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Management of rice production systems to increase productivity

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(1) Higher mineralization rate in the rhizosphere <strong>of</strong> upland <strong>rice</strong><br />

compared with other crops. Upland <strong>rice</strong> may enhance nitrogen<br />

mineralization in soils by the secretion <strong>of</strong> some enzymes such as<br />

protease and/or materials promoting microorganism activity.<br />

(2) Upland <strong>rice</strong> has greater ability <strong>to</strong> take up organic nitrogen directly.<br />

If a crop is capable <strong>of</strong> taking up organic nitrogen in the form <strong>of</strong> amino<br />

acids, peptides and protein, the crop could absorb nitrogen with less<br />

competition from microorganisms, as compared with crops which<br />

absorbs nitrogen mainly as nitrate (Yamagata and Noriharu, 1999).<br />

Nitrogen, usually found as ammonium in anaerobic lowland soils, is<br />

found as nitrate in aerobic upland soils. Nitrate is sufficiently mobile in the<br />

soil that root morphology and uptake properties do not limit uptake until soil<br />

N levels are very low (Drew, 1990). When ammonium nitrate is applied, the<br />

plant absorbs the ammonium faster than the nitrate. The optimum pH is<br />

lower for nitrate uptake than ammonia. At optimum pH, nitrate is as effective<br />

as ammonia as a source <strong>of</strong> nitrogen for <strong>rice</strong> (Tanaka et al., 1984), but nitrate<br />

leaches from an upland field faster than in lowland culture (Yoshida, 1975).<br />

Increases in the cost <strong>of</strong> inorganic fertilizers make it important <strong>to</strong><br />

examine the relationships between grain yield and nitrogen utilization. Parr<br />

(1973) defines fertilizer N use efficiency as the percentage recovery <strong>of</strong> fertilizer<br />

N by the crop. This may be estimated as the difference in uptake by the<br />

aboveground portions <strong>of</strong> fertilized and unfertilized plants and expressed as<br />

percent <strong>of</strong> the N applied. This method is <strong>of</strong>ten used by researchers <strong>to</strong><br />

interpret results obtained from fertilizer N experiments. This conventional<br />

method <strong>of</strong> expressing the fertilizer N utilization includes the uptake <strong>of</strong> both<br />

applied fertilizer and native soil N (Reddy and Patrick, 1980).<br />

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