Effects of cattle slurry and nitrification inhibitor application on spatial soil O2 dynamics and N2O production pathways.

Application of cattle slurry to grassland soil has environmental impacts such as ammonia volatilization and greenhouse gas emissions. The extent, however, depends on application method and soil conditions through their effects on infiltration and oxygen (O 2 ) availability during subsequent decomposition. Here, we applied O 2 planar optode and N 2 O isotopomer techniques to investigate the linkage between soil O 2 dynamics and N 2 O production pathways in soils treated with cattle slurry (treatment CS) and tested the effect of the nitrification inhibitor 3,4-dimethyl pyrazole phosphate, DMPP (treatment CSD). Two-dimensional planar optode images of soil O 2 over time revealed that O 2 depletion ultimately extended to 1.5 cm depth in CS, as opposed to 1.0 cm in CSD. The 15 N site preference (SP) and δ 18 O of emitted N 2 O varied between 11-25‰ and 35–47‰, respectively, indicating a mixture of production sources during the incubation. An early peak of N 2 O emission occurred in both manure treated soils by day 1, with the highest SP values and δ 18 O-N 2 O indicating that fungal denitrification of nitrate in the soil was the main contributor to the early peak. During the first five days, N 2 O fluxes in CS and CSD treatments were similar, and hence nitrification did not influence N 2 O emissions for several days under the experimental conditions of this study. The second peak of N 2 O emission occurring only in CS peaking around day 14, could be due to both nitrification and bacterial denitrification of nitrate produced during incubation. Over 18 days, the application of DMPP substantially mitigated N 2 O emissions by 60% compared to untreated CS in the investigated system which in terms of aeration status corresponded to wet or compacted grassland soil. Using this novel combination of O 2 planar optode imaging and N 2 O isotopomer analysis, our results provide a better understanding of the coupled O 2 and N 2 O dynamics in manure-amended soils, and they illustrate the roles of bacterial and fungal denitrification in N 2 O production in grassland soil under high soil water content. [ABSTRACT FROM AUTHOR]