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N and P losses from a paddy field plot in central Korea
Authors:Cho Jae-Young  Han Kang-Wan  Choi Jin-Kyu  Kim Young-Joo  Yoon Kwang-Sik
Institution:1. Department of Agricultural Chemistry , Chonbuk National University , Chonju, 561-756, Korea;2. Department of Agricultural Engineering , Chonbuk National University , Chonju, 561-756, Korea;3. Department of Agricultural Engineering , Chonnam National University , Kwangju, 500-757, Korea
Abstract:Abstract

The study was carried out to investigate the water balance and runoff and infiltration losses of nutrients in a paddy field plot located in southern Korea. Field monitoring was carried out during the cropping season from May 1, 1999 to September 30, 2000. The soil of the experimental paddy field belonged to the Jisan series (SiL; fine loam, mixed, mesic Fluventic Haplaquepts) covering on area of 5,000 m2 (100 m × 50 m). The measured input quantities of N and P into the paddy field were as follows: 122 and 140 kg N ha?1 and 29 and 30 kg P2O5 kg ha?1 from chemical fertilizer, 20 and 28 kg N ha?1 and 0.35 and 0.36 kg P ha?1 from precipitation, and 26 and 35 kg N ha?1 and 0.57 and 0.72 kg P ha?1 from irrigation water, respectively. The measured outputs of N and P during the study period were as follows: 48 and 52 kg N ha?1 and 1.1 and 1.6 kg P ha?1 from runoff water, and 9 and 12 kg N ha?1 and 0.04 and 0.05 kg P ha?1 from infiltration. The runoff loading was the highest in June, presumably because of the higher concentrations of chemical components associated with chemical fertilizer application. The runoff losses of nutrients were compared to the amounts of nutrients supplied by chemical fertilizers. It was found that the losses of N accounted for 34.3 and 42.6% of the chemical fertilizer applied, while those of P accounted for 3.8 and 5.3%. The ratio between nutrient losses by infiltration and the chemical fertilizer applied was 6.4 and 9.8% for N and 0.1 and 0.2% for P, respectively.
Keywords:agricultural non-point source  infiltration  nutrients  runoff
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