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Management of rice production systems to increase productivity

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3.1.4. Improved Water <strong>Management</strong> System – Repeated Wetting and Drying<br />

Many irrigation <strong>systems</strong> do not maintain adequate drainage<br />

mechanisms. Drainage canals are rarely cleaned, and because farmers believe<br />

that <strong>rice</strong> does best if water is supplied in abundance, they do not see a need for<br />

a drainage system except at harvest time. This practice is not only wasteful,<br />

but it also leads <strong>to</strong> leaching <strong>of</strong> soluble nutrients, inhibits or changes soil<br />

microbial finally activities, slows down mineralization and nutrient release<br />

from the soil complexes. Cel<strong>to</strong>n and Marquette (1972) reported that good<br />

water control on Madagascar Tananarive Plains resulted in <strong>rice</strong> yield <strong>increase</strong>s<br />

<strong>of</strong> 155 <strong>to</strong> 261%. In 1993 the Madagascar’s Agricultural Extension Ministry<br />

reported similar <strong>increase</strong>s in <strong>rice</strong> yield due <strong>to</strong> water control. Bhuiyan et al.,<br />

(1994) reported yields <strong>of</strong> 6.7T and 7.4T in the Philippines under soils saturated<br />

throughout the growing period for wet‐seeded and transplanted <strong>rice</strong>,<br />

respectively.<br />

3.1.5. Influence <strong>of</strong> Repeated Wetting and Drying on Soil Microbial Activity<br />

……...and Nitrogen Mineralization<br />

Worldwide nitrogen is the most limiting nutrient <strong>to</strong> <strong>rice</strong> <strong>production</strong>;<br />

therefore <strong>increase</strong>d nitrogen use efficiency will translate in<strong>to</strong> yield <strong>increase</strong>. In<br />

spite <strong>of</strong> extensive research and advances in fertilizer management, <strong>rice</strong> in the<br />

lowlands generally utilizes less than 40% <strong>of</strong> applied N, mainly because <strong>of</strong> N<br />

losses that occur via NH3 volatilization from the floodwater after NH3<br />

79

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