Contribution of Liquid Manure and Inorganic Fertilizers to the Production of N2 O in Dairy Forage Production Systems.

Poster Number 23

See more from this Division: Poster
See more from this Session: Climate Change Adaptation and Mitigation
Friday, March 7, 2014
Grand Sheraton, Magnolia Foyer
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Cristina Lazcano, William R. Horwath and Martin Burger, Land, Air and Water Resources, University of California Davis, Davis, CA
Intensive dairy production generates large amounts of manure which is typically used as fertilizer for the production of forage, together with inorganic N fertilizers. Dairy forage production systems typically receive high annual inputs of N, having a great potential for large N2O emissions. The present study was carried out in three dairy silage corn production fields of the Central Valley of California where liquid manure containing N mainly as ammonium was applied in irrigation water together with inorganic N fertilizers. The objectives of the study were to determine (i) the proportion of the N inputs emitted to the atmosphere as N2O, and (ii) the main sources (liquid manure vs. inorganic N fertilizer) of the N2O. Total N inputs and N2O emissions were assessed over two corn cropping seasons at each farm, together with soil inorganic N (NH4+-N, NO3--N), moisture and temperature. In order to determine the proportion of liquid manure and inorganic N in the emitted N2O, the field data were complemented with 48-hour laboratory incubations of the three soils amended with liquid manure and 15N labeled or unlabeled inorganic fertilizers. Further, both the N inputs and field N2O samples were analyzed for their stable isotope signature (δ15N-N2O). Results showed that between 0.63 and 1.26% of the applied N was released as N2O. Multiple regression analysis suggested that emissions were controlled by soil moisture and inorganic N availability. The incubations with 15N-labeled inorganic N indicated that mixtures of liquid manure and inorganic N released a larger portion of the inorganic N than the same amount of each N amendment alone. The δ15N-signature of the N2O collected in the field was best explained by the finding that the δ15N values of N2O produced under laboratory conditions depended mainly on N availability, soil moisture, and N2O production rate. Results of this study suggest that a tighter management of N fertilization and irrigation with small and incremental instead of large inorganic N applications produce lower N2O emissions.
See more from this Division: Poster
See more from this Session: Climate Change Adaptation and Mitigation