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@ARTICLE{Sintermann:14711,
author = {Sintermann, J. and Spirig, C. and Jordan, A. and Kuhn, U.
and Ammann, C. and Neftel, A.},
title = {{E}ddy covariance flux measurements of ammonia by high
temperature chemical ionisation mass spectrometry},
journal = {Atmospheric measurement techniques},
volume = {4},
issn = {1867-1381},
address = {Katlenburg-Lindau},
publisher = {Copernicus},
reportid = {PreJuSER-14711},
pages = {599 - 616},
year = {2011},
note = {We thank the Swiss National Science Foundation for funding
this project (TERMS, 200021-117686/1). In addition, the
research leading to these results has received funding from
the (EU) Seventh Framework Programme - (FP7/2007-2013) under
grant agreement no (PIEF-GA-2008-220842) - as well as from
the EU project NitroEurope (Contract 017841) that is funded
under the EC 6th Framework Programme for Research and
Technological Development. We are very grateful to Kerstin
Zeyer and Lukas Emmenegger from the Swiss Federal
Laboratories for Materials Science and Technology (EMPA) who
provided the in-field calibration device. Finally, we thank
Markus Jocher from our group for his constant support.},
abstract = {A system for fast ammonia (NH3) measurements with chemical
ionisation mass spectrometry (CIMS) based on a commercial
Proton Transfer Reaction-Mass Spectrometer (PTR-MS) is
presented. It uses electron transfer reaction as ionisation
pathway and features a drift tube of polyetheretherketone
(PEEK) and silica-coated steel. Heating the instrumental
inlet and the drift tube to 180 degrees C enabled an
effective time resolution of similar to 1 s and made it
possible to apply the instrument for eddy covariance (EC)
measurements. EC fluxes of NH3 were measured over two
agricultural fields in Oensingen, Switzerland, following
fertilisations with cattle slurry. Air was aspirated close
to a sonic anemometer at a flow of 100 STP L min(-1) and was
directed through a 23 m long 1/2" PFA tube heated to 150
degrees C to an air-conditioned trailer where the gas was
sub-sampled from the large bypass stream. This setup
minimised damping of fast NH3 concentration changes between
the sampling point and the actual measurement.
High-frequency attenuation loss of the NH3 fluxes of 20 to
$40\%$ was quantified and corrected for using an empirical
ogive method. The instrumental NH3 background signal showed
a minor interference with H2O which was characterised in the
laboratory. The resulting correction of the NH3 flux after
slurry spreading was less than $1\%.$ The flux detection
limit of the EC system was about 5 ng m(-2) s(-1) while the
accuracy of individual flux measurements was estimated
$16\%$ for the high-flux regime during these experiments.
The NH3 emissions after broad spreading of the slurry showed
an initial maximum of 150 mu g m(-2) s-1 with a fast decline
in the following hours.},
keywords = {J (WoSType)},
cin = {IEK-8},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000288911000016},
doi = {10.5194/amt-4-599-2011},
url = {https://juser.fz-juelich.de/record/14711},
}