A phase-field model for systems with coupled large deformation and mass transport Wei Hong1,2* and Xiao Wang2 1 Department of Aerospace Engineering, Iowa State University, Ames, IA 50011, USA 2 Department of Materials Science and Engineering, Iowa State University, Ames, IA 50011, USA Abstract Phase-field model is a powerful tool for studying the microstructure evolution of materials. This paper seeks to introduce phase-field modeling to the field of soft materials, especially for studying polymeric gels. A general framework for the field theory of coupled large deformation and mass transport is established, and two specific models of diffuse interface are proposed. The ideal liquid-like interface has a deformation-independent energy and gives rise to a constant surface tension, and a nonideal interface would result in a strain-dependent surface stress. Either model gives a stress field consistent with the effect of interface line force. The field theory is implemented into a finite-element code, and several numerical examples are calculated with representative material models in which deformation is weakly or strongly coupled with mass transport. The numerical models demonstrate the versatility of the phase-field methodology, and reveal some interesting phenomena due to the coupling. For example, the composition of a separated phase is significantly affected by the kinematic constraint, and varies during coarsening. Keywords: phase-field model, finite strain, interface model *whong@iastate.edu 1. Introduction Phase field is a versatile tool for modeling phase transition and morphological and microstructure evolution in condensed matter, and has undergone continuous development for various applications (Boettinger et al., 2002; Chen, 2002; Emmerich, 2008). In this paper, we seek to advance the theory to incorporate concurrent finite deformation and mass transportation. Besides the classic problem of diffusional solid-state transition in alloys (Cahn, 1961; Onuki, 1989a; Onuki and Furukawa, 2001), a typical problem requiring such considerations is the volumetric phase separation of polymeric gels (Shabayama and Tanaka, 1993; Matsuo and Tanaka, 1988; Shibayama and Nagai, 1999; Hu et al., 2001). A swollen gel consists of a crosslinked polymer network and a solvent. Under certain conditions, a homogeneous gel may separate into shrunk and swollen phases characterized by the drastic differences in both solvent concentration and the stretch of polymer network (Tanaka, 1979; Hochberg and Tanaka, 1979). During the phase separation of a gel, the growth of one phase is enabled by absorbing swelling liquid from its neighbors, as well as spatially replacing other phases (Shabayama and Tanaka, 1993). Understanding the physics of this model system will provide further insights towards the role of elasticity in pattern formation in soft materials during more complicate processes, such as gelation (Bansil et al., 1991; Matsuo et al., 1993; Hong and Chou, 2000), transient gel formation during 1 viscoelastic phase separation (Tanaka 2000), phase dynamics in polymer-stabilized liquid crystals (Lapena et al., 1999), vesicle dynamics (Du et al., 2004; Biben et al., 2005;), and even the growth of biological tissues (Lappa, 2004). Unfortunately, most established theoretical analysis are limited to the small-strain region (Cahn, 1961; Tanaka et al., 1985; Onuki ,1988, 1989a, b; Onuki and Furukawa 2001; Garcke, 2003) or homogeneous deformation (Hirotsu and Onuki 1989; Cai and Suo 2011), whereas the inhomogeneous stress plays an dominant role in the morphology (Nishimori and Onuki, 1990; Onuki 1999; Onuki and Furukawa, 2001) and the kinetics of pattern growth (Tanaka, 2000), and the typical strain involved is several hundred percent, for soft materials in particular. A few efforts have been made to consider finite deformation and its coupling with swelling, and interesting structures similar to experimental observation have been revealed (Onuki, 1999; Uchida, 2002; Zhou, 2010). The effect of introducing both kinematic and physical nonlinearity is yet to be discussed, and the detailed phase separation processes in these systems are far from being fully understood. Phase-field models are distinguished by two principle characteristics: a continuous phase field to differentiate domains of dissimilar microstructures (Laudau & Khalatikow, 1963), and a diffuse interface across which physical properties smoothly transition from one phase to another (van der Waals, 1894). Depending on the nature of the problem, the phase field could be an auxiliary variable (Collins and Levine 1985; Karma et al., 2001), or a physical parameter (Cahn & Hilliard, 1958; Laudau & Khalatikow, 1963; Cahn and Allen, 1977). In either case, the diffuse interface is associated with an excess free energy, which is often written as a function of the spatial gradient of the phase field. However, in a large-deformation context, it is unclear whether the gradient should be taken with respect to the deformed configuration or the reference configuration. It has recently been shown that by using the gradient in the deformed configuration, the interface energy function could recover the behavior of surface tension (Levitas and Samani, 2011). As will be shown in the current paper, such an interface model represents a liquid-like interface, on which the molecules are capable of rearranging themselves. The corresponding interface energy per unit current area is independent of the state of deformation. More generally, the interface energy may vary with deformation. For example, for a solid-like interface that preserves its atomic structure during deformation, the surface tension may be a function of strain, and is often referred to as the surface stress (Shuttleworth, 1950; Gurtin et al, 1998). Although the effect of surface tension/stress on deformation or stress field could often be neglected on macroscopic structures, it is of importance to nanomaterials (Levitas and Samani, 2011) in which the interfacial layer occupies a significant portion of the total volume, and at a much larger length scale to soft materials which deform under very low forces. In this work, we aim at formulating a general framework for the phase-field model of coupled deformation and mass transport, and developing interface models which describe the behaviors of liquid-like and solid-like interfaces. Thermodynamic theories of coupled mass transport and elastic deformation date back at least to Gibbs (1878), who formulated the equilibrium theory of a solid that absorbs liquid. The more general non-equilibrium theory that describes the transport processes is known as poroelasticity (Biot, 1941; Rice and Cleary, 1976). Specifically for polymeric gels, existing models include nonlinear poroelasticity (e.g. Srinivasa 2004; Hong et al., 2008; Duda et al., 2010; Chester and Anand, 2010), and multi-phasic 2 models (e.g. Doi 2009; Rajagopal, 2003). However, with these continuum field theories alone, it is difficult to deal with problems like phase separation, in which a boundary between domains could spontaneously emerge, migrate, and vanish. In this paper, we extend the capability of nonlinear poroelasticity by combining it with a phase-field model. In Section 2, by introducing the gradient energy terms, the basic non-equilibrium thermodynamic theory is modified to incorporation the interface contribution. Two interface models and their coupling with elastic deformation is introduced in Section 3. The theory is then specialized with a detailed material model and tested with finite-element calculations in Section 4. It is shown both analytically and numerically that the liquid-like interface model gives a thermodynamically consistent contribution to the stress field. The coupling behavior of elastic deformation and mass-transport-enabled phase separation is illustrated through several numerical examples. The effect of strong coupling and elastic misfit between separated phases is demonstrated through a numerical model by assuming the molecular incompressibility. The effect of strain-dependent interface stress is exemplified through a model with stress-induced interface anisotropy. 2. Non-equilibrium thermodynamics The microstructure evolution of a multicomponent material system usually involves mass transportation and structure reconfiguration. To track the deformation, we introduce the reference by assuming that at least some material particles do not change relative positions and the aggregate remains to be a continuum during the evolution process. An example of the background continuum frame is the polymer network of a permanently crosslinked gel. Imagine attaching to these material particles a set of markers, with coordinates X in the reference state. We will associate the properties of a material particle to the local marker, by writing the physical fields as functions of X and time t . The coordinates of a material particle at time t , for example, is written as xX, t . The field of deformation gradient, FiK X, t xi X, t , X K (1) measures the deformation of the continuum part of the material. Just as all phase-field models in a small-deformation context, we differentiate dissimilar phases using a continuous phase field, and write it also as a function of the reference coordinates and time, C X, t . The phase field may be conservative, such as the concentration of a species, or non- conservative, such the internal variable characterizing the state of damage. While the general framework is applicable to both cases, in the current paper, we will illustrate it through the conservative case, in which C represents the number concentration of a mobile species. In the current paper, we will refer to the mobile species simply as the solvent. To simplify description, we assume the homogeneous state of a material particle to be fully determined by F and C . The theory could easily be extended when more physical fields are present. Let the free energy stored in a material cell with unit volume in the reference state be 3 W F, C, C . (2) The explicit dependence of the free energy on the spatial gradient of phase field C is essential in a phase-field model. A material point on an interface differs from one in a homogenous bulk in the abrupt but continuous change of the phase field. The excess energy associated with C is the interface contribution. Although whether to take the gradient with respect to the current coordinates or the reference coordinates is a question yet to be discussed, the general form of (2) should always be valid, given the obvious relation between these two gradients: . FiK X K xi (3) In this paper, we use to represent the gradient operator with respect to the reference configuration, and x that with respect to the current configuration. To simplify presentation, we neglect all body forces and body sources. On a boundary, the potential of traction t is t x , while that of a solvent reservoir is μI , where is the chemical potential of the species in the reservoir and I is the total number of molecules entering the material from the reservoir. The material, the traction, and the reservoir constitute a thermodynamic system. In equilibrium, the total free energy of the system x, C W F, C, C dV ti xi dA IdA (4) is minimized. Utilizing the variational principle and the divergence theorem, we can write the minimization problem as X K W FiK W xi dV C X K W C ,K CdV W W ti N K xi dA N K CdA IdA 0 FiK C, K , (5) for arbitrary test fields x and C , where C, K represents the components of C , and N K those of the unit normal vector on a surface. In equilibrium, the nominal stress s W F satisfies siK 0 X K (6) siK N K ti (7) in the volume, and 4 on a surface where traction t is prescribed. Noticing the conservation of species, CdV IdA , we can deduce the equilibrium chemical potential of solvent W C X K W C ,K . (8) The equilibrium morphology of the material depends on the energy landscape in term of the phase field C . If W has a single minimum, a homogeneous phase given by W C is stable, and the dependence of W on C does not affect the equilibrium state. If W has multiple minima, the homogeneous material may simultaneously separate into coexisting phases, each corresponding to a local minimum of W . Inside the diffuse interface, the continuous phase field changes abruptly, where the local state of material differs from that in the bulk, due to the non-zero contribution from the last term of Eq. (8). The theoretical framework can be extended to model a close-to-equilibrium transient process. As phase separation is enabled by mass transport, the interface propagation is much slower than sound speed, and the inertia of the material could safely be neglected, with the partial mechanical equilibrium holds as in Eqs. (6) and (7). On the other hand, if we assume the linear kinetics on solvent migration, the nominal flux (the number of particles going through a material surface of unit area in the reference state per unit time) is related to the spatial gradient of chemical potential as J K M KL , X L (9) where M is the mobility tensor. The chemical potential is still given by Eq. (8) if we insist local equilibrium at every material point. Further substituting Eq. (9) into the conservation equation of the solvent, we arrive at the evolution equation of the phase field C C t X K M KL . X L (10) Equations (6) and (10) consist a PDE system of the time-varying fields xX, t and C X, t , and can be integrated numerically when initial and boundary conditions are properly prescribed. The nature of this thermodynamic framework is that the system is always driven towards a state of lower total energy, and the long-term solution of a closed system would be at (or close to) equilibrium, as given by Eqs. (6-8). The actual equilibrium morphology and the process of evolution is determined by the detailed form of the free-energy function W F, C, C and the mobility tensor M . In the following sections, we will illustrate the framework through some representative free-energy functions, and the different dependences on C . On the kinetics of mass transportation in finite-deformation bodies, simple models are available for materials that are isotropic in the current configuration (Hong et al,. 5 2008) or in the reference configuration (Chester and Anand, 2010). In the current paper, we will assume the kinetic properties of the material to be isotropic in the current state, and independent of deformation, so that the true flux measure with respect to the current area ji cD , kT xi (11) where c C det F is the true concentration of the solvent, D the coefficient of diffusion, and kT the temperature in the unit of energy. Using the geometric relation between corresponding quantities in the reference and current configurations, Eq. (11) can be written equivalently into the form of Eq. (9), with the mobility tensor M KL DC H iK H iL , kT (12) where H is the inverse tensor of the deformation gradient F . As this paper focuses on the general formulation of the coupled deformation and phase transition, especially on the effect of phase boundaries, the difference between various types of kinetic laws and the dependence of mobility on deformation will not be studied. In some cases, the migration of solvent and the deformation are coupled, such that the concentration C and the deformation gradient F are not independent. For example, if molecular incompressibility is assumed, such as in a swelling polymeric gel, the volumetric deformation det F is directly related to the concentration C , and consequently the phase transition is coupled with the heterogeneous deformation. In this strongly coupled case, the general constraint, det F f C , could be enforced numerically by adding to the free-energy function W , 2 det F f C 2 , (13) with a large bulk modulus . The constraint enters the expression of nominal stress as siK W det F f C det FH Ki , FiK (14) and chemical potential as W det F f C f C C X K W C ,K . (15) Alternatively, the incompressibility constraint may also be enforced by employing a Lagrange multiplier (Hong et al,. 2008). 6 The incorporation of Eqs. (14) and (15) into Eqs. (6) and (10), together with the constraint det F f C , forms a differential-algebraic system for the unknown fields xX, t and C X, t . 3. Interface models Following the usual approach of phase-field modeling, we assume the free-energy density to be the sum of three contributions: W F, C, C We F Wm C Wi F, C, C . (16) Here, We is elastic energy, and is assumed to be a function of only the deformation gradient. Wm is the energy of mixing, which is assumed to be deformation independent. Wi is the contribution from the coherent interface between dissimilar phases, and it must be an even function of C . Different from regular phase-field models in the context of small deformation, the interface energy is deformation dependent through F . Typical interfacial models that give rises to specific forms of Wi will be discussed in the following subsections. For clarity in description, we will focus on the effect of interface and leave the coupling between elasticity and mixing (i.e. that between Wm and Wi ) to the discussion on specific examples in Section 4. 3.1 Ideal interface In conventional phase-field models, a deformation-independent interface energy, Wi C C 2 X K X K , (17) is often assumed, where is a parameter controlling the magnitude of interface energy between two phases distinguished by different solvent concentrations. Such an approach assumes a phase field totally independent of deformation. For example, the equilibrium thickness of the interface between coexisting phases, measured in the reference configuration, is a constant, although the true thickness of a boundary will change with deformation in the current state. The stress field and deformation, on the other hand, is never influenced by the presence of an interface. In the small-strain limit, this treatment recovers the interface model commonly used for hard materials (Cahn 1961; Onuki, 1988, 1989a; Onuki and Furukawa 2001). Recently, Levitas and Samani (2002) propose to use the gradient (of a non-conservative phase field) with respect to the current spatial coordinates, xC , in the interface-energy function. Following their approach, we assume the interface energy of a compressible material Wi (C ) 2 det F C C (C ) C C det FH Ki H Li . xi xi 2 X K X L 7 (18) Substituting the energy functions in Eqs. (16) and (18) into the equations of state, (14) and (15), we have the nominal stress siK We C C C C det FH Mj H Li H Ki det FH Mj H Lj H Ki , FiK X M X L 2 X M X L (19) and the chemical potential dWm 1 C C C det FH Li H Ki det FH Ki H Li dC 2 C X K X L X L X K . (20) The physical significance of the added terms in the stress expression can be made clear when written in the current configuration. Utilizing the simple geometric relation, σ det F s F , we have the true stress ij FjK We C C C C ij . det F FiK xi x j 2 xn xn (21) Compared to the through-thickness tress (in the direction of C ), the hoop stress along the interface is higher by xC . As shown in Appendix, in equilibrium, the total excess energy per unit current 2 volume of a diffuse interface equals xC . Therefore, the added hoop stress equals the excessive 2 energy per unit volume in the current state. By integrating through the thickness of an interface, the resultant line force, i.e. the interface tension, equals the interface energy per unit area in the current configuration. Through this analysis, it is clear that the interface-energy function, Eq. (18), results in an ideal interface, namely a liquid-like interface of which neither the actual thickness in the current state nor the surface tension depends on deformation. The inclusion of this energy function provides a thermodynamically consistent means of introducing the effect of interface tension to a phase-field model with coupled mechanical deformation. 3.2 Non-ideal interface In this section, we will construct an interface-energy function for the mechanical behavior of a non-ideal interface. The interface or surface of a solid differs from that of a liquid when the solid is subject to deformation. Due to the permanent structure of a solid interface, the surface stress, namely the resultant force per unit length on the interface is dependent on the local deformation state (Gurtin 1998; Fischer et al,. 2008). In the limit of small deformation, surface stress is often treated to be linearly proportional to the in-plane strain of an interface. Although the choice of the energy function for an ideal interface is quite limited, that for a non-ideal interface is more or less arbitrary – almost any functional of the concentration gradient and the deformation gradient other than Eq. (18) would give 8 non-ideal behaviors. Inspired by the fact that the presence of surface stress is a consequence of the different solid structure on the interface between two materials, we take a modified form of the elastic energy density as the interface contribution: Wi C C 2 X K X K We F . (22) Here, the parameter measures the stiffness of the interface relative to the bulk. The corresponding nominal stress reads siK We FiK C C 1 , 2 X X L L (23) and the chemical potential dWm C We F . dC X K X K (24) Along the interface, where the non-vanishing gradient of phase field C exists, the stiffness of the material is effectively increased by 2 C . The resultant force per unit length of the interface, i.e. 2 the interface stress, is dependent on the local deformation through We F . In the small-deformation limit, the interface stress is also linear in the strain tangential to the interface. 4. Numerical examples In this section, the theoretical framework of coupled deformation and phase field, together with the two interface models will be illustrated through some representative examples. As the examples are created for the illustration purpose, we will not take specialized material models. Instead, we use a compressible neo-Hookean model for the elastic energy of deformation: We G FiK FiK 3 2 ln det F det F 12 , 2 2 (25) and the regular solution model for the energy of mixing: Wm kT det F ln 1 ln 1 1 , (26) where G is the initial shear modulus, the bulk modulus, and c the volume fraction of the solvent, with being the volume occupied by each particle. The first two terms in the bracket of Eq. (26) is the entropy of mixing, while the third represents the enthalpy of mixing. Consider the simple case when the elastic deformation and phase field variable are decoupled, the phase stability is 9 determined entirely by the energy of mixing, and the interaction parameter controls the thermodynamics stability of system. The system has a critical point at 2 . When 2 , the energy of mixing has a single well, and a homogeneous phase is stable; when 2 , the energy of mixing has double wells, and a mixture with initial composition satisfying 2Wm 2 0 separates into two phases spontaneously. Besides , the system has two more dimensionless parameters: the dimensionless stiffness G kT , and the relative compressibility G . To demonstrate the coupling effect, we consider a relatively soft material with dimensionless stiffness G kT 0.1 (note that the dimensionless energy of mixing Wm kT is on the order of 0.1 for intermediate values of ). The competition between the energy of mixing and the interface contribution gives rise to an intrinsic length L0 / kT . In the case of a phase transition physically decoupled from deformation, the thickness of an equilibrium phase boundary scales with L0 , which may be a means of estimating the actual value of parameter . The following calculations are carried out with dimensionless variables, by normalizing all lengths with L0 , all energies with kT , and time with L20 D . We implement the coupled large deformation and phase-field model, specifically the equation system (6), (10), (14) and (15), into a finite-element code through the commercial software COMSOL Multiphysics 4.2a. The concentration C and chemical potential are interpolated using linear elements, while the displacement field is interpolated with quadratic Lagrange elements. To ensure accurate representation of the interface, a uniform mesh of element size no larger than L0 3 is used. In the fully coupled deformation and phase transition model, the deformation is often unstable, involving various types of mechanical instabilities, such as the coalescence of two more swollen phases. In the general formulation described in Section 2, as the volumetric strain is coupled with the field of concentration by the incompressibility constraint (13), the dilatational deformation of the material is limited by the mass transportation process given by Eq. (10). The deviatoric part of the deformation, however, is undamped. A local pure shear deformation, which involves no solvent migration, takes place instantaneously whenever it is energetically more favorable. Numerically, an instantaneous deformation may cause convergence issues in the nonlinear solver. To stabilize the numerical procedures, we slightly damp the system by introduce a viscous dissipation term to the energy functional (Wang and Hong 2012), where d ij 1 2 v i 2 det F dij dij 13 dii x j v j xi is the strain rate 2 tensor, and is the artificial viscosity. The characteristic time for viscous deformation is set to be much shorter than the diffusion time of a single element to avoid numerical artifact. 4.1 Weakly coupled phase transition and deformation We will first consider the special case, when the phase field variable is decoupled from elastic deformation, to verify the numerical method and the analysis of surface tension and surface stress in 10 Section 3. Here, the decoupled physics indicates that the state of mixing does not contribute to deformation, i.e. the material does not swell upon solvent intake, and thus there is not elastic misfit between phases. However, the stress field is still influenced by the structure of coexisting phases, due to the presence of the interface tension. We therefore refer to this case as the weakly coupled system. To enable phase separation, we set 2.5 , so that the energy of mixing, Eq. (26), has double wells at 0.145 and 0.855 . By assuming the material to be nearly incompressible, i. e. det F 1, the two energy minima correspond to the concentrations of the coexisting phases, C 0.145 and C 0.855 . As the elastic deformation is physically decoupled from the phase transition behavior, no numerical damping is necessary in this case. We will examine the structure and mechanical contribution of an equilibrium interface through two numerical examples: 1) a large bi-phase domain divided by a straight interface, and 2) a circular interface surrounding an island of dissimilar phase in a large domain. In the first example, a square sample much larger than the interface thickness ( 50 L0 50L0 ) with a phase boundary in the middle is calculated. As initial conditions, the concentration in the left half domain is C 0.145 while that on the right is C 0.855 , and a smooth transition is prescribed in between. Mechanically, the sample is subject to uniaxial tension in the vertical direction, and is free to deform laterally, as sketched in Fig. 1a. The system is then given ample time for relaxation to equilibrium. The solvent transportation is subject to a periodical condition on the top and bottom boundaries, and a zero-flux condition on the side boundaries. The additional normal stress due to the presence of the straight interface ( y minus its value far from the interface) is plotted in Fig. 1b. The integration of this stress across the interface region would result in the surface tension, 0.184 L0kT for the material parameters chosen. The numerical results also show that this stress equals the excessive free energy Wm Wi compared to the background homogeneous phases, just as proven in Appendix. Fig. 1b also shows that the structure of the interface, as well as the excessive stress due to the interface, is independent of the deformation in the current configuration, within the error of the numerical calculation. The deformation independent interface behavior is a direct consequence of the physically decoupled model assumption. 11 Excessive stress /kT y Phase 2 Interface b Phase 1 a 0.08 y (=0) y (y =10%) 0.06 y (y =20%) W m+W i 0.04 0.02 0 -10 -5 0 5 Deformed coordinates x/L0 10 Fig. 1. (a) Sketch of the bi-phase sample calculated. (b) Equilibrium distribution of the excessive stress and free energy near an ideal interface in a large, weakly coupled system. The stress under different strain values are plotted, all in the deformed configuration, as functions of the dimensionless coordinate x L0 . Using the same setup, we also test the effect of interface stress by using the non-ideal interface model described in Section 3. To demonstrate the surface-stress effect, we pick a (maybe non-physically) high dimensionless parameter 50 . The same interface energy, Eq. (18), as in the ideal case, is retained to enable phase separation in absence of strain. The same values of all other material parameters as in the previous case are taken. The resulting distribution of the hoop stress across a straight interface is plotted in Fig. 2a. To show the effect of the interface, the background stress, i.e. that in a homogeneous state is deducted. At zero strain, the interface effect is identical to the idealinterface case. When the material is stretched, as the change in interface energy is relatively small, the weak coupling still results in an almost constant interface thickness in the deformed state, as shown by Fig. 2a. We then integrate the excessive stress through the interface thickness, and plot in Fig. 2b the resultant line force as a function of the strain along the interface. As a positive value of is used, the interface tension f is a monotonically increasing function of strain. In the small-strain limit, the relation is linear, with the dimensionless interface stiffness (i.e. the slope of the interface tension-strain curve) f GL0 0.18 . In the model presented here, the interface stiffness slightly decreases at a relative large strain. Such an effect is due to the specific form of the interface energy function (22), as the concentration gradient with respect to the reference configuration would decrease when the material shrinks laterally. If a specific form of the surface stress-strain dependence is needed, Eq. (22) may be modified accordingly. 12 b 0.1 0.08 0.06 =0 =0.06 =0.12 =0.2 0.04 0.02 0 0.12 Interface force f /L kT Excessive stress /kT y a 0 0.25 0.2 0.15 0.1 0.05 0 -5 0 5 Deformed coordinates x/L0 0 0.05 0.1 Strain 0.15 0.2 Fig. 2. Behavior of a non-ideal interface. (a) The equilibrium distribution of the excessive stress near a straight interface in a physically decoupled system. The stress under different strain values are plotted, all in the deformed configuration. (b) The resultant interface force, plotted as a function of the strain along the interface. In the second example, we study the equilibrium interface structure of a circular island of dissimilar phase. The computational domain is shown by Fig. 3a. Symmetric boundary conditions are taken on the left and bottom edges, while the top and right edges are left traction free. Due to the presence of interface tension, the pressure inside the circular island is higher than that outside. For clarity, in this example, we only use the ideal interface model, Eq. (18). Fig. 3a plots the equilibrium pressure distribution for an island of radius 10L0 . We then vary the radius of the island r and plot the pressure drop across the interface as a function of the normalized curvature L0 r in Fig. 3b, and compared it to the Laplace-Young equation, p r (with the numerical value of surface tension 0.184 L0kT obtained from the previous example). The good agreement with the Laplace-Young equation numerically verifies the consistency of the interface-energy formulation. The results in Fig. 3b also shows that this formulation tends to overestimate the interface effect when the size of the domain is comparable with the interface thickness. Since the distribution of fields through the thickness of an interface is given by the artificially prescribed interface energy function, the phase-field method is thus incapable of predicting the behaviors taking place at a length scale comparable to the interface thickness. To ensure numerical accuracy, domain size (or radius of curvature) needs to be at least one order of magnitude larger the interface thickness. 13 a Pressure drop p /kT b p kT 0.02 0.015 0.01 0.005 0 0.02 p=/r numerical results 0.04 0.06 0.08 Normalized curvature L0/r 0.1 Fig. 3. (a) Distribution of the normalized pressure p kT in a system with a circular island of radius 10L0 . (b) The pressure drop across the interface, plotted as a function of the normalized curvature L0 r , and compared with the Laplace-Young equation, p r . 4.2 Strongly coupled phase transition and deformation We will now illustrate the model through an example of strongly coupled phase field and elastic deformation. In this example, the molecular incompressibility of solvent is assumed, so that the substrate expands upon intake of the solvent. The elastic energy of deformation is slightly modified to incorporate this coupling: We G FiK FiK 3 2 ln det F det F 1 C 2 . 2 2 (27) In the limit when the mixture is incompressible, the large bulk modulus enforces the constraint commonly invoked in modeling polymeric gels (Hong et al,. 2008; Doi 2009), C det F 1 . (28) In the numerical calculations, we take a relatively large bulk modulus 103 G , so that the constraint is approximately satisfied. Due to the strong coupling, the condition for phase separation is different from that given the energy of mixing only. Using constraint (28), the dilatational part of the elastic energy can be written as a function of C , which in turn is related to the volume fraction as 1 C 1 1 . The phase separation behavior is coupled with elastic deformation not only through the coupled free energy, but also via the kinematic compatibility between dissimilar phases that are highly distorted. To demonstrate these two levels of coupling, let us first look at the contribution from the coupled free energy. By neglecting the kinematic compatibility, we imagine the scenario in which both phases deform homogeneously and freely. In a plane-strain deformation state with the through-thickness stretch 0 , 14 the isotropic in-plane stretch 1 C 0 , and the free energy per unit current volume of the material Wm We G2 kT ln 1 ln 1 1 20 3 1 G1 ln 1 .(29) det F 2 0 The dependence on 0 is not very strong. For illustration, we take 0 1.1 and plot Eq. (29) in Fig. 4 against the non-coupled energy of mixing. Even with the mechanical constraints between dissimilar phases neglected, the phase separation behavior given by Eq. (29) is already very different from that in the decoupled case. Using the same dimensionless parameter 2.5 , the energy landscape is still non-convex and phase separation is possible, but the volume fractions for the coexisting states have shifted to 1 0.168 and 2 0.815 , which correspond to the normalized concentrations of C 0.201 and C 4.41 , respectively. It is noteworthy that a misfit of approximately 4.21 in relative volume expansion is present between the two phases. The large misfit would essentially invalidate the homogeneous assumption. Free energy W /kT 0.1 Decoupled Coupled no constraint 0.05 0 2 -0.05 1 -0.1 0 0.2 0.4 0.6 Volume fraction ( ) 0.8 1 Fig. 4. The free-energy profile in a homogeneous system with coupled deformation and phase field variable compared to that of a decoupled system. 15 t=2×103 t=500 t=1×104 C t=5×104 t=2×105 t=2×103 t=1×104 t=5×104 t=2×105 t=2×103 t=1×104 t=1×106 Low concentration 0 0.3 t=500 Mid concentration t=1×106 0 0.43 t=500 High concentration t=5×104 t=2×105 t=1×106 0 0.55 Fig. 5. Evolution processes in a system of strongly coupled phase transition and deformation. Snapshots at various times during the phase-separation processes are presented, with the dimensionless times indicated on each plot. The deformation is shown by distorted mesh (drawn to scale), and the normalized solvent concentration is shown by the color scale. 16 Now let us include the effect of kinematic constraints between coexisting phases. Using the same set of material parameters, we numerically solve the phase-field equations in a square unit cell measured 300L0 in width. On all four boundaries, periodical boundary conditions are prescribed for both the displacement of the matrix material, and the concentration C and chemical potential of the solvent. The initial condition is taken to be a close-to-uniform distribution of solvent, with large enough perturbation to enable the nucleation of dissimilar phases. The simulation is started from three initial concentrations, with corresponding volume fractions of solvent 0 being 0.3, 0.43, and 0.55. Snapshots of the evolution processes are shown in Fig. 5. Just as in regular spinodal decomposition, the amplitude of initial fluctuation grows with time, followed by the coarsening of phases to reduce interface energy. Depending on the initial concentration, the coexisting phases exhibit the morphologies of solvent-rich islands (at a relatively low concentration), labyrinth pattern (at an intermediate concentration), and solvent-poor islands (at a relatively high concentration). Due to the large volumetric mismatch, the separated phases are distorted, i.e. the deformation is highly non-uniform, especially near the phase boundaries. The large distortion, together with the interface tension, gives rise to a non-uniform stress field, even in a close-to-equilibrium state. We plot the distribution of hydrostatic pressure in different phases in Fig. 6. The states plotted here correspond to the final states after long-time evolution shown in Fig. 5. The representative dimensionless pressure p kT 0.5 has a non-negligible contribution to the chemical potential of solvent. Due to the large volume expansion, the solvent-rich phases always bare higher pressure. The numerical results demonstrate that the effect of mechanical mismatch dominate over that of interfacial tension, especially for coarser phases. Due to the different dependencies of the elastic strain energy and the interface energy on the size of an island of dissimilar phase (the former scales with the area while the latter scales with the circumferential length), for large enough islands, the elastic contribution always wins. p kT Fig. 6. Distribution of hydrostatic pressure at close-to-equilibrium states of phase separation with coupled elastic deformation. The three images correspond to the last stages of the three evolution processes in Fig. 5. The solvent-rich phase is always under higher compression. In contrast to the behavior of a liquid solution, the presence of the kinematic-constraint-induced stress causes the composition of each phase to be dependent on its size during the coarsening process. 17 Even at equilibrium, the solvent concentrations in the coexisting phases differ significantly from the prediction of the homogenous model by neglecting the constraints. As shown by Fig. 5, the difference is more significant in the solvent-rich phases, where the actual concentration C 2.8 is much lower than that given by Fig. 4, C 4.41. The size-dependent composition change in the coarsening stage may lead to non-self-similar growth, a phenomenon previously solely explained by the dynamical asymmetry of individual phases (Tanaka 2000). The material-specific details of the difference between these two processes are not well studied, but the discussion is beyond the scope of the current paper. To illustrate the effect of an non-ideal interface, we add to the numerical model the contribution from Eq. (22) and take the dimensionless parameter 10 . The initial boundary conditions are taken to be the same as that in the low-concentration case of the ideal-interface simulations (Fig. 7). All parameters are taken to be the same, except that an initial strain 0 10% is added to the unit cell of computation in the horizontal direction, as sketched in Fig. 7. Snapshots at different stages during the evolution process are also shown in Fig. 7. Due to the presence of straindependent interface stress and the applied strain, the microstructure evolution is no longer isotropic. As interface energy increases with strain, forming a horizontal phase boundary is energetically more expensive than forming a vertical one. As a result, the separated solve-rich phase takes the shape of an ellipse, with the longer axis perpendicular to the direction of applied strain. In other words, the phase boundaries exhibit higher curvature (larger tension) on horizontal segments than vertical segments. Although the results are not shown here, similar phenomena could also been observed on simulations under other solvent concentrations. ε0 ε0 t=2×103 t=500 t=1×104 C t=5×104 t=1×106 t=2×105 Fig. 7. Evolution process in a system of strongly coupled phase transition and elastic deformation. The unit cell is under horizontal tension of 10% strain. A non-ideal interface model is adopted so that the interface stress increases with strain. The deformation is shown by distorted mesh, and the normalized concentration is shown by the color scale. 18 C t = 3×106 t = 4×106 t = 5×106 0 0.87 t = 1.2×107 t = 8×106 t = 1.5×107 Fig. 8. Snapshots during the phase-separation processes of a PNIPAM gel, with the dimensionless times indicated on each plot. The deformation is shown by distorted mesh (drawn to scale), and the normalized solvent concentration is shown by the color scale. By adopting material-specific free-energy functions, our theory can be readily applied to the phase separation of polymeric gels. As the last example, we consider the thermo-sensitive Poly(Nisopropylacrylamide) (PNIPAM) hydrogel by replacing the energy of mixing in Eq. (26) with the FloryHuggins-Staverman model: Wm kT det F1 ln 1 1 . (30) The enthalpy of mixing depends on temperature and concentration as 0 1 (1 ) , 0 12.95 0.04496T , 1 17.92 0.05690T (Afroze et al, 2000). Here for simplicity, temperature T is assumed to be uniform. PNIPAM gel is known to be swollen at lower temperature and collapse with a phase transformation at T 307 K , depending on network stiffness. In the numerical example, we test a initially homogenous gel with swelling ratio det F 8 ( 0 0.87 ), and overheat it to an unstable temperature T 314K . The interface between swollen and shrunken phases is assumed to be liquid like. We assume the gel to be large enough, and only look at a representative block in the middle by neglecting the solvent loss from free surfaces. As shown by Fig. 8, a sponge structure gradually forms with highly swollen domains embedded in a network of shrunken domain, similar to experimental observations (e.g. Hu et al. 2001). Details of this process, however, fall out of the focus of the current paper. Nevertheless, comparison between the simulated morphology and that observed may provide another means of estimating the magnitude of some physical 19 parameters. For example, by comparing the results shown in Fig. 8 to the experimental observation (Hu et al. 2001), we estimate the characteristic length L0 ~ 2nm and an interface energy of ~ 0.08 J m 2 . 5. Conclusions In this paper, the general framework for a phase-field model with concurrent finite deformation and mass transportation is constituted. On top of this framework, several diffuse interface models have been proposed and their properties studied theoretically and numerically. It has been shown that under the finite-deformation context, the interface models give rise to a stress field consistent with the line force exerted by the interface, i.e. they recover the classic Laplace-Young equation. Specifically, an ideal interface, which has liquid-like properties, would induce a deformation-independent surface tension. A solid-like non-ideal interface, on the other hand, can give rise to the more general strain-dependent surface stress. The coupled phase-field model is further implemented in to a finite-element code to enable numerical simulations for both weakly coupled and strongly coupled systems. In the weakly coupled system, the stress and elastic deformation is influenced by phase transition through the interface effect, but both mass transport and phase transition are deformation-dependent. In the strongly coupled system, on the other hand, the phase transition and elastic deformation are coupled through molecular incompressibility. Due to the kinematic constraint between dissimilar phases with drastically different strains and the resultant inhomogeneous stress fields, the compositions in the coexisting phases differ from that predicted by a homogeneous model. In contrast to the commonly accepted view of spinodal decomposition, the composition varies with time as the island size of each phase coarsens. The effect of strain-dependent surface stress on phase transition is demonstrated through a numerical example, in which anisotropy is introduced by a uniaxial stretch on the originally isotropic material. As a practical example, we apply the framework to study of phase-separation process of a thermo-sensitive gel and the calculation reveals the formation of a sponge-like structure. By introducing finite-deformation phase-field modeling to the mechanics of soft materials, it is foreseeable that the theoretical framework and numerical procedures can be used to study various intriguing phenomena, such as gelation, microstructure evolution, damage initiation and propagation. Appendix The purpose of this appendix is to show that the excess energy per unit volume on an ideal diffuse interface, as defined by Eq. (18) in Section 3, is det F xC . Consider the spatial gradient of 2 the energy of mixing Wm in an equilibrium state: Wm dWm C . dC Assume the size of an equilibrium phase to be much larger than the characteristic thickness of the interface, so that the phase boundary can be regarded as close to straight and infinitely long when 20 (A.1) studying the through-thickness change of the fields. Let us now construct a local coordinate system with one axis, , along the normal direction of the interface in the reference configuration (i.e. the direction of C ). Equation (A.1) can be rewritten in the local coordinates as We Wm We dWm C . dC (A.2) If we further neglect the shear deformation along a phase boundary, the normal of the surface would coincide with a principal direction of the deformation gradient. Let be the stretch along the axis. Utilizing Eq. (20), we further write the gradient of Wm as 2 Wm 1 det F C det F C C . 2 2 C 2 (A.3) Here, without losing generality, we have taken the equilibrium state to be the reference for the chemical potential, 0 . 2 We Wm We det F C 2 2 det F C 2 . 2 2 (A.4) The normal stress across the interface is continuous 2 We det F C s . 2 2 (A.5) Integrating Eq. (A4) along yields 2 det F C We Wm s W W s , 2 2 0 e 0 m 0 (A.6) where the quantities with superscript 0 represent those in a homogeneous bulk phase. Adding the contributions from We and Wm in Eq. (A.6) to Eq. 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