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@ARTICLE{Wang:16355,
author = {Wang, R. and Willibald, G. and Feng, Q. and Zheng, X. and
Liao, T. and Brüggemann, N. and Butterbach-Bahl, K.},
title = {{M}easurement of {N}2, {N}2{O}, {NO} and {CO}2 emissions
from soil with the gas-flow-soil-core technique},
journal = {Environmental Science $\&$ Technology},
volume = {45},
issn = {0013-936X},
address = {Columbus, Ohio},
publisher = {American Chemical Society},
reportid = {PreJuSER-16355},
pages = {6066 - 6072},
year = {2011},
note = {This work was funded by the German Research Foundation
(DFG, FG536, MAGIM), the National Natural Science Foundation
of China (40805061, 41021004), and the NitroEurope project.
Technical assistance from Meike Sauerwein, Guangren Liu,
Yinghong Wang, Yang Sun, and Dongsheng Ji is acknowledged.},
abstract = {Here we describe a newly designed system with three
stand-alone working incubation vessels for simultaneous
measurements of N(2), N(2)O, NO, and CO(2) emissions from
soil. Due to the use of a new micro thermal conductivity
detector and the redesign of vessels and gas sampling a
so-far unmatched sensitivity (0.23 μg N(2)-N h(-1) kg(-1)
ds or 8.1 μg N(2)-N m(-2) h(-1)) for detecting N(2) gas
emissions and repeatability of experiments could be
achieved. We further tested different incubation methods to
improve the quantification of N(2) emission via
denitrification following the initialization of soil
anaerobiosis. The best results with regard to the
establishment of a full N balance (i.e., the changes in
mineral N content being offset by simultaneous emission of N
gases) were obtained when the anaerobic soil incubation at
25 °C was preceded by soil gas exchange under aerobic
conditions at a lower incubation temperature. The ratios of
N and C gas emission changed very dynamically following the
initialization of anaerobiosis. For soil NO(3)(-) contents
of 50 mg N kg(-1) dry soil (ds) and dissolved organic carbon
(DOC) concentrations of approximately 300 mg C kg(-1) ds,
the cumulative emissions of N(2), N(2)O, and NO were 24.3 ±
0.1, 12.6 ± 0.4, and 10.1 ± 0.3 mg N kg(-1) ds,
respectively. Thus, N gas emissions accounted (on average)
for $46.2\%$ (N(2)), $24.0\%$ (N(2)O), and $19.2\%$ (NO) of
the observed changes in soil NO(3)(-). The maximum N(2)
emission reached 1200 μg N h(-1) kg(-1) ds, whereas the
peak emissions of N(2)O and NO were lower by a factor of
2-3. The overall N(2):N(2)O and NO:N(2)O molar ratios were
1.6-10.0 and 1.6-2.3, respectively. The measurement system
provides a reliable tool for studying denitrification in
soil because it offers insights into the dynamics and
magnitude of gaseous N emissions due to denitrification
under various incubation conditions.},
keywords = {Anaerobiosis / Atmosphere: chemistry / Carbon Dioxide:
analysis / Chemistry Techniques, Analytical / Models,
Chemical / Nitrogen: analysis / Nitrogen Oxides: analysis /
Soil: chemistry / Nitrogen Oxides (NLM Chemicals) / Soil
(NLM Chemicals) / Carbon Dioxide (NLM Chemicals) / Nitrogen
(NLM Chemicals) / J (WoSType)},
cin = {IBG-3},
ddc = {050},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Engineering, Environmental / Environmental Sciences},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:21678900},
UT = {WOS:000292850200022},
doi = {10.1021/es1036578},
url = {https://juser.fz-juelich.de/record/16355},
}