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Vergara - 1976 - Physiological and morphological adaptability of ri

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454 ctnxuna mo RICE<br />

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l6<br />

X<br />

l2-<br />

X<br />

3»- X<br />

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* i<br />

I?<br />

X<br />

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4“ X X<br />

O 1 l 1 l L<br />

B 2O 24 28<br />

Mean olr tunporutun (‘Cl<br />

I. Correlation between mean air temperature <strong>and</strong> the<br />

relative growth rate <strong>of</strong> leaf area. LRGR. in young <strong>ri</strong>ce<br />

plants grown at va<strong>ri</strong>ous locations (h-‘lflllfil <strong>and</strong> htlurata.<br />

1970). Different va<strong>ri</strong>eties at seven stations are included.<br />

measured pe<strong>ri</strong>od being du<strong>ri</strong>ng the 6 weeks starting from<br />

transplanting in I967. The correlation ciretlicient is<br />

0.8581. significant at the 0.1 percent level.<br />

temperatures. However. the total number <strong>of</strong> tillers per IOU seedlings was highest<br />

at 31 °C, the actual value being 30 for 16°C. 140 for 21 °C, 245 for 31 “C. <strong>and</strong> 210<br />

for 36 "C.<br />

Under natural conditions. daily average air temperature <strong>and</strong> water temperatu1'e<br />

generally do not differ greatly. although there may be some time lag between<br />

them. Thus. it may be concluded that the optimum air temperature for tille<strong>ri</strong>ng<br />

<strong>of</strong> <strong>ri</strong>ce is around 31 °C. It is expected that the higher the temperature, the more<br />

active are both tillc<strong>ri</strong>ng <strong>and</strong> leaf grovrth within the range lower than 31 “C. The<br />

results shoivn in Fig. l can be well explained in this may.<br />

Solar radiation <strong>and</strong> leaf area development<br />

Since most <strong>of</strong> the ltxzatitinal differences in the rate <strong>of</strong> leaf area development at<br />

the same growth stage <strong>of</strong> the plant are att<strong>ri</strong>butable to the difference in temperature.<br />

it may be inferred that the influence <strong>of</strong> solar radiation <strong>and</strong> other climatic<br />

factors is comparatively small. Solar radiation also could have had considerable

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