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

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136 5 Penetration <strong>of</strong> Ionic <strong>Solute</strong>s<br />

−ln (1−M t /M o )<br />

4.0<br />

3.5<br />

3.0<br />

2.5<br />

2.0<br />

1.5<br />

1.0<br />

0.5<br />

Populus<br />

0.0<br />

0<br />

0 20 40 60 80 100<br />

Time (h)<br />

Stephanotis<br />

Schefflera<br />

Pyrus<br />

Malus<br />

Fig. 5.8 Penetration <strong>of</strong> CaCl2 across astomatous CM isolated from Populus canescens, Pyrus communis,<br />

Malus domestica, Stephanotis floribunda <strong>and</strong> Schefflera actinophylla leaves. A 5-µl donor<br />

droplet containing 5gl −1 45 CaCl2 <strong>and</strong> 0.2 Glucopon 215 CSUP as wetting agent was applied to<br />

the outer surface <strong>of</strong> the CM <strong>and</strong> after droplet drying, penetration <strong>of</strong> CaCl2 was measured at 20 ◦ C<br />

<strong>and</strong> 90% humidity. Error bars are 95% confidence intervals. (Redrawn from Schönherr 2000)<br />

5.3.3 Rate Constants Measured with Leaf CM from Different<br />

Species<br />

Rate constants for CaCl2 penetration differed considerably among species, <strong>and</strong> not<br />

all penetration plots were linear to the end (Fig. 5.8), but linearity was maintained<br />

until about 80% <strong>of</strong> the dose had penetrated. Populus CM (grey poplar) had the<br />

highest rate constants (8.4 × 10 −2 h −1 ), whereas lowest k (1.4 × 10 −2 h −1 ) were<br />

measured with Schefflera. This corresponds to a factor <strong>of</strong> 6 between the two species,<br />

with lowest <strong>and</strong> highest permeability for CaCl2. This shows that aqueous pores<br />

occur in CM <strong>of</strong> all <strong>of</strong> these species tested, but they may differ in number <strong>and</strong>/or size.<br />

These rate constants measured with CaCl2 may be compared with water permeance<br />

(Pw) in Table 4.8. Pw <strong>of</strong> poplar CM (26.8 × 10 −10 ms −1 ) was 5.7 times higher than<br />

Pw <strong>of</strong> Stephanotis CM (4.7 × 10 −10 ms −1 ). For rate constants <strong>of</strong> CaCl2 penetration,<br />

this ratio is only 2.9. This difference might be related to the fact that water also diffuses<br />

across the waxy pathway, which is excluded for CaCl2. Too much should not<br />

be made <strong>of</strong> this comparison, however, because different lots <strong>of</strong> CM were used for<br />

estimating Pw <strong>and</strong> k for CaCl2.<br />

Another factor should be pointed out which is not visible in Fig. 5.8. Reproducible<br />

data <strong>and</strong> reasonably short error bars are obtained only with very large<br />

sample sizes <strong>of</strong> 50–100 CM. Rate constants measured with individual CM vary<br />

greatly, <strong>and</strong> in each population cuticles occurred which were practically imperme-<br />

98<br />

97<br />

95<br />

92<br />

87<br />

78<br />

63<br />

39<br />

Percent penetrated

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