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Vergara - 1976 - Physiological and morphological adaptability of ri

Vergara - 1976 - Physiological and morphological adaptability of ri

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190 crux-tars AND RICE<br />

SD 0t temperature t°Cl<br />

SDol sunshine tioursthrl<br />

4 '- - 2.0<br />

3 \-- — l5<br />

Z —<br />

m IO<br />

—=-—<br />

Heading<br />

0 | | | | | | | | | | | 0<br />

-6O -4O -2O O 02D 040<br />

Stage from heading time (11015)<br />

2. Changes in st<strong>and</strong>ard deviations (SD) <strong>of</strong> temperature<br />

<strong>and</strong> sunshine hours in the data. Value averaged for 20<br />

days: n — 22R.<br />

1<br />

influenced strongly by the climatic factors at the inherent stage. The author.<br />

using field data, intended to elucidate the changing patterns in climatic effectiveness<br />

on individual yield components <strong>and</strong> to determine the stages most<br />

sensitive to climatic factors. The differences in climatic effectiveness among<br />

va<strong>ri</strong>ous growth stages were expressed by compa<strong>ri</strong>ng the multiple correlation<br />

coefficients (R ). which were calculated from temperature (t) <strong>and</strong> sunshine hours<br />

(s) at each stage, <strong>and</strong> a yield component (l1). Another expression was made by<br />

compa<strong>ri</strong>ng the gradients <strong>of</strong> r-l’, curves or s-Y, curves at each stage.<br />

The second procedure is to find good mathematical models which serve to<br />

express the complex surface composed <strong>of</strong> t. s, <strong>and</strong> 1' dimensions.<br />

The selection <strong>of</strong> sensitive stage <strong>and</strong> determination <strong>of</strong> model are mutually<br />

dependents Needless to say. the R values are computed by some model. If the<br />

model is inadequate, the R values in every stage become lower. Thus. it is<br />

difficult to find the sensitive stage. On the other h<strong>and</strong>. if the climatic data at<br />

insensitive stage are used to improve a model. a good result is not obtained<br />

One <strong>of</strong> the methods for avoiding such a vicious cycle is to use data which<br />

are stratified by certain ranges <strong>of</strong>t or s. The surface composed <strong>of</strong> I, s, <strong>and</strong> Y,<br />

dimensions is very complex with a wide range <strong>of</strong>! <strong>and</strong> s, but monotonously plane<br />

with a narrow range stratified by 1 or s (Fig. 3).<br />

When the data \vere stratified by" temperature (Fig. 3a). the s-Y, relations<br />

were Sl10\Vll by the following model:<br />

__<br />

--<br />

Y, = bit + bps + 11,1 + c (type I)<br />

where

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