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Handbook of Solvents - George Wypych - ChemTech - Ventech!

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154 Christian Wohlfarth<br />

where:<br />

a,b,c,d empirical fitting parameters for the χ-function<br />

β00 , β01, β10 , β11<br />

empirical fitting parameters for the g-function<br />

T absolute temperature<br />

P pressure<br />

All these fitting parameters may be concentration dependent and may be included into<br />

Equations [4.4.15 or 4.4.16]. Details are omitted here. More theoretical approaches will be<br />

discussed shortly in Subchapter 4.4.4.<br />

The χ-function can be divided into an enthalpic and an entropic parts:<br />

∂χ<br />

∂χ<br />

χ = χ + χ χ =− χ<br />

∂<br />

∂<br />

⎛ ⎞<br />

⎜ ⎟ =<br />

⎝ ⎠<br />

⎛ T ⎞<br />

H S with H T and S ⎜ ⎟<br />

T<br />

⎝ T ⎠<br />

p,<br />

ϕ P,<br />

ϕ<br />

[4.4.18]<br />

where:<br />

χH enthalpic part<br />

χS entropic part<br />

An extension <strong>of</strong> all these equations given above to multi-component mixtures is possible.<br />

Reviews <strong>of</strong> continuous thermodynamics which take into account the polydisperse character<br />

<strong>of</strong> polymers by distribution functions can be found elsewhere. 52-54<br />

4.4.3 EXPERIMENTAL METHODS, EQUIPMENT AND DATA REDUCTION<br />

4.4.3.1 Vapor-liquid equilibrium (VLE) measurements<br />

Investigations on vapor-liquid equilibrium <strong>of</strong> polymer solutions are the most important<br />

source for obtaining solvent activities in polymer solutions. Therefore, emphasis is laid to<br />

the experimental methods which use this equilibrium. These methods are:<br />

(i) absolute vapor pressure measurement,<br />

(ii) differential vapor pressure measurement,<br />

(iii) isopiestic sorption/desorption methods, i.e. gravimetric sorption,<br />

piezoelectric sorption, or isothermal distillation,<br />

(iv) inverse gas-liquid chromatography (IGC) at infinite dilution,<br />

IGC at finite concentrations, and head-space gas-chromatography<br />

(HSGC),<br />

(v) ebulliometry and<br />

(vi) the non-equilibrium steady-state method vapor-pressure<br />

osmometry (VPO).<br />

The measurement <strong>of</strong> vapor pressures for polymer solutions is generally more difficult<br />

and more time-consuming than that <strong>of</strong> low-molecular mixtures. The main difficulties can be<br />

summarized as follows: Polymer solutions exhibit strong negative deviations from Raoult’s<br />

law. These are mainly due to the large entropic contributions caused by the difference between<br />

the molar volumes <strong>of</strong> solvents and polymers, as was explained by the classical<br />

Flory-Huggins theory 46,47 about 60 years ago, Equation [4.4.12]. However, because <strong>of</strong> this<br />

large difference in molar mass, vapor pressures <strong>of</strong> dilute solutions do not differ markedly<br />

from the vapor pressure <strong>of</strong> the pure solvent at the same temperature, even at polymer concentrations<br />

<strong>of</strong> 10-20 wt%. This requires special techniques to measure very small differences<br />

in solvent activities. Concentrated polymer solutions are characterized by rapidly<br />

increasing viscosities with increasing polymer concentration. This leads to a strong increase<br />

in time required to obtain real thermodynamic equilibrium caused by a slow solvent diffu-

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