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@ARTICLE{Fuhrmann:845567,
author = {Fuhrmann, Irabella and He, Yao and Lehndorff, Eva and
Brüggemann, Nicolas and Amelung, Wulf and Wassmann, Reiner
and Siemens, Jan},
title = {{N}itrogen fertilizer fate after introducing maize and
upland-rice into continuous paddy rice cropping systems},
journal = {Agriculture, ecosystems $\&$ environment},
volume = {258},
issn = {0167-8809},
address = {Amsterdam [u.a.]},
publisher = {Elsevier},
reportid = {FZJ-2018-02792},
pages = {162 - 171},
year = {2018},
abstract = {Water scarcity and economic incentives favor the
introduction of upland crops into permanent paddy rice
systems during dry seasons. However, introducing upland
crops into permanently flooded cropping systems temporarily
changes soil conditions from anaerobic to aerobic, affecting
nitrogen (N) dynamics profoundly. We hypothesized that under
maize and dry rice, total fertilizer 15N recovery in soil as
well as the immobilization of fertilizer 15N in microbial
residues is reduced compared with continuous paddy rice
cropping. Furthermore, we expected enhanced emissions of
fertilizer 15N in form of nitrous oxide (N2O) under maize
and dry rice. To test these hypotheses, we traced the fate
of a 15N-urea pulse in a field experiment in the Philippines
with three different crop rotations: continuous paddy rice,
paddy rice – dry rice, and paddy rice – maize for two
years. Indeed, the 15N recovery in the first 5 cm of bulk
soil was lowest in the paddy rice – maize rotation
(arithmetic mean with standard error: $19.2 ± 1.8\%$ of
applied 15N), while twice as much was recovered in the first
5 cm of bulk soil of the continuous paddy rice cropping
systems $(37.8 ± 2.2\%$ of applied 15N) during the
first dry season. The 15N recovery in the plant biomass
(shoots and roots) in the continuous paddy rice cropping was
$13\%$ larger than in the dry rice plant biomass and $5\%$
larger than in the maize plant biomass during the first dry
season. Fertilizer 15N remained longest in paddy rice –
maize (mean residence time = 90 ± 25 days) and in
continuous paddy rice (mean residence
time = 77 ± 30 days), compared with dry rice –
paddy rice rotation (mean residence
time = 16 ± 5 days). After 2 years, $10\%$ (paddy
rice – dry rice, paddy rice – maize) to $23\%$
(continuous paddy rice) of the applied fertilizer 15N were
still stored in soil. The largest fraction of this 15N was
immobilized by soil microbes, which stored $3–4\%$ of
applied 15N in the form of amino sugars as specific cell
wall constituents, in all cropping systems. Nevertheless,
introducing upland crops into continuous paddy rice systems
likely increased N leaching losses and resulted in initial
losses of urea- 15N to N2O, which thus has to be considered
in climate smart mitigation strategies.},
cin = {IBG-3},
ddc = {330},
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:000429394600017},
doi = {10.1016/j.agee.2018.02.021},
url = {https://juser.fz-juelich.de/record/845567},
}