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Yoshida - 1981 - Fundamentals of Rice Crop Science

Yoshida - 1981 - Fundamentals of Rice Crop Science

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34 FUNDAMENTALS OF RICE CROP SCIENCE<br />

1.32. Relationship between total dry weight and root dry weight <strong>of</strong> 4 rice varieties<br />

(IRRI 1978).<br />

where W R is root dry weight, W T is total dry weight (i.e., shoot dry weight plus<br />

root dry weight), and H and h are constants. Equation 1.4 can be converted into<br />

a logarithmic form:<br />

Log W R = log H + h log W T . (1.5)<br />

Thus, log W R is a linear function <strong>of</strong> log W T . The above relationship has been tested<br />

for different rice varieties under different environmental conditions. One such<br />

study gives the following formula:<br />

W R = 0.212 W T<br />

0.936<br />

(1.6)<br />

where the weight is expressed in milligrams (Fig. 1.32). Thus, when the plants are<br />

small (substitute 1 for W T ), W R /W T is about 0.2; W R /W T value approaches 0.1 as the<br />

plant grows larger (substitute 10 5 for W T ). In other words, the ratio <strong>of</strong> root dry<br />

weight to total dry weight ranges from about 0.2 at the seedling stage to about 0.1<br />

at heading.<br />

The above relationship between root and total dry weight gives an estimate <strong>of</strong><br />

root mass left in the soil if shoot weight is known. For instance, when a crop<br />

produces a shoot dry weight <strong>of</strong> 3 t/ha at heading, a root dry weight <strong>of</strong> about 330<br />

kg/ha is left in a recoverable form in the soil. Since it is known for other cereal<br />

crops that a considerable amount <strong>of</strong> organic substances is released into the soil<br />

from roots as root exudates (Barber and Martin 1976), the actual amount <strong>of</strong>

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