25.02.2013 Views

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

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

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

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

100 4 <strong>Water</strong> <strong>Permeability</strong><br />

P w (m/s)<br />

2.5e-9<br />

2.0e-9<br />

1.5e-9<br />

1.0e-9<br />

5.0e-10<br />

P w = 6.63 x 10 7 (1/m) D SA - 4.49 x 10 −11 (m/s)(r 2 = 0.90)<br />

0.0 0.0 5.0e-18 1.0e-17 1.5e-17 2.0e-17 2.5e-17 3.0e-17 3.5e-17<br />

D SA (m 2 /s)<br />

Fig. 4.15 <strong>Water</strong> permeances Pw <strong>of</strong> isolated CM plotted as a function <strong>of</strong> DSA (diffusion coefficient<br />

<strong>of</strong> stearic acid) in reconstituted cuticular waxes <strong>of</strong> 24 plant species. (Data from Table 4.7)<br />

the amorphous phase (Riederer <strong>and</strong> Schreiber 1995), whereas the crystalline phase<br />

is not accessible. With an increasing amorphous fraction in the wax, sorption is<br />

expected to increase. Since diffusion <strong>of</strong> water <strong>and</strong> stearic acid takes place in the<br />

same amorphous wax phase, path length <strong>of</strong> diffusion might increase as well, <strong>and</strong><br />

thus the ratio <strong>of</strong> Kww/ℓτ could be very similar for all investigated species. This<br />

hypothesis could help to explain why Pw is correlated with DSA.<br />

Diffusion coefficients for lipophilic solutes in CM <strong>and</strong> wax (Sect. 6.3.2.3: “Variability<br />

<strong>of</strong> <strong>Solute</strong> Mobility with Size <strong>of</strong> <strong>Solute</strong>s” <strong>and</strong> Sect. 6.5.2) differ among species<br />

because tortuosity <strong>of</strong> the diffusion path differs. This implies that differences in DSA<br />

(Table 4.7) are caused by differences in length <strong>of</strong> the diffusion paths (ℓτ). Since<br />

water in CM <strong>of</strong> all species diffuses in the waxy pathway, the path lengths <strong>of</strong> stearic<br />

acid <strong>and</strong> water should be the same for both. Hence, partition coefficients (Kww) may<br />

vary little among species, <strong>and</strong> since Kww/ℓτ is constant (6.6 × 10 7 m −1 ) differences<br />

in Pw should mainly be due to differences in lengths <strong>of</strong> the diffusion path.<br />

Data on sorption <strong>and</strong> diffusion <strong>of</strong> water in cuticular waxes could help us to better<br />

underst<strong>and</strong> the waxy barrier. There are data on water concentration in polyethylene<br />

<strong>and</strong> liquid hydrocarbons. <strong>Water</strong> concentration in polyethylene at 25 ◦ C <strong>and</strong><br />

100% humidity is about 7 × 10 −4 gg −1 (Table 4.1). According to Schatzberg (1965)<br />

the solubility <strong>of</strong> water in a liquid alkane (hexamethyl tetracosane) at 25 ◦ C is<br />

5.5 × 10 −5 gg −1 or 55mgkg −1 . Sorption <strong>of</strong> water in isolated <strong>and</strong> reconstituted solid<br />

cuticular waxes has not been studied, for good reasons as the following example<br />

will show. Starting with the assumption that the above paraffin/water partition<br />

coefficient (5.5 × 10 −5 gg −1 ) is valid for cuticular waxes, we can estimate the concentration<br />

<strong>of</strong> tritiated water (THO) needed to detect THO in a wax sample <strong>of</strong> 1 mg.<br />

For a reasonable counting statistic, we aim at 100Bqmg −1 wax, <strong>and</strong> we can calculate<br />

the concentration <strong>of</strong> THO in water from the definition <strong>of</strong> K (2.12). The ratio

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

Saved successfully!

Ooh no, something went wrong!