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Yoshida - 1981 - Fundamentals of Rice Crop Science

Yoshida - 1981 - Fundamentals of Rice Crop Science

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MINERAL NUTRITION OF RICE 163<br />

3.28. Relationship between<br />

Eh and sulfate reduction<br />

(Yamane and<br />

Sato 1961).<br />

the extraction procedures can be used to estimate the available soil sulfur for<br />

lowland rice.<br />

b. Irrigation water. Irrigation water is an important source <strong>of</strong> sulfur to irrigated<br />

rice. The sulfate content in irrigation and river waters ranges from 0.2 ppm in Jari<br />

River, Brazil, to 4.7 ppm for the average <strong>of</strong> river waters in Japan (Table 3.30). If<br />

1,000 mm water is used for a rice crop, 1 ppm S in the irrigation water supplies 10<br />

kg/ha during the entire growth cycle. A little less than 2 kg/ha is required to<br />

produce 1 t rice from an improved variety (see Table 3.11). This calculation<br />

clearly indicates the importance <strong>of</strong> sulfur provided by irrigation water.<br />

c. Atmosphere and precipitation. Fumes from active volcanoes, burning trees,<br />

and grasses in shifting agriculture, fumes from chemical plants. exhausted gases<br />

Table 3.30. Sulfur content in irrigation and river waters.<br />

Location<br />

IRRI, Philippines, irrigation water<br />

Bulacan, Philippines, irrigation water<br />

Ngale, Indonesia, irrigation water<br />

Jari River, Brazil a<br />

Japan, river waters b<br />

Thailand, river waters b<br />

Asia, river waters c<br />

World, river waters c<br />

Sulfur (ppm)<br />

2.3<br />

3.9<br />

0.9<br />

0.2<br />

4.7<br />

1.1<br />

2.8<br />

4.1<br />

a Wang, et al (1976b). b Kobayashi, J. (1958).<br />

c Livingstone (1963).

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