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Vergara - 1976 - Physiological and morphological adaptability of ri

Vergara - 1976 - Physiological and morphological adaptability of ri

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429<br />

Compa<strong>ri</strong>sons <strong>of</strong> <strong>ri</strong>ce growth in<br />

different environments<br />

A. Tanaka<br />

SUMMARY<br />

is a phenomenon resulting from the cnvironmcnt-ira<strong>ri</strong>cty-cultural<br />

Growth practice interaction. lt is a sequential development <strong>of</strong> vegetative, reproductive.<br />

<strong>and</strong> <strong>ri</strong>pening phases. As the climatic environment <strong>of</strong> <strong>ri</strong>ce cultivation is extremely<br />

diverse due to diversity <strong>of</strong> the location <strong>and</strong> season in which <strong>ri</strong>ce is grown.<br />

there are va<strong>ri</strong>ous types <strong>of</strong> growth patterns.<br />

The ideal growth pattern is a balanced vigor throughout a smooth succession<br />

ot‘ the three growth phases. Va<strong>ri</strong>eties <strong>and</strong> growing seasons should be selected to<br />

take advantage <strong>of</strong> climatic resources at their maximum efficiency. <strong>and</strong> cultural<br />

practices should be selected to make the grou-‘lh pattern ideal by filling thc gap<br />

between the nature <strong>of</strong> va<strong>ri</strong>eties <strong>and</strong> environmental conditions.<br />

An agroecologieal interpretation <strong>of</strong> grovrth is a tool to synthesize information<br />

obtained from expe<strong>ri</strong>ments conducted in well-controlled. but artificial. conditions<br />

into a practical <strong>ri</strong>ce-cultivation technology,<br />

ENVIRONMENT<br />

In this paper EIIVWOITIIIQITT means the “natural climatic environment." ic, the<br />

complex <strong>of</strong> seasonal sequential changes in the combination <strong>of</strong> climatic factors<br />

occur<strong>ri</strong>ng in nature. <strong>and</strong> “agronomic modification." i.c. the cultural practices<br />

uscd by fanners to improve the crop. with economic pr<strong>of</strong>it.<br />

Day length is short in winter. gradually becomes long in summer. <strong>and</strong><br />

decreases again gradually until winter. <strong>and</strong> this seasonal change is greater at<br />

higher than at lmvcr latitudes. Day length has a strong influence on the groivth<br />

duration <strong>of</strong> <strong>ri</strong>ce plants. depending upon their sensitivity to photope<strong>ri</strong>od. No<br />

practical effort. however. is being made by farmers to change the day length for<br />

<strong>ri</strong>ce cultivation.<br />

Air temperature changes Wlllt the season. <strong>and</strong> soil or i-vatcr temperatures<br />

change accordingly. The annual mean temperature decreases. as a rule. from<br />

lower to higher latitudes, <strong>and</strong> also from lmver to higher altitudes. In temperate<br />

areas the temperature is low in sp<strong>ri</strong>ng. increases in summer, <strong>and</strong> dccrcascs<br />

again in autumn". the duration <strong>of</strong> a season suitable for grov<strong>ri</strong>ng <strong>ri</strong>ce is limited.<br />

Thc seasonal change is generally gradual, ‘out sometimes sudden changes result<br />

from irregular weather fluctuations; <strong>and</strong> a large fluctuation <strong>of</strong> seasonal change<br />

A. Tanaka. Faculty <strong>of</strong> Ag<strong>ri</strong>culture. Hokkaido Llniversit)’. Sapporo. Japan.

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