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The formation of N2O as a result of denitrification was monitored under laboratory conditions in samples of a waterlogged Italian soil that had been amended with rice straw, KNO3 and (NH4)2HPO4. Redox potential and pH were also monitored. After four days of incubation N2O‐N production reached a peak of 184.2 μg/d which declined to 29.05 μg/d on the seventh day. The production of N2O stabilized around this level for about 10 days and then declined to 1.57 μg/d, where it remained till the end of the experiment.
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Pedrazzini et al. (1983) studied this question.
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