Abstract
Vertical flux densities of ammonia, water vapour and sensible heat were measured over a flooded rice field in China following the application of ammonium bicarbonate fertilizer. Aqueous and gaseous phase transfer resistances for ammonia were deduced from these measurements. The aqueous phase resistance was maximal in the morning and least in the afternoon. Stable stratification of the floodwater immediately adjacent to the air-water interface was observed during the morning when evaporation rates were low, and may be responsible for inhibiting the transfer of ammonia to the atmosphere.
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Trevitt, A.C.F., Freney, J.R., Denmead, O.T. et al. Water-air transfer resistance for ammonia from flooded rice. J Atmos Chem 6, 133–147 (1988). https://doi.org/10.1007/BF00048336
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DOI: https://doi.org/10.1007/BF00048336