Paride
Azzari
a and
Raffaele
Mezzenga
*ab
aDepartment of Health Sciences and Technology, ETH Zürich, Schmelzbergstrasse 9, 8092 Zürich, Switzerland. E-mail: raffaele.mezzenga@hest.ethz.ch
bDepartment of Materials, ETH Zürich, Wolfgang Pauli Strasse 10, 8093 Zurich, Switzerland
First published on 14th February 2023
We compare the process of Liquid–Liquid Phase Separation (LLPS) of flexible macromolecular solutions, with the Liquid–Liquid Crystalline Phase Separation (LLCPS) of semiflexible polymers and rigid filamentous colloids, which involves the formation of a liquid phase that possesses a directional alignment. Although the observed phase separation follows a similar dynamic path, namely nucleation and growth or spinodal decomposition separating two phases of dilute and concentrated compositions, the underlying physics that defines the theoretical framework of LLCPS is completely different from the one of LLPS. We review the main theories that describe the phase separation processes and relying on thermodynamics and dynamical arguments, we highlight the differences and analogies between these two phase separation phenomena, attempting to clarify the inner mechanisms that regulate those two processes. A particular focus is given to metastable phases, as these intermediate states represent a key element in understanding how phase separation works.
In the Flory Huggins treatment of LLPS, the entropy favors mixing as it introduces degrees of freedom via the position (center of mass) and configuration of macromolecules and it is intrinsically related to the capability of these components to adopt different configurations in a solution. However, when the macromolecules become progressively more rigid, these degrees of freedom are lost down to the level that, for infinite rigidity, their configuration in solution is described only by their positional and angular distribution.21 In this limit, the Flory–Huggins theory no longer holds and the traits of LLPS change fundamentally into a distinct phase separation mechanism called liquid–liquid crystalline phase separation (LLCPS). The main difference between LLCPS and LLPS is that the most concentrated phase among the two phase-separated is now characterized by an orientational order of the rigid macromolecules, that is, is controlled by the presence of liquid crystalline interactions. Ultimately, it is the ratio between the contour length of the polymer L and its persistence length LP that determines whether phase separation occurs via LLPS (L ≫ LP) or LLCPS (L < LP).22,23 Liquid crystals are an intermediate state of matter, which show liquid mechanical properties, and an ordered structure typical of crystalline systems, where the order is exhibited in the alignment of the liquid crystal molecules. This order makes possible the formation of nematic phases, that is anisotropic phases in which all the liquid crystalline molecules are aligned along a specific direction.24 These molecules, which form anisotropic phases, are called nematogens, and they are usually elongated rigid molecules. Liquid crystalline solutions, at certain concentrations, can trigger a process of phase separation.25 From a completely isotropic system, the solution will form domains of aligned fibrils and eventually phase separate into a nematic phase.26 These nematic domains are named tactoids. Liquid crystalline tactoids have been intensively studied: the structure and nematic field have been analyzed and interpreted in detail;26,27 however, only recently the formation of tactoids through the process of nucleation and growth, has been formalized for liquid crystals.22 In the phase of growth, nematic tactoids increase in size to reach thermodynamic equilibrium and attain a macroscopically phase-separated system.28 Liquid crystalline phases have been strongly used in health science and biomedical applications29 and in pharmaceutical technologies.30 The most typical biological macromolecules, that self-assemble in liquid crystalline structures, are collagen, actin, cellulose and filamentous viruses.31 In recent years, nematic and cholesteric phases have been reported in amyloid fibrils.32 These fibrils, formed from β-sheet aggregates, have revealed unique self-assembly capabilities, displaying an unprecedented palette of morphologies in the liquid crystalline phases.26 Amyloid fibrils have also grown a strong interest in many disciplines: from health sciences to food science, for their importance and their role in biological processes.33,34 Moreover, amyloid fibrils have reached a wider audience, since their functional characteristics, made them a key element in various fields from material science to bionanotechnology.32,34,35 Before these positive roles, amyloid fibrils were, however, initially known for their association with neurodegenerative pathological conditions, for example, Parkinson's disease and Alzheimer's disease.36 Therefore, understanding the processes behind the emergence of liquid crystalline phases, and revealing the mechanisms behind LLCPS in comparison to standard LLPS, may even give a stronger foundation to understand the nature and formation of amyloid deposits, and eventually devise successful treatments for these conditions.
To date, the processes of liquid–liquid phase separation and liquid–liquid crystalline phase separation are not well differentiated. The purpose of this work is to analyze the mechanisms that are underlying the two different processes and understand their similarities and differences.
F = Vf(φ), | (1) |
![]() | (2) |
ΠΔV(φ + ε) − ΠV(φ) ∼ εφf′′(φ) | (3) |
This expression is obtained, for very small ε, from Π = f′(φ)φ − f(φ). Therefore, we can deduce that the concavity of f influences the volume flow, generated by this pressure imbalance. When f′′ is greater than zero, any fluctuation in the system is balanced by an increase in pressure, which forces a volume flow that restores the initial condition, therefore this is called a stable state. Otherwise, when f′′ is negative, the system is unstable. The given subvolume has a pressure imbalance that amplifies the volume difference. This thermodynamical instability is the basis of phase separations.37
For systems where F is of the form of eqn (1), we can define the spinodal line as the points where f changes concavity, i.e. f′′(φ) = 0. The spinodal line delimitates the spinodal region where f′′ is negative, in which the system is in an unstable state. From this condition, the system will evolve into stable states through a phase separation process called spinodal decomposition.38
If the fluid phase separates into two different phases, we want to understand the equilibrium conditions for the coexistence of these two stable states. Let Ftot be the sum of two subsystems in two different phases:
Ftot = V1f(φ1) + V2f(φ2) | (4) |
μ1 = μ2 and Π1 = Π2. | (5) |
Phase coexistence can be identified as the states sharing the same potentials. When the chemical potential and pressure are not balanced, the system will spontaneously evolve to restore thermodynamic equilibrium. The states where the potentials are equal form the so-called coexistence or binodal lines. The system can exist in two different phases, if the binodal conditions are met.21 For a more indepth analysis, see ref. 39.
![]() | (6) |
Although for macromolecules, n is of the order of 103 or 104,21 here we consider n = 10. This parameter influences the symmetry of the free energy, but not the topology, in which we are interested. In contrast, the parameter χ, strongly influences the shape of the curve fFH. For each value of χ, we can determine the equilibrium points and the stable and unstable zone of the system, as described before. By varying χ we can identify two different behaviors of the free energy, as shown in Fig. 1(a). Below a critical χc, fFH is always convex, while above that value a concave region is formed, i.e. in between the red points in Fig. 1. This concave region is the spinodal region. The green points in Fig. 1(a) are those giving equality of the chemical potential and osmotic pressure, see eqn (5), that is the binodal points. The critical value of the parameter χ can be obtained by minimizing the spinodal, i.e., in the case of n = 10, we have χc = 0.87. This parameter is a factor determined by the interaction energies between the components and the temperature. Similarly, the critical concentration can be obtained as
, for n = 10, φc = 0.24. For a more in-depth analysis see the references.41–43
The spinodal and binodal lines for varying χ, have been plotted in Fig. 1(b). The stable region is in white. Each point in the white area is stable and will not evolve or phase separate. The red zone is the unstable region, where , with the spinodal curve surrounding it (highlighted in dark red). The spinodal line generates a miscibility gap, solutions with certain volume fractions are not stable, and for high values of χ, only low or high concentrations are stable and do not phase separate. The binodal line (black) is encircling the spinodal region. Solutions with volume fractions on this line at fixed χ, can coexist in the same system. The region between the binodal and spinodal line is a metastable zone, here phase separation is possible, but there is an energetic barrier to overcome.44 Any metastable solution will eventually nucleate and grow droplets to reach a stable phase. The spinodal and binodal lines meet in the critical point at χc = 0.87 for n = 10.
We want to study the same system from a dynamical system point of view. Following a solution of initial concentration φ = 0.24, for χ lower than χc. By slowly increasing the parameter χ, the solution will remain in a stable state until the critical point is reached χc, see Fig. 1(c). For higher values, the volume fraction of 0.24 becomes unstable, and the solution will divide into two different phases, a more concentrated one (upper green branch) and a more diluted one (lower green branch). The plot shown in Fig. 1(c) is called bifurcation diagram, where the bifurcation point is the critical point for the Flory–Huggins model, χc = 0.87 and φ = 0.24. This type of bifurcation is called supercritical pitchfork bifurcation,45 a type of bifurcation that can be observed in other physical systems, such as ferromagnets, and other second-order phase transitions.39,46
![]() | (7) |
![]() | (8) |
![]() | (9) |
Using the Onsager trial function, we can evaluate σ1 and σ2, and compute the order parameter s that minimizes the free energy fO at each concentration ϕ. From the phase separation generalities discussed before, we can calculate the thermodynamic potentials (chemical potential and osmotic pressure) for eqn (8). Equating them for the isotropic and nematic case we obtain the two values of ϕI = 3.34 and ϕN = 4.49. The functions σ1 and σ2 are integral functions of the orientation distribution ψ, which in turn depends on the order parameter s. Minimizing eqn (8) with respect to s, to obtain the equilibrium order parameter for different values of ϕ cannot be done analytically. Only numerical solutions are possible, as discussed in detail in ref. 48. However, to better understand how these quantities interact to form nematic and isotropic phases, a simplified approach is given in the appendix. A more detailed discussion on the Onsager functional can be found in ref. 24. For values of ϕ below ϕI, the isotropic state is the only possible stable state, while for values of ϕ greater than ϕN, the only available state is the nematic one. The values of ϕ in between those two values form the coexistence window, where both nematic and isotropic phases are coexisting together. Phase separation is only possible between these two values.
We want to investigate the thermodynamic stability of the two phases in the coexistence window. We start by analyzing the free energy landscape as a function of the order parameter s, for varying concentration ϕ. We identified four different scenarios that are summarized in Fig. 2(a). For ϕ lower than 3.659, the state s = 0 is the only minimum of the system, Fig. 2 (a, black). At ϕS = 3.659 a minimum appears in a nematic state where s > 0. This state remains metastable, i.e. a local minimum, until ϕC = 3.681. For concentrations higher than this number, this nematic state becomes the absolute minimum, that is the equilibrium state of the system, while the isotropic, changes into a (meta)stable one. This critical concentration ϕC is a first-order phase transition in the alignment s. This is also shown in Fig. 2(b), where the discontinuity in the slope of fO, clearly underlines this phase transition from isotropic to nematic, by an increase in the concentration.24 At a concentration higher than ϕ > 4, the isotropic state changes from a minimum of fO to a maximum, therefore, the isotropic state becomes unstable from ϕ > 4. This is a bifurcation point for the isotropic state s = 0.49 The position of these critical points of fO is depicted as lines in Fig. 2(c), for changing ϕ. The horizontal axis where s = 0 shows the three different stability attained by the isotropic state. We now focus on the nematic state, where s > 0. This state has an absolute minimum only from ϕ > ϕC = 3.681. For values lower than ϕC, up to ϕS = 3.659 the nematic state is not the absolute minimum, but still a local minimum of fO. The free energy fO diverges when s = 1, therefore the perfect parallel alignment is unachievable, according to this formulation. For values of ϕ lower than ϕS, there are no stationary points of the free energy fO. This concentration is the first bifurcation of the Onsager model, called saddle-node bifurcation.45 For ϕ lower than ϕS, no nematic states are present neither stable nor unstable. At ϕS two states, a (meta)stable one and an unstable one are created. The unstable branch eventually connects to ϕB = 4, forming another bifurcation, called trans-critical bifurcation.45 As in Flory–Huggins, Onsager's theory predicts two coexisting phases for 3.34 < ϕ < 4.49. That this is possible can be appreciated by looking at the curves of Fig. 2(a), for example at concentrations 3.659 < ϕ < 4, where the two minima observed for the free energy for two differently ordered states (s = 0 isotropic and s > 0 for the nematic) bear full analogy with the two minima of the Flory–Huggins free energy leading to the equilibrium between a diluted and concentrated phase (see Fig. 2(a)). Contrary to the Flory–Huggins theory, however, Onsager's theory shows a richer palette of bifurcations.50 The saddle-node bifurcation is typical of first-order phase transitions, while the trans-critical bifurcation can be seen in laser threshold systems.51 The joint diagram of Fig. 2(c), which includes the two bifurcations, represents a typical pattern that can be observed in other physical systems that undergo hysteresis processes, like magnetic hysteresis.52 Starting from an initial stable isotropic state, by increasing the concentration, when we reach ϕ = 4 the system will spontaneously evolve towards the nematic branch. Similarly, bringing back the concentration at ϕ lower than 4, we would still be on the stable nematic branch, at the concentration lower than 4. However, such an effect would be extremely difficult to observe experimentally, since concentrations in these values would eventually undergo nucleation and growth.22,25
fFH = ΔS(φ) + χΔU(φ). | (10) |
With this formulation, the free energy components are much more evident. The entropy ΔS and internal energy ΔU depend on φ, while χ is a parameter that balances the two contributions. For low values of χ the entropy dominates the system: for every volume fraction φ, the solution is stable; on the other side, for values of χ higher than the critical value χc, the energy contribute dominates the free energy and the interaction between the components generates a miscibility gap. Volume fraction values between the spinodal points become unstable and will eventually phase separate into two distinct phases. Only high and low volume fractions are accessible, therefore LLPS forces the system into an up-concentrated phase and into a more diluted one. With the metastable zone surrounding the unstable region. The stability diagram of the Flory–Huggins theory is shown in Fig. 3(a).
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Fig. 3 Stability diagrams for the Flory–Huggins theory (a) and the Onsager theory (b). The former shows an unstable state, surrounded by metastable (M) and stable (S) states only for χ > χc = 0.87. For this plot, we set n = 10 and χ = 1. The latter has a stability divided by isotropic and nematic phases. Nematic phases are stable for ϕ > 4.49 and unstable for ϕ < ϕS = 3.659. Isotropic ones, on the contrary, are stable for ϕ < 3.34 and unstable for ϕ > ϕB = 4. In between those values, the states are metastable. A complete analysis of the differences is in Section 6. The letter S and B identify the respective bifurcation, as shown in Fig. 2. |
Onsager's theory relies on a pure interplay between entropic contributions.24,48 The free energy from eqn (8) can be regrouped as
fO = ΔSor(s) + ϕΔSex(s) | (11) |
The two entropy addenda represent the orientational and excluded volume contributions. Contrary to the Flory–Huggins case, in the Onsager's model we minimize the free energy fO with respect to the order parameter s, while the concentration ϕ is the balancing factor between the two terms. While in the previous case, by changing the interaction χ, it is possible to split the concentration of the system φ into two different concentrations corresponding to the new phases, in the Onsager model, by changing the concentration ϕ it is possible to split the system into two new phases with different order: isotropic and nematic. Therefore, in Onsager, the composition plays an analogue role than the χ in the Flory–Huggins model; reversely, the order parameter s in Onsager plays a similar role of the concentration in fFH, as independent parameter (comparing eqn (10) and (11)). This similarity is best grasped by tilting by 90° the Onsager diagram of Fig. 2(c), which immediately starts to show similarities with the binodal lines of the Flory–Huggins theory in Fig. 1(b).
In Fig. 3(b), we plotted the stability diagram for the Onsager theory, divided into nematic and isotropic phases. The stable states exist only left of 3.34 for the isotropic state and right of 4.49 for the nematic state. The isotropic state becomes unstable for a value greater than ϕB = 4. While for nematic alignments, the unstable branch ends at ϕS = 3.659. Nematic and isotropic alignments induce a miscibility gap in hard rods system, where only concentrations below ϕI = 3.34 are stable in an isotropic single phase, and concentrations higher than ϕN = 4.49 are stable in an aligned single phase. In between these two compositions, the system only exists in a two-phase heterogeneous state.
Another type of metastability occurs in the phase coexistence window. In the Flory–Huggins model, metastable states surround the spinodal region and are delimited by the binodal lines. While binodal lines determine the coexistence, for values of the concentrations that range in the metastable zone, the difference in potentials is such that the concentrated phase has a lower potential than the diluted phase, creating an ‘up-hill’ diffusion, where the solute diffuses from the low-concentration to the high-concentrated phase,22,55 triggering a phase separation that brings the two phases to the equilibrium. When only one phase is present in the metastability window, the second phase will form by nucleating droplets of the opposite concentration,56 as shown in Fig. 4(a).
The same mechanism of uphill diffusion is present in the LLCPS, an isotropic state brought to a metastable state where ϕ > 3.34, will nucleate and form domains of nematic and more concentrated solutions. These newly formed domains will grow in volume and concentration until the phase equilibrium is reached.22 At the same time, nematic phases at concentrations lower than 4.49 will nucleate isotropic domains, often called negative tactoids.57 For unstable states, phase separation is led by spinodal decomposition, which will form new nematic and isotropic states depending on the concentration.58 These two behaviors are depicted in Fig. 4(b). Lastly, we notice that the metastable states for the nematic and isotropic fluids are overlapping each other, and both are possible for the same concentrations, between ϕS and ϕB. This is a result of the hysteresis behavior concealed in the physics of the Onsager model. Depending on the history of the system, we can have both tactoids nucleating from a supersaturated isotropic solution or negative tactoids in a nematic background, at the same concentration values. We resort to two thought experiments to clarify this behaviour. In the first one, we take a solution of hard rods, whose scaled concentration ϕ is just above the isotropic boundary ϕI. By fixing the initial order parameter at s = 0, we have a supersaturated isotropic solution, where nematic tactoids will nucleate, and eventually grow until phase separation is reached. This has already been observed in many different experimental systems.25,26,32 If the initial concentration is higher than ϕB = 4, spinodal decomposition will drive the phase separation, while for ϕ > ϕN = 4.49, the fluid will simply change in alignment without undergoing phase separation. See Fig. 4(b). Conversely, if we take a solution in a nematic state, and we decrease the concentration ϕ below 4.49, the undersaturated nematic phase will nucleate negative tactoids and start to phase separate. If we bring down the concentration faster than the transport rates typical of nucleation and growth, and reach values lower than 3.659, the nematic state will become unstable and the solution will undergo phase separation through spinodal decomposition. For LLCPS, this other type of metastability is sketched in Fig. 4(b). To summarize: any liquid crystalline system described by the Onsager theory at an initial concentration 3.34 < ϕ < 4.49 will phase separate into two phases set at ϕI = 3.34 and ϕN = 4.49, as these are the only two phases equalizing simultaneously chemical potential and osmotic pressure in the two phases. However, the way by which phase separation will proceed, and thus the final morphologies, will depend on the initial state (isotropic or nematic) as well as the initial composition. For an initially isotropic phase such that 3.34 < ϕ < 4, the isotropic state is metastable, i.e. it exists as a minimum (absolute or relative) on the Onsager excess free energy (see Fig. 2(a)) and phase separation will occur by nucleation and growth of nematic tactoids within an isotropic continuous phase; for 4 < ϕ < 4.49, the excess free energy has no longer a minimum at the isotropic phase (s = 0), and the isotropic state is unstable leading to spinodal decomposition (see Fig. 4(b)). Reversely, for an initially nematic phase such that 3.659 < ϕ < 4.49, the nematic state is metastable, i.e. it exists as a minimum (absolute or relative) on the Onsager excess free energy (see Fig. 2(a)) and phase separation will occur by nucleation and growth of isotropic tactoids within a nematic continuous phase; for 3.34 < ϕ < 3.659 the excess free energy has no longer a minimum at the nematic state (s > 0) phase, the nematic state becomes unstable leading to spinodal decomposition (see Fig. 4(b)).
fO = σ1(ψ) + ϕσ2(ψ) | (12) |
![]() | (13) |
The above described quantities, σ1 and σ2, can be written as
σ1(α) ∼ log![]() | (14) |
![]() | (15) |
From these expressions, we see that σ1 grows slowly as the log of α, while σ2, the excluded volume term, decreases in magnitude with increasing alignment. If we minimize eqn (12), we obtain:
![]() | (16) |
The alignment grows quadratically with the concentration, for nematic phases. From eqn (12), using the above approximations, we can compute the osmotic pressure Π and chemical potential μ:
![]() | (17) |
![]() | (18) |
By equating ΠI = ΠN and μI = μN, we obtain
ϕI = 3.36 ϕN = 4.68 | (19) |
Those values are sufficiently close to the exact values calculated by Onsager,48 where ϕI = 3.34 and ϕN = 4.49.
Footnotes |
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