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Yoshida - 1981 - Fundamentals of Rice Crop Science

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160 FUNDAMENTALS OF RICE CROP SCIENCE<br />

Table 3.29. Absorption and translocation <strong>of</strong> iron, and ironexcluding<br />

power <strong>of</strong> the rice plants grown in culture solution<br />

deficient in various nutritional elements. a<br />

Status <strong>of</strong><br />

plant<br />

Complete<br />

– N<br />

– P<br />

– K<br />

– Ca<br />

– Mg<br />

– Mn<br />

Iron content (ppm)<br />

Upper Lower Culm<br />

leaves leaves stem<br />

423 732 390<br />

398 830 495<br />

458 864 407<br />

617 983 808<br />

544 910 413<br />

602 998 480<br />

601 826 570<br />

Translocation Ironpercentage<br />

<strong>of</strong> excluding<br />

iron b power c (%)<br />

3.5 60<br />

2.5 60<br />

3.7 30<br />

4.5 20<br />

4.6 22<br />

5.5 27<br />

5.4 38<br />

a Tadano (1976). b Amount <strong>of</strong> iron translocated to the shoot relative<br />

to the total amount <strong>of</strong> iron absorbed by the plant. c Defined as<br />

formula: ( a – b )/ a × 100 (%), where a is the amount <strong>of</strong> iron, in<br />

milligrams, contained in the same volume <strong>of</strong> culture solution as<br />

that <strong>of</strong> water absorbed by the plant and b is the amount <strong>of</strong> iron, in<br />

milligrams, actually absorbed by the plant.<br />

3.11.5. Varietal performance on iron-deficient and iron-toxic soils<br />

Some degree <strong>of</strong> varietal difference in the ability to absorb iron appears to exist<br />

(Fig. 3.26). When 12 rice varieties were grown on synthetic soil with different<br />

moisture regimes and at different pH values, plant color differed greatly, as<br />

illustrated by the chlorophyll content <strong>of</strong> leaves. Variety Tetep showed a consistently<br />

high ability to absorb iron from the synthetic soil. Varieties also differ in<br />

their tolerance for iron toxicity (Ponnamperuma 1976a).<br />

3.1 2. MANGANESE<br />

3.12.1. Occurrence <strong>of</strong> deficiency and toxicity<br />

Manganese deficiency and toxicity seldom occur in field-grown rice. There are,<br />

however, reports on manganese deficiency <strong>of</strong> lowland rice grown on highly<br />

degraded paddy soils in Japan (Hashimoto and Kawamori 1951) and manganese<br />

toxicity from areas affected by manganese mining (Iwata 1975).<br />

3.12.2. Manganese in soil solution<br />

Concentrations <strong>of</strong> manganese in the soil solution increase after submergence (Fig.<br />

3.27). Manganese is more readily reduced and rendered soluble than iron. The<br />

release <strong>of</strong> manganese into the soil solution, therefore, precedes that <strong>of</strong> iron. This<br />

increase in availability <strong>of</strong> manganese is beneficial for rice at a near-neutral pH. In<br />

solution culture, 0.1–0.5 ppm Mn is sufficient for maximum rice growth and<br />

concentrations higher than 10 ppm are toxic (Ishizuka et al 1961, Tanaka and<br />

Navasero 1966a).

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