% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Zhang:902357,
author = {Zhang, Bowen and Zhou, Minghua and Zhu, Bo and Xiao,
Qianying and Wang, Tao and Tang, Jialiang and Yao, Zhisheng
and Kiese, Ralf and Butterbach-Bahl, Klaus and Brüggemann,
Nicolas},
title = {{S}oil type affects not only magnitude but also thermal
sensitivity of {N}2{O} emissions in subtropical mountain
area},
journal = {The science of the total environment},
volume = {797},
issn = {0048-9697},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2021-04206},
pages = {149127 -},
year = {2021},
abstract = {It is a concern whether the effect of soil type on N2O
emissions has to be considered for regional mitigation
strategies and emission estimates in mountainous areas with
inherent spatial heterogeneities of soil type. To date,
there were few field experiments which investigated soil
type effects on N2O emissions. Thus a 2-year field study was
conducted to measure N2O emissions and soil environmental
variables from three different soils that were formed from
similar parental rock under the same climate. Seasonal N2O
fluxes ranged from 0.18 to 0.40 kg N ha−1 for wheat
seasons and 0.40 to 1.50 kg N ha−1 for maize seasons
across different experimental soils. The intra- and
inter-annual variations in N2O emissions were mainly
triggered by temporal dynamics of soil temperature and
moisture conditions. On average, seasonal N2O fluxes for
acidic soils were significantly lower than for neutral and
alkaline soils in cold-dry wheat seasons while significantly
greater than for neutral and alkaline soils in warm-wet
maize seasons. These determined differences of N2O emissions
were mainly caused by differences of initial soil properties
across different soils. Moreover, seasonal N2O fluxes were
positively correlated with soil pH in wheat seasons, but
negatively correlated in maize seasons. The temperature
sensitivity coefficient (Q10) of soil N2O emissions for
acidic soil (4.06) were significantly greater than those for
neutral (1.82) and alkaline (1.15) soils. Overall, N2O
emissions for acidic soils were not only higher than those
for neutral and alkaline soils but also more sensitive to
changing temperature. The present study highlights that soil
type is needed to be carefully considered for regional
estimate and proposing mitigation strategy of N2O emissions
especially in subtropical mountain regions with inherent
great heterogeneity of soil type.},
cin = {IBG-3},
ddc = {610},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217)},
pid = {G:(DE-HGF)POF4-2173},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:34311350},
UT = {WOS:000704363800014},
doi = {10.1016/j.scitotenv.2021.149127},
url = {https://juser.fz-juelich.de/record/902357},
}