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Yoshida - 1981 - Fundamentals of Rice Crop Science

Yoshida - 1981 - Fundamentals of Rice Crop Science

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150 FUNDAMENTALS OF RICE CROP SCIENCE<br />

3.17. Responses <strong>of</strong> two varieties to different levels <strong>of</strong> applied phosphorus (drawn from<br />

Koyama et al 1973).<br />

3.9.2. Potassium in soil solution<br />

Submergence increases the concentration <strong>of</strong> potassium in the soil solution. The<br />

increases are higher in sandy soils rich in organic matter and are associated with<br />

soluble ferrous iron and manganese (Table 3.24). This can be considered one <strong>of</strong><br />

the benefits <strong>of</strong> flooding. A disadvantage, however, would be the loss in coarsetextured<br />

soils with drainage.<br />

3.9.3. Partial productive efficiency<br />

The partial productive efficiency <strong>of</strong> potassium for grain is generally high at early<br />

growth stages, declines, and becomes high again at later stages (Table 3.25). Since<br />

rice requires large quantities <strong>of</strong> potassium, a sustained supply is necessary up to<br />

heading when the reproductive stage is complete. Note that only 20% <strong>of</strong> the<br />

absorbed potassium is translocated to the panicles; the rest remains in the vegetative<br />

parts at maturity (see Table 3.11).<br />

3.9.4. Partial replacement <strong>of</strong> potassium by sodium<br />

Since most <strong>of</strong> the enzymes requiring univalent cations are not activated by sodium

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