Summary
A laboratory study was made of the losses of nitrogen through ammonia volatilization from four flooded, tropical soils. The soils used varied considerably in pH, organic matter content, and cation exchange capacity. Losses were measured from the unamended soils, and from ammonium sulphate and urea-treated soils. Two rates of nitrogen application (approximately 50 and 200 kg/ha N) and two methods of application (simulated field broadcast and fertilizer incorporation) of the nitrogen were used.
Losses of ammonia were detected for each of the unamended soils, including an acid sulphate soil of pH 3.6. Increased application of both ammonium sulphate and urea resulted in increased losses of ammonia through volatilization. Incorporation of the nitrogen into the mud of the flooded soils significantly decreased losses due to volatilization. It was concluded that the initial or ‘aerobic’ pH of the soils was the soil characteristic most closely related to the magnitude of losses due to volatilization.
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Macrae, I.C., Ancajas, R. Volatilization of ammonia from submerged tropical soils. Plant Soil 33, 97–103 (1970). https://doi.org/10.1007/BF01378201
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DOI: https://doi.org/10.1007/BF01378201