
is the unit vector of the slip plane normal,
36,37) and
Eel is the elastic energy. Note that the “crystalline” energy
36) is not included in
Eq. (4), because
p
α
(i)
(
r,
t) defined by
Eq. (1) does not assume integer values.
37) The
fL({
φi}) is approximated by the Landau polynomial expansion with respect to {
φi(
r,
t)}:
18,19,20)
f
L
=Δf{
a
2
∑
i=1
3
φ
i
2
-
b
3
∑
i=1
3
φ
i
3
+
c
4
(
∑
i=1
3
φ
i
2
)
2
}.
| (5) |
With the conditions
a −
b +
c = 0 and 6
a − 4
b + 3
c + 12 = 0, Δ
f represents the driving force for the MT. In this study,
a = 1,
b = 15, and
c = 14 are chosen.
20) The
Eel({
φi},{
p
α
(i)
}) is given by
14,34)
E
el
=
∫
r
[
1
2
C
ijkl
{
ε
ij
(r, t)-
ε
ij
0
(r, t)
}{
ε
kl
(r, t)-
ε
kl
0
(r, t)
}
]dr
,
| (6) |
where
Cijkl is the elastic constant,
εij is the total strain, and
ε
ij
0
is the eigenstrain. Note that the Einstein summation convention is applied in
Eq. (6). For simplicity, the material is assumed to be isotropic, and the tensor
Cijkl is expressed in terms of Lamé’s constants:
Cijkl =
λδijδkl +
μ(
δikδjl +
δilδjk), where
δij is the Kronecker delta function. By solving mechanical equilibrium equation (∂
σij/∂
rj = 0,
σij = C
ijkl{
εkl(
r,
t) −
ε
kl
0
(
r,
t)}) in Fourier space, we calculate the total strain
εij from the spatial distribution of the eigenstrain
ε
ij
0
. Here, the body is assumed to be fully clamped (strain-controlled boundary condition) and the macroscopic strain
εij≡∫
r εijdr/
V, where
V is the system volume, is assumed to be zero. In this study, following the model of Zhang
et al.,
22) we model heterogeneous nucleation in the MT by assuming a static defect in the undercooled
γ phase. The eigenstrain
ε
mn
0
is defined by
ε
mn
0
(r, t)
=
∑
i=1
3
{
ε
mn
(i)
φ
i
(r, t)+
∑
α=1
n
n
α
(i)
⊗
b
α
(i)
+
b
α
(i)
⊗
n
α
(i)
2|
b
α
(i)
|
p
α
(i)
(r, t)
}
+
ε
mn
(d)
ζ(r).
| (7) |
Here,
ε
mn
(i)
is the transformation strain (Bain strain) derived from the fcc → bct MT,
ε
mn
(d)
is the stress-free transformation strain induced by the static defect in the
γ phase, and ζ(
r) is a shape function that is equal either to unity if
r is inside the static defect or to zero otherwise. In the undercooled
γ phase, the MT is triggered by the static defect. As the
α′ phase grows, the eigenstrain field of the static defect, which is described by
ε
mn
(d)
ζ(
r) in
Eq. (7), is assumed to be inherited into the
α′ phase. The
ε
mn
(i)
is given by
ε
mn
(1)
=(
ε
a
0
0
0
ε
a
0
0
0
ε
c
)
,
ε
mn
(2)
=(
ε
c
0
0
0
ε
a
0
0
0
ε
a
)
,
ε
mn
(3)
=(
ε
a
0
0
0
ε
c
0
0
0
ε
a
)
,
| (8) |
where the coordinates are along the 〈100〉 axes of the
γ phase and
εa =
2
aα′/
aγ−1 and
εc =
cα′/
aγ−1 are the tetragonal transformation strains along the
a and
c axes, respectively. In the martensitic domains of
φ1 = 1,
φ2 = 1, and
φ3 = 1, the [001]
α′ coincides with the [001]
γ, [100]
γ, and [010]
γ, respectively. The Bain crystal lattice correspondence in each of the three tetragonal martensitic domains
15) is summarized in the Appendix.
2.2. Simulation Conditions
We used 64 × 64 × 64 computational grids for three-dimensional simulations. The periodic boundary conditions are assumed along all three dimensions. Equations (2) and (3) were solved by the finite difference method. In numerical analysis, all the physical parameters were reduced to dimensionless quantities using the scaling factors of RT for energy, l0 for length, and (LφRT)−1 for time, where R is the gas constant, T is the absolute temperature, and l0 is the unit grid size. The unit time step Δt*, where the superscript * denotes a dimensionless quantity, was selected as Δt* = 0.001 to maintain numerical accuracy and stability. The parameters used in the simulation are summarized in Table 1. The difference between the free energies of the austenite and ferrite phases in Fe–0.1mass%C at 300 K was assumed to be the driving force for the MT and was estimated from the Thermo-Calc TCFE7 database. Zhang et al.22) solved the PFM equation for two (110) twin-related martensitic domains and calculated the reduced domain wall tension coefficient. Through the use of their calculation result as a reference, the coefficient κφ was estimated by assuming the interphase boundary to be semicoherent (the interface energy γsemicoh~0.24 J m−2 38)); the estimated κφ gave a unit grid size l0~8 nm (the system size was 522×522×522 nm3). The coefficient κp was determined so as to guarantee a smooth transition of
p
α
(i)
(r, t) across the boundary between the sheared and unsheared regions.37) Lattice parameters aγ, aα′, and cα′ in Fe–0.1mass%C at 300 K were estimated from the literature39) and from the empirical formula (c/a)α′ = 1 + 0.045(mass%C).40) Elastic constants of pure iron were used.39) Because of the lack of experimental data, the kinetic coefficients Lφ and Lp were not well determined and were assumed to be equal to each other.
Table 1. Parameters used in the simulation.
Driving force for the MT (J m−3) | Δf = 7.25 × 108 |
Gradient energy coefficients (J m−1) | κφ = 1.90 × 10−8, κp = 1.78 × 10−7 |
Lattice parameters (10−10 m) | aγ = 3.60, aα′ = 2.87, cα′ = 2.88 |
Elastic constants (GPa) | λ = 123, μ = 72 |
The Landau energy density fL for φ2 = φ3 = 0 is shown in Fig. 1. As shown in the inset in Fig. 1, a local maximum describes the chemical energy barrier of the transformation. With respect to the slip in the α′ phase, the time evolution of
p
α
(i)
(r, t) was solved for four specific slip systems (α = 1,2,3,4) listed in Table 2, whereas, in practice, a number of slip systems would be activated during the MT. This assumption is based on the experimental result that dislocations with Burgers vector aα′/2〈111〉α′ occur in the lath martensite.3) Note that the slip is confined to the α′ phase and that the time evolution of
p
α
(i)
(r, t) is solved in the region where φi(r, t) ≥ 0.4; plastic yield criterion of the α′ phase is not considered. Figure 2 shows the initial microstructure of the simulation; the homogeneous γ phase contains a static defect (dislocation loop) on the (111)γ plane at the center of the computational cell. The coordinate axes of the computational cell correspond to the [100]γ, [010]γ, and [001]γ axes. The dislocation loop is assumed to have the Burgers vector b = M
b
ˆ
in the (111)γ slip plane (n = 〈1/
3
, 1/
3
, 1/
3
〉), where
b
ˆ
= aγ/2[110]γ is an elementary Burgers vector, and M is a multiplicity factor characterizing the number of dislocation loops located within the same slip plane.22) Then, the stress-free transformation strain
ε
mn
(d)
in Eq. (7) is given by
ε
mn
(d)
= (b⊗n + n⊗b)/2l0.36) The multiplicity factor is set to be M = 30, which is sufficiently large to describe the athermal MT triggered by the dislocation loop.22) The effect of the magnitude of M on the MT is beyond the scope of this paper and will be reported elsewhere.
Table 2. Slip systems in the
α′ phase assumed in the simulation.
α | Slip system |
---|
1 | (101)α′[111]α′ |
2 | (101)α′[111]α′ |
3 | (101)α′[111]α′ |
4 | (101)α′[1 11]α′ |
3. Results
3.1. Formation of (111)γ Habit Plane
First, simulation results obtained without considering slip in the α′ phase are shown in Fig. 3. Here, instead of Eq. (7), the eigenstrain
ε
mn
0
is defined by
ε
mn
0
(r, t)=
∑
i=1
3
ε
mn
(i)
φ
i
(r, t)+
ε
mn
(d)
ζ(r)
.
| (9) |
In
Fig. 3, the
γ phase is transparent; three different colors represent three tetragonal domains (Bain variants) of the
α′ phase that are twin-related with each other, and
t* represents the dimensionless time step in the numerical analysis. The parent phase inside the dislocation loop first transforms to a martensitic domain (
φ3 ≥ 0.7 in red), which is subsequently surrounded by the other two martensitic domains (
φ1 ≥ 0.7 in green and
φ2 ≥ 0.7 in greenish yellow). This result is consistent with a previous simulation result reported by Zhang
et al.22) that the martensitic nucleus prefers a multidomain, stress-accommodating cluster. As evident in
Fig. 3, the MT progresses with the growth of the multidomain complex composed of the three tetragonal domains. The twin boundary between the two adjacent martensitic domains is on the {110}
γ plane. However, specific habit planes are not observed between the
γ and
α′ phases. In contrast,
Fig. 4 shows the simulation results obtained with consideration of slip in the
α′ phase. In this case, the eigenstrain
ε
ij
0
contains the term associated with
p
α
(i)
(
r,
t), as given by
Eq. (7). The growth of the martensitic cluster composed of the three tetragonal domains is observed; notably, as shown in
Fig. 5, the habit plane of the multidomain cluster emerges near the (111)
γ plane (the blue-colored (111)
γ plane is inserted in
Fig. 5 for reference). As evident in
Figs. 3,
4,
5, the habit plane close to the (111)
γ plane is formed when the slip in the
α′ phase is considered in the simulation. This result suggests that the slip in the
α′ phase plays a prominent role in the formation of the (111)
γ habit plane, which is characteristic of the lath martensite with a high dislocation density.
3.2. Slip Distribution in the α′ Phase
In the simulation shown in Fig. 4, the evolution of
p
α
(i)
(r, t) is solved for four slip systems (α = 1,2,3,4) listed in Table 2. Figure 6(a) shows the multidomain martensitic cluster at t* = 6, whereas Fig. 6(b) shows the domain of φ1 ≥ 0.7 on a cross-section of the martensitic cluster. The spatial distributions of
p
1
(1)
,
p
2
(1)
,
p
3
(1)
, and
p
4
(1)
in the domain of φ1 ≥ 0.7 on the corresponding cross-section are shown in Figs. 6(c), 6(d), 6(e), and 6(f), respectively. As evident in Fig. 6, all four of the slip systems are activated; however, the magnitude of
p
α
(1)
(α = 1,2,3,4) differs among the four slip systems. In the region marked by the circle in Fig. 6, the magnitudes of
p
3
(1)
and
p
4
(1)
(corresponding to the (101)α′ [111]α′ and (101)α′ [1 11]α′ slip systems, respectively) are larger than that of
p
1
(1)
and
p
2
(1)
(corresponding to the (101)α′ [111]α′ and (101)α′ [111]α′ slip systems, respectively). This result is reasonable because the α′ phase is under tensile stress along the c axis of the tetragonal lattice after the fcc → bct MT; given the Burgers vectors of the four slip systems, the combination of
p
3
(1)
and
p
4
(1)
(or
p
1
(1)
and
p
2
(1)
) can obviously effectively reduce the elastic energy associated with the Bain strain. Notably, however, the magnitude of
p
3
(1)
is slightly larger than that of
p
4
(1)
in the region marked by the circle in Fig. 6. This result presumably suggests that the equivalent activation of the (101)α′ [111]α′ and (101)α′ [1 11]α′ slip systems is not necessarily effective for elastic energy minimization.
There are twenty-four α′ variants for the K–S orientation relationship (OR). These variants are divided into four groups (CP groups); each of the group contains the six K–S variants whose close-packed planes ({011}α′) are parallel to one of the four close-packed planes of the γ phase ({111}γ). In each of the CP groups, the {111}γ habit plane is shared by three Bain variants, and each of the Bain variants is shared by two K–S variants.15,16) In this study, as we assumed the Bain crystal lattice correspondence shown in the Appendix, six K–S variants can derive from the three Bain variants, which share the (111)γ habit plane, as a result of the slip in the α′ phase; the activation of the slip systems shown in Figs. 6(c)–6(f) would give rise to two K–S variants in the Bain variant domain of φ1 ≥ 0.7, and in the same way, the other four K–S variants would emerge in the Bain variant domains of φ2 ≥ 0.7 and φ3 ≥ 0.7. As the phase-field model in this study is based on the microelasticity theory,14) which is formulated in terms of strain that is invariant with respect to rigid body rotation, the OR between the γ and α′ phases cannot be predicted directly by the simulation. However, as discussed by Gao et al.,41) there is one-to-one correspondence between the OR and invariant plane orientation. Hence, the OR can be determined if the invariant plane normal is predicted by the phase-field simulation based on the microelasticity theory.
3.3. Effect of the Initial Microstructure on the Habit Plane Formation
As shown in Figs. 4 and 5, the formation of the (111)γ habit plane during the MT was simulated by the phase-field simulation. However, the configuration of the static defect (dislocation loop) shown in Fig. 2 could influence the simulation results; if the dislocation loop is located on a plane other than the (111)γ plane, another simulation result would be obtained. Accordingly, a simulation was performed where the dislocation loop with the Burgers vector b = M
b
ˆ
(M = 30 and
b
ˆ
= aγ/2[110]γ) was located on the (111)γ plane (n = 〈1/
3
, 1/
3
, −1/
3
〉) at the center of the computational cell, as shown in Fig. 7. The stress-free transformation strain
ε
mn
(d)
in Eq. (7) is given by
ε
mn
(d)
= (b⊗n + n⊗b)/2l0. The simulated microstructure evolution is shown in Fig. 8, where the MT is observed to progress with the growth of the martensitic cluster composed of three tetragonal domains. The habit plane is not clearly observed until t* = 2; however, it emerges near the (111)γ plane as the α′ phase grows. Figure 9 shows the simulated microstructure at t* = 6. A portion of the α′ phase grows out of the (111)γ habit plane, as indicated by the arrows in Fig. 9; however, its effect on the habit plane formation appears to be negligible. Although this search was not exhaustive and more simulations with different initial microstructure are needed, we presumed that the formation of the (111)γ habit plane is energetically favorable, irrespective of the configuration of the static dislocation loop.
4. Discussion
4.1. Slip Condition for an Invariant Plane to Exist
As previously mentioned, no elastic strain occurs along an invariant plane; hence, the invariant plane formation is effective for minimizing the elastic energy associated with the MT. The slip condition for an invariant plane to exist is considered on the basis of crystallographic theory, as shown below.14) Let the atom positions of the γ phase (rγ) shift to atom positions of the α′ phase (
r
′
α
′
) under the MT. For the martensitic domain of φ1 = 1, the transformation can be written in the fcc crystal lattice basis as:
where the transformation matrix
A is given by
A=(
A
11
A
12
A
13
A
21
A
22
A
23
A
31
A
32
A
33
)
|
A
11
=(
1-
1
2
m
3
(1)
-
1
2
m
4
(1)
)
η
1
,
A
12
=(
1
2
m
3
(1)
+
1
2
m
4
(1)
)
η
1
,
A
13
=(
1
2
m
3
(1)
-
1
2
m
4
(1)
)
η
1
,
A
21
=(
1
2
m
1
(1)
+
1
2
m
2
(1)
)
η
1
,
A
22
=(
1-
1
2
m
1
(1)
-
1
2
m
2
(1)
)
η
1
,
A
23
=(
-
1
2
m
1
(1)
+
1
2
m
2
(1)
)
η
1
,
A
31
=(
-
1
2
m
1
(1)
+
1
2
m
2
(1)
-
1
2
m
3
(1)
+
1
2
m
4
(1)
)
η
3
,
A
32
=(
1
2
m
1
(1)
-
1
2
m
2
(1)
+
1
2
m
3
(1)
-
1
2
m
4
(1)
)
η
3
,
A
33
=(
1+
1
2
m
1
(1)
+
1
2
m
2
(1)
+
1
2
m
3
(1)
+
1
2
m
4
(1)
)
η
3
.Here,
η1 =
2
aα′/
aγ and
η3 =
cα′/
aγ.
m
α
(i)
are the average number of lattice planes between neighboring regions sheared by dislocations of slip system
α and are related to
p
α
(i)
through
Eq. (1). In general, the matrix
A can be represented as the product of symmetric matrix
F and rigid body rotation matrix
R as
If
A+ is the transposed matrix of
A, then
A
+
A=
(RF)
+
(RF)=
F
+
(
R
+
R)F=
F
2
.
| (12) |
If an invariant plane is present, one of the eigenvalues of
F2 will be less than unity, the other will be equal to unity, and the third will be greater than unity.
14) Figures 10(a) and 10(b) show the slip conditions for an invariant plane to exist when
m
1
(1)
= 20 and
m
1
(1)
= 80, respectively; an invariant plane exists if the slip condition is on the curvilinear surface shown in
Figs. 10(a) and 10(b). We see that the geometry of the curvilinear surface has a small dependence on the magnitude of
m
1
(1)
. The values of
m
2
(1)
,
m
3
(1)
, and
m
4
(1)
in the simulation shown in
Fig. 4 (at
t* = 6) are extracted by
Eq. (1) and are plotted in
Figs. 10(c) and 10(d). Here,
m
1
(1)
values are outside our scope of concern and are not shown in the figure. The simulated slip conditions shown in
Figs. 10(c) and 10(d) distribute near the curvilinear surface shown in
Figs. 10(a) and 10(b). This result suggests that the slip systems assumed in the simulation have been activated so as to form an invariant plane and to reduce the elastic energy during the MT. Interestingly, as a result of the slip in the
α′ phase, the (111)
γ habit plane of a multidomain martensitic cluster was simulated (see
Figs. 5 and
9) without any a prior assumption about the habit plane formation.
4.2. Plasticity during the MT
According to the phase-field microelasticity theory of dislocations,36) dislocations exist where the value of
p
α
(i)
(r, t) varies. From the simulated spatial distribution of
p
α
(i)
(r, t), the local dislocation density can be estimated by
ρ(r, t)=
∑
i=1
3
∑
α=1
4
|
n
α
(i)
×∇
p
α
(i)
(r, t)
|
|
b
α
(i)
|
.
| (13) |
Figure 11 shows the change in the spatially-averaged dislocation density during the MT. The dislocation density increases as the MT progresses, and, when the transformation completes, it reaches a value of approximately
ρ = 3.7 × 10
16 m
−2 (solid line in
Fig. 11); this value is an order of magnitude greater than the experimentally measured value.
2,6) In
Eq. (13), by use of the central difference formula, the value of ∇
p
α
(i)
(
r,
t) is calculated from the values of
p
α
(i)
(
r,
t) on the neighboring computational grids and the unit grid size
l0, which we estimated to be
l0~8 nm by assuming that the interphase boundary is semicoherent. However, if the interphase boundary is assumed to be incoherent (the interface energy
γincoh = 0.5 – 1.0 J m
−2 42)),
l0 should be much larger and the value of
ρ would therefore be smaller. As an example, if the interface energy is assumed to be
γincoh = 1 J m
−2, then the
l0 and
ρ are estimated to be
l0~34 nm and
ρ~8.9 × 10
15 m
−2, respectively (see the dashed line in
Fig. 11). Furthermore, the values of kinetic coefficients
Lφ and
Lp in
Eqs. (2) and
(3) could influence the value of
ρ. If the value of
Lφ is significantly larger than that of
Lp, the value of
ρ will decrease. A detailed discussion on the effect of these modeling parameters on the value of
ρ will be presented in a separate paper.
On the basis of the simulation results shown in Figs. 3 and 4, formation of the (111)γ habit plane can be attributed to the slip in the α′ phase. This result is consistent with the fact that the {111}γ habit plane is characteristic of the lath martensite that contains a high dislocation density. However, the plastic deformation has also been reported to occur in the γ phase surrounding the lenticular and lath martensite in ferrous alloys.43,44,45) Furthermore, it has been noted that the dislocation in the γ phase is inherited by the α′ phase near the interface region.44) Although the plastic strain in the γ phase would be smaller than that in the α′ phase,23,24,26) the plastic deformation in the γ phase could reduce the elastic energy associated with the MT and hence could influence the transformation kinetics and martensitic morphology. In future works, the plasticity in the γ phase should also be incorporated into the model and its effect on the habit plane formation should be explored.
The MT is influenced by materials parameters such as kinetic coefficients Lφ and Lp, driving force for the MT, Bain strain, elastic constants, and plastic yield criteria of the γ and α′ phases. As the phase-field model in this study allows both twinning and slip modes, some parametric simulations, where each of the materials parameters is systematically changed, should be effective for elucidating the key materials parameters that determine whether to twin or to slip. In other words, in the near future, parametric simulation study would give an appropriate explanation of the experimental observations that twinning happens mainly in high-carbon steels at relatively low temperature while slip happens mainly in low-carbon steels at relatively high temperature.
5. Conclusions
The fcc → bct MT and the evolution of dislocations with Burgers vector aα′/2〈111〉α′ in the α′ phase were modeled simultaneously using the phase-field method. By assuming a static defect (dislocation loop) in the undercooled γ phase, we simulated heterogeneous nucleation in the MT. The transformation progressed with formation of the stress-accommodating cluster composed of the three Bain variant domains of the α′ phase. As the α′ phase grew, the habit plane of the multidomain martensitic cluster emerged near the (111)γ plane, whereas it was not observed in the simulation where the slip in the α′ phase was not considered. The habit plane formation was also simulated in the case where the configuration of the static dislocation loop was changed, which presumably implies that the formation of the (111)γ habit plane is energetically favorable, irrespective of the configuration of the static dislocation loop. We observed that the formation of a habit plane close to the (111)γ plane, which is characteristic of the lath martensite with a high dislocation density, can be attributed to the slip in the α′ phase during the MT.
Acknowledgements
This work was supported by Grant-in-Aid for Young Scientists (B) (Grant Number 26820282) of the Japan Society for the Promotion of Science (JSPS), and was also supported by ISIJ Research Promotion Grant.
Appendix
The Bain crystal lattice correspondence in each of the three tetragonal martensitic domains is summarized.
“Martensitic domain of φ1 = 1”
[
a
b
c
]
γ
=(
1/2
1/2
0
-1/2
1/2
0
0
0
1
)
[
u
v
w
]
α
′
|
(hkl)
γ
=
(pqr)
α
′
(
1
-1
0
1
1
0
0
0
1
)
|
“Martensitic domain of φ2 = 1”
[
a
b
c
]
γ
=(
0
0
1
1/2
1/2
0
-1/2
1/2
0
)
[
u
v
w
]
α
′
|
(hkl)
γ
=
(pqr)
α
′
(
0
1
-1
0
1
1
1
0
0
)
|
“Martensitic domain of φ3 = 1”
[
a
b
c
]
γ
=(
-1/2
1/2
0
0
0
1
1/2
1/2
0
)
[
u
v
w
]
α
′
|
(hkl)
γ
=
(pqr)
α
′
(
-1
0
1
1
0
1
0
1
0
)
|
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