2.1. Van der Waals Universal Equation of State for a Pure Fluid
The universal, or reduced, form of the van der Waals equation of state for a pure one-component fluid is,
In this form all quantities are dimensionless. For example,
p is the ratio of the physical pressure
P to the value of the pressure at the critical point
. Thus
when the fluid is in its critical state. Similarly,
, where
T is the Kelvin temperature, and
the critical temperature, so that
t is also equal to unity at the critical point. The number density of the fluid is the number of molecules per unit volume, and
is the ratio of the number density to its value at the critical point, where
. For simplicity, we refer to the “renormalized” quantities
, and
as pressure, temperature, and density. Notice that the maximum value of density is 3 (closely packed liquid), while for low densities, the equation reduces to
(dilute gas with negligible interactions, or, simply, an ideal gas).
Figure 1 displays four isotherms according to Equation (
1), supercritical, critical, and two subcritical isotherms. The supercritical isotherm for
shows the progressive transition from a vapor state at low density to a high-density liquid state. The isotherm for
passes through the critical state of infinite compressibility,
, at
. For the subcritical isotherms
, there are intermediate ranges of densities where the compressibility is negative. Such states are unstable and, if formed, would immediately disappear, yielding to stable coexistence of vapor and liquid phases observed as a discontinuous transition. For these isotherms, a horizontal line intersects liquid and vapor regions of positive compressibility. However, for the “coldest” isotherm shown, at
, a horizontal line at negative pressure intersects only the liquid portion of the isotherm, indicating that only a liquid can stably exist at negative pressure (i.e., under tension).
2.2. Van der Waals Equation of State for a Solution
The universal van der Waals equation is applicable to a pure fluid consisting of identical and independent, albeit interacting, molecules. As such, it cannot serve by itself as a minimal model for the volume transition of a gel, since a minimal gel model must at least recognize, first, that a gel is a two-component, solute/solvent, system; and second, that the gel material (solute) is a networked mesh. The first requirement is easily accomplished. The McMillan–Mayer theory of solute/solvent free solutions is among the few exact statistical mechanical theorems. It states that the virial series for the pressure P of a real gas goes over to a virial expansion for the osmotic pressure of a solution (the difference between the pressure of the solution and the pressure of pure solvent at equilibrium across a membrane impermeable to solute). The only difference is that the intermolecular forces in vacuum underlying the virial coefficients for the real gas must be replaced by the corresponding solute-solute interactions as they exist in free solution as mediated by solvent. A corollary of the McMillan–Mayer theorem is that any equation of state for a gas has its counterpart as an equation of state for osmotic pressure. An obvious example is the van’t Hoff equation as the solution analog to the ideal gas equation of state .
To apply these considerations in the present context, we write a universal van der Waals equation for the osmotic pressure of a free solution in analogy to Equation (
1),
Here, the dimensionless temperature
t has unchanged meaning; the dimensionless density
is the number density of the solute; and
is the dimensionless osmotic pressure of the solution. Aside from the analogy between osmotic pressure and pressure, there is another important distinction between Equations (
1) and (
2). In the van der Waals theory of a pure fluid, the interaction constants
a (measuring pairwise attraction) and
b (the excluded volume parameter) are independent of temperature. For a solution the solute–solute interactions are mediated through the random movements of solvent molecules and therefore must depend on temperature. The parameter
in Equation (
2) is the ratio
, and
. Thus
and
are identically equal to unity if
a and
b do not depend on temperature, and if they do depend on temperature, they are both equal to unity at the critical point
.
In
Figure 2 we show three solution isotherms. We expect the excluded volume parameter to be relatively insensitive to temperature, and so have set
for all three cases. The black curve for
is the same as the critical isotherm in
Figure 1, since
when
. The red isotherm is for
, that is, subcritical. For this isotherm, we have assumed
to be insensitive to temperature, so that
. This isotherm is therefore very similar to the
isotherm in
Figure 1. In the unstable range of solute densities, the solution separates into solvent-rich and solvent-lean phases. The blue isotherm is for
, a supercritical isotherm. It also exhibits an unstable range of solute densities, hence phase separation, because we have taken
as temperature-dependent in generating this isotherm, arbitrarily setting
as a numerical example. In other words, we have assumed here that the intermolecular attraction among solute molecules increases with temperature, as might be true, for example, if the solvent is water while the solute is soluble but contains a hydrophobic moiety. In this case the temperature dependence of phase separation is inverted; phase separation occurs at
t higher than critical. We can conclude that ordinary van der Waals theory, adapted to solutions, provides the basic physics underlying the full range of phase behavior of free polymer solutions.
The effect of solute-solute interactions can be seen by comparing this equation with the form it takes at low density,
. But a more direct measure of solute-solute interactions is provided by the solute activity coefficient
, which can be obtained first by solving Equation (
2) for
in the form of a correction from low densities given by the osmotic coefficient factor
, and then by integrating the Gibbs–Duhem equation,
. We find,
The deviation of the activity coefficient from its value unity in the dilute limit
is a measure of solute-solute interactions. See the original paper [
5] for a plot of
as a function of density at various temperatures for the case
.
2.4. The Gel Isopotentials
The local solute chemical potential
is the ideal vehicle for combining all three effects—the tendency to outward diffusion of the gel material, the inward-acting networking forces restraining diffusion, and solvent-mediated van der Waals interactions—into an equilibrium state,
where
is a constant. We have written the chemical potential as dimensionless, in units of
. The three terms on the right-hand side represent the three effects. The location dependent entropy of mixing term
expresses the tendency to free outward diffusion, the activity coefficient term accounts for the van der Waals interactions, and the potential energy
resists diffusion. The condition for equilibrium is that the chemical potential must be constant throughout the gel,
, and integration of this condition produces “isopotential” lines, that is, curves of constant chemical potential
. The isopotentials are gel density profiles that show how
varies with distance
r from the gel center.
In the following series of figures,
Figure 4,
Figure 5 and
Figure 6, we show some examples of these isopotentials, or density profiles (we use these terms interchangeably). Because the Langevin network potential energy
u is defined from Equation (
4) as the inverse function
, it turns out that these profiles are displayed as inverse functions
, where the free parameter
, the density at
, originates as an integration constant. Radial distance
r is on the vertical axis, density
on the horizontal axis. The figures show numerical results for a “lower critical temperature” gel, i.e., a gel that undergoes its volume phase transition toward collapse when the temperature
t decreases. In these figures,
. See Figure 9 of the original paper [
5] for numerical analysis of the upper critical temperature case.
All of the curves in
Figure 4 were calculated for the same temperature
. This value of
t is critical in the sense that if
, gels of different densities cannot coexist. The different isopotentials in
Figure 4 result from different choices of the free parameter
, the density at
. For example, the density profile with
represents a highly cross-linked gel, so that the gel must have a very high density of gel material even when fully swollen (recall the value 3 as the maximum, i.e., close packing, value of
). In this case the density remains nearly constant up to the periphery
, then abruptly falls to zero. For a gel prepared to be dilute when swollen, for example,
, the density falls off more gradually to zero at
. But for each gel (each value of
), there is only a single density profile, representing the swollen gel as extending all the way to the maximum boundary
.
When
a new phenomenon appears. In
Figure 5 we have set
. We also chose a single value
for the free parameter, so that
Figure 5 displays only a single isopotential. But this isopotential is disconnected. It is not single-valued for all values of
r. It is single-valued only for
. A horizontal line drawn at any value of
r greater than 0.15 intersects only one value of the density
. These values of
are relatively small (ranging from 0.52 at
to zero at the periphery
). The gel is therefore fully swollen (it extends to
), and its outer part (
) is uniformly dilute. Next, we describe the inner part of the gel in
Figure 5, that is,
. A horizontal line drawn for any of these smaller values of
r intersects the isopotential at three distinct values of the density
. For example, regard the horizontal axis itself,
. Even though we chose a single value of the free parameter
, this value, unity, representing density at
, appears on the horizontal axis only along with two others, one smaller, the other larger. We have proved in the original paper [
5] that the intermediate value
is unstable. The lower and higher ones are stable,
, and
. The physical meaning is that at the temperature
, condensation nuclei appear at the origin
. These “liquid” gel nuclei with density 1.47 coexist (fluctuate) with a much more dilute “vapor” gel phase with density 0.58. As another example, take a horizontal line at
. It intersects the left-most, dilute, branch of the isopotential at
, and it touches the right-most “bulge” of the density profile at its maximum at
. In the spherical shell of the gel with radius
, a “vapor” gel phase with density 0.52 coexists with condensed “liquid” nuclei with density 1.27.
Another consideration is displayed in
Figure 6. In this figure, there is a single isopotential at
with the free parameter chosen as
. The isopotential as shown is double-valued, because in the figure we have not drawn the unstable part of the condensation bulge (it exists, as in
Figure 5, but it is not drawn in
Figure 6). The amount of gel material is the same in both branches, that is, the areas to the left of each branch, normalized for spherical symmetry, are equal.
Figure 6 therefore represents the volume phase transition for the gel at
. The dilute density profile on the left is the swollen gel, and the collapsed high-density gel is on the right. The radius of the swollen gel is
, while the radius at the outer periphery of the condensed gel is seen from the figure to be 0.42. The volume of the collapsed phase at the transition temperature is therefore reduced to 7.4 per cent of the swollen volume for a spherical gel. As the temperature is lowered past the transition temperature, the condensed gel contracts further (not shown).
The detailed numerical analysis in the original paper for the choice
can be summarized. When
, the gel is fully swollen up to the maximum periphery
. The density is dilute, tapering to zero at
. When
t falls below 0.9443…, nuclei of dense gel material appear. When
t reaches the value 0.87, the gel volume transition occurs.
Figure 6 here shows the density profiles of swollen and collapsed gels in equilibrium at
. The isopotential colored orange in Figure 8 of the original paper [
5] shows density profiles at an intermediate
, when nuclei of dense gel material are present inside the swollen gel.
2.5. The Bulk Modulus
The bulk modulus
is defined as the inverse of the thermodynamic compressibility of the material [
6]. Noting that
K has the units of pressure, we can define a universal modulus
, and then in terms of universal quantities,
For a van der Waals pure fluid, the equation of state Equation (
1) can be solved for pressure
p and straightforwardly differentiated to give,
At the critical point
,
vanishes, as can also be seen visually from the isotherm at
in
Figure 1.
The bulk modulus of gels has been measured [
4,
7]. In the neighborhood of the volume phase transition,
K for the fully swollen gel is an order of magnitude less than for the collapsed phase. We can also obtain this result for our universal gel. We can show that
for the gel is identical to Equation (
7) for a van der Waals fluid with the important exception that for the gel
replaces the uniform value
in Equation (
7). In other words, for the gel
is a local quantity. To compare with experiment, we take an average,
with
the radius of the spherical gel at its periphery. Since
r can be expressed as a function of
, and
as a function of
from Equation (
7) above,
Numerical evaluation of the integral at the transition temperature
(for
, see
Figure 6), results in
for the swollen gel,
; and for the collapsed phase with
,
, an order of magnitude greater.
An interesting aspect of the gel volume transition is the softening of the gel as the transition is approached, as detected by a marked decrease of the bulk modulus [
4] (or Young’s modulus [
7]). It is expected that density fluctuations are the underlying cause [
8,
9]. Our universal gel exhibits this behavior, as indicated in
Figure 5. For example, at
, the density does not fluctuate in the outer part of the swollen gel (
in
Figure 5, where the density is single-valued and dilute, left branch). But for
, the density fluctuates between low-density and high-density values, as discussed in connection with
Figure 5. For a fixed value of
r in this fluctuating region, the pressure does not change but the density undergoes discrete changes. The modulus
therefore vanishes in this region (stress is absorbed by the density changes with no resistance). The points in
Figure 7 were calculated by taking an average in the range
while setting
for
.
2.6. Gibbs Phase Rule
An equilibrated swollen gel is a binary solution in which the free outward diffusion of solute is prevented by the networking of the solute itself. The mechanical restraint on free outward diffusion creates a balancing pressure gradient that can, if one wishes, be called an osmotic pressure. But it is important, at least for conceptual purposes, not to regard gel swelling as caused by osmotic pressure. The difference between the pressure inside the gel and outside is a consequence, not a cause, of mechanically restrained swelling. One of the dubious concepts sometimes inserted into the theory and even computer simulations of the volume transition of gels is requirement of a negative pressure. Although the
van der Waals isotherm in
Figure 1 possesses a stable region of negative pressure
p, the pure liquid to which it applies is not a gel. For the gel, the hydrostatic equation,
implies that the pressure inside an equilibrated gel is always positive (assuming ordinary conditions in the bathing solvent outside the gel, for example, 1 atm) [
5].
The pressure difference inside and outside the gel is responsible for failure of the Gibbs phase rule to describe the number of “degrees of freedom” of equilibrated gel systems, but the basic physics underlying the Gibbs rule is still valid, and there is no need to invoke metastable gel states. The case of the three-phase gel system (swollen and collapsed gel coexisting in bathing solvent) is discussed in detail in the original paper [
5]. Here we review only the simplest related example, a standard two-phase osmotic system consisting of a solute-solvent solution (one phase) separated from pure solvent (the other phase) by a semi-permeable membrane. In general non-equilibrium conditions, each phase has its own temperature, its own pressure, and the solution phase has its solute concentration, for a total of five non-equilibrium degrees of freedom. At equilibrium, there are two constraints, the equality of temperatures and of solvent chemical potentials. The degrees of freedom at equilibrium are in number, therefore, equal to
, and the three equilibrium degrees of freedom are the values of temperature, pressure in the pure solvent phase, and solute concentration in the solution phase. Thus, even though rote application of the Gibbs phase rule gives the wrong answer,
, the standard osmotic pressure experiment requires no introduction of new considerations.