Citation: Songlin Zheng, Yong Ni, Linghui He. Concurrent interface shearing and dislocation core change on the glide dislocation-interface interactions: a phase field approach[J]. AIMS Materials Science, 2015, 2(3): 260-278. doi: 10.3934/matersci.2015.3.260
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Computer modeling and simulation of defects ensemble and their elastic interactions from atomistic scale to continuum scale are important to get insights into mechanism-based strength or plasticity in materials [1,2]. Especially computational modeling capable of bridging multiple time and length scales becomes one of the fast growing areas in understanding the mechanical response of materials [3]. In metallic multilayers, the strength shows a maximum at a critical layer thickness [4,5,6,7]. The maximum is closely related to the critical stress required to transmit a glide dislocation across an interface wherein the interface acts as a barrier to impede the movement of the dislocation [7,8,9]. How the interfacial properties influence on the interfacial barrier strength has been widely studied by theoretical [10,11,12,13,14,15,16,17,18] and atomistic models [19,20,21,22,23,24,25,26].
Shen and Anderson [16,17] study the interfacial barriers of both welded (non-slipping) and slipping interface. Their results predict that significant interfacial sliding delocalizes the dislocation core within the slipping interface and creates a larger barrier to slip transmission in comparison with the welded interface. By using atomistic modeling, Rao and Hazzledine [20] show that screw dislocations in Cu prefer to spread on the Cu-Ni interface rather than to transmit into Ni. The molecular dynamics simulations performed by Hoagland et al. [21] indicate that opaque interfaces composed of two different crystal structures (e.g., Cu-Nb) present larger barrier strength than transparent interfaces with nearly continuous slip systems (e.g., Cu-Ni). The atomistic simulation results given by Wang et al. [22,23,24] demonstrate that these opaque interfaces with low shear strength (“weak” interfaces) exhibit strong barrier. They also show that the slip transmission barrier calculated by the chain of states method increases with the decrease of the interface shear strength [25]. By using the Green function method for anisotropic bimaterials, Chu et al. [18] employ dislocation-based interface shear models to systematically discuss the dislocation-interface interaction for possible implementation into large scale dislocation dynamic simulations. These models suggest that the interface shear results in an attractive force to trap the glide dislocation at the interface and thus leads to a barrier to dislocation transmission.
The force on the glide dislocation exerted by the interface is attractive only if the total energy increases as the glide dislocation is away from the interface. The maximum attractive force that should be overcome by the external stress can be viewed as the interfacial barrier strength during the dislocation escaping from the interface. Recent atomistic simulations further indicated that the interface shear involves the nucleation and growth of interfacial dislocations, and there is indeed an abrupt energy decrease like an energy well when the glide dislocation approaches the interface [21,22,23,24,25]. The weaker interface in shear shows a wider glide dislocation core spreading, results in a deeper energy drop at the interface, and produces a larger attractive force and thus a stronger interfacial barrier strength for slip transmission [25]. The energy decrease is significantly influenced by both the dislocation line energy change due to the core spreading [16], and the complicated cross-slip interaction between the glide dislocation and the induced interfacial dislocations [25]. Their contributions to the interfacial barrier strength are not additive due to the nonlinear coupling wherein the dislocation core change adaptively counteracts the stress concentration induced by the glide dislocation and the induced interfacial dislocations.
Developing a continuum model taking into account concurrent interface shearing and dislocation core change to reproduce the energy change during the glide dislocation across the interface is useful. In contrast to the dislocation-based interface shear model wherein the dislocations are described as line defects with compact cores, phase field model of dislocations could describe arbitrary dislocation core configurations, elastic interactions between arbitrary dislocations coupled with external applied stress [27,28,29,30,31,32,33,34,35,36]. After incorporating the stacking fault energy (SFE) of the shearable interface into the PFM model, similar to the case of γ-surface [30,32,37], a phase field approach could be applied to study the glide dislocation-interface interaction [36]. In addition different relaxation rate constants in the phase field model could characterize different dislocation mobilities on the glide plane and the interface, the rate competition between the transmission processes and the interface shearing process can be addressed as well [36]. In this paper such phase field approach is adopted to discuss the effect of concurrent interface shearing and dislocation core change on the interfacial barrier strength for the glide dislocation transmission. It is worth to mention that recently the large-deformation phase field theory is developed and applied for the interaction between dislocations and phase interfaces [38,39,40,41,42,43,44]. The important mechanism of interface motion elucidated by this improved model is enlightening for dislocation-interface interaction. Although in the current study we use the small-deformation phase field model, and these calculations are not yet material specific because the simple stacking fault energy surfaces for the glide plane and the interface are adopted. It would provide valuable trend in what determines the width and depth of the energy well, the interfacial barrier strength for slip transmission and give insight into the limitations of continuum model of the dislocation without the core-width change.
In the current model we consider a screw dislocation across a bi-material coherent interface shown in Figure 1. The glide plane is denoted by z=0 and the interface between phases I and II is viewed as a mathematically sharp plane denoted by x=0. To focus on the effects of the concurrent interface shearing and the dislocation core change, the lattice mismatch between the two phases is ignored. A pre-existing dislocation at the glide plane in phase II tends to glide across the interface under an external shear, σextyz. The straight glide dislocation with the Burgers vector and the line direction both parallel to y axis is assumed to be a pure screw type for simplicity, the resultant shear stress by the dislocation only has the component along y axis, and thus the stress-driven nucleated interfacial dislocation only includes pure screw component. Because the initial glide dislocation is straight and the external stress is pure shear, the glide dislocation and the nucleated interfacial dislocation keep straight and pure screw all the time. We adopted a 3D PFM model to treat the interplay between the dislocation glide and the movement of interfacial dislocations. In the PFM modeling [27], the phase field variables η(α,mα,r) are used to represent the amount of relative slips in the slip plane α and the slip direction mα in units of the Burgers vector b(α,mα). The evolution of η(α,mα,r) characterizes the dislocation assembly towards equilibrium, driven by minimizing the total system free energy including the crystalline energy Ecryst caused by localized slips, their elastic interaction energies Eelas and the additional energy Eext induced by applied stress
Etot=Ecryst+Eelas+Eext. |
(1) |
Here two phase field variables, ηs(r), ηint(r) are introduced as shape functions of the slipped regions. ηs(r)=1 and ηint(r)=1 are in the slipped area at the glide plane and the interface respectively, while ηs(r)=0 and ηint(r)=0 are in the unslipped area at the glide plane and the interface respectively. Following the treatment in the PFM, formulating the total free energy in Eq.(1) as a function of the two phase fields can be obtained. The crystalline energy (interplanar potential energy) caused by localized slip is given by
Ecryst=∫∑α,mαΦ[Δ(α,mα,r)]d3r, |
(2) |
Φ=γ(α,mα)d(α)sin2[πΔ(α,mα,r)b(α,mα,r)] |
(3) |
τ=∂Φ∂Δ(α,mα,r)d(α)=πγ(α,mα)b(α,mα,r)sin[2πΔ(α,mα,r)b(α,mα,r)]. |
(4) |
Δs=bsηs(r)+πdsγsμbssin(2πΔsbs), |
(5) |
Δint=bintηint(r)+πdintγintμbintsin(2πΔintbint), |
(6) |
ε0ij(r)=bsinsjdsηs(r)+bintinintjdintηint(r), |
(7) |
Eelas=12∫|ξ|≠0[Cijkl˜ε0ij(ξ)˜ε0kl(ξ)∗−ei˜σ0ij(ξ)Ωjk(e)˜σ0kl(ξ)∗el]d3ξ(2π)3, |
(8) |
Eext=−∫σextijε0ij(r)d3r−V2C−1ijklσextijσextkl, |
(9) |
∂{ηs(r,t),ηint(r,t)}∂t=−LδEtotδ{ηs(r,t),ηint(r,t)}+ζ(α,mα,r,t), |
(10) |
∂ηs(r,t)∂t=−L[πγsdsbssin(2πΔsbs)∂Δs∂ηs−σijbsinsjds]+ζ(α,mα,r,t), |
(11a) |
∂ηint(r,t)∂t=−L[πγintdintbintsin(2πΔintbint)∂Δint∂ηint−σijbintinintjdint]+ζ(α,mα,r,t), |
(11b) |
ws=|x|ηs=0.75−x|ηs=0.25| |
(12) |
Xs=∫10x(ηs)dηs. |
(13) |
The interfacial barrier to glide dislocation slip transmission is influenced by both the dislocation core changes and the cross-slip interaction between the glide dislocation and induced interfacial dislocations. The results consist of two sub-sections. In Section 3.1, the interface is assumed to be strongly bonded so that it is non-shearable, and the effect of the SFE mismatch on the dislocation core change as well as the interface resistance is investigated. In Section 3.2, the interface with weak interfacial bonding can be sheared by the stress field of the glide dislocation and the influence of the interface shear on the interfacial barrier is studied.
If the interface is non-shearable, ˉγint is viewed as infinite and we assumed ηint(r,t)≡0. For a bi-material system with the given SFE mismatch characterized by ˉγI = 1.0, ˉγII = 0.2, Figure 2 shows the change of the core width of the glide dislocation decreases rapidly during its transmission across the interface from phase II to phase I under the external shear σextyz/μ = 0.021. The change of the line is piece-wise in this figure, because the minimum resolution for the core width determined by Eq. (12) is the spatial length 0.25b. This trend of the core width change is consistent with the known predicting ws/b~1/ˉγs in elastic homogenous phases [14].
The rapid decrease of the core width near the interface would cause large energy change of the system during the transmission process. Figure 3 plots the energy change with respect to the position of the glide dislocation when it spontaneously moves from phase I to phase II with ˉγI = 1.0, ˉγII = 0.2 in the absence of applied stress. Therefore the negative derivative of the energy with respect to the position of the glide dislocation generates a resistance force for the transmission of the glide dislocation from phase II to phase I. This resistance force is originated from the energy change of the dislocation core change due to the SFE mismatch between the two phases. Figure 4 plots the profile of ηs(x) with respect to x/b at the glide plane under different levels of applied shear stress under given parameters ˉγI = 1.0 and ˉγII = 0.2. The results show that the glide dislocation can slip transmission over the interface from phase II to phase I only if the applied stress exceeds a critical value. This critical applied stress, σextyz/μ = 0.021, is equal to the maximum resistant force that should be overcome during the dislocation transmission across the interface and is defined as the interfacial barrier strength τ∗.
According to the definition of the interfacial barrier strength in Figure 4,the interfacial barrier strengths without interface shear are calculated for different ˉγI and ˉγII. Figure 5 shows τ∗ increases linearly with difference Δˉγ=ˉγI−ˉγII and is insensitive to the average ˉγavg=(ˉγI+ˉγII)/2. The calculated result is consistent with the analytic solution given by Anderson and Xin [14] in the case of no elastic mismatch. These results demonstrate that the larger SFE mismatch induces the larger dislocation core change during the transmission process and causes more rapid change of the dislocation energy near the interface, and leads to larger interfacial resistance.
When the interface has limited shear strength and it could be sheared by the stress field of the glide dislocation. To investigate the effects of interface shear, we keep ˉγI = ˉγII=1.0 and only vary the value of ˉγint. The distribution of normalized interfacial shear stress σxy/μ plotted with respect to z/b at the interface in Figure 6 clearly shows that the interface shearing could effectively counteract the shear stress concentration induced by the glide dislocation at the interface under the given parameters ˉγI = ˉγII=1.0 and σextyz/μ=0. Figs. (7), (8), plot the profiles of ηs(x) and ηint(z), respectively, under different levels of applied shear stress with the given parameters ˉγI = ˉγII=1.0 and ˉγint=0.2. Figure 7 shows that the glide dislocation cannot transmit across the interface until the external shear stress is up to a critical value. After σextyz/μ≥0.0277, the glide dislocation can slip across the interface, it indicates that the interface barrier strength is τ∗=0.0277μ. In comparison with τ∗=0 in the similar case without interface shear as simulated in Figure 5,we believe that it is the interface shear leading to the significant increase of τ∗, which is consistent with the previous results of atomistic simulation and modeling [21,22,23,24,25]. From Figure 7,the dislocation core is constricted heavily when it reaches the interface. The reason is that the interface shear can reduce the elastic energy by counteracting the shear stress, the dislocation core tends to be trapped and constricted onto the sharp interface to relieve the elastic energy.
The interface shearing at the interface results in an inelastic shear zone via nucleation and growth of interfacial dislocations. Figure 8 shows that the inelastic shear zone is noticeable when the glide dislocation is trapped at the interface under σextyz/μ=0.001, it subsequently shrinks and disappears as the increased external shear stress is up to σextyz/μ=0.0277 consistent with the glide dislocation away from the interface. It is worth to note that when the glide dislocation is trapped at the interface, there are oscillations on the profiles of the field variables as shown in Figure 7 and 8. The reason is that we use the periodic Fast Fourier Transformation to solve the elastic filed of the almost singular glide dislocation trapped in the sharp interface, and these unphysical oscillations can be mitigated when the interface is treated as diffuse. The calculated sequential contour-maps of the profiles of ηs(r,t) and ηint(r,t) during the glide dislocation transmission is shown in Figure 9. The snapshots in Figure 9 clearly show that the inelastic shear zone adaptively changes through the reversible movement of the interfacial dislocation driven by the stress field of the glide dislocation close to or away from the interface.
Figure 10 plots the profile of ηint(z) under different values of ˉγint when the glide dislocation is trapped at the interface in the absence of applied shear stress under the given parameters ˉγI = ˉγII=1.0. The results in Figure 10 show that a wider inelastic shear zone is developed for the interface with a lower shear strength. We performed numerical simulations for the glide dislocation transmission across the interface with different interfacial shear strength under external shear stress. Figure 11 plots the simulated interfacial barrier strength as a function of ˉγint under the given parameters ˉγI = ˉγII=1.0. It is found that the interfacial barrier strength significantly increases as the value of ˉγint is lower than 0.8. When the value of ˉγint is larger than 0.8, the interfacial barrier strength reaches a minimum (zero), which is the same as the prediction in the case without interface shear. Herein the enhancement of the interfacial barrier strength due to the interface shearing is neglectable. This is because the inelastic shear zone almost disappears at ˉγint=0.8 as indicated in Figure 10. These results reproduce some atomistic simulations trends revealing the “weak” interface strengthening mechanism [25].
The resistant force of the glide dislocation with interface shearing is originated from the increase of the total free energy as the glide dislocation away from the interface. Figure 12 plots the elastic energy Eelas and crystalline energy Ecryst as a function of the position of the glide dislocation Xs for ˉγint=0.2 and ˉγint=0.8 in the absence of applied shear stress. Both Eelas and Ecryst decrease when the glide dislocation is close to the interface. The interface involving interface shearing acts as an energy well, which can trap the glide dislocation at the interface. The energy well for Xs for ˉγint=0.2 is deeper and narrower than that for ˉγint=0.8. The deeper the energy well at the interface, the larger the attractive force on the glide dislocation, and the higher the interfacial barrier strength. The results in Figure 12 indicate that the attractive force is attributed to not only the elastic interaction between the glide dislocation and interfacial dislocation [12,18] but also the crystalline energy change due to the core-width change of the dislocations [16]. At the continuum scale, the dislocation core change is usually ignored in the dislocation-based models [12,18]. In such situation the resistant force on the glide dislocation is only related to the change of the elastic energy and therefore is underestimated. The current simulation results show that the change of the dislocation crystalline energy induced by the core change also has large contribution to the interfacial barrier strength, especially for the weak interface.
In summary, 3D PFM modeling and simulation are adopted to investigate a glide dislocation transmission across a coherent sliding interface. The interfacial barrier strength for the transmission is investigated with and without interface shear. In the case without interface shear, the resistant force on the glide dislocation across the interface mainly depends on the core-width change induced by the SFE mismatch, which is in good agreement with the theoretical solutions. In the case with interface shear, we show that weak interface develops a wide inelastic shear zone under the stress field of the glide dislocation, and can exert a large attractive force on the glide dislocation and thus largely enhance the interfacial barrier strength. The attractive force is attributed to both the elastic interaction between the glide dislocation and interfacial dislocation and the core change of them. The continuum model for the dislocation transmission across the weak interface without the core-width change may significantly underestimate the interfacial barrier strength.
This work was supported by the Basic Research Program of China (Grant No. 2011CB302100) and the National Natural Science Foundation of China (Grant No. 11222219, 11132009).
The authors declare no conflicts of interest in this paper.
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