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

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46 2 Quantitative Description <strong>of</strong> Mass Transfer<br />

When working with weak electrolytes, Creceiver may be maintained at zero by using<br />

a buffer as receiver in which the solute is fully ionised. Lipophilic solutes may be<br />

scavenged <strong>and</strong> trapped in phospholipid vesicles, which maintains the concentration<br />

<strong>of</strong> the aqueous phase <strong>of</strong> the receiver at practically zero. Rearranging (2.25) leads to<br />

ln(Cdonor/C0)<br />

t<br />

= −PA<br />

= −k. (2.26)<br />

Vdonor<br />

When ln (Cdonor/C0) is plotted vs time, a straight line is obtained with slope −k.<br />

Equations (2.4)–(2.26) treat mass transfer as a first-order process (model 3), <strong>and</strong> k<br />

is the first-order rate constant. Permeance (P) can be calculated when k, A <strong>and</strong> Vdonor<br />

are known. Equation (2.26) states that Cdonor/C0 decays exponentially with time<br />

Cdonor<br />

C0<br />

= e −kt , (2.27)<br />

<strong>and</strong> once k has been determined experimentally, the donor concentration can be<br />

calculated for any time interval. The time required for the donor concentration to<br />

decrease to one half is<br />

ln0.5 = −kt (2.28)<br />

<strong>and</strong> the half time (t 1/2) is 0.693/k. A simple experiment will help to demonstrate<br />

the use <strong>of</strong> the above equations.<br />

2.5.1 The Experiment<br />

Again, we want to study diffusion <strong>of</strong> 2,4-D across an isolated pepper fruit CM. It<br />

is inserted into our transport apparatus (Fig. 2.1). As donor solution, a buffer (1 ml)<br />

having pH 2.73 is used, <strong>and</strong> as receiver (10 ml) we use borax buffer with pH 9.2. At<br />

this pH, 2,4-D is fully ionised, <strong>and</strong> the concentration <strong>of</strong> the non-ionised species is<br />

always zero. The membrane area exposed to solutions is 1cm2 . The experiment is<br />

started by adding 2,4-D to the donor solution at a total concentration <strong>of</strong> 2molm −3 .<br />

At 24-h intervals the receiver solution is quantitatively withdrawn, replaced by fresh<br />

buffer <strong>and</strong> analysed for 2,4-D. The solute fraction (Mt/M0) <strong>of</strong> 2,4-D which penetrated<br />

into the receiver <strong>and</strong> was sampled from it is calculated <strong>and</strong> plotted against<br />

time (Fig. 2.9a). It increases in a non-linear fashion (circles), while the fraction<br />

lost from the donor decreases with time (squares). It took nearly 3 days for half <strong>of</strong><br />

the 2,4-D to penetrate into the receiver. Plotting ln (Cdonor/C0) vs time results in<br />

a straight line with a slope <strong>of</strong> −0.25day−1 (Fig. 2.9b). This is evidence that our<br />

mass transport <strong>of</strong> 2,4-D was in fact a first-order process. Next we calculate t1/2 as<br />

ln 0.5/ −0.25day −1 , which is 2.77 days. Permeance is obtained using (2.26) <strong>and</strong> SI<br />

units<br />

P = kVdonor<br />

A<br />

=<br />

�<br />

2.89 × 10−6s−1 �� 1 × 10−6 m3� 1 × 10−4 m2 = 2.89 × 10 −8 ms −1 . (2.29)

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