28.02.2013 Views

Handbook of Solvents - George Wypych - ChemTech - Ventech!

Handbook of Solvents - George Wypych - ChemTech - Ventech!

Handbook of Solvents - George Wypych - ChemTech - Ventech!

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

346 <strong>George</strong> <strong>Wypych</strong><br />

Temperature, K<br />

310<br />

300<br />

290<br />

280<br />

270<br />

260<br />

0.25 0.3 0.35 0.4 0.45 0.5 0.55<br />

A comparison <strong>of</strong> equations [7.1.7]<br />

and [7.1.8] shows that the slope and sign <strong>of</strong><br />

swelling curve are determined by the quan-<br />

g/lorcr<br />

tity ΔH1 . Since the melting enthalpy <strong>of</strong><br />

water is much larger than the transfer<br />

enthalpy <strong>of</strong> water, the swelling curves <strong>of</strong><br />

gel in liquid water are very steep. The sign<br />

<strong>of</strong> the slope is determined by the heat transfer<br />

<strong>of</strong> the solvent which may be negative,<br />

positive or zero depending on the quality <strong>of</strong><br />

solvent. The melting enthalpy is always<br />

positive and therefore the swelling curve in<br />

the presence <strong>of</strong> crystalline solvent is flat<br />

with a positive slope. A positive slope in<br />

temperatures below zero (for ice) means<br />

that gel has to deswell (release water to its<br />

surrounding, or dry out) as temperature<br />

decreases. 13 Figure 7.1.10 illustrates this.<br />

For practical purposes, simple equations<br />

are used to study swelling kinetics.<br />

The degree <strong>of</strong> swelling, α, is calculated from the following equation: 17<br />

V −V<br />

α=<br />

V<br />

1 0<br />

0<br />

where:<br />

V1 volume <strong>of</strong> swollen solid at time t=t<br />

V0 volume <strong>of</strong> unswollen solid at time t=0<br />

The swelling constant, K, is defined by:<br />

K k1<br />

α<br />

= =<br />

k 1−α<br />

2<br />

PEO/water<br />

PEO/ice<br />

Mass fraction <strong>of</strong> water<br />

Figure 7.1.10. Swelling <strong>of</strong> crosslinked polyurethane in<br />

water and ice. [Adapted, by permission, from B Hladik,<br />

S Frahn, W Borchard, Polym. Polym. Compos., 3, No.1,<br />

21-8 (1995).]<br />

[7.1.9]<br />

[7.1.10]<br />

where:<br />

k1 rate constant <strong>of</strong> swelling process<br />

k2 rate constant <strong>of</strong> deswelling process<br />

This shows that the swelling process is reversible and in a dynamic equilibrium.<br />

The distance <strong>of</strong> diffusion is time-dependent:<br />

distance (time) n<br />

∝ [7.1.11]<br />

The coefficient n is between 0.5 for Fickian diffusion and 1.0 for relaxation-controlled<br />

diffusion (diffusion <strong>of</strong> solvent is much faster than polymer segmental relaxation). 18 This<br />

relationship is frequently taken literally 19 to calculate diffusion distance from a measurement<br />

<strong>of</strong> the change <strong>of</strong> the linear dimensions <strong>of</strong> swollen material.<br />

The following equation is used to model changes based on swelling pressure measurements:

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!