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@ARTICLE{Nguyen:836749,
author = {Nguyen, Quan Van and Wu, Di and Kong, Xianwang and Bol,
Roland and Petersen, Søren O. and Jensen, Lars Stoumann and
Liu, Shurong and Brüggemann, Nicolas and Glud, Ronnie N.
and Larsen, Morten and Bruun, Sander},
title = {{E}ffects of cattle slurry and nitrification inhibitor
application on spatial soil {O} 2 dynamics and {N} 2 {O}
production pathways},
journal = {Soil biology $\&$ biochemistry},
volume = {114},
issn = {0038-0717},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2017-05802},
pages = {200 - 209},
year = {2017},
abstract = {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 (O2) availability during
subsequent decomposition. Here, we applied O2 planar optode
and N2O isotopomer techniques to investigate the linkage
between soil O2 dynamics and N2O 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 O2 over time revealed that O2
depletion ultimately extended to 1.5 cm depth in CS, as
opposed to 1.0 cm in CSD. The 15N site preference (SP) and
δ18O of emitted N2O varied between 11-25‰ and 35–47‰,
respectively, indicating a mixture of production sources
during the incubation. An early peak of N2O emission
occurred in both manure treated soils by day 1, with the
highest SP values and δ18O-N2O indicating that fungal
denitrification of nitrate in the soil was the main
contributor to the early peak. During the first five days,
N2O fluxes in CS and CSD treatments were similar, and hence
nitrification did not influence N2O emissions for several
days under the experimental conditions of this study. The
second peak of N2O 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 N2O 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 O2 planar optode
imaging and N2O isotopomer analysis, our results provide a
better understanding of the coupled O2 and N2O dynamics in
manure-amended soils, and they illustrate the roles of
bacterial and fungal denitrification in N2O production in
grassland soil under high soil water content.},
cin = {IBG-3},
ddc = {570},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000411546600021},
doi = {10.1016/j.soilbio.2017.07.012},
url = {https://juser.fz-juelich.de/record/836749},
}