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Vergara - 1976 - Physiological and morphological adaptability of ri

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324 CLIMATE AND RICE<br />

Photosynthesis tno-cozcm-Ks")<br />

iso<br />

I20 __<br />

Maize<br />

O -4 -B -|2 -l6<br />

Leaf water potmtlul (bun)<br />

1. Leaf elongation <strong>and</strong> net photosynthesis in maize having va<strong>ri</strong>ous leaf wvater<br />

ptttentials. Note the responsiveness <strong>of</strong> leaf elongation even at high leaf Witter<br />

potentials <strong>and</strong> compare this with the response <strong>of</strong> net photosynthesis. The 30-dayold<br />

plants were growing in soil from which water was withheld. For the leaf<br />

enlargement data. the plants were placed in a dark. humid chamber tor 36 hr at<br />

26‘C. <strong>and</strong> measurements <strong>of</strong> water potential <strong>and</strong> leaf length were made before <strong>and</strong><br />

afier the last 24 hr under those conditions. Net photosynthesis <strong>of</strong> intact shoots was<br />

measured by infrared gas analysis. Leaf water potentials were determined with a<br />

thermocouple psychmmeter using the isopiestic technique (Boyer. 1969) on leaf<br />

disks lrom the same leaves on which the physiological measurements were made<br />

(data adapted from Boyer. l970a).<br />

enlarging cell. In growing cells, the yielding <strong>of</strong> the cell walls under the action<br />

0f turgor effectively places a limit on the tnaximurn turgor that cart occur. This<br />

in turn controls the water potential <strong>of</strong> the cell relative to its environment. <strong>and</strong><br />

hence a gradient in water potential is formed. Thus. the water potential <strong>of</strong>leaves<br />

remains below the water potential <strong>of</strong> the water supply for as long as growth<br />

occurs. ("rrowth then reflects a balance bettveen expansion on the one h<strong>and</strong> <strong>and</strong><br />

the gradient in water potential that supplies the ivater for expansion, on the<br />

other (Boyer. 1968). This appears to be the reason that leaf water potentials<br />

are —l.5 to —2.5 bars instead <strong>of</strong> virtually zero n=hen plants are growing in<br />

\‘t’6ii—\\'€ll€f€d soil.<br />

Dcsiccation <strong>of</strong> short duration. such as might occur du<strong>ri</strong>ng a clear summer<br />

day. appears to have a reversible effect on leaf growth (Acevedo ct al.. 1971).<br />

<strong>and</strong> rapid rates resume when leaf nutter potentials return to —l.5 to —2.5<br />

bars. If leaf water potentials are continuously less than optimum for several<br />

days. l1o\\-'e\~'cr. there is evidence that leaves itiay not grovr at the o<strong>ri</strong>ginal rate<br />

upon rewate<strong>ri</strong>ng (Boyer. 1970a). Therefore. the duration <strong>of</strong> a drought has an<br />

effect on the subsequent regrovath <strong>of</strong> the vegetative plant.

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