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Water and Solute Permeability of Plant Cuticles: Measurement and ...

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8.1 Sorption from Aqueous Solutions 237<br />

partition coefficients was exclusively due to a temperature effect on solute activity<br />

in the aqueous phase, that is, on water solubility <strong>of</strong> 4-NP. With increasing<br />

temperature water solubility increased, <strong>and</strong> as a consequence partition coefficients<br />

decreased. Sorption in tomato fruit MX differed. Here, k ′ increased with temperature<br />

from about 5 to 14, showing that the number <strong>of</strong> available sorption sites increased<br />

with temperature. The plot k ′ vs T has plateaus at 7–22 ◦ C <strong>and</strong> 22–32 ◦ C. A gradual<br />

increase occurred between 22 <strong>and</strong> 47 ◦ C (Riederer <strong>and</strong> Schönherr 1986a). This<br />

indicates structural changes in the cutin matrix, <strong>and</strong> the step character can be interpreted<br />

as phase transitions which lead to a loosening <strong>of</strong> the polymer chains, with a<br />

concomitant increase in number <strong>of</strong> sorption sites.<br />

8.1.2 Thermodynamics <strong>of</strong> Sorption<br />

Sorption in cuticles can be further characterised by Gibbs free energy (∆G) involved<br />

in transfer <strong>of</strong> 1 mol <strong>of</strong> 4-NP from the aqueous phase to the cuticle phase.<br />

∆Gsorption = −RT lnK (8.3)<br />

∆Gsorption is proportional to ln K, <strong>and</strong> since ln K is always >1, Gibbs free energy<br />

is always negative. This is expected for a spontaneous (exergonic) process. ∆Gsorption<br />

was largest at low internal concentrations (about −12 to −10kJ mol −1 ), <strong>and</strong><br />

decreased with increasing internal 4-NP concentration to about −9 to −8kJ mol −1 .<br />

At low internal concentration, ∆Gsorption was larger with MX than with CM (Riederer<br />

<strong>and</strong> Schönherr 1986a). ∆Gsorption depends on heat <strong>of</strong> sorption (Hs) <strong>and</strong> entropy (Ss):<br />

Substituting (8.3) into (8.4) leads to<br />

∆Gsorption = ∆Hs − T∆Ss<br />

lnK = ∆Hs<br />

RT<br />

+ ∆Ss<br />

R<br />

(8.4)<br />

(8.5)<br />

Plotting ln K vs T −1 (in Kelvin) results in a straight line having the slope ∆Hs/R,<br />

<strong>and</strong> the y-intercept is ∆Ss/R. A large entropy is characteristic for sorption on solid<br />

substrates, which leads to a higher degree <strong>of</strong> order. For ∆Gsorption to be negative, the<br />

large T∆Ss term must be overcompensated by the heat <strong>of</strong> sorption (∆Hs). This was<br />

the case at all temperatures <strong>and</strong> concentrations (Riederer <strong>and</strong> Schönherr 1986a).<br />

With both species, a striking difference between CM <strong>and</strong> MX exists for the<br />

effect <strong>of</strong> sorbate concentration on ∆Hs. At low concentration the heat <strong>of</strong> sorption<br />

<strong>of</strong> CM was constant, <strong>and</strong> decreased only if the internal concentration exceeded<br />

10 −2 mol kg −1 (Fig. 8.2a). Sorption sites in the CM seemed to be energetically<br />

homogeneous as long as the internal concentration was

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