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

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4.6 <strong>Water</strong> <strong>Permeability</strong> <strong>of</strong> Isolated Astomatous Cuticular Membranes 105<br />

<strong>Water</strong> loss (mg)<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

AgCl<br />

precipitation<br />

0<br />

0 5 10 15 24 28 32<br />

Time (h)<br />

Fig. 4.19 <strong>Water</strong> permeability <strong>of</strong> an isolated Populus canescens CM before <strong>and</strong> after counter diffusion<br />

<strong>of</strong> NaCl <strong>and</strong> AgNO 3 . The slope <strong>of</strong> the linear transpiration kinetic is significantly decreased by<br />

64% after the formation <strong>of</strong> AgCl precipitations in the CM. Data were taken from Schreiber et al.<br />

(2006)<br />

4.6.2.5 Effect <strong>of</strong> AgCl Precipitates on <strong>Water</strong> Permeance<br />

Polar functional groups contribute to the sorption <strong>of</strong> water to the MX (Sect. 4.3)<br />

<strong>and</strong> to the formation <strong>of</strong> aqueous pores (Sect. 4.4). <strong>Water</strong> permeability <strong>of</strong> some CM<br />

increases with humidity (Sect. 4.6.2, subsection: “Effect <strong>of</strong> Partial Vapour Pressure<br />

(Humidity) on <strong>Permeability</strong> <strong>of</strong> CM”) <strong>and</strong> if they are traversed by aqueous pores<br />

they are permeable to hydrated ions (Chap. 5). As hydrated ions diffuse exclusively<br />

in aqueous pores, it was attempted to selectively block these pores in CM membranes<br />

with insoluble AgCl precipitates. CM were inserted in the transpiration cups<br />

(Fig. 9.2), <strong>and</strong> water permeance was determined gravimetrically with 0.01moll −1<br />

NaCl as donor solution. Partial pressure <strong>of</strong> the receiver was practically zero. With<br />

NaCl still in the donor, the outer surface <strong>of</strong> the CM was treated with 0.01moll −1<br />

AgNO 3 in deionised water for 24 h. This was done by adding AgNO 3 solution to<br />

the outer side <strong>of</strong> the CM, sealing the chambers with adhesive tape <strong>and</strong> incubating<br />

them on a rolling bench, which guaranteed homogeneous wetting <strong>of</strong> both sides <strong>of</strong><br />

the CM. After blotting <strong>of</strong>f the silver nitrate solution, water permeability was again<br />

determined gravimetrically (Schreiber et al. 2006). When Ag + <strong>and</strong> Cl − diffusing<br />

towards each other in aqueous pores <strong>of</strong> the CM meet, insoluble precipitates are<br />

formed. These precipitates could at least partially block aqueous pores, <strong>and</strong> water<br />

permeability should decrease. This is exactly what happened (Fig. 4.19). If water<br />

loss was plotted vs time, slopes decreased after the formation <strong>of</strong> AgCl precipitates.

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