3.9 Article

Estimating nitrous oxide emissions from flood-irrigated alkaline grey clays

Journal

AUSTRALIAN JOURNAL OF SOIL RESEARCH
Volume 41, Issue 2, Pages 197-206

Publisher

C S I R O PUBLISHING
DOI: 10.1071/SR02068

Keywords

soil pH; denitrification; nitrogen fertiliser; cotton

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Concern has mounted over recent decades regarding the emission of nitrous oxide (N2O) to the atmosphere through human activities. Modern agriculture has contributed to this with elevated use of nitrogenous fertilisers and irrigation. Irrigated cotton grown on alkaline heavy clay soils often uses nitrogen fertiliser inefficiently, due largely to N loss ( commonly 50-100 kg N/ha) through denitrification. However, the amount of denitrified N emitted as N2O has rarely been measured. This paper derives estimates of the quantities of N2O emitted from N fertiliser applied to alkaline grey clays. A negative exponential function between the N2O/N-2 mole fraction and soil pH was derived from a search of laboratory and field studies published by numerous authors using a wide range of soil types. A greater proportion of N2O relative to N-2 is emitted from acid soils; approximately equivalent amounts of each gas are emitted from soil of pH 6.0. For the alkaline grey clays ( pH 8.3-8.5), the N2O/N-2 mole fraction was about 0.024. The quantities of N2O emitted from alkaline grey clays during the growth of a cotton crop were estimated by applying this relationship to N-15 balance studies where N fertiliser losses had been measured. Using this approach, about 2 kg N/ha (similar to1.1% of the N applied) was calculated to be lost as N2O during the cotton-growing season. This is similar to the value of 1.25% commonly used to estimate N2O emissions from N fertiliser, but this estimation should only be applied to alkaline soils; a larger percentage of the fertiliser N denitrified from acid soils should be emitted as N2O-N. These estimates of N2O emissions require validation with field experimentation. The low (negligible) values for N2O emission from flooded fields compared with laboratory observations are discussed. It is possible that high N2O emissions observed under laboratory conditions result from the shallow depth of soil, decreasing the opportunity for N2O to be further reduced as it diffuses through the soil profile. Management strategies that have the potential to reduce N2O emissions are discussed.

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