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

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118 4 <strong>Water</strong> <strong>Permeability</strong><br />

about 31 carbon atoms (Jenks et al. 1996), <strong>and</strong> using (4.21) the average thickness<br />

<strong>of</strong> a monolayer would be 4.0 nm. With a wax amount <strong>of</strong> 1.6µgcm −2 at most, 4–5<br />

monomolecular layers <strong>of</strong> wax molecules could be established.<br />

4.7 Permeances <strong>of</strong> Adaxial <strong>and</strong> Abaxial <strong>Cuticles</strong><br />

The analysis <strong>of</strong> water permeance <strong>of</strong> cuticles presented in this chapter relies on<br />

data obtained with isolated astomatous cuticular membranes <strong>and</strong> with reconstituted<br />

waxes. However, most leaves have stomata at least on one side, <strong>and</strong> due to this lateral<br />

heterogeneity we have at least three parallel pathways <strong>of</strong> water: (1) diffusion<br />

across stomatal pores, (2) diffusion across cuticles over guard cells <strong>and</strong> accessory<br />

cells, <strong>and</strong> (3) diffusion across cuticles over ordinary pavement cells.<br />

A more sophisticated approach permits the quantification <strong>of</strong> the fluxes <strong>of</strong> water<br />

vapour across cuticles <strong>and</strong> across stomatal pores (Santrucek et al. 2004). It is based<br />

on the fact that water diffusion in the vapour phase depends on density <strong>of</strong> the vapour,<br />

whereas the water diffusion through the solid phase <strong>of</strong> the cuticle remains unaffected.<br />

The total flux Ftotal across an isolated cuticle with stomatal pores is the sum<br />

<strong>of</strong> the two fluxes occurring across the solid cuticle Fcuticle <strong>and</strong> the stomatal pore<br />

Fstoma<br />

Ftotal = Fcuticle + Fstoma. (4.22)<br />

Transpiration experiments were carried out using the experimental setup depicted in<br />

Fig. 4.22 <strong>and</strong> 3 H-labelled water vapour in either a pure helium (He) or pure nitrogen<br />

(N) atmosphere at ambient pressure. Radio-labelled water diffuses from the donor<br />

across the membrane into the receiver, where it is trapped <strong>and</strong> sampled in regular<br />

time intervals. Different gas phases can be obtained by flushing the receiver chamber<br />

with either helium <strong>of</strong> nitrogen gas.<br />

The two fluxes <strong>of</strong> water FtotalHe in helium <strong>and</strong> FtotalN in nitrogen can be measured<br />

using isolated stomatous cuticles<br />

FtotalHe = Fcuticle + FstomaHe, (4.23)<br />

FtotalN = Fcuticle + FstomaN. (4.24)<br />

This experimental approach is based on the fact that the diffusion coefficient <strong>of</strong><br />

water in helium DwHe is 3.6 times higher than the diffusion coefficient <strong>of</strong> water in<br />

nitrogen DwN (Cussler 1984). Thus, using membranes with pores (e.g., stomatous<br />

cuticles) higher fluxes will be measured in a helium atmosphere compared to a nitrogen<br />

atmosphere (4.25). However, no differences occur with a non-porous membrane<br />

(e.g., astomatous cuticle) <strong>and</strong> fluxes in both gases (helium <strong>and</strong> nitrogen) will be the<br />

same<br />

FstomaHe<br />

=<br />

FstomaN<br />

DwHe<br />

= 3.6. (4.25)<br />

DwN

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