Xiao-Wei Guoab,
Shun Zoua,
Xuejun Yanga,
Xue-Feng Yuan*ab and
Miao Wanga
aState Key Laboratory of High Performance Computing, National University of Defense Technology, Changsha, Hunan, China
bSchool of Chemical Engineering and Analytical Science, Manchester Institute of Biotechnology, University of Manchester, Manchester, M13 9PL, UK. E-mail: xuefeng.yuan@nscc-gz.cn
First published on 7th November 2014
A unified model by combining the Rolie–Poly constitutive model and the Flory–Huggins mixing free energy functional through a two fluid approach is presented for studying flow-induced phase separation in polymer mixtures. It is numerically solved in two-dimensional flow with monotonic and non-monotonic constitutive behaviour. The results are analyzed and show that this model can capture the essential dynamic features of viscoelastic phase separation reported in literature. The steady-state shear-banding and interface instabilities are reproduced. In the case with a non-monotonic constitutive behaviour, It is observed that the band structures are strongly unstable both in time and in space. The correlations between the microstructure evolution and chaotic rheological responses have been identified. A vortex structure emerges within the central band. Numerical results obtained from this study suggest that the dynamic features of rheochaos can be captured by the proposed model without introducing extra parameters.
A typical experimental system targeted by this work is the Couette cell described in ref. 8. Fluids are contained in the gap between the stationary inner cylinder and the rotating outer cylinder. Various shear rates are applied by superimposing different angular velocities to the rotating cylinder. Focused on the bulk fluid behaviour, we simulate the shear flow in a rectangular region. A commonly accepted idea is that the flow field can cause stress imbalance between different components of polymer mixtures and relative motion can thus take place. By an adequate formulation of polymer blends, and careful control of temperature and flow fields, it is possible to manipulate the morphology of materials in micromorphological engineering.
Phase separations in classical binary fluids have been extensively studied both experimentally and theoretically over several decades.16 Theoretical frameworks for modelling the effect of flow on phase transitions in polymer mixtures must incorporate both thermodynamic and viscoelastic forces into dynamic equations. Most theoretical research are based on the two fluid model, which combines thermodynamics, hydrodynamics, and viscoelasticity in a natural, physical way.
Few numerical results were presented for the two fluid model, especially regarding the effects of flow on phase diagram. Most of the early solutions of the two fluid model were obtained from approximations to the model, such as linearization of the diffusive equation and the adiabatic approximation,17–19 in which time dependence of the viscoelastic stress tensor was not considered to seek a possible steady state solution. Some recent research20–22 aim to numerically study the phase separation in a binary fluid, and large scale 2D and 3D simulations are carried out, but in absence of a realistic constitutive model, all of them can not accurately capture the viscoelastic effects. Modeling the phase separation in viscoelastic complex fluids with a realistic model remains elusive.
Jupp and Yuan23–25 presented a two fluid model (FH–JS model) to investigate the flow-induced phase mixing and demixing of polymer mixtures, which coupled the Flory–Huggins mixing free energy function and the Johnson–Segalman constitutive model in a unified way. The numerical results were obtained by solving the time-dependent two fluid model without any simplification used widely in early studies. Fielding and Olmsted26,27 proposed a different version of the two fluid model for the coupling between shear banding and shear-induced demixing, which still retained a diffusive stress term in the J–S constitutive equation. It is questionable whether or not such an ad hoc treatment for mechanical interface is justifiable as the origin of the diffusive stress is molecular diffusion across the streamlines and has already been considered in a thermodynamically consistent way in the original two fluid model.
Moreover, the J–S model is a phenomenological constitutive model. The Rolie–Poly model28 is a simplified version of the full molecular model based on the tube dynamics,29 yet still includes all dynamic modes considered in the full theory, including the reptation, chain stretch, contour length fluctuation, and thermal/convective constraint releases (CCR). Many numerical results30–33 were carried out using a diffusive Rolie–Poly model, which verified that the Rolie–Poly constitutive model has the capability to accurately capture the rheological responses in a complex fluid. Recently, Cromer34 predicted the steady-state shear-banding with Rolie–Poly constitutive model for a monodisperse polymer solution, which coupled the concentration and the stress through a two-fluid approach, but only one-dimensional calculations had been presented. To the best of our knowledge, this is the first attempt to couple the Rolie–Poly constitutive model with a two fluid model without adding a diffusive stress term. However, compared to Cromer's model, the framework of FH–JS model23–25 is more general and can model not only the polymer solutions with a reduced formulation but also the binary polymer mixtures in which both of components are viscoelastic.
In this study, the FH–JS model is modified by replacing the J–S constitutive model with the Rolie–Poly model. It is not only inherent all the advantages of the original model, but also can accurately capture polymer dynamics in flow-induced phase separation. Simulation work focuses on the shear-induced phase transition of polymer mixtures in which the volume fractions of the two components are equal. Both of transient and steady-state phase transition behaviour and corresponding rheological responses will be presented. In some cases, rather than reaching a steady state, the numerical results show erratic fluctuations. This phenomenon, often named as rheochaos, has been observed in many complex fluids, including wormlike micelles,35–37 associative polymer networks11 and lamellar phase systems.38,39 In order to capture the key features of chaotic flows, several models40,41 have been studied by introducing some coupling parameters between flow and microstructure. Numerical results presented in this study demonstrate that the dynamic features of rheochaos can be captured by our model without introducing any extra parameters. The correlations between microstructure evolution and chaotic rheological responses are also identified.
The remainder of the paper is organized as follows. In the next section a detailed description of the two fluid model integrated with the Rolie–Poly constitutive model is presented. Detailed numerical algorithms used in this paper are described in Section 3; Simulation results and discussions are provided in Section 4, in which the dynamic phase separation and rheological behaviour for both monotonic and non-monotonic constitutive relationships are analyzed through numerical simulations implemented using finite volume method. Section 5 contains our conclusions.
To establish a theoretical framework for describing the phase separations of polymer blends, we coupled the Flory–Huggins free energy function with the Rolie–Poly constitutive model. The two-fluid model provides a physical approach to capture the inhomogeneous polymer dynamics. In the standard framework of the two-fluid model, the system consist of two components: the polymer and the solvent. A constitutive equation is required to describe the viscoelastic stress of the polymer component, and the solvent is pure Newtonian.
Compared to the original two-fluid approach,19,42,43 there are two main distinctions in our model. Firstly, both components are viscoelastic, and some mixing rules are introduced for calculation of the viscoelastic stress. This general formulation for binary polymer mixtures can be easily reduced to the standard two-fluid framework. Secondly, we replace the phenomenological constitutive model with a molecular-based model: Rolie–Poly model, which can provide more realistic predictions of the viscoelastic response under flow.
For polymer blends with two components, let ϕA(, t) and ϕB(
, t) be the volume fractions of the component A and component B at some point
and time t, and let
A(
, t) and
B(
, t) be their velocities, respectively. The volume average velocity
is given by
(
, t) = ϕA
A(
, t) + ϕB
B(
, t). The evolution equation for the volume fraction follows is given by the conservation law of mass, and may be written in terms of the volume average velocity:
![]() | (1) |
The essential term of eqn (1) can be expressed by the velocity difference between the two components, which depends on the osmotic force, μ and the force due to inhomogeneity in polymer viscoelastic stress,
·σve:
![]() | (2) |
For the polymer inhomogeneity, we introduce a dimensionless coefficient α, and different from the previous work, the ratio of relaxation times is replaced by the ratio of the entanglements number,
![]() | (3) |
The osmotic force can be computed by the chemical potential difference μ, which is defined as the functional derivative of the mixing free energy with respect to local volume fraction, i.e.,
![]() | (4) |
Here we take the first order approximation of Flory–Huggins free energy function form44,45 as
![]() ![]() ![]() | (5) |
Apart from the osmotic force, another force the polymer experiences is the viscoelastic stress σve(, t), which can be calculated by constitutive equations. In our model, we replace the original JS model with the Rolie–Poly model. As the stress in entangled polymer systems is supported by chain molecules, a stress gradient would create a net force on the chains resulting in their relative migration. Thus
T should be used in the viscoelastic constitutive equation rather than
.
The tube velocity given by , may be expressed in terms of the volume average velocity by
![]() | (6) |
The relaxation modulus of a binary viscoelastic fluid must depend on its composition. For polymer linear blend, the relaxation modulus may be described as G(t) = GR(t) + Gd(t), where GR(t) describes the high-frequency polymer relaxation (Rouse process) and Gd(t) describes the disentanglement process of the chains. For the Rouse process, the linear mixing rule46 is adopted as,
![]() | (7) |
The ‘double reptation’ rule offers much better agreement with experimental data than the ‘linear mixing rule’ for disentanglement process, hence a quadratic mixing rule is suggested in the form47,48 of
![]() | (8) |
![]() | (9) |
In this representation the quantity Wi is the viscoelastic strain and stress GiWi is parameterized by the elastic modulus Gi. According to the mixing rules, the elastic modulus can be expressed as GAA = ϕAGAR + ϕA2GAd, GBB = ϕBGBR + ϕB2GBd and . Accordingly the relaxation times can be written as τAAd = τAd, τBBd = τBd and τABd = 2τAdτBd/(τAd + τBd). For the Rouse time, there is no interactive part, so τAAR = τAR, τBBR = τBR and τABR = 0.
After applying the mixing rules to the Rolie–Poly constitutive model, the evolution equation of viscoelastic strain Wi may be written as,33
![]() | (10) |
![]() | (11) |
![]() | (12) |
![]() | (13) |
fAB2 = β | (14) |
We assume, for simplicity, that the components are of equal density, ρ. The motion of an incompressible, isothermal viscoelastic binary fluid is governed by the continuity equation
![]() | (15) |
![]() | (16) |
The equations above complete the Flory–Huggins–Rolie–Poly (FH–RP) fluid model in this study. The parameter β is the CCR magnitude coefficient and δ is an exponent to quantify the CCR. For simplicity, but without much loss of generality, the same value for β and δ for the three parts of σve is assumed. By exploring the parameter space of the FH–RP model in terms of η0, τAR, τAd, τBR, τBd, GAR, GBR, GAd, GBd (Gi = GiR + Gid) and shear rate, the details of nonlinear dynamic behaviour in shear-induced phase transition of polymer mixtures could be systematically studied.
The iterative solution algorithm used in this paper is a PISO-based algorithm, which have been well tested in a numerical study for the dynamics of polymer solutions in contraction flow.50 The numerical method involves a modification to the standard PISO algorithm by introducing polymer stress and the chemical potential unknowns into the momentum equation, as a part of the source term. In the absence flow, our simulation could reproduce the equilibrium phase behavior defined by the Flory–Huggins mixing free energy functional. Also the simulation results of homogeneous fluids under shear flow converge to the solution of the constitutive model with satisfactory accuracy. Moreover a similar OpenFOAM based viscoelastic flow solver has been critically validated under benchmark flow problems.50
We summarised the key procedure of the iterative algorithm as follows
Step 1: assuming νn+1 = νn, integrate the constitutive equations implicitly to get the polymer viscoelastic stress components, σve(, t)n+1.
Step 2: compute the force field μ and
·σve, then solve eqn (1) to get ϕn+1A.
Step 3: solve the momentum equation without the contribution of the pressure gradient term to obtain the estimated velocity components Un+1.
Step 4: use the estimated velocity Un+1 to solve the pressure-correction equation of PISO algorithm, get the pressure field pn+1.
Step 5: use the estimated pressure field pn+1 to calculate the corrected velocity field νn+1.
Step 6: use the corrected velocity field νn+1 to solve the constitutive equation and the composition field evolving equation (eqn (1)) again to get the corrected stress field and the corrected composition field.
Step 7: repeat the steps 3–6, using the corrected variable νn+1, pn+1, σve(, t)n+1 and ϕn+1A as improved estimates until all corrections are negligibly small for the solutions at the present time.
Step 8: repeat from the step 1 and advance to the next time step.
Here the superscript n and n + 1 represent the past and the present times, respectively. The numerical scheme solves the non-linear governing equations in time and it is capable of modeling the unsteady flow.
For simplicity but without much loss of generality, the parameters are set as: MA = MB = 1, kBT = 1.3, Γ = 1, ζ = 0.1, η0 = 0.1. Thus the equilibrium phase diagram is always symmetric with respect to ϕA = 0.5. The critical point is at χ = 2. Therefore, χ = 1.0 for the FH–RP fluid means far away from the phase-coexistent region at equilibrium and the fluid is homogeneous for the entire composition range at this temperature.
A Gaussian random noise with an intensity of 10−3 was superimposed on a specified initial uniform composition field ϕ0A = 0.5 in all simulations reported here. Each component of the viscoelastic stress tensor σve, including σi, = 1, 2, 3, are initially set to zero. A wall velocity of U0 = (L/2) is applied to the top and bottom walls in equal speed and opposite direction to achieve a required shear rate
, where L is characteristic length (distance between the walls).
By choosing appropriate values for the parameters β, δ, Gi, τid and τiR, the FH–RP model exhibits different constitutive behaviour. Both of the monotonic and non-monotonic constitutive relationships will be analyzed in the following sections.
Kabanemi and Chung31,32 set a much lower value of β, and in some cases β = 0 to produce non-monotonic constitutive curve. In general, the value of β should be determined from experimental data, hence allow the FH–RP model to capture various physical features of complex fluids.
The simulation results presented in this section are obtained by setting the model parameters β = 0.2 and δ = −0.5, GA = 1.0 (GAR = 0.1, GAd = 0.9), GB = 4.0 (GBR = 0.2, GBd = 3.8), τAR = 1.0, τBR = 0.01, , and
(i.e., ZA = 6.67, ZB = 66.67). Those parameters give a strictly monotonic constitutive equation for all values of ϕA, and define a binary polymeric system which is miscible under equilibrium condition and shows shear-induce phase separation in a range of shear rates. The steady state solutions of the model are calculated by solving eqn (9) to eqn (14) under a fixed composition field ϕA using the pre-defined ODE solvers available in MATLIB and are shown in Fig. 1. The absolute differences between the numerical results obtained from the OpenFOAM solver and the MATLAB calculation for a homogenous Rolie–Poly fluid are less than 0.003.
![]() | ||
Fig. 1 The scaled steady-state shear stress Txy versus ![]() ![]() ![]() ![]() |
With this set of the parameters, all the constitutive curves of homogenous fluid under various ϕA are monotonic as indicated in Fig. 1. There is no intrinsic constitutive instability. Under low shear rate (e ≲ 6.0), the calculated shear stress and first normal stress difference exactly match the corresponding analytical results of homogeneous fluid (ϕA = 0.5). The phase separation only occurs in a range of shear rates: 7.0 ≲
e ≲ 38.0, in which the homogeneous phase with initial small composition fluctuation separates into A-component-rich and B-component-rich phases in a form of shear bands. In the higher shear rate region of
e ≳ 40.0, the simulation results again coincide with the analytical calculations for a homogeneous fluid and no phase separation is observed over the duration of our simulations. Fig. 1 shows that no stress plateau exists. It was also reported in the previous study of the FH–JS model24,25 and a liquid crystalline model.51
The transient behaviour corresponding to several points in Fig. 1 are presented in Fig. 2(a) for shear stress and Fig. 2(b) for first normal stress difference. Within the phase separation region, the numerical results of the shear stress and the first normal difference coincide with the theoretical solution of a homogeneous FH–RP fluid but then turn into a two-phase solution as a significant drop (the second drop in shear stress) of Txy and N1 appears. It takes as long as 70τA to reach a steady state.
![]() | ||
Fig. 2 Transient shear stress and first normal stress difference for various values of the Weissenberg number ![]() ![]() ![]() |
Snapshots of the composition field at several instant during phase separation for the case of e = 20.0 have been shown in Fig. 4. The evolution of the shear rate field and the stress field follow the same pattern as that of the composition field shown in the figure. The letters a to j mark the points along the transient stress curves in Fig. 2 which refer to the individual images in Fig. 4, respectively. From the evolution of composition field, there are two dynamical mechanisms by which the shear bands reach to a steady state: diffusive mechanism and convective through wave instability. They have also been observed in a 30/70 polymer mixture,24 but only a purely diffusive mechanism was seen in 50/50 polymer mixtures.25 At t = 0, the composition is homogeneous. The significantly stress dropping between points b and d in Fig. 2, corresponding to Fig. 4(b)–(d), shows the direct formation of fine composition bands by nucleation and unstable wave structure interacting with each other. At point d, the stress has reached a low plateau but the composition field is still unstable. As approaching to the steady state, there is an interesting dynamical process observed between point e and g referring to the snapshots shown in Fig. 4(e)–(g): a wave structure breaks up forming droplet, then the droplet interacts with the remaining bands and subsequently forms into a coarser band. This phenomenon explains the stress fluctuations in Fig. 2; It is not only seen in this specific case for
e = 20.0, but also for all the cases shown in Fig. 2, fluctuations always appear along with a process breaking wave into droplet then to much coarser band. From t = 30τA, the band structures gradually grow via diffusive mechanism, and shortly after the small oscillation around t = 85τA corresponding to another wave to droplet process, the shear bands get much coarser and far away from each other. From t = 100τA, the remaining bands change very little and reach the steady state.
![]() | ||
Fig. 4 Snapshots of the composition field ϕA at various instant t for an initially homogeneous viscoelastic binary fluid of ![]() ![]() ![]() |
It is worth to note that our numerical results show a dynamic steady state, unlike the previous studies presenting a strictly smooth shear bands with J–S model,24,25 there are wavy band structures moving with the flow without further coarsening. Fig. 3 shows the composition profiles across the simulation box. As seen in the top figure, the fluid formed into band structures and the maximum value of ϕA is less than 0.8 in steady state. In order to reveal structural evolution of the unstable interfaces, we plot the composition profile along the flow direction near the band interfaces, as shown in the bottom figure of Fig. 3, which presents a typical moving pattern: a wavy structure moves along the flow direction.
Recently, a growing body of data reveals that the shear bands can fluctuate. Most of the observations suggest a wavy structure oscillating between two bands. Many experimental results identify such fluctuations in complex fluids9,52–57 and the interface instabilities have also been observed in numerical studies with a diffusive J–S model27,55,58 and a two-species model.59 The simulation results demonstrate that the proposed FH–RP model can capture the essential instabilities in complex fluids through a thermodynamically consistent way.
The intrinsic constitutive curves of various values of ϕA have been presented in Fig. 5, all of which are non-monotonic. The numerical simulation results of the shear stress have also been plotted in this figure. In the homogeneous range for low shear rate (e ≲ 7.0) and high shear rate (
e ≳ 80), the simulation results exactly coincide with the FH–RP constitutive curve in a homogenous state, which are indicated by the circles in Fig. 5. Similar to the monotonic case, in the region of 8 ≲
e ≲ 77, flow-induced phase separation takes place and the stress deviation is observed. Different from previous cases in which the shear stress always can reach a steady state, in this system the stress does not reach a steady value, but continuously fluctuates. The fluctuation range of the shear stress is indicated with the vertical error bars in Fig. 5. Another significant difference is that the flow curve of shear stress versus shear rate is not linear as the monotonic case, but exhibits some wavy structure within the phase separation region. This may attribute to the large fluctuations in the simulations. In order to check whether or not the final state achieved here, it is necessary to use a much larger simulation box and this will form part of our future research. However, in an experimental study of associative polymer networks, Sprakel11 presented similar fluctuations of the flow curves and their work revealed rheochaos of the transient stress response, which is similar to our simulation results.
The transient behaviour of the stress components at various shear rates corresponding to several points in Fig. 5 are shown in Fig. 6(a) for shear stress Txy and Fig. 6(a) for first normal stress difference N1. Under low shear rate (e = 10), the magnitude of the fluctuation is small. In the middle of the phase separation region, such as
e = 20 and
e = 30, the fluctuations become much larger. In even higher shear rate region, the stress oscillation reduces as shown in the case of
e = 40. If looking into the detailed evolutions of the transient behaviour of the stresses, it reveals some special patterns. For
e = 40, the stress continuously oscillates with the same amplitude and periodically repeats similar patterns. Surprisingly, the case of
e = 20 shows a quite difference behaviour. Except for the larger fluctuations, there is a quiet region in which the stress oscillation vanishes.
![]() | ||
Fig. 6 Transient shear stress and first normal stress difference revealing rheochaos for various values of the Weissenberg number ![]() ![]() ![]() |
Snapshots of the composition field during phase separation for the case of e = 20 with a non-monotonic constitutive curve are shown in Fig. 7. The letters a–j marked in Fig. 6 refer to the individual images in Fig. 7 and indicate the points along the transient stress curves corresponding to each image. At t = 0, the composition is homogeneous with a small random noise. After the initial stress overshoot, at t = 0.95τAd, the composition field forms smooth band structures. Shortly it is found that the flat bands have been broken as shown in Fig. 7(c). From here, the chaotic stress response emerges, and typical phase transitions corresponding to the rheochaos can be seen in Fig. 7(d)–(g). At the beginning, the bands stay with unstable interfaces, then a vortex structure emerges within the central band, and this turbulence gradually subsides at t = 20.7τAd. We plot the snapshots of streamlines in Fig. 8 between t = 17.16τAd and t = 20.7τAd, from which we can find a symmetric vortex clearly appearing within the central band. This process repeat for a long period and lead to large fluctuations in stress curves. Although the results in an experimental study of telechelic polymers11 suggest that the fluctuating stress is caused by interface instabilities, our simulations reveal another possible cause: the vortex instability inside the band structure. We hope more visualization experiments could be conducted to confirm our observations in the future.
![]() | ||
Fig. 7 Snapshots of the composition field ϕA at various times t for an initially homogeneous viscoelastic binary fluid of ![]() ![]() ![]() |
![]() | ||
Fig. 8 Snapshots of streamlines corresponding to typical rheochaos, which clearly show a vortex structure emerges for an initially homogeneous viscoelastic binary fluid of ![]() |
At t = 61.36τAd, corresponding to a smooth region of the stress curves showed in Fig. 6, the band structures also form a more stable state in Fig. 7(h): the central band becomes uniform with a smooth interface, and the fine bands near the wall combine into darker ones after interacting with each other. This smooth region terminates at around t = 70.95τAd, thus the stress curves come back to the fluctuations. The composition field has been shown in Fig. 7(i) and (j). It is seen that instabilities emerge within the central band, and it is still unstable by t = 100τAd. This particular intermittent rheochaos have not been observed in the numerical studies with a FH–JS model.
The visual impression of this vortex structure shown in Fig. 7 and 8, are observed in all of the cases with large rheological fluctuations. A more careful analysis is presented in Fig. 9. It shows the average Fourier spectra of the intensity reflected by composition field along the velocity direction in the central of the simulation box, which exhibits power law decay over one decade of frequency. Similar to the case of elastic turbulence,60,61 the power spectrum in wave vector seems to approximately follow a power law up to kd ∼ 33(Δx)−1, where is the lattice size in this study. The case of
e = 10 shows significant difference from other cases in Fig. 9, as indicated in the figure, the critical value kd′ < kd. Compared to other cases, with
e = 10, we find that the stress fluctuation is relatively small and the shear bands are more stable, and this also leads to a much smaller vortex structure in the streamline plot. Since k−1d is related to the stress correlation length, we may conclude that larger vortex and rheological fluctuations are relevant to a smaller stress correlation length.
The simulations reproduce many dynamic phenomena reported in literature, including the steady-state shear-banding, the interface instabilities between the bands, and the dynamic mechanisms to reach stable band structures. With a non-monotonic constitutive equation, we have also observed that the band structures are strongly unstable both in time and in space. The stress continuously fluctuates in a chaotic manner. The correlations between microstructure evolution and chaotic rheological responses have been identified. Other than the interface instability, our results reveal another possible cause of the rheochaos: a vortex structure emerges within the central band.
Coupled with a realistic constitutive model, the computational model presented here could provide valuable guidance to new experimental work and could also be used to quantitatively study some outstanding problems by appropriately selecting the parameters to mimic the real physical systems. Motivated by many experimental observations, we hope to address an in-depth quantitative study of the rheochaos in complex fluids in future simulations, including large-scale three-dimensional simulations.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c4ra08448a |
This journal is © The Royal Society of Chemistry 2014 |