Yoshida - 1981 - Fundamentals of Rice Crop Science
Yoshida - 1981 - Fundamentals of Rice Crop Science
Yoshida - 1981 - Fundamentals of Rice Crop Science
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152 FUNDAMENTALS OF RICE CROP SCIENCE<br />
Table 3.26. Effects <strong>of</strong> a moderately high concentration <strong>of</strong> sodium chloride on the<br />
growth and potassium requirement <strong>of</strong> the rice plant at the vegetative growth stage. a<br />
Nutrient content <strong>of</strong> shoot (%)<br />
Potassium Dry shoot wt<br />
supply (g) K Na<br />
(ppm)<br />
No 1000 ppm No 1000 ppm No 1000 ppm<br />
NaCl NaCl NaCl NaCl NaC l NaCl<br />
1 9.0 15.7 0.33 0.30 0.14 1.63<br />
2 16.0 21.8 0.56 0.56 0.15 1.76<br />
5 24.2 30.4 0.76 0.77 0.12 1.39<br />
10<br />
31.7 38.5 1.23 0.92 0.10 1.24<br />
50<br />
33.4 36.3 1.18 1.11 0.12 1.37<br />
100<br />
39.9 36.7 1.51 1.34 0.09 1.03<br />
200 47.7 44.2 2.75 1.80 0.10 0.98<br />
a <strong>Yoshida</strong> and Castañeda (1969).<br />
3.10. ZINC<br />
3.10.1. Occurrence <strong>of</strong> deficiency<br />
Zinc deficiency <strong>of</strong> lowland rice occurs widely in near-neutral to alkaline soils,<br />
particularly calcareous soils. In a severe case <strong>of</strong> zinc deficiency, transplanted rice<br />
seedlings may die or direct-sown seeds may fail to emerge. In most cases,<br />
however, symptoms become visible about 2–3 weeks after transplanting and a<br />
spontaneous recovery from the deficiency may occur 6–8 weeks after soil submergence.<br />
3.10.2. Zinc in soil solution<br />
The availability <strong>of</strong> both soil zinc and applied zinc is much higher in upland soils<br />
than in submerged soils (<strong>Yoshida</strong> 1975c). Soil submergence causes a substantial<br />
decrease in the zinc concentration in the soil solution (Fig. 3.18). After prolonged<br />
submergence, the zinc concentration tends toward an ultimate value between 0.02<br />
and 0.03 ppm. In a solution culture experiment using 2 varieties, the critical low<br />
concentration for zinc deficiency was about 0.01 ppm (Fig. 3.19). Zinc concentrations<br />
in the culture solution for other plant species to attain maximum growth range<br />
from 0.003 to 0.016 ppm (Carroll and Loneragan 1968).<br />
In Maahas and Luisiana soils, soil pH increases substantially during the first 3<br />
weeks after submergence, during which zinc concentrations fall rapidly. Since the<br />
solubility <strong>of</strong> zinc decreases with increasing pH, decreases in zinc concentration<br />
might be predicted; however, factors other than soil pH could be operating. For<br />
example, in Kala Shah Kaku soil, where zinc deficiency occurs, a substantial<br />
decrease in zinc concentration during the first 2 weeks is not accompanied by any<br />
increase in soil pH. The ultimate value <strong>of</strong> the zinc concentration in the soil<br />
solution, however, is considered adequate for healthy plant growth. Thus, zinc